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    Guide toConductingWell Pumping

    TestsWater Stewardship Inormation Series

    How is the pumped water discharged? 6

    Is a water sample required or analysis? 7

    Are there special conditions to be aware o when

    conducting or interpreting the pumping test? 7

    Who can interpret pumping test data? 8

    What should be in a pumping test report? 8

    Further inormation and resources on pumping tests 8

    Table o Contents

    Whats the dierence between a well yield test

    and a pumping test? 1

    When are pumping tests needed? 1

    Who can conduct a pumping test? 2

    What are the key things to consider when designing

    and planning a pumping test? 2

    What time o year should a pumping test be done? 2

    Are there natural variations in the groundwater levels? 2

    Should other well owners be notied about the

    pumping test? 2

    What type o pump should be used and at what depth

    should it be placed? 2

    How much time will the pumping test take? 3

    How is the pumping rate selected? 3

    How is the pumping rate controlled and measured? 3

    How and at what intervals will changes in water levels

    be measured? 4

    When should neighbouring wells and/or stream levels

    be measured? 6

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    Figure 1. This fgure shows the impact o a pumping well on the water level

    and on a neighbouring well (observation well) in an unconfned aquier.

    As the water is pumped rom the well, the original water level lowers, i.e.,

    drawdown in the well. A cone o d epression is ormed in the aquier around

    the pumping well as the water level declines due to pumping. Note that

    drawdown in the observation well is much less than in the pumping well.

    Figure 2. Graph showing the dierent phases o a constant rate

    pumping test the pumping phase and the recovery phase.

    This guide provides general inormation and guidance on

    best pumping test practices or qualied well drillers and

    qualied well pump installers In addition, the guide oers

    general inormation to developers and local governments on

    the pumping test requirements or proving up water supplies

    (ie, to determine i sucient groundwater is available or

    residential developments) and an explanation o the benets o

    a properly conducted pumping test This guide is not meant to

    be a substitute or proessional guidance and the appropriatestandards o care

    What s the derence between a well yeldtest and a pumpng test?

    A well yield test is a short (eg, approximately one hour)

    fow test, usually done by a qualied well driller once the well is

    completed to provide a rough estimate o the wells yield It is

    generally recorded in the well construction report by the driller

    Well yield tests are done using bailing1 or air liting2 methods

    Well yield tests are not as reliable as a pumping test in theollowing situations

    when well yield is low (eg, typical bedrock well);

    where maximum yield rom the well is required;

    when reliable estimates o aquier properties are needed;

    and

    when assessing impacts o proposed pumping on

    neighbouring wells

    A pumping test is a practical, reliable method o estimating

    well perormance, well yield, the zone o infuence o the well

    and aquier characteristics (ie, the aquiers ability to storeand transmit water, aquier extent, presence o boundary

    conditions and possible hydraulic connection to surace water)

    A pumping test consists o pumping groundwater rom a

    well, usually at a constant rate, and measuring water levels in

    the pumped well and any nearby wells (observation wells) or

    surace water bodies during and ater pumping (see Figure 1)

    These data are used to plot drawdown and recovery as shown

    on Figure 2 Pumping tests can last rom hours to days or even

    weeks in duration, depending on the purpose o the pumping

    test, but traditional pumping tests typically last or 24 to

    72 hours

    Pumping test water level measurements should be made prior

    to, during and immediately ollowing the pumping periord(see

    Figure 2)The inormation collected during the recovery period is

    used to veriy the results o the pumping test

    When are pumpng tests needed?

    Wells can be pump tested solely to provide a greater

    condence in the drillers estimated well yield These tests are

    typically shorter in duration (eg, 4 to 12 hours) and are

    commonly done on domestic or single-residence wells

    Longer duration pumping tests are commonly required to:

    prove up water quantity under local government bylaws or

    new residential developments or regulatory requirements,

    eg, Certicate o Public Convenience and Necessity (CPCN);

    determine the maximum sustainable well yield;

    assess impacts on neighbouring wells or water bodies such

    as streams rom the proposed use o the well; and/or

    obtain aquier properties such as permeability and

    boundary conditions

    Cone ofDepression

    PumpingWater Level

    PumpingWell

    ObservationWell

    Original (Static)Water Table

    Distance from Pumping Wellto Observation Well

    Drawdown

    Pumping Rate

    Land Surface

    Aquifer

    Aquitard

    WaterDepthBelowOriginal

    Pre-PumpingStaticWaterLevel(metres)

    Elapsed Time Since Start Of Pumping (minutes)

    Pump

    Shutdown

    Pump

    Start-up PumpingPhase

    RecoveryPhase

    Original StaticWater LevelDrawdown

    Recovery

    1 Water is removed rom the well in a cylindrical bailer lowered rom the drilling rig mast

    2 Compressed air is injected into the well to blow air and water out o the well

    1

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    Who can conduct a pumpng test?

    Under Section 70 o the Water Act, the ollowing persons can

    conduct a pumping test:

    a qualied well driller;

    a qualied well pump installer; or

    a person working under the direct supervision o the

    qualied well driller, qualied pump installer or qualiedproessional with competency in hydrogeology

    A qualied proessional3 with competency in hydrogeology

    should be responsible to plan, design, implement and interpret

    the pumping test in the ollowing situations:

    where a pumping test or a well is required by an approving

    agency; or

    where the yield o the well needs to be maximized; or

    when data needs to be interpreted, or example:

    - when there is a need to assess the impact o the pumping

    well on nearby surace and groundwater resources; and- when estimates o an aquiers properties are required

    What are the key thngs to consder whendesgnng and plannng a pumpng test?

    Designing and planning a pumping test is critical prior to

    testing Lack o planning can result in delays, increased costs,

    technical diculties and poor or unusable data

    Some things to consider in the pre-planning stage are:

    4time o year the pumping test should be done

    4 natural variations in the groundwater levels that occur

    during the test that needs to be accounted or

    4 inorming others who may be aected

    4 depth o pump setting and type o pump

    4 pumping duration

    4 pumping rate

    4 control and measurement o the pumping rate

    4 requency o measurements o the water levels

    4 measuring water levels in neighbouring wells and/or

    streams

    4 discharge o pumped water

    4 collection o water samples or water quality analysis

    4 special conditions to be aware o eg, salt water intrusion

    in coastal aquiers

    What tme o year should a pumpng testbe done?

    An approving agency may require a pumping test to be

    conducted during a low recharge period (eg, dry period) or other

    time o the year For ractured bedrock and other low-yielding

    wells, a pumping test should be done during a dry period when

    water tables are at their lowest levels to allow or a conservative

    estimate o long-term yield Optimal times or testing in BC aresummer and all in coastal areas and all and winter in the Interior

    Are there natural varatons n thegroundwater levels?

    Natural variations in water levels caused by tidal, river and

    barometric changes can infuence water levels during pumping

    and recovery Even diurnal variation can occur in shallow water

    tables due to the great dierence between night and day

    evapotranspiration Pre-pumping and post-pumping (recovery)

    water level measurements in the pumping well and any

    observation well(s), can be used by the qualied proessionalhydrogeologist to lter out natural fuctuations

    Should other well owners be notfed about

    the pumpng test?

    I the pumping test involves pumping a large volume o water or

    a long duration (eg, 24 to 72 hours), owners o neighbouring wells

    (ie, any well within 300 eet or 100 meters o the pumping well)

    should be notied Pumping o these neighbouring wells during

    the pumping test could aect the results o the test, especially i the

    neighbouring wells are to be used as observation wells

    What type o pump should be used and atwhat depth should t be placed?

    The pump is normally placed above the well screen to maximize

    the amount o drawdown or the pumping test The intake o

    the pump should not be placed within the well screen as this

    may cause increased velocities resulting in sanding and potential

    casing deteriorization, along with screen plugging For bedrock

    wells the pump is set at or just above the uppermost major water-

    bearing racture (reer to the drillers well construction report)

    There are several actors to consider when determining the typeo pump to use and the depth at which it should be set, including:

    well diameter;

    desired pumping rate;

    total dynamic head including the pumping water level, the

    above ground head (i applicable) and all riction losses in

    the casing, pipes, ttings, etc;

    reliability o power source; and

    horsepower requirements3 Qualied proessionals who are registered with the Association o Proessional

    Engineers and Geoscientists o British Columbia

    2

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    As well, consider whether the pump is submersible and has

    variable speeds Power needs to be continuously available to

    the pump during the test I power is interrupted, it may be

    necessary to terminate the test, allow the well to recover and

    run a new test

    How much tme wll the pumpng test take?

    The duration o the pumping test depends on the purpose

    o the well, the type o aquier and any potential boundaryconditions Aquier types and potential boundary conditions

    can be obtained rom:

    well construction reports or the pumping well and any

    neighbouring well(s);

    inormation on the aquier and surace water bodies, such

    as lakes or rivers in the vicinity o the well; and

    qualied well drillers and proessional hydrogeologists

    Minimum durations o traditional pumping tests are 24 to

    72 hours unless stabilization occurs Local by-laws, regulatory

    requirements or a qualied proessional can stipulate minimum

    pumping durations Duration is generally longer, eg, 72 hours,

    or bedrock wells due to uncertainties associated with bedrock

    aquiers, and 48 hours or wells completed in unconned

    aquiers due to the delayed release o water as the water level

    goes down or delayed yield eect

    How s the pumpng rate selected?

    The well should be pumped at or above the required yield

    and the well should not be rated above the pumping rate used

    during the test

    Other considerations or setting the pumping rate are:

    wells should not be pumped at a rate higher than the

    manuacturers recommended transmitting capacity or the

    well screen to avoid damage to the well and aquier near

    the well Check the well screen details in the drillers

    construction report and reer to the section on entrance

    velocities in Groundwater and Wells

    wells completed in unconsolidated aquiers (eg, sands and

    gravels) with an open bottom (eg, no well screen) should

    not be pumped at a rate which could cause the heaving o

    aquier materials into the well and locking up the pump

    bedrock wells should not be overpumped (ie, water

    levels should not be drawn down past the uppermost

    water bearing racture) because turbulence at the

    borehole/well interace could damage the aquier

    ormation and result in excessive turbidity in the water

    A qualied proessional involved in the design o a pumping

    test may determine a step drawdown test is needed beore the

    constant rate pumping test is conducted I a step drawdown test

    is done, the well should be rested between the step test and the

    constant-rate pumping test to allow or the water level to recover

    A qualied proessional should determine the optimum pumping

    rate or traditional pumping and step drawdown tests

    Another consideration when selecting the pumping rate is

    borehole storage (eg, water stored in the well casing) In most

    cases, or a short period ater pumping begins, all the pumped

    water comes rom borehole storage However, in some cases,

    where the well is deep and the rate o intended use is low,the borehole storage may never be pumped out In these

    instances, the pumping rate can be initially set higher than the

    rate o intended use to remove the borehole storage and then

    the pumping rate is cut back to match the rate o intended use

    How s the pumpng rate controlled andmeasured?

    Control o the pumping rate during the test is important as it

    allows or reliable drawdown data to be collected to determine

    the yield o the well and aquier properties Controlling the

    pumping rate by adjusting the pump speed is generally notsatisactory It is better to use a gate valve to adjust the pumping

    rate to keep it constant The discharge pipe and the valve should

    be sized so that the valve will be rom to open when

    pumping at the desired rate The valve should be installed at a

    sucient distance rom the fow measurement device to avoid

    any impacts rom turbulence Measuring the discharge o pumped

    water accurately is also important and common methods o

    measuring discharge include the use o an orice plate and

    manometer (see Figure 3), an inline fow meter (see Figure 4), an

    inline calibrated pitot tube, a calibrated weir or fume, or observing

    the length o time taken or the pumped water to ll a container

    o known volume (see Figure 5) The fow measurement device

    should be compatible with the expected pumping rate Calibrated

    in-line fow meters and orice weirs are used to measure pumping

    rates or high production wells I an orice weir is used, the

    discharge pipe should be straight and level or a distance o at

    least six eet (18 meters) beore the water reaches the orice plate

    For relatively low pumping rates (eg,

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    How and at what ntervals wll changes n

    water levels be measured?

    Prior to the test, all water monitoring instruments should be

    checked to be sure they are working properly Fresh replacement

    batteries should be available or all manual sounding probes

    Beore the test begins, synchronize the watches o all observers

    and data loggers time-o-day settings All stop watches should

    be started at the time the pump starts pumping water orstopped i doing a recovery test

    Establish initial conditions by measuring static water levels

    in the well and any observation well(s) or a period o time

    beore starting the pumping test As a general rule, the period

    o observation beore the start o the test should be at least

    one week All observers should use the same measuring point

    on the top o the well casing or each well I static water levels

    in the aquier are changing due to recharge or other actors, a

    qualied proessional should be consulted on establishing the

    water level prior to the test

    A sounding tube or access tube, typically a to 1 (19 to 25 mm)

    diameter PVC pipe that extends rom the top o the casing

    down to 3 to 4 eet (09 to 12 meters) above the pump, can

    be used to take water level measurements without the probe

    getting tangled in the pump wiring Water levels can be

    measured using water level probes (see Figure 6) or pressure

    transducers (see Figure 7) I pressure transducers are used, select

    types that cover the range o drawdown anticipated Pressure

    transducers should be calibrated beore and ater the test Take

    manual readings o the water level prior to and ollowing the test

    and periodically throughout the test to conrm the water levelmeasurements by the transducer Measurements should be taken

    to the nearest 1/8 or 1/4 (03 to 06 cm)

    During a constant-rate pumping test the pumping rate must

    be measured correctly and recorded regularly In general, the

    lower the pumping rate, the more accurate and careul the fow

    measurement must be An unrecorded change o as little as

    two per cent in the pumping rate can aect the interpretation

    o the data, ie, indicate a alse stabilization or a boundary

    condition At the beginning o the test the pumping rate should

    be set as quickly and accurately as possible and should remain

    constant or the duration o the test For example, the pumping

    rate should not vary by more than ve per cent and should

    generally be within two to three per cent or higher pumpingrates It is good practice to measure and record pumping rates

    requently at the beginning o the test (eg, every 15 minutes

    or the rst hour) and hourly thereater or tests o one to three

    days Checking the pumping rate allows or adjustments to be

    made i the rate has drited, and conrms the selected pumping

    rate has been maintained Adjustments to the pumping rate

    should be recorded along with the measured rate and water

    levels during the pumping test Good record keeping is key to

    interpreting the pumping test results

    Figure 5. A ve gallon bucket (~20 liters) and a stop watch can be

    used to estimate low pumping rates.

    Figure 4. In-line fow meter.

    Figure 6. Water level measurement using water level probe and

    sounding tube.

    Sounding Tube

    WellWater Level Probe

    4

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    The Ministry o Environment has developed a Pumping Test

    Report orm to record inormation and data collected rom the

    pumping and recovery test http://wwwenvgovbcca/wsd/plan_protect_sustain/groundwater/brochures_ormshtml An

    Excel spreadsheet has also been developed to record the test

    drawdown and recovery data The recommended minimum

    intervals or water level measurements in both the pumping and

    observation well(s) during the pumping and recovery phases

    is shown inTable 1 as well as on the back o the Pumping Test

    Report orm Data collection at the minimum specied intervals

    will establish conditions that aect groundwater fow to the well It

    may not always be possible to take the drawdown measurements

    at the specied intervals In these cases, water level readings would

    be recorded with the actual time the drawdown was recorded

    Monitoring water level recovery ater the pump has stopped is

    very important because it aids the interpretation o the pumping

    test Recovery data also tend to smooth out variations in the

    pumping rate, should variations occur To obtain accurate recovery

    data, a check valve should be installed at the bottom o the pump

    discharge pipe to eliminate backfow o water into the well

    Typically, the duration o the recovery test is directed by the

    qualied proessional At a minimum, recovery water levels in the

    well should be monitored or the same duration o the pumping

    test or at least until 90 per cent recovery has been achieved

    The pump should not be removed rom the well until the waterlevel has returned to 85-90 per cent o the pre-pumping or

    static water level or until the supervising qualied proessional

    indicates the pump can be removed However, generally or a

    24-hour pumping test, 90 per cent recovery occurs within two to

    three hours ater the pump is stopped and the pump can then

    be removed This event should be recorded on the data sheet I

    the water does not recover within the same time duration o the

    pumping test (eg, 24 hours) the water level should be monitored

    daily or an additional week

    I the water does not return to 90-95 per cent o the starting

    water level ater a week, the test pumping rate is likely higher than

    the aquiers capacity to sustain this rate and urther testing (ie,

    longer pumping time and lower pumping rate) may be required I

    this happens, a qualied proessional should interpret the pumping

    test and recovery data and recommend a course o action

    Good record keeping is key to interpreting the data collected

    rom a pumping test Occasionally, fuctuations in the water level

    will occur, due to nearby pumping o another well, sudden rainallevents, tidal variations or changes in surace loading o the aquier

    due to heavy equipment (eg, trains) It is important to accurately

    Table 1

    Recommended minimum intervals for water level

    measurements for pumping tests.

    Well being pumped

    during pumping:

    Every minute or the rst 10 minutes**

    Every 2 minutes rom 10 minutes to 20 minutes** Every 5 minutes rom 20 minutes to 50 minutes**

    Every 10 minutes rom 50 minutes to 100 minutes**

    Every 20 minutes rom 100 minutes to 200 minutes**

    Every 50 minutes rom 200 minutes to 500 minutes**

    Every 100 minutes rom 500 minutes to 1000 minutes**

    Every 200 minutes rom 1000 minutes to 2000**

    Every 500 minutes rom 2000 minutes to 5000 minutes**

    Every 24 hours rom 5000 minutes onward**

    Final water level measurement just prior to end o pumping

    during reCovery:

    Every minute or the rst 10 minutes ater end o pumping***

    Every 2 minutes rom 10 minutes to 20 minutes ater end o

    pumping***

    Every 5 minutes rom 20 minutes to 50 minutes ater end o

    pumping***

    Every 10 minutes rom 50 minutes to 100 minutes ater end

    o pumping***

    Every 20 minutes rom 100 minutes to 200 minutes ater end

    o pumping***

    Every 50 minutes rom 200 minutes to 500 minutes ater endo pumping***

    Every 100 minutes rom 500 minutes to 1000 minutes ater

    end o pumping***

    Every 200 minutes rom 1000 minutes to 2000 minutes ater

    end o pumping***

    Every 500 minutes rom 2000 minutes to 5000 minutes ater

    end o pumping***

    Every 24 hours rom 5000 minutes onward***

    Figure 7. A pressure transducer can be used or automatic

    measurement and recording o water level and temperature,

    specic conductance or other parameters during the pumping test.

    5

    http://www.env.gov.bc.ca/wsd/plan_protect_sustain/groundwater/brochures_forms.htmlhttp://www.env.gov.bc.ca/wsd/plan_protect_sustain/groundwater/brochures_forms.htmlhttp://www.env.gov.bc.ca/wsd/plan_protect_sustain/groundwater/brochures_forms.htmlhttp://www.env.gov.bc.ca/wsd/plan_protect_sustain/groundwater/brochures_forms.html
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    note down data and to record events that occur during the

    pumping test Key points to note are as ollows:

    changes in the pumping rate;

    any periodic cycling on and o o well pumps in the area; sta changes during the pumping and recovery tests;

    i and when equipment (eg, sounding probe) was

    changed during the test;

    i the pumping test was conducted in a well eld, or when

    other wells were pumping;

    when the pump was pulled out;

    times and pumping rates o any observations wells;

    precipitation that occurred during the test;

    presence o sediments in the pumped water;

    presence o any smell rom the discharged water eg,rotten egg (H

    2S); and

    evidence o cascading water inside the well

    When should neghbourng wells and/or

    stream levels be measured?

    Monitoring o water levels in neighbouring wells (observation

    wells) and/or streams to assess the impact o the pumping well

    should be specied by the qualied proessional, especially where:

    obServATion Well*

    during pumping:

    Every 10 minutes or the rst 100 minutes**

    Every 50 minutes rom 100 minutes to 500 minutes**

    Every 100 minutes rom 500 minutes to 1000 minutes**

    Every 500 minutes rom 1000 minutes to 5000 minutes**

    Every 24 hours rom 5000 minutes onward**

    Final water level measurement just prior to end o pumping

    during reCovery:

    Every 10 minutes or the rst 100 minutes ater end o

    pumping***

    Every 50 minutes rom 100 minutes to 500 minutes ater

    end o pumping***

    Every 100 minutes rom 500 minutes to 1000 minutes

    ater end o pumping***

    Every 500 minutes rom 1000 minutes to 5000 minutes

    ater end o pumping***

    Every 24 hours rom 5000 minutes onward***

    * I the observation well is located in close proximity to the pumping

    well it may be possible to take more requent measurements

    ** Time since the real start time o the pumping or time immediately

    ater a step change in pumping

    *** Not required i time is beyond the specied duration o recovery

    measurements

    the pumping rate is high;

    there are regulatory requirements; and/or

    neighbouring wells or stream levels could be impacted by

    the pumping

    Existing wells may be used i they are within the same aquier

    ormation and the well owner has provided consent Water

    levels in at least one observation well need to be monitored i an

    aquier storativity value is required The observation well should

    not be pumped during the pumping test I this is unavoidable,

    the times and pumping rates should be recorded Oten, water

    levels may not vary as much in observation wells as they will in

    the pumping well, thereore it is important to establish reliable

    background conditions prior to the pumping test

    How s the pumped water dscharged?

    Proper discharge o the pumped water is important to

    ensure there is no damage due to erosion, fooding or sediment

    deposits in streams (see Figure 3) It is important to assess the

    volume o pumped water, i storage or treatment are needed,

    and disposal alternatives early in the planning process For land

    disposal, direct the water rom the pumping well in a down-hill

    direction at a sucient distance rom the pumping well This

    will prevent re-circulation o the pumped water into the well

    or aquier and will preserve both the pumping water level and

    the integrity o the pumping test Several hundred eet or more

    o discharge line may be needed (see Figure 8) I the aquier

    is conned (reer to the lithology section o the drillers well

    construction report), the water can generally be conveyed a

    shorter distance away rom the pumping well without aecting

    the pumping water level

    In an urban setting, the pumped water may be discharged to

    a storm sewer but local government approval may be required i

    the pumping rate is above a certain threshold

    For large production wells, where disposal will be to

    an adjacent water body or wetland, the local Ministry o

    Environment and Department o Fisheries and Oceans (DFO)

    oces must be advised as an approval may be required Even i

    the well water is potable, discharging the water to an adjacent

    Figure 8. Discharge pipe or a large volume pumping test in Merritt.

    6

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    In ractured bedrock aquiers it is important to know the

    depth o any major water-bearing racture(s) (usually ound in

    the drillers well construction report) to:

    ensure the water level is not drawn down below the

    racture during the pumping test; and

    enable meaningul interpretation o the pumping test and

    the wells sustainable yield

    A qualied proessional hydrogeologist should be consulted

    i the major water-bearing racture(s) are not known

    water body could mobilize sediment and impact sh habitat

    To eliminate or minimize this, a proper conveyance channel

    should be used Ensure the channel is either rock-lined or

    vegetated to prevent erosion (see Figure 9) and that the outlet

    to the receiving water body does not harm sh habitat by

    destabilizing stream banks or eroding instream habitat such asriparian vegetation, river banks or beds

    is a water sample requred or analyss?

    A pumping test is a good time to collect water quality samples

    to assess the chemical, physical and bacterial properties o the

    water Water samples should be collected when conditions

    have stabilized (ie, usually near the end o the pumping test)

    Sanitize the sampling port or bib with isopropyl alcohol or a

    dilute chlorine solution beore collecting a sample, taking care

    not to introduce the sanitization fuid to the water sample

    Consult with the qualied proessional responsible or the test orthe approving authority (eg, regional health authority or local

    government) to determine what water quality parameters to

    analyze Consult a qualied proessional i eld measurements

    are required (eg, pH, temperature, conductivity, alkalinity,

    dissolved oxygen and turbidity) Consult the laboratory or

    sampling procedures, sampling bottles, coolers and holding

    times or delivery o water quality samples to the laboratory

    A th sca cts t awaf wh cct tt th

    tst?Ihydroracturing (racking) has been used to increase the

    productivity o the well, it may advisable to wait up to a week

    beore conducting the pumping test Hydroracturing uses large

    volumes o water (eg, up to 2,000 US gallons or 76 m3/min)

    that either need to be pumped out or dissipate into the

    surrounding rock beore the pumping test is done Dissipation

    eects o hydroracturing can be checked by measuring the

    water level immediately ater the hydroracturing has occurred

    and over subsequent hours or days

    Small unconsolidated (sand and gravel) aquifers (eg,

    covering up to a ew km2 in area) have a limited storage and

    recharge capacity and are oten bounded by low permeability

    deposits such as silt, clay, till or bedrock (see Figure 10) The

    drawdown behaviour in the early part o the pumping test may

    give a alsely optimistic impression o the long-term yield The

    aquiers limits are reached when the drawdown rate increases

    noticeably (ie, an impermeable geologic boundary or barrier

    may have been reached) Wells pumped in coastal aquifers

    have the potential or salt water intrusion, particularly wherepumping occurs on ocean waterront properties (see Figure

    11) In this case, a qualied proessional hydrogeologist should

    be involved Monitoring a parameter like specic conductance

    throughout the pumping test will indicate whether salt water

    intrusion is occurring during the test For example, when specic

    conductance has risen to greater than 1,000 micro Siemens

    per centimetre (S/cm) which is equivalent to ~250 mg/L o

    chloride, it is likely salt water intrusion is being initiated Specic

    conductance can be monitored using a specic conductance

    PumpingWater LevelStatic Water

    Level

    AquiferBEDROCK

    Static Water Level

    Flow of Water to Well

    PumpingWater Level

    EncroachingSalt Water

    Figure 9. Conveyance channel constructed to reduce erosion rom

    discharged pumped water.

    Figure 10. Drawdown behaviour in small unconsolidated unconned

    aquier bounded by bedrock.

    Figure 11. Pumping test o a well adjacent to the ocean.

    7

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    probe or meter A qualied proessional should be consulted

    The qualied proessional will design the pumping test and

    determine whether sentinel or observation wells (ie, monitoring

    wells located between the oreshore and aults or racture zones

    adjacent to sea water and the pumping well) should be installed

    or monitored, as well as the parameters to monitor where there is

    a reasonable concern about salt water intrusion On the advice o

    a qualied proessional, pumping should be stopped i intruding

    salt water could aect the water quality in the coastal aquier

    Who can nterpret pumpng test data?

    Interpretation o pumping test data should be done by

    a qualied proessional with expertise in hydrogeology,

    especially in the ollowing situations:

    when required by an approving agency;

    where the maximum well yield is needed;

    to assess impacts o the pumping well; or

    when estimates o aquier properties are needed

    Where wells are tested solely to provide greater condencein the drillers estimated yield, a qualied well driller or pump

    installer with competency in pumping test interpretation may

    be able to interpret the pumping test data

    What should be n a pumpng test report?

    The ormal report or a pumping test should contain the

    ollowing:

    inormation on the well (ie, the well construction report,

    type o well and a diagram showing the wells location on

    the property, etc); inormation on eld procedures and personnel involved in

    the test (ie, person responsible or the pumping test, such

    as a qualied well pump installer)

    inormation on the hydrogeologic setting, including

    reerences to mapped aquiers, when available;

    pumping test inormation including the date o the

    pumping test, all data on the pump type, depth o pump

    setting, pumping rates, method o fow measurement,

    observations made during the pumping test, duration o

    the test, available drawdown, specic capacity, method o

    water level measurements and water levels/times recorded

    during the pumping test and recovery period;

    analysis and assessment o the pumping test data including

    an assessment o the long-term sustainable yield and

    potential impacts to neighbouring wells and/or streams;

    the qualied proessionals opinion on the short and

    long-term capacity o the well and its ability to meet the

    applicable production criteria (eg, subdivision by-law or

    private sources, projected demand or water systems);

    assessment o the water quality results, including copies o

    laboratory results; and

    signature and proessional seal o the qualied proessional

    responsible or the report

    Further normaton and resources onpumpng tests

    Reference books and ReportsSterrett R. J., 2007. Groundwater and Wells, 3rd edition

    New Brighton: Johnson Screens

    Allen, D.M., 1999. An assessment o the methodologies

    used or analyzing hydraulic test data in British Columbia.

    Queens Press

    Internet Resources

    Ministry o Environment Pumping Test Report orm -

    http://wwwenvgovbcca/wsd/plan_protect_sustain/

    groundwater/brochures_ormshtml

    Guidance document on conducting pumping tests orwells requiring a Certifcate o Public Convenience and

    Necessity (CPCN) -

    http://wwwenvgovbcca/wsd/plan_protect_sustain/

    groundwater/library/eval_well/indexhtml

    Checklist or Pumping Test Reports in Support o

    Certifcate o Public Convenience and Necessity -

    http://wwwenvgovbcca/wsd/plan_protect_sustain/

    groundwater/library/eval_well/well-07ht m

    Listing o Groundwater Consultants in BC -

    http://wwwenvgovbcca/wsd/plan_protect_sustain/

    groundwater/library/consultantshtml

    Provincial registry o qualifed well drillers -

    http://wwwenvgovbcca/wsd/plan_protect_sustain/

    groundwater/wells/applications/well_drillers_regpd

    Provincial registry o qualifed well pump installers -

    http://wwwenvgovbcca/wsd/plan_protect_sustain/

    groundwater/wells/applications/pump_install_regpd

    BC Water Resource Atlas for information on aquifers and

    wells - http://wwwenvgovbcca/wsd/data_searches/wrbc/

    indexhtml

    Photos by Vicki Carmichael, Jim Fye and Mike Simpson

    ISBN 978-0 -7726-7033-5

    8

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