groundwater project 8
TRANSCRIPT
1 . INTRODUCT ION1 . INTRODUCT ION
India is facing serious water constraints today. India is not on the whole a water
scarce country. The present per capita availability of water in India of
approximately 2200 cub. M. per annum (1998). India should be able to harness
and manage its water resources more effectively to support intensive agriculture,
to fulfill drinking water and sanitation needs of both rural and urban populations,
and also to satisfy the needs of industry.
Current water resource constraints in India, in terms of both quality and quantity,
can be expected to manifest themselves even more rapidly in the coming years.
In the past, with lower population and development levels, there was still
substantial room for each sector to satisfy its water needs and concerns
independently. Now, as the gap between the availability of water resources and
the demands on such resources narrows, the past approach to water
management pursued in India is no longer tenable. Competition for water
between agricultural and urban sectors will be a major challenge in the
forthcoming century. Further, expansion in irrigation, industry, and domestic
water demands will have serious implications for competing non-consumptive
uses, such as hydropower and navigation. Provision for environmental and
ecological concerns will have to be made.
During the last few decades, creation of surface reservoirs and the associated
irrigation canal networks had formed the backbone of our water management
strategy. Where the canal network could not reach, ground water has been
heavily exploited for irrigation. A piquant situation has, therefore, arisen; the
areas are facing declining groundwater levels. The need, therefore, is to increase
our ability to conjunctively manage ground water in a region.
The hard rock areas of the country face special problems due to the sub-surface
void space being localized to regions of fractures and fissures resulting in limited
ground water potential. Fractures may transmit large quantities of water; in other
areas, they may be nearly impervious. Because of the complex distribution of
fractures in almost every type of rock, no single method can unambiguously map
SRTRI GROUNDWATER - PROJECT PROPOSAL
fractures and their capacity for fluid movement. The need, therefore, is to develop
more efficient and reliable methods for locating zones of fractures and fissures
and estimating their water yielding potential both under natural as well as
stressed condition. In this connection, satellite remote sensing, electromagnetic
waves, electrical, optical and microwave sensors may prove to be advantageous
in identifying potential ground water areas.
In alluvial areas where ground water availability is not restricted to zones of
fractures and fissures, there has generally been large scale over exploitation of
this resource. All over the country the need is, therefore, to develop innovative
methods for conservation of rain water and renewal and reuse of waste water,
wherever possible. While conservation is necessary to evolve methods for its sub-
surface storage in large quantities in aquifers in an economical manner without
endangering their water quality. In this context it is worth noting that as a result
of over exploitation during the last four decades, both in hard rock and alluvial
areas, we have inadvertently created a void space the volume of which is several
times more than the total surface reservoir capacity in the country. Further, this
reservoir space is more where relatively more use of ground water takes place.
Successful exploitation of this space for artificial recharge of ground water under
Indian conditions with highly seasonal rainfall necessitates providing a temporary
storage for the large volume of runoff generated during short spells of high
intensity rainfall and accelerating its percolation to the water table.
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SRTRI GROUNDWATER - PROJECT PROPOSAL
2 . PROJECT RAT IONALE2 . PROJECT RAT IONALE
With increase in population and the demand more and more people are
dependent on the groundwater resources for Agriculture, Livestock, Domestic and
Drinking. Especially in the interior and higher parts of the Andhra Pradesh State,
the situation is acute because of low rainfall and variability. Presently many
regions are over exploited and have become critical areas where rate of
exploitation is higher as compared to recharge. Moreover there is impact of
Climate Change i.e., decrease in precipitation and increase in temperatures
effecting the semi-arid parts of Andhra Pradesh State. It is also evident that the
dependency on the groundwater resources for irrigation is ever increasing as
compared to other sources available (see Graph 1).
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Graph 1 Net Area Irrigated by Different Sources, Andhra Pradesh, 1993-94 to 2002-03
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3 . AREAS OF CONCERN IN 3 . AREAS OF CONCERN IN
ANDHRA PRADESHANDHRA PRADESH
Limitations for drilling borewells
It is generally thought
that borewells can be
drilled every where and
any where. This is not
true. There is a wide
variation in the hydro-
geological conditions
within short distances.
Number of factors viz.
hydro-geological
conditions, spacing
between wells etc., have
to be considered for well
site selection. Similar is
the case for selection of
an artificial recharge
structures. At a particular
place an aquifer should
be available to recharge
it.
Based on the
groundwater estimation if
X wells are feasible in an
area, say a Mandal, it
Case Study 1 A farmer, Ananthapur District
Beneath the surface frivolity, though, is a frightening struggle for survival in a district which has seen four successive crop failures. Reddy's graveyard borewells, too, are yielding less than he had hoped for. In all, this Village Officer (VO) has spent over a million rupees in his search for water. His debts mount by the month. "Last week, I phoned on the government helpline," he says. "I cannot carry on like this. We must have some water." The helpline was set up by the State's new Government to deal with those in distress amid continuing farmers' suicides. In a State hit worse than any other by farmers' suicides, Anantapur district has seen the maximum number. Here, in the past seven years, there have been over 500 in the `official' count. And many times that number in other estimates. Reddy's call on the helpline should serve as a clear warning signal. He is in a vulnerable group, right in the danger zone. Dreaming of water, drowning in debt. The horticulture in which he has so heavily invested is in ruins. So are his many borewells. The very rich are well placed to exploit this kind of crisis. Private water markets have swiftly emerged. Desperate farmers can buy a "wetting" for their fields at a cost of Rs. 7,000 or more an acre. This might mean paying a neighbour who has managed to corral access to whatever water there is. You can also buy that resource by the tanker load for a wetting. In this setting, commerce long ago overrode community. "Can you imagine what all this does to our costs per acre?" asks Reddy.
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SRTRI GROUNDWATER - PROJECT PROPOSAL
may not be necessary that all the X number of wells can be sunk there. Detailed
surveys for site selection have to be taken up depending on the hydro-geological
conditions, well density, spacing between wells etc. Therefore, as mentioned
above in order to overcome these problems a basin approach for groundwater
development is necessary.
The present form of groundwater utilization has resulted in haphazard
development, and is reaching alarming proportions. Every sphere of activity, be it
domestic or municipal water supply; agriculture; or industry is dependent on
groundwater for its sustenance, either fully or partially. Coupled with this is
reduced natural recharge due to frequent erratic spells or even failure of
monsoon. This has resulted in over exploitation in certain areas. It is evident from
the fact that there is a deepening of water table, reduction in yields of wells,
drying up of many shallow wells especially dug wells, failures of new wells
constructed, salinity and quality problems.
For a developing society groundwater development is a must, but on proper and
scientific lines keeping in view the availability of the sources and requirement for
different sectoral needs; sustainability of the extraction structures and yield of
water there from, potentiality and demand and socio-economic conditions of an
area.
Future Strategies
Every one is aware of need for groundwater management, artificial recharge,
legislation etc. These tasks call for collection of a large volume of data
representing all the actual field conditions, we have in the State. Without correct
basic data and going ahead with proposed management practices, will not yield
desired results. Hence, the basic information should be cent percent, instead of
random nature of collection of data with sample checks. After getting the
information, we must proceed with further development, monitoring and
management including artificial recharge etc. As a part of this program
registration of wells is going on under WALTA.
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SRTRI GROUNDWATER - PROJECT PROPOSAL
Assessment of Groundwater resources in Andhra Pradesh
(See Annexure 1)
Type of Groundwater micro basins identified: Over Exploited - 118, Critical -
79, Semi-Critical - 192 and Safe - 710
Due to changing groundwater scenario and addition of more than 50,000
extraction structures every year, it is proposed to take-up revision of
estimates at periodic intervals as envisaged in the “National Water Policy” and
WALTA-02.
Andhra Pradesh Water Land and Trees Act (APWALTA) With this scenario in
place the Government of Andhra Pradesh has brought in WALTA-02. The people
intending to drill a borewell in their fields for irrigation needs should take
permission from the Groundwater Departments of the respective Districts and
having met certain criteria and procedures:
1. The particular village is not banned against drilling any new bore-wells as per
the GO issued this year.
2. A professional Geologist / Hydro-geologist / Geophysicist registered with the
Groundwater department need to explore the area using the Geophysical
prospecting instruments and should issue a certificate on the possibility of striking
the aquifer successfully and finding water.
3. Before drilling a borewell based on the report need to approach an Insurance
agency and pay the premium against failure of the borewell.
4. The borewell drilling companies are permitted to drill only after referring to the
above certificates and receipt of the Insurance premium paid.
5. Permission is also needed form the electricity department for power
connection.
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SRTRI GROUNDWATER - PROJECT PROPOSAL
The Gap
Most important lacuna in the whole process is the non-availability of the number
of professionals registered with the State Groundwater department. As of now
only around 250 members have registered. And most of them are concentrated
only in some areas and are not accessible to all areas. Even by rough estimate at
least 1000 such professionals are needed for serving all the 1126 Mandals in the
State for covering 21,908 Gram Panchayats.
Another lacuna is that professionals registered with the government are following
only Electrical Resistivity (ER) Method for prospecting and issuing the certificate
to the farmers. Although it is one of the most important dependable traditional
methods, it has its own advantages and disadvantages. The professionals need to
apply integrated tools and techniques for maximum probability of striking an
aquifer. There are other issues too like groundwater contamination, salinity, etc.,
and there is huge demand for such information too.
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SRTRI GROUNDWATER - PROJECT PROPOSAL
Article 1 State lacks muscle to regulate sinking of borewells
Wednesday, Sep 08, 2004, The Hindu. By K. Venkateshwarlu
HYDERABAD, SEPT. 7. Much as the Government and the well-meaning citizens may wish, implementation of the recently-amended Andhra Pradesh Water, Land and Trees Act (WALTA), aimed at regulating and spacing borewells to check overexploitation of groundwater, seems to have hit roadblocks, with grossly inadequate hydro geologists /geophysicists, ill-equipped machinery, lack of database and uncooperative rig owners.
"Going by the estimates of 50,000 borewell sites per annum, we require 140 teams of hydro geologists/ geophysicists, to complete the task of investigating these sites. This is against the available strength of 22 teams that will be enough for 8000 sites. The number of vacant posts of field officers is 59 with whom additional 10,000 sites could be investigated," said B. N. Prasad, Director of the Ground Water department.
Demand-supply gap
Apart from Government staff, at present, there were only 41registered private geologists/ geophysicists. Eleven of them were based in Hyderabad city and the remaining in districts leaving eight to nine districts unrepresented. In view of the huge task, the Department has also proposed creation of division-level offices. All this simply means a huge demand- supply gap.
The role of geologists has become important, as it has now been made mandatory under the Act, for the rig owner to drillbore wells only at sites identified by them. This was to guard against borewell failure, found to be one of the main reasons for farmers' committing suicide. The rig owners have to submit a certificate from department or registered geologists to the authorities.
Major obstacle
Another major obstacle in the implementation is lack of database of all groundwater structures in the State. However painstaking and laborious the task, registration of all wells and rigs needs to be taken up right away, an essential pre-requisite for regulating new bore wells, the space between them and over exploitation of ground water. The GW department has suggested that registration be taken up on a campaign mode, assigning the job to village secretary in rural areas and the Municipal Commissioner in urban areas, after a wide publicity.
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SRTRI GROUNDWATER - PROJECT PROPOSAL
4 . PROPOSED TRA IN ING CENTRE 4 . PROPOSED TRA IN ING CENTRE
AT SRTR IAT SRTR I
There is a huge demand and gap of professionals required; at least 750 people
are needed in the State to meet the demand for groundwater prospecting. It is
worth to note that even earlier there was demand for professionals, in the
absence of such professionals people were dependent on other means like water
divining, which is neither scientific nor dependable.
To meet the above demand SRTRI intends to establish a “Training Center for
Groundwater Prospecting” as a potential livelihood opportunity for the rural
youth. SRTRI was established in the year 1995 is committed to play a pro-active
role in the case of rural development. Institute has identified 40-45 (trades) most
viable rural friendly livelihood options for each District. The hands on training on
rural technologies are provided to rural youth; about 70 % of them have turned
into rural entrepreneurs.
This project proposal is prepared based on
1. The information collected from Literature survey & Secondary data
(information collected from various sources).
2. Critical analysis of the existing and appropriate tools and methodologies for
successful Groundwater prospecting suitable for the Geo-hydrological
conditions existing in Andhra Pradesh State.
3. Literature survey & secondary data collected on the tools and methodologies
existing like ER and VLF methods.
4. Study of scope and potential for reliable groundwater prospecting services.
5. Need for establishment of Groundwater Prospecting Training facility at SRTRI
campus for imparting trainings.
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SRTRI GROUNDWATER - PROJECT PROPOSAL
3.1 Training Strategy
The people identified for training would be youth who are qualified
graduates / postgraduates with Geology, Hydrogeology, Water Resources
Engineering, Geophysics and other appropriate sciences.
In this proposed center interested youth would be given training on
Groundwater Prospecting with specialization on hard rock areas.
Trainees would be oriented on all appropriate and latest technologies
available. Intensive training with practical exposure would be given on the
two important tools, Electrical Resistivity Method and Very Low-frequency
(VLF) Method. Presently most of the existing institutes are providing
training and exposure only on the traditional ER method.
The long term course would be of 3 weeks duration @ one training per
month, for the qualified youth. Trainings would be done in batches and
there would be about 20 members in each batch. Total number of trainings
/ batches covered in a year would be 12 nos and the trainees covered
would be about 240 nos in a year.
The short duration orientation trainings of 3 days duration is for orientation
to the professionals on the latest technologies. These are the
professionals who are already working in the field. The short duration
orientation trainings would be conducted once in every two months and at
least 120 professionals would be covered in a year @ 20 people per
batch.
3.2 Components of Training
Study of types of geological / geohydrological situations and the
groundwater conditions in the context of AP.
Study of various types of tools and technologies existing for ground water
prospecting, recharging, salinity and identification of contaminants, etc.
Theory and pratical exposure on the ER and VLF tools.
3.3 Livelihood Opportunities
This training would cover diverse components related to the prospecting of
groundwater in diverse geological conditions, with special reference ot hard rock
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SRTRI GROUNDWATER - PROJECT PROPOSAL
areas. The trainees would have multiple opportunities to choose after training,
like
As professionals can lead an independent consultancy service. All the
professionals would be immediately registered with the State Ground
water department.
Can join a consultancy group as a professional for groundwater
prospecting and recharging.
Environmental studies – contaminants, salinity, pollutants etc.
With stringent laws in place for eg. WALTA and dearth of professionals in the
State, there are ample livelihood opportunities.
Budget Requirement
A. Facilities Existing at SRTRI
Particulars
1. Lecture halls / training halls
2. Diverse topography for practicals and exposure.
3. Hostel - Boarding and Lodging facilities at SRTRI
4. Resource persons to train
B. Tools / Instruments
Aspect Quantit
y
Rate Amount
(Rs.)
Remarks
1 VLF instrument 1 @Rs
12,00,000
1200000 Based on the
make and
features
2 Electrical
Resistivity Meter
and accessories
5 nos @Rs. 40,000 200000 Best resistivity
meters
3 Computer 1 no @Rs. 25,000 25000 For data
analysis and
interpretation
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SRTRI GROUNDWATER - PROJECT PROPOSAL
4 Survey
instruments,
brunton compass
and other
accessories
5 nos @Rs. 5,000 25000 For laying grid
Total 250000
C. Training Material - Annual
Aspect Rate Amount (Rs.)
1 Books, Charts, Training
Material etc.
@ Rs. 1,000 per month 12000
Total 12000
D. Personnel Costs - Annual
Aspect Amount (Rs.)
1 Training expert/s for Long term
trainings
@Rs. 15,000 per batch
of training (total 12
trainings in a year)
180000
2 Training expert/s for short
term trainings
@Rs. 10,000 per batch
of training (total 6
trainings in a year)
60000
Total 240000
SUMMARY
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SRTRI GROUNDWATER - PROJECT PROPOSAL
PARTICULARS AMOUNT IN
RS.
REMARKS
A. Physical Infrastructure
Existing at SRTRI
- Contribution from SRTRI - the
basic infrastructure
B. Tools / Instruments 0 Repairs or maintenance as per
the warrentyC. Training Material - Annual 12000 Recurring annuallyD. Personnel Costs - Annual 12000 Recurring annually
Total Fixed cost (B) 24000
Total operation costs
(C+D)
252000 Excluding boarding lodging for
the 240 trainees, which is as
per the actualTOTAL COST (B + C + D) 300000
For establishing the proposed training center at SRTRI the total fixed costs are Rs.
1450000/- and the operational and other costs are Rs. 252000/- (excluding the
boarding and lodging for the trainees) to organize 12 batches of long term
trainings for one year and 6 batches of short term trainings.
Total budget required is Rs. 1702000
Or SAY Rs. 17,00,000/-
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SRTRI GROUNDWATER - PROJECT PROPOSAL
5 . APPL ICAT ION OF GEOPHYSICS5 . APPL ICAT ION OF GEOPHYSICS
FOR GROUNDWATER STUDIESFOR GROUNDWATER STUDIES
Geophysical groundwater prospecting techniques, base themselves on the
detection of the abnormal physical fields associated with inhomogeneities that the
geological evolution has “printed” on the Earth’s crust structure and geological
composition (graph 2).
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SRTRI GROUNDWATER - PROJECT PROPOSAL
Graph 2 Inhomogeneous earth crust
The use of geophysics for both groundwater resource mapping and for water
quality evaluations has increased dramatically over the last 10 years in large
parts due to the rapid advances in microprocessors and associated numerical
modelling solutions.
Near-surface geophysics for groundwater investigations is usually restricted to
depths of 250m below the surface of the Earth. Specific groundwater applications
of the near-surface geophysics include mapping the depth and thickness of
aquifers, mapping the aquitards or confining units, locating preferential fluid
migration paths such as fractures and fault zones and mapping contamination to
the groundwater such as that from saltwater intrusion.
Many geophysical techniques have been applied to groundwater investigations
with some showing more success than others. In the past, geophysics has either
been used as a tool for groundwater resource mapping or as tool for groundwater
character discrimination. For groundwater resource mapping it is not the
groundwater it self that is the target of the geophysics rather it is the geological
situation in which the water exists. Potential field methods, gravity and
magnetics, have been used to map regional aquifers and large scale basin
features. Seismic methods have been used to delineate bedrock aquifers and
fractured rock systems. Electrical and electromagnetic methods have proved
particularly applicable to groundwater studies as many of the geological formation
properties that are critical to hydrogeology such as the porosity and permeability
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SRTRI GROUNDWATER - PROJECT PROPOSAL
of rocks can be correlated with electrical conductivity signatures. General
methods of practice have been produced for geophysical technqiues in
groundwater exploration; situations with complex geology and hydrogeology do
not lend themselves to this and require specific targeting of methods for
particular problems. Most geophysical techniques have been used for
groundwater characterization but once again it is with the electrical and
electromagnetic methods that the greatest success has been shown in
directly mapping and monitoring clean and contaminated groundwater.
The use of geophysics for groundwater studies has been stimulated in part by a
desire to reduce the risk of drilling dry holes and also a desire to offset the costs
associate with poor groundwater production. Today the geophysicist also provides
useful parameters for hydrogeological modelling of both new groundwater
supplies and for the evaluation of existing groundwater.
Designing a Successful Survey
Achieving a successful geophysical survey is reliant on three features:
implementing the geophysical survey early in the project planning stages,
designing the correct geophysical survey and choosing the appropriate
geophysical contractor.
Planning the Survey
Ideally the use of geophysics should be discussed early in the planning stages of a
survey in order to gain most benefit from the geophysics. Unfortunately this is not
always the case and geophysics is only used when all other investigation
techniques have failed. This has led to bad publicity for geophysics as if all else
has failed then it is unlikely that the geophysics will be successful. Geophysics is
only one tool that can be applied to a groundwater investigation and its success
must rely on the careful interpretation and integration of the results with the
other geologic and hydrogeologic data for the site. Only then will the geophysics
be a success.
Geophysics is typically used in one of two ways. Either it is used to project an
interpretation of the geology and hydrogeology from boreholes and surface
exposure into a formation or the geophysics is used in an area of unknown
geology and hydrogeology in order to better focus the direct sampling
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SRTRI GROUNDWATER - PROJECT PROPOSAL
programme. For both of these types of use, if the geophysics is discussed early in
the proceedings then the most appropriate techniques can be found and used in
the most cost effective manner.
Designing the Geophysical Survey
Paramount to designing a successful geophysical survey is the definition of a clear
set of objectives and the choice of appropriate methods. The objectives must be
based on reasonable, geophysically achievable criteria. For this it is important
that the geophysical target has physical properties that can be distinguished from
background signatures (geological and hydrogeological features) and background
noise (ambient cultural noise together with system induced noise). The next stage
in defining a project is to be able to provide an adequate site description along
with any previous data that has been collected, site maps or other data that
would pertain to the project. This includes logistical features such as access to the
site, noise sources and working restrictions. Finally if the results are not presented
in a manner that the client can fully understand and utilize then they are as good
as useless results.
Choosing the appropriate geophysical methods and applying the methods in an
appropriate manner is also critical to a successful survey. Only once the
objectives have been defined clearly and agreed on by both the client and the
professional can the appropriate geophysical methods be chosen. The incorrect
choice of technique and insufficiently experienced personnel conducting
the investigation has been cited as primary reasons for the failure of
many geophysical surveys.
Quality control throughout all stages of the work is paramount to a successful
outcome. Field quality control should include basic equipment calibration
procedures, accurate field reporting including field printouts of digital data,
checks for digital data recording and up-loading to computers and repeat
measurements at base or calibration sites. During processing this quality control
will include manual calculations of computer-processed data, documentation of
processing steps and separate data reviews by an independent person not
directly involved in the project.
Choosing a Professional
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SRTRI GROUNDWATER - PROJECT PROPOSAL
A successful survey requires the choice of an appropriate professional. This will be
one who has the general knowledge to be able to suggest the most appropriate
geophysical survey tools to meet the objectives. A good professional should also
possess the knowledge and professional integrity to admit the inadequacies of the
geophysics if it is not likely to meet the survey objectives. The professional should
then have sufficient specialist knowledge to be able to carry out the geophysics or
to suggest an expert who has the necessary specialized knowledge. It may be
that more than one professional is needed with experts for field acquisition, for
data processing and for data integration. It may often be beneficial to use more
than one professional on large investigations and have them conduct trial surveys
to test various methods before a commitment is made to a full survey
programme. This allows more precise models of the geology and geophysics to be
constructed in order to maximise the results of the geophysics. It is important
throughout the process of choosing a professional to be aware of who shall have
responsibility for the different parts of work.
6 . TOOLS AND TECHNIQUES6 . TOOLS AND TECHNIQUES
There are various tools and techniques available for groundwater prospecting
(see Annexure 2). The electrical resistivity and VLF are the two techniques found
to be most useful and effective in hard rock areas. In Andhra Pradesh State the
reliable groundwater prospecting is most needed in the drought prone, semi-arid
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SRTRI GROUNDWATER - PROJECT PROPOSAL
areas. Majority of such areas are located in the hard rock areas. Therefore these
two techniques are discussed here.
Electrical Resistivity
(see Annexure 3 for more details)
The electrical resistivity technique of geophysical exploration is one of the earliest
methods. The Schlumberger brothers in France in the early part of the 20th
Century did much of the early development. It is one of the most useful
techniques in groundwater hydrology exploration because the resistivity of a rock
is very sensitive to its water content. The resistivity of water is very sensitive to
its ionic content. Different stratigraphic units in a geologic section can also be
mapped as long as the units have a resistivity contrast. The utility of the method
is wholly dependent upon the size of the target and the differences between its
electrical resistivity and the resistivity of the rock surrounding the target. Often
this is connected to rock porosity and fraction of water saturation of the pore
spaces
The electrical resistivity method typically employs a direct current (DC) or a very
low frequency (<10 Hz) current which is applied to the ground using electrodes in
contact with the ground. The voltage potential is then measured between a
second pair of electrodes. A number of possible patterns of electrodes can be
used, depending upon the depth of penetration needed and the resolution
desired. A mathematical combination of the current, potential, and electrode
spacing yields the apparent resistivity of the subsurface.
Resistivity measurements are used to measure lateral or vertical changes in the
resistivity of the subsurface. To investigate the variation of resistivity with depth,
electrode spacings are gradually increased. A fixed electrode separation is
maintained along a profile line to determine lateral variations.
There are basically three types of arrays Schlumberger (pronounced “schlum-bur-
zhay”), Wenner arrays and Dipole-Dipole arrays.
The technique has been successfully employed for investigating:
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SRTRI GROUNDWATER - PROJECT PROPOSAL
1. Groundwater depth
2. Lithology favorable for groundwater
3. Well siting / Aquifer exploration
4. Detection of fractures and dikes
5. Location of sinkholes and cavities
6. Contamination of groundwater / Groundwater quality
7. Depth to freshwater-saltwater interface
8. Brine plumes
9. Seawater intrusion
10. Thickness of overburden
11. Geologic structure / General stratigraphic mapping
12. Archeological sites
13. Electrical grounding of large electrical installation
14. Electrical grounding of cell phone transmitting towers
Advantages of the technique are:
1. The equipment is light, portable and
inexpensive
2. Less costly than drilling
3. Qualitative interpretation of the data is
rapid and straightforward
4. Field expenses are minimal
5. It is flexible and can be used for various
purposes and depths of investigation
6. It can be used for both soundings and
profiling
7. Shallow investigations are rapid
Disadvantages of the technique are
1. Deep investigations require long cables
and consume much field time
2. Interpretation of complex geologic structures is difficult and ambiguous
3. Cultural problems cause interference, e.g., power lines, pipelines, buried
casings, fences, metal pipes, and electrical grounds can complicate
interpretation
4. Resolution.
5. Data acquisition can be slow compared to other geophysical methods,
although that difference is disappearing with the very latest techniques.
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Figure VLF technique used for detecting the anomaly.
SRTRI GROUNDWATER - PROJECT PROPOSAL
2. Very Low Frequency (VLF) Technique
(See Annexure 4 for More Details)
The VLF (Very Low Frequency) technique, can summarily be characterized as the
detection of electromagnetic anomalies (figure 1) caused by induction from a
primary magnetic field of worldwide distributed military use VLF transmitters
operating in the 10-30Khz range (Graph 3) and measures distortions created by
local changes in the underlying conductivity of the earth. VLF transmitters are
located throughout the world (Map1).
Graph 3 VLF as compared to other waves
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SRTRI GROUNDWATER - PROJECT PROPOSAL
Map 1 Very low frequency / low frequency site locations
Principles of Operation
VLF falls in the broad category of electromagnetic (EM) methods of geophysics.
The primary field (the transmitted radio signal) causes eddy currents to be
induced in conductive geologic units or structures. Faraday’s principle of
electromagnetic induction tell us that any oscillating magnetic field (e.g.,the radio
wave) will produce an electric field and hence an electric current in a conductive
media. Those eddy currents in turn create a secondary magnetic field which is
measured by the VLF receiver. The secondary or perturbed field may be phase
shifted and oriented in a different direction than the primary field depending on
the shape or geometry of the conductor, the orientation of the conductor, and the
conductivity contrast with the surrounding material (e.g., the host rock). The
instrument measures both the primary and secondary fields together (graph 4).
All VLF instruments measure two components of the magnetic field or
equivalently the “tilt angle” and ellipticity of the field. Some instruments also
measure the third magnetic component and/or the electric field. The electrical
field is measured by inserting two probes in the ground, spaced about 5 meters
apart, and measuring the potential difference at the transmitter frequency. The
22
Photo A VLF Instrument, (WADI, ABEM)
SRTRI GROUNDWATER - PROJECT PROPOSAL
electric field provides additional information about the overburden thickness and
conductivity.
Interpretation
VLF interpretation is generally qualitative or subjective in nature. Anomalous
areas are identified and a gross characterization attached to the anomaly (e.g.,
steeply dipping conductor or thickening conductive overburden). Some simple
modeling may be carried out for simple geometric structures.
Field Procedures
VLF instruments are “back pack” portable and operated by one person generally
weigh 5-10 kg (10-20 pounds) (Photo 1). Productivity depends on the terrain and
vegetation, but generally several kilometers of line may be covered in a good day.
State of-the-art instruments include software to store the data with survey
coordinates, and may be dumped to a laptop computer at the end of the day.
Magnetic field measurements do not
require ground contact and can be
made in less than a minute at each
station. Station spacing may vary from
5 to 20 meters (15 to 60 feet)
depending on the geologic objective. If
electric field data are also acquired,
Graph 4 Primary and Secondary waves
23
SRTRI GROUNDWATER - PROJECT PROPOSAL
probes must be pushed into the ground at each station and hence the
measurement time at each station is increased.
Advantages of VLF
Useful for detecting the water bearing zones, such as fracture or fault zones of
high electric conductivity acting as conductors, imbedded in high electric
resistivity geological formations. These features, along with the portability and
low cost effectiveness use of the VLF equipment, make it the ideal tool for
groundwater prospecting associated with deeper paths along sub-surface water
bearing bodies (fractures and fault zones) in hard rock geological environments.
They are also useful in mapping the extent of sedimentary basins (limestones,
sandstones) to define gross lithology and locating vertical faults containing water,
clay or other conductive materials.
Limitations / Disadvantages of VLF
VLF is used primarily as a reconnaissance tool to identify anomalous areas for
further investigation, either with other geophysical methods or drilling.
Weaknesses of the method include:
VLF measurements are sensitive to “cultural interference” from pipelines,
utilities, fences, and other linear, conductive objects.
Interpretation is generally qualitative in nature; quantitative modeling
requires a high data density and a well constrained model.
Topographic effects can bias the data, are difficult to remove, and are
model dependent.
VLF transmitters are subject to outages for scheduled or unscheduled
maintenance.
Unfavorable ionospheric conditions may compromise the quality of the
data.
24
SRTRI GROUNDWATER - PROJECT PROPOSAL
7 . APPL ICAT ION AND7. APPL ICAT ION AND
L IM ITAT IONS OF VARIOUSL IMITAT IONS OF VARIOUS
GROUNDWATER EXPLORAT IONGROUNDWATER EXPLORAT ION
TOOLSTOOLS
Interpretation of the geophysics requires ground truth information in order to
calibrate the data. The noise can be electrical noise and metallic structures that
will influence electric, electromagnetic and magnetic techniques and vibration
noise that will influence the seismic techniques. In addition, geologic noise can be
defined as any signature other than the target that is present in the subsurface.
However, these small changes in physical property that are manifest in changes
in geophysical signatures, are often not evident when only considering one
geophysical signature. Thus a multi-technique approach is essential to any site
investigation. The multi-technique approach includes not only the combination of
different geophysical techniques but also the combination of both borehole
logging and surface techniques.
Surface geophysics should be used for initially locating the boreholes and for
providing information between boreholes. Integration of the surface geophysical
data and the point specific sedimentological data may be achieved by down-hole
logging of geophysical properties in cased boreholes.
The optimal ground water surveying method is no doubt drilling. This method
ensures that all necessary information is being brought up from the geological
formations. However, in order to obtain a desired degree of information from the
subsurface of a project area, drilling alone is normally not a feasible alternative.
There are a number of efficient and inexpensive geophysical surveying methods
available to the project hydrogeologist. It is worth noting at this point that these
25
SRTRI GROUNDWATER - PROJECT PROPOSAL
are, without exception, indirect methods. This implies that neither method
measure directly what we are actually looking for. With geophysical surveys, the
target features are therefore invariably associated features. This implies that
unless we understand the water context of these features, our geophysical
surveys will be less than meaningful.
In addition, a number of complications and limitations apply. For example, during
interpretation of a resistivity survey, a thick resistive layer may have the same
signature as a thin low resistive layer; the principle of equivalence. Highly
conductive layers may limit the depths of investigation short of the target
features. A thorough knowledge of a method's limitations and assets is vital. As a
rule, considerable effects of synergy can be achieved if more than one method is
applied.
Rational for Choosing the Appropriate Method
The next logical step is then to find the most appropriate method. that fits the
project's Term of Reference, budget, as well as local conditions, the identified
target features, appropriate technology levels, logistics, etc.
A systematic approach is encouraged in the selection of adequate methods. There
are many considerations; some few examples of pitfalls are illustrated below:
A VLF survey is highly productive but would provide little useful
information if the target aquifer is a porous gravel aquifer.
A magnetic survey could be next to useless over homogenous and
unfractured sandstones.
A particular method may prove inappropriate with regards to technology
transfer within the project context.
Data acquisition and processing could be too expensive for the project
budget
Use of explosives for seismic surveys could prove to be impractical.
26
SRTRI GROUNDWATER - PROJECT PROPOSAL
A N N E X U R E 1A N N E X U R E 1
G R O U N D W A T E R R E S O U R C E S &G R O U N D W A T E R R E S O U R C E S &
C L A S S I F I C A T I O N C L A S S I F I C A T I O N
A N D H R A P R A D E S HA N D H R A P R A D E S H
Total
Replenis
h able
Ground
Water
Resourc
es
(m.ha.m
/ Yr)
Provisio
n for
Domesti
c,
Industri
al &
Other
Uses
(m.ha.
m/ Yr)
Availabl
e
Ground
Water
Resourc
es for
Irrigatio
n In Net
Terms
(m.ha.
m/ Yr)
Utilizabl
e
Ground
Water
on
Resourc
e for
irrigatio
n in net
Terms
(m.ha.
m/ Yr)
Gross
Draft
Estimat
ed on
Prorata
basis
(m.ha.m
/ Yr)
Net
Draft
(m.ha.m
/ Yr)
Balance
ground
Water
Resourc
e for
Future
use in
net
terms
(m.ha.m
/ Yr)
Level o
ground
water
develo-
pment
(%)
Weighte
d
average
delta
(m)
Utilizabl
e
irrigatio
n
potentia
l for
develo-
pment
(m.ha)
3.52916 0.52938 2.99978 2.69981 1.01318 .070922 2.29056 23.64 0.047-
1.472
3.96008
Source: Central Ground Water Board
Years Type of Wells Yield Well
density/sq.km
1982 Dugwells 60 - 150 cu.m < 5
1983-84 Dugwells/ Dug cum borewells 60 - 150 cu.m 5 - 10
1984-94 Dugwells/ borewells 40 - 100 cu.m /
150 - 600 lpm
> 10
1994-98 Borewells/ Dug cum borewells 50 - 400 lpm / 30 -
60 cu.m
> 15
27
SRTRI GROUNDWATER - PROJECT PROPOSAL
1998-04 Borewells/ Few dug cum borewells 50 - 150 lpm / 20 -
40 cu.m
> 20
Source: State Ground Water Board
Categorization of Over-Exploited and Dark Mandals, Andhra Pradesh
S.No Districts Over Exploited
Mandals
(>100%)
Dark Mandals (100 to 85%)
1 Anantpur - 1. Rolla, 2. Parigi 3. Yadiki
2 Chittoor 1. Tirupati 1. Chandragiri 2. Somala 3. Kammapalle
3 Cuddapah 1. Vempalli 1. Proddatur
4 Guntur - 1. Thullar
5 Karimnagar - 1.Bejjanki 2. Ramadugu 3. Veenavanka. 4
Elkathurthy 5. Metpalli 6. Kothalapur 7.
Boinappalli
6 Mahaboobnagar 1. Midjil -
7 Medak - 1.Daulatabad
8 Nalgonda - 1. Chityal 2. Marguda 3. Nutankal
9 Nizambad - 1. Armoor 2. Sirikonda 3. Kammarapally
10 Rangareddy - 1. Moinabad
11 Warangal 1 Duggondi 2
Ghanpur
1. Bachchannapet
12 West Godavari 1.
Undrajavaram
-
A N N E X U R E - 2A N N E X U R E - 2
G R O U N D W A T E R S T U D I E S - S U R V E Y T O O L S G R O U N D W A T E R S T U D I E S - S U R V E Y T O O L S
A N D T E C H N I Q U E SA N D T E C H N I Q U E S
The range of geophysical techniques used in groundwater investigations is only
briefly described herein in order to provide an introduction to the methods and
some useful literature references. All geophysical techniques measure variations
in a material's physical properties. For soils and rocks the properties can be
divided into a framework or matrix component and the pore content component.
28
SRTRI GROUNDWATER - PROJECT PROPOSAL
Different materials exhibit different parameter signatures such as their resistivity
or its inverse conductivity, acoustic velocity, magnetic permeability and density.
These parameters are influenced by the mineral type, grain packing arrangement,
porosity, permeability, and pore content (i.e. gas or fluid type). In general no one
property is unique to any material, rather a material is described by ranges of
each property. In most geophysical surveys it is important that changes in the
geophysical parameters are measured and compared. The criteria such as fluid
type (100% fresh water saturated vs. saline water saturated),
porosity/permeability and mineral type for distinguishing different soil/rock or
aquifer/aquitard conditions is importance.
For groundwater investigations, the most significant parameters that have been
used for describing an aquifer system are ones that relate to the porosity and
permeability of the aquifer and surrounding aquitards. Electrical conductivity or
its inverse resistivity is the proportionality factor relating the electrical current
that flows in a medium to the applied electric filed. It is the ability of an electrical
charge to move through a material. It has been correlated with porosity. A
relationship often exists between electrical conductivity and the clay content or
fluid type.
Seismic velocity for both compressional waves and shear waves is related to the
elastic moduli and the density of a material. Compressional wave velocity has also
been correlated with porosity and used for determining fluid content.
The successful use of each geophysical technique is dependent not only on the
careful design of the survey but also on the consideration of a number of key
geological and cultural factors together with the geophysical data:
Nature of the target: The target geophysical signature must be different to that
of the background geology or hydrogeology.
Depth of burial of target: The depth of burial of the feature of interest is
important as different techniques have different investigation ranges. The depth
range is technique dependant however there is always a trade off between
penetration depth and resolution of the technique with respect to the feature of
interest. A technique that will look deep into the earth generally has lower
resolution than a technique that is only looking to shallow depths
29
SRTRI GROUNDWATER - PROJECT PROPOSAL
Target size: An estimation of the target size is necessary prior to selecting
appropriate techniques.
The target size should be considered in conjunction with the depth range for
individual techniques.
Measurement station interval: This will depend on the burial depth, target size
and technique selected. Geophysical surveys have traditionally been conducted
along line profiles or on grids and therefore the station spacing along the lines
must be calculated together with the line separation in order to not miss a
particular target size or to result in spatial aliasing the target (REF). A rough rule
of thumb is that a geophysical anomaly will be approximately twice the size of the
object causing the anomaly so this will give the maximum line and station
spacing.
Calibration of the data: The key to success of any geophysical survey is the
calibration of the geophysical data with both hydrogeological and geological
ground truth information. Calibration data may be provided by both down-hole
geophysical logs in boreholes, samples derived from boreholes by continuous
sampling and by measuring what goes into and comes out of a system.
Magnetic (or geo-magnetic) Techniques
Magnetic techniques measure the remnant magnetic field associated with a
material or the change in the Earth's magnetic field associated with a geologic
structure or man-made object. They have been used for regional surveys since
the early 1900’s in the hydrocarbon industry and for longer in mineral prospecting
however little use has been made directly for groundwater studies. This is mainly
because magnetic properties have no direct relation to those properties that are
of concern to groundwater surveys. The main use for regional groundwater
investigations has been as part of combined surveys with gravity for defining
large-scale basin structures.
Magnetic surveys have also been used to identify basement faulting and other
locations of crustal weakness that may represent preferential fluid flow paths.
Large areas can be covered using airborne magnetic surveys with line and station
spacing tens of meters wide. Results of magnetic surveys are usually presented
as line profiles or magnetic anomaly maps. The airborne Magnetic and
Electromagnetic surveys were then conducted with a 100m line spacing in order
to identify the major structural controls and geologic boundaries. The airborne
30
SRTRI GROUNDWATER - PROJECT PROPOSAL
geophysics was followed by a ground-based programme of magnetic and
electromagnetic surveying. The results showed that the major fault and shear
zones represented highly fractured good aquifers could be mapped in relatively
sparse groundwater regions. A recommendation to conduct future airborne
mapping at 50m line spacing was made. The application of magnetic surveying
for unconsolidated sequences has been somewhat limited as the magnetic
signatures for different sediment horizons are often weak.
Gravity
Common uses of gravity or micro-gravity surveys have been to record the
changes in density of material. While gravity methods have not been widely used
for groundwater applications, there are some notable examples of its use for
mapping the location of low density rocks (typically sedimentary sequences)
within more dense basement rocks. A combination of electromagnetics and
microgravity can be used to design a strategic approach to mapping karstic
features.
Other common applications are the detection of voids within the subsurface
where the small changes in the Earth's gravitational attraction caused by such
contrasts in density can be recorded with modern instrumentation. Interpretation
of gravity data however is difficult as the causes of the changes in gravitational
field can be many and varied. In addition, the collection of gravity data is typically
a slow process and thus expensive. Results are presented in a similar manner to
those of magnetic data as gravity maps and 3D models.
Electrical and Electromagnetic
Electrical and electromagnetic techniques have been extensively used in
groundwater geophysical investigations because of the correlation that often exist
between electrical properties, geologic formations and their fluid content. Most
electrical techniques induce an electrical current in the ground by directly
coupling with the ground. The resulting electrical potential is then used to
measure the variation in ground conductivity, or its inverse, resistivity.
Different materials, and the fluids within them, will show different abilities to
conduct an electric current. In general, sequences with high clay contents show
higher conductivity as do saturated sequences and especially sequences where
saline (or sometimes other contamination) fluids are present. Common field
31
SRTRI GROUNDWATER - PROJECT PROPOSAL
practice for electrical surveying relies on directly placing an electrical current into
the ground (direct current electrical resistivity surveying) and measuring the
response (the electrical potential drop) to that current over a set distance.
The typical results of electrical surveys are electrical profiles or geo-electric
images and geo-electric depth soundings. The profile or transect method for
mapping lateral resistivity changes is now largely replaced by electromagnetic
techniques as the electrical technique is slow (when probes have to be placed
directly into the ground) and thus is not cost effective relative to the
electromagnetic techniques. Electrical methods are still widely used however for
conducting soundings and electrical cross-sections. Electrical techniques can be
divided into a number of types based on the configuration of the electrodes that
are used to input the electrical currents into the ground and the nature of the
electrical signature.
DC resistivity
The direct-current (DC) electrical resistivity method for conducting a vertical
electrical sounding (VES) has proved very popular with groundwater studies due
to the simplicity of the technique and the ruggedness of the instrumentation.
Before the vertical electrical sounding were used a failure rate of over 82% was
recorded for boreholes. With the geophysics and a combination of geological and
photogeological inspection this was dramatically reduced to less than 20%.
It has been demonstrated the potential of these techniques when combined with
those of TDEM soundings for regional schemes of hydrogeophysical
investigations. They illustrate this approach using large-scale surveys in Denmark
where widespread problems exist in supplying increasing quantities of high
quality drinking water. Of particular note in these studies is the ability to obtain
high data coverage over densely populated areas where cultural noise and man-
made conductors make geophysical surveys difficult. Also, they demonstrate the
efficient nature of the surveys where 10 to 15km of data can be obtained by a
two-person crew per day.
Induced polarisation (IP)
The measurement of induced polarisation (IP) is made using conventional
electrical resistivity electrode configuration where the voltage between electrodes
32
SRTRI GROUNDWATER - PROJECT PROPOSAL
is measured as a decay function with time after the current has been switched off
or as the current is switched on. The technique has found most use in the search
for mineral deposits but has had some limited success in groundwater
applications.
Spontaneous Potential
The method of spontaneous potential or self potential geophysics uses naturally
occurring ground potentials from mineral bodies, geochemical reactions, and
groundwater movement. The techniques have most often been used in
exploration for mineral deposits and successful applications have been seen for
groundwater surveying in association with geothermal systems.
Telluric Methods
Telluric methods that utilize natural fluctuations in the Earth’s magnetoshpere
causing low frequency currents within the ground have been developed for
regional (deep) geologic studies over the last 30years. In the early 1970’s
controlled sources were introduced to the method (CSAMT) for increasing the
reliability of the source signatures.
Electromagnetic
Electromagnetic techniques have been extensively developed and adapted over
the last 15 years to map lateral and vertical changes in conductivity with some
spectacular examples of their use being shown for groundwater studies. While the
final output is similar to that from electrical techniques, several advantages with
the electromagnetic techniques result in an increased resolution and more cost-
effective application.
Two types of electromagnetic survey are currently practiced, i) time domain
electromagnetic (TDEM) surveys which are mainly used for depth soundings and
recently in some metal-detector type instruments, and ii) frequency domain
electromagnetic (FDEM) surveys that are used predominantly for mapping lateral
changes in conductivity. In both electromagnetic survey techniques no direct
contact is made with the ground and thus the rate of surveying can be far greater
than for electrical techniques where electrode probes must be placed in the
ground for every measurement. Both techniques measure the conductivity of the
ground by inducing an electric field through the use of time varying electrical
33
SRTRI GROUNDWATER - PROJECT PROPOSAL
currents in transmitter coils located above the surface of the ground. These time-
varying currents create magnetic fields that propagate in the earth and cause
secondary electrical currents which can be measured either while the primary
field is transmitting (during frequency domain surveys) or after the primary field
has been switched off (for time domain surveys). Instrumentation exists to survey
to a range of depths in either transect mode or as discrete soundings. A detailed
description of the use of both FDEM and TDEM for conducting soundings is given
below.
Frequency-domain Electromagnetics (FDEM)
The technique is usually used to measure lateral conductivity variations along line
profiles either as single lines or grids of data. Further recent improvement in
FDEM has seen the integration of GPS technology with the FDEM instruments and
thus has led to a dramatic increase in the rate at which electromagnetic surveys
can be accomplished. Typical survey results for FDEM surveys are contour maps
of conductivity and 2D geo-electric sections showing differences in conductivity
along a line profile. Changes in conductivity are often associated with differences
between lithological sequences and over disturbed ground such as faulted or
mineralized zones.
Time-domain Electromagnetics (TDEM)
TDEM techniques produce one-dimensional and two-dimensional geo-electric
cross-sections in a similar manner to electric cross-sections. Survey depths for
TDEM are from 5m to in excess of 100s of meters with high vertical and lateral
resolution. The techniques do not however give high resolution from 5m to the
surface. It is also possible to conduct electromagnetic surveying using logging
tools in non-metal cased boreholes. This procedure has been shown to be
extremely sensitive to lithological changes and is important for the calibration of
the surface geophysics with sub-surface geology. Additional correlation between
electrical/electromagnetic measurements and physical samples can be obtained
by measuring resistivity in the laboratory on borehole samples.
Seismic
The use of seismic surveys in groundwater evaluation has been somewhat limited
for groundwater contamination studies however a number of examples have been
34
SRTRI GROUNDWATER - PROJECT PROPOSAL
shown for groundwater exploration. These studies have traditionally relied on
seismic refraction techniques using compressional waves rather than seismic
reflection as used in the hydrocarbon industry because of the high costs
associated with the very close spacing necessary for the recording intervals when
looking at shallow depths. A few recent studies have used both shear waves and
surface waves but until relatively recently the technologies were not available for
correctly processing data generated from these wave types.
The majority of seismic studies have used the refraction technique to better
define the geometry of an aquifer system, that is to map the geometric relation of
the soil and rock. Some further use has been made with compressional wave
seismic for mapping the water table as there is a significant velocity increase
across the water table.
Since the late 1980’s the increase in power of personal computers and the
decrease in cost of digital acquisition systems has led to an increase in the
number of seismic reflection surveys that have been conducted. However, for
most shallow aquifers (less than 100m deep) a very close refection shot and
receiver spacing, typically less than 3m, is necessary to avoid spatial aliasing of
the data. This close spacing means that costs for conducting seismic reflection
surveys are still high. Furthermore, the processing of the seismic reflection data is
still a complex task that requires
Ground Penetrating Radar
Ground penetrating radar has seen a significant increase in use through the
1990's in near surface investigations with a number of case histories now
recorded for groundwater surveys. The increase in use has in part be stimulated
by an increase in computing power and the decrease in cost of computing.
Ground penetrating radar is an electromagnetic technique for measuring the
displacement currents in the ground. Displacement currents are defined by the
movement of charge within the ground by polarization and can be related to the
applied electrical field by the electric permitivity of the ground or the dielectric
constant.
35
SRTRI GROUNDWATER - PROJECT PROPOSAL
A N N E X U R E - 3A N N E X U R E - 3
E L E C T R I C A L R E S I S T I V I T Y M E T H O DE L E C T R I C A L R E S I S T I V I T Y M E T H O D
The electrical resistivity method is used to map the subsurface electrical
resistivity structure, which is interpreted by the geophysicist to determine
geologic structure and/or physical properties of the geologic materials. The
electrical resistivity of a geologic unit or target is measured in ohm-meters, and is
a function of porosity, permeability, water saturation and the concentration of
dissolved solids in pore fluids within the subsurface. Electrical resistivity methods
measure the bulk resistivity of the subsurface as do the electromagnetic methods.
The difference between the two methods is in the way that electrical currents are
forced to flow in the earth. In the electrical resistivity method, current is injected
into ground through surface electrodes, whereas in electromagnetic methods,
currents are induced by the application of time-varying magnetic fields.
Advantages A principal advantage of the electrical resistivity method is that
quantitative modeling is possible using either computer software or published
master curves. The resulting models can provide accurate estimates of depths,
thicknesses and electrical resistivities of subsurface layers. The layer electrical
36
SRTRI GROUNDWATER - PROJECT PROPOSAL
resistivities can then be used to estimate the electrical resistivity of the saturating
fluid, which is related to the total concentration of dissolved solids in the fluid.
Limitations of using the electrical resistivity method in ground water pollution
investigations are largely due to site characteristics, rather than in any inherent
limitations of the method. Typically, sites are located in industrial areas that
contain an abundance of broad-spectrum electrical noise. In conducting an
electrical resistivity survey, the voltages are relayed to the receiver over long
wires that are grounded at each end. These wires act as antennae receiving the
radiated electrical noise that in turn degrades the quality of the measured
voltages. Electrical resistivity surveys require a fairly large area, far removed from
powerlines and grounded metallic structures such as metal fences, pipelines and
railroad tracks. This requirement precludes using this technique at many ground
water pollution sites.
However, the electrical resistivity method can often be used successfully off-site
to map the stratigraphy of the area surrounding the site. A general “rule of
thumb” for electrical resistivity surveying is that grounded structures be at least
half of the maximum electrode spacing away from the axis of the electrode array.
Electrode spacings and geometries or arrays (Schlumberger, Wenner, Dipole-
dipole) are discussed in detail in the section below entitled, “Survey Design,
Procedure, and Quality Assurance”. Another consideration in the electrical
resistivity method is that the fieldwork tends to be more labor intensive than
some other geophysical techniques. A minimum of three crew members are
required for the fieldwork. Instrumentation Electrical resistivity instrumentation
systems basically consist of a transmitter and receiver. The transmitter supplies a
low frequency (typically 0.125 to 1 cycles/second or “Hertz”) current waveform
that is applied across the current electrodes. Power for the transmitter can be
supplied by either batteries or an external generator depending on power
requirements. In most cases, the power requirements for most commonly used
electrode arrays, such as Schlumberger (pronounced “schlum-bur-zhay”) and
Wenner arrays, are minimal and power supplied by a battery pack is sufficient.
Other electrode configurations, such as Dipole-dipole arrays, generally require
more power, often necessitating the use of a power generator. The sophistication
of receivers range from simple analog voltmeters to microcomputer-controlled
systems that provide signal enhancement, stacking, and digital data storage
capabilities. Survey Design, Procedure, And Quality Assurance Survey design
depends on the specific characteristics of the site and the objective of the survey.
The three most common modes of electrical resistivity surveying are profiling,
37
SRTRI GROUNDWATER - PROJECT PROPOSAL
sounding, and profiling-sounding, each having its own specific purpose. If the
purpose of the survey is to map the depths and thicknesses of stratigraphic units,
then the electrical resistivity data should be collected in the sounding mode.
Lateral electrical resistivity contrasts, such as lithologic contacts, can best be
mapped in the profiling mode. In cases where the electrical resistivity is expected
to vary both vertically and horizontally, such as in contaminant plume mapping,
the preferred mode is profiling-sounding. Sounding Mode: The two most common
arrays for electrical resistivity surveying in the sounding mode are the
Schlumberger and Wenner arrays. Electrode geometries for both arrays are shown
below. The depth of exploration is increased by increasing the separation of the
outer current electrodes, thereby driving the currents deeper into the subsurface.
Profiling Mode
The two most common arrays for electrical resistivity surveying in the profiling
mode are the Wenner and dipole-dipole arrays. The electrode geometry for the
Wenner array is the same as the sounding mode — the difference is that in
profiling mode the entire array is moved laterally along the profile while
maintaining the potential and current electrode separation distances.
The electrode geometry for the dipole-dipole array is shown in Figure 9-1. In the
profiling mode, the distance between the potential and current dipoles (a dipole
38
SRTRI GROUNDWATER - PROJECT PROPOSAL
consists of a pair of like electrodes) is maintained while the array is moved along
the profile. Profiling-Sounding Mode: As in the profiling mode, the Wenner and
dipole-dipole arrays are the most common arrays used in the profiling-sounding
mode. As the name implies, this mode is a combination of the profiling and
sounding modes. In the Wenner array the typical field procedure is to collect the
data in a succession of profiles, each having a different electrode separation. The
resulting data therefore contains information about the lateral and vertical
electrical resistivity variations.
39
SRTRI GROUNDWATER - PROJECT PROPOSAL
In the dipole-dipole array, the typical field procedure is to transmit on a current
dipole while measuring the voltages on up to six of the adjacent potential dipoles.
When the data collection is completed for the particular transmitter dipole, the
entire array is moved by a distance equal to one dipole separation and the
process is repeated.
The most frequent source of inaccuracy in electrical resistivity surveying is the
result of errors in the placement of electrodes when moving electrodes and/or
expanding the electrode array. These distance measurement errors are easily
detected on apparent electrical resistivity versus electrode separation curves and
for this reason the apparent electrical resistivities should be plotted as the data is
40
SRTRI GROUNDWATER - PROJECT PROPOSAL
acquired in the field. A qualified field geophysicist will recognize these errors and
direct the field crew to check the location of the electrodes. The second most
common source of error in electrical resistivity surveying is caused by the
electrical noise generated by powerlines. The most effective means of reducing
powerline noise is to minimize the contact electrical resistance at the potential
electrodes. This can be easily accomplished by using non-polarizing potential
electrodes along with wetting the soil under the electrode with water. Non-
polarizing electrodes are recommended instead of metal potential electrodes,
because the metal electrodes generate electrical noise due to oxidation reactions
occurring at the metal-soil (pore water) interface. Resistivity Data Reduction And
Interpretation Reducing electrical resistivity data is a simple process in which the
apparent electrical resistivity is calculated by dividing the measured voltages by
the applied current and then multiplying this quotient by the geometric factor
specific to the array used to collect the data. Once the apparent electrical
resistivities have been calculated, the next step in the interpretation process is to
model the data in order map the geologic structure. The method used to model
the apparent electrical resistivity data is specific to each data acquisition mode.
Electrical resistivity data acquired in the sounding mode, using either the Wenner
or Schlumberger array, can be modeled using master curves or computer
modeling algorithms. When using master curves, the interpreter attempts to
match overlapping segments of the apparent electrical resistivity versus electrode
separation plots with a succession of two-layer master curves. This modeling
method provides coarse estimates of the model parameters, is time consuming,
and requires skill on the part of the interpreter. An alternative method of
modeling sounding resistivity data is to use readily available computer modeling
software packages (Sandberg, 1990).
There are a variety of different types of algorithms; some assume discrete
electrical resistivity layers while others assume that electrical resistivity is a
smooth function of depth. The discrete layer algorithms require interaction on the
part of the interpreter, but allow for constraining model parameters to adequately
reflect known geologic conditions. The continuous electrical resistivity algorithms
are automatic, that is, they require no interaction on the part of the operator, and
therefore geologic constraints cannot be incorporated into the models. The
modeling of profiling and profiling-sounding mode data is much more involved
than in the case of sounding data. The profiling-sounding data reflects electrical
resistivity variations in the lateral and vertical directions, resulting in a much
more complicated computer simulation of the potential fields. The computer
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techniques capable of simulating these fields are finite difference, finite elements
and integral equation algorithms. All of these techniques are extremely time
consuming, and therefore expensive, and require a detailed understanding of the
underlying physical principles on the part of the interpreter. For these reasons
most profiling-sounding mode data is interpreted in a qualitative manner, with the
accuracy of the interpretation being based solely on the experience of the
geophysicist. Presentation Of Results Listings of the electrode separations, current
amplitudes, measured voltages and reduced apparent resistivities should be
included in the report. Any specific information regarding the manner in which the
data were reduced or modeled should outline in the report. As with data
interpretation, presentation of the final results are specific to the mode of data
collection. Sounding Mode: The electrical resistivity data collected in the sounding
mode are presented as a bilogarithmic plot of electrical resistivity versus the
distance from the current electrodes to the center of the array. If the d ere
modeled, the apparent electrical resistivities, as calculated from the model,
should be presented on the bilogarithmic plot with the observed apparent
electrical resistivities. In addition, the model should be presented in a section plot.
Profiling Mode: Data collected in the profiling mode are presented in a plot of
apparent electrical resistivity versus distance. Any modeling results, either using
computer algorithms or by “rule-of-thumb” methods should be presented and
include a legend indicating any parameter values. Profiling-Sounding Mode: Data
collected in the profiling-sounding mode are presented in psuedosection format in
which the apparent electrical resistivity is plotted as a function of position and
electrode separation. Any modeling results either using computer algorithms or
qualitative methods should be presented and include a legend indicating
parameter values.
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SRTRI GROUNDWATER - PROJECT PROPOSAL
A N N E X U R E - 4A N N E X U R E - 4
V E R Y - L O W F R E Q U E N C Y ( V L F ) M E T H O DV E R Y - L O W F R E Q U E N C Y ( V L F ) M E T H O D
The very-low frequency (VLF) electromagnetic method detects electrical
conductors by utilizing radio signals in the 15 to 30 kiloHertz (kHz) range that are
used for military communications. The VLF method is useful for detecting long,
straight electrical conductors, such as moderate to steeply dipping waterfilled
fractures or faults.
The VLF instrument compares the magnetic field of the primary (transmitted)
signal to that of the secondary signal (induced current flow within the subsurface
electrical conductor). In the absence of subsurface conductors the transmitted
signal is horizontal and linearly polarized. When a conductor is crossed, the
magnetic field becomes elliptically polarized and the major axis of the ellipse tilts
with respect to the horizontal axis (McNeill, 1988). The anomaly associated with a
conductor exhibits a crossover. As with other frequency domain electromagnetic
systems,both the in-phase (“real” or “tilt-angle”) and the outof-phase
(“imaginary”, “ellipticity”, or “quadrature”) components are measured.
A number of VLF transmitting stations operated by the military are located
worldwide; the most commonly used in North America are Annapolis, Maryland
(21.4 kHz), Cutler, Maine (24.0 kHz), and Seattle, Washington (24.8 kHz) stations.
Commercially available VLF systems utilize one or more of these transmitting
stations for survey applications.
Advantages
The VLF method is very effective for locating zones of high electrical conductivity,
such as water-filled fractures or faults within the bedrock. Structures often act as
conduits along which ground water and contaminants flow. The information from
a VLF investigation can be used to optimally locate monitor and/or treatment
wells in order to intercept these hydrologic conduits. Another advantage of VLF is
that data collection is fast, inexpensive and requires a field crew of only one or
two people.
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Limitations
The VLF method is affected by all electrical conductors, including those that are
man-made (powerlines, wire fences, pipes, and so on). The bearing or direction
from the VLF transmitting station to the intended target must be located nearly
parallel to strike (or long axis) of the conductor, or intended target for it to be
detected. Unfortunately there are only a limited number of transmitting stations
available with enough primary field strength to be usable, thus limiting the
direction that traverses can be collected. Therefore, the geometry of the target,
the survey traverses and the bearing to the VLF transmitting station(s) must be
resolved in the survey plan.
VLF transmitting stations often shut down for scheduled and unscheduled
maintenance. If this happens, another transmitting station may have to be used
or data collection may have to be halted until the transmitting station resumes
operation. Care must be taken to make sure that the antenna of the VLF receiver
is correctly and consistently oriented (always oriented in the same direction for all
stations of a traverse).
Instrumentation
VLF instruments have historically fallen into two types. Early instruments were
hand-held, and measured the tilt-angle of the major axis of the magnetic field
polarization ellipse. This angle is obtained by rotating the instrument until a null is
obtained (indicated audibly through a speaker); then, the angle is read from an
inclinometer mounted on the instrument case. Some instruments of this type also
could provide reading indicating the magnitude of the maximum inphase
component.
More recent instruments are either belt or backpack mounted due to the
increased weight of batteries needed for microprocessors which control these
devices. These instruments measure both in-phase and quadrature components
of the ratio of horizontal-to-vertical magnetic field. Some instruments have real-
time interpretive capability for use while still collecting data.
In either case, the measured quantity is such that variations in the source field
over time (from atmospheric fluctuations or actual signal-strength changes) are
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normalized out and the resulting information is repeatable hour-to-hour or day-to-
day.
Survey Design, Procedure, and Quality Assurance VLF data are normally collected
along traverses, and anomalies are correlated from traverse to traverse.
When planning a VLF survey several considerations must be taken into account.
First, is the direction of strike of the target. Traverses must be located
perpendicular to strike so that anomalous zones can be compared to background
levels. Every effort should be made to avoid putting traverses in areas that
contain a number of cultural features that may mask anomalies associated with
the intended target. Second, consideration must be given to which transmitting
stations are available for use during the survey. The direction toward the
transmitting station must be nearly perpendicular to the traverse (or in line with
the strike of the target).
When designing a survey, several traverses should be placed parallel to one
another and close enough (25 to 50 feet apart) so that anomalies can be
correlated from traverse to traverse. It is crucial that traverses are long enough
that the entire anomaly caused by the target is covered and the readings return
to a background level. Data can be collected on a grid; however, the data must be
collected along grid lines that are perpendicular to the target. Station spacing
should be close enough together that the entire form of the anomaly can be
observed (15 to 30 feet).
Each traverse must be accurately located on a map and related to a point or
landmark that can be recovered later.
During data collection, care must be taken to properly orient the VLF receiver
antenna and to consistently collect data facing the same direction. Failure to do
so will result in anomalies that do not “cross-over” in the proper sense and could
result in improper interpretation of these data. Careful field notes should be kept
while collecting data, noting the location of any cultural features (including buried
pipes, wire fences, powerlines, fieldstone or concrete walls, and building
foundations). Keeping careful and observant field notes will save time when
interpreting the data.
If the transmitter stops transmitting during data collection, another transmitter
may have to be used. If this happens, the entire traverse should be read again
using the new transmitter station. In some cases, another transmitter that is
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SRTRI GROUNDWATER - PROJECT PROPOSAL
located in the correct orientation may not be available. In this instance, data
collection will have to cease until the transmitter station resumes operation. It is
best if the same transmitter station can be used during the entire survey, because
strength and orientation of different transmitters can lead to slightly different
shaped anomalies, making the data more difficult to interpret.
To ensure data quality and to help in data interpretation, it is suggested that
readings be taken along the traverse using more than one transmitting station.
This does not add significantly to the amount of time it takes to collect data, and
often improves the accuracy of the interpretation.
Data Reduction and Interpretation
Most commonly used VLF interpretation methods are qualitative. Data collected in
the field can be interpreted without further data reduction. By plotting the “real”
and “imaginary” components versus distance along a traverse, an experienced
geophysicist can often interpret where fractures or zones of high electrical
conductivity are located.
Filtering techniques are often used to enhance data and make tilt-angle
crossovers easier to identify. Two commonly used filtering methods include the
Fraser filter (Fraser, 1969) and the Karous-Hjelt filter (Karous and Hjelt, 1985). The
Fraser filter simply converts tilt-angle crossovers into peaks. The Karous-Hjelt
filter calculates the equivalent source current at a given depth, commonly known
as current density.
This current density position can aid in the interpretation of the width and dip of a
fracture with depth. Commercial programs are available to calculate and plot data
using the Karous-Hjelt filter. Using such a program, current density can be plotted
with respect to depth and gray-tone plots can be created to further aid in
interpretation.
In order to determine the strike direction of a fracture it is necessary to have two
traverses (preferably more) close enough to one another so that the same
anomaly can be correlated from one traverse to the other. By stacking sets of
profiles it is then possible to correlate fractures or conductive zones across the
entire survey area. Once the strike direction of a fracture has been determined,
the fracture can be projected along strike to determine if it intersects any areas of
interest. Projecting fracture zones along strike can also aid in determining where
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SRTRI GROUNDWATER - PROJECT PROPOSAL
to place monitor and/or treatment wells, or where contaminants can migrate in a
fracture-flow system.
More quantitative methods of interpretation include curve matching. Vozoff and
Madden (1971) developed a number of interpretive curves which can help in the
interpretation of VLF data. Simple, numerical forward modeling can be
accomplished done using formulas found in Telford and others (1976). It must be
emphasized that when modeling, a number of assumptions are made, some of
which may be incorrect in a given situation.
If enough parallel traverses are collected it is possible to contour the data to
further aid in identifying zones of increased conductivity. If the data is to be
contoured, filtered data should be used so that the zones of increased
conductivity correspond to “highs” on the contour map.
Presentation of Results
The report should explain the methods and the reasoning behind the methods
used for data collection.
Explanations for what transmitting station was used, the traverse station spacing
and field procedures should be discussed in the report. Any problems encountered
during data collection (such as a transmitting station shutting down, or excessive
atmospheric interference) should be noted.
The most common way to present VLF data is to plot the “real” and “imaginary”
component values on the y-axis and distance along a traverse on the x-axis of a
plot.Plots for each traverse should appear in the appendix of the report. All of the
plots should be drafted at the same vertical and horizontal scales for consistency
and ease of comparison. The location of cultural features, as well as areas
interpreted as fracture zones should also be indicated on annotated plots.
The locations of the traverses should be shown on a base map. It is also useful to
identify anomalies interpreted as fracture zones on the map. The correlation of
anomalies from traverse to traverse should also be indicated on the map, in order
to delineate the continuation of interpreted fractures.
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SRTRI GROUNDWATER - PROJECT PROPOSAL
Case Study Groundwater exploration using VLF
Study in Granitic terrains of Northwestern Portugal
A groundwater exploration program using the VLF technique was carried out in
the Vieira do Minho area (Northwestern Portugal). Geological setting is dominated
by biotite-rich coarse-grained porphyritic granite crossed by quartz veins and
some basic rock dikes. Several sets of fractures break up the granite massif
yielding a chaotic relief constituted by the individual rock blocks generated by
rock fracturing.
The VLF data was collected with WADI, a two component magnetic receiver
developed by ABEM Corporation that operates in the frequency range 15-30 kHz.
The measurements of the VLF campaign over the area were carried out with
various profiles of varying length. Readings along those profiles stepwise 5 m
intervals. Another important issue involved in the planning of the surveys was the
necessity to maintain the orientation of the profile when taking the readings along
its length. So, a system was constructed to help in this matter, consisting of a wire
marked every 5 meters tightly stretched along the profiles.
The profile schematic applied on the area consisted of grid and isolated profiles.
The first aimed at determining the spatial distribution, accordingly to the terrain
possibilities, of the promising structures detected by the exploration goal of the
seconds. Thus far, the VLF campaign over the study area has generated 21
profiles between grid and isolated forms. The data of these profiles that,
summarily, is analyzed on the base of the relation between the horizontal primary
magnetic field and a vertical secondary magnetic field originated by induction on
a sub-surface conductor, was performed automatically with ABEM’s SECTOR
program. The Karous Hjelt filter offers the possibility to generate current density
pseudo-sections which, by showing the distribution of the apparent current
density along the depth, provides a pictured image that can give an idea of the
conductors geometry that originated the anomaly.
The data thus far gathered suggests that most of the anomalies detected are
small and shallow. They also seem more to translate a series of high density
fracture zones, poorly penetrating, rather than one isolated big fracture or fault
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SRTRI GROUNDWATER - PROJECT PROPOSAL
zone, being difficult to extract a general dip orientation. Supporting this
conclusion is a grid with 10 profiles oriented N240º that, when analyzed with filter,
depths below 10 meters depict two more conspicuous lineaments with a general
orientation of 190º-200º, thus requiring a reorientation of the profiles in order to
explore an adequate perpendicular direction to those lineaments. The current
density pseudo-sections for these profiles reveal a rather small depth reach of
most conductors, although in some profiles some conductors reach as much as 30
to 40 meters deep. Also, a grid consisting of 3 parallel profiles orientated N-S
shows two lineaments approximately perpendicular to that orientation. In one
case, there is a profile with an orientation N52º that clearly depicts a shallower
(20 meters deep aprox.) conductor at 120-130 meters in length indicating a dip
towards NE and a deeper (40 meters aprox.) vertical conductor at 150-170 meters
in length.
The interpretation of the data so far gathered in the VLF prospecting campaign
enables to define some promising areas of hydrogeological potential, on the basis
of preferential lineaments identified and also taking in to consideration the
general depth of the conductors they contain.
As an end remark, a reference should be made to the difficulty of selecting an
adequate transmitter whenever the profiles require their orientation to be around
NW. This leads to the conclusion that the prospecting potential of this equipment
could greatly be enhanced with a portable VLF primary magnetic field generator
with the inherent disadvantages that such equipment would carry.
By Dr. N. Sai Bhaskar Reddy
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