14 drainage
TRANSCRIPT
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Drainage
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Introduction
Water is component of all landscape designs that cannotbe ignored.
Water issues include:
1. Too much
2. Not enough
3. Water being at an undesirable point
4. Water flowing across an undesirable point
5. Frost heave
Too much water can be handled by drainage.
Not enough water can be resolved by using irrigation.
Drainage can also be used to move water from unwanted
areas. Drainage structures can be used to reroute water.
Drainage can also be used to reduce the effects of frostheave.
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Site Analysis
Before starting to survey a site for drainage purposes it isimportant to evaluate the site.
If the site adjoins a waterway, do not remove the vegetation
adjacent to and along the stream bank.
This vegetation is an essential buffer zone that will help maintain
the water quality and curb erosion problems.
Check your survey or plat for the location of nearby flood plains.
If the land is in a flood plane, it is reasonable to expect the area will
be inundated with water at some point.
It is important that no structures, especially homes, are built within
a designated flood plane.
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Drainage
Drainage is the natural orartificial removal of surface
and sub-surface water from
a given area.
Drains can be either surface
or subsurface.
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Need For Drainage
A landscape design that does not properly control runoff maycause damage to and devaluation of the property.
To prevent damage or devaluation of property, three questions
must be answered.
What is the elevation of the design property in relation to adjacent
properties. Will water run onto the property, if so, were does it enter and were
does it exit?
How will the landscape plan change the drainage at the site.
Drainage is needed to handle rooftop, driveway, and overland
run off.
Four main issues to consider when caring for soil and grass roots
are fertilization, drainage, aeration, and thatch control.
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Eight Drainage Principles
1. Water flows downhill
2. Whenever it rains you have the potential for runoff.
3. The greater the intensity of the rain--the greater the potential for
runoff.
4. Reducing the permeability of the soil increases runoff.
5. Increasing the non-permeabile area will increase runoff.6. Water or silt on walkways during, or after a rain, is an indication
of poor design.
7. A good landscape plan includes drainage in the plan.
8. Drainage plans rely upon slope, pipes, berms or other
structures to control the direction the water flows.
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Slope
Any area that is exposed to rainfall should always have some
slope to direct the flow of water.
Water will puddle on flat, horizontal surfaces.
The amount of slope varies with the surface and the conditions
of the site.
Turf areas = 2 - 3%
Paved areas = 2%
Foundations = special requirements
One recommendation is
a six inch drop within
the first 10 feet.
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Surface Drains
Surface drainage is controlling the
flow of water using slope andshaped surfaces.
Shaped surfaces
Swales
Ditches
Berms
Surface drainage works best withsmall sites or for sites with a smallamount of runoff.
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Subsurface Drain
Subsurface drain is a system ofcollecting and disposing of rain water.
Common means of collection are a drain
grate or perforated pipe.
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Drain Outlet
Both surface and sub surface drains must have an outlet. Modification of existing outlets is usually not very problematic,
changing the location of an outlet may cause problems.
One alternative is to direct the water towards the street.
May require a permit.
Greater problem if the drain is a redirect and not the natural path.
Part of drainage plan that most municipalities require for
development.
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Drain Outlet--cont.
If codes do not allowed the redirection of water to the street, whatare the options?
Unless you already have a landscape drainage system in place
(allowing you to route the runoff into that system), you have two
(2) options.1. Channel the water to a location on
the site (but make sure its not a
neighbor's!) where it's less
troublesome and where it can
percolate into the ground.
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Drain Outlet-cont.
2. Build a pond and direct the water into it.
A pond may be constructed of stone or
concrete
A storm detention cell may be a
code requirement.
or natural.
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Estimating Runoff
Before a decision is made on the
type and size of drainage structureor storage structure that is needed,
the peak runoff rate and total
volume of runoff must be
determined.
The peak rate of runoff is
required when sizing
drainage channels and
pipes.
The total amount ofrunoff is needed to size a
pond.
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Estimating Peak Runoff Rates
Several different methods are available. Rational
Useful for estimating peak runoff rates from small areas.
Does not estimate volume of runoff.
USDA-NRS Technical Release 55 (TR-55)
Most popular method
Two methods
Tabular method
Graphical discharge method
US Army Corps of Engineers HEC-1 Model
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Rational Method
The rational method is useful for estimating peak runoff ratesfrom small
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Runoff Coefficient (C)
The runoff coefficient (C) is defined as the ratio of the peakrunoff rate to the rainfall intensity.
The runoff coefficient mathematically indicates whether the
runoff is likely to be high or low for the watershed.
The value of C depends on the type and characteristics of thewatershed.
Values for C are usually determined from tables.
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Coefficient
Table
Area Description Runoff Coe ffic ient CBusiness
Downtown 0.70 -0 .95 Neighbor hood 0.50 -0.70
Residenti alSingle -Family 0.30 -0.50 Multiunits, detached 0.40 -0.60 Multiunits, attached 0.60 -0 .75 Residenti al (suburban) 0.25 -0.40
A partment 0.50 -0.70 Indust rial
Light 0.50 -0.80 Heavy 0.60 -0 .90 Railroad yard 0.20 -0.35 Unimproved
0.10 -0.30
Parks, ceme t eries 0.10 -0.25 Playgrounds 0.20 -0.35
Character o f surface Runoff Coe ffic ient CPavement
Asphaltic and concret e 0.70 -0 .95 Brick 0.70 -0.85
Roofs 0.75 -0 .95 Lawns, sandy soil
Flat, 2 percent 0.05 -0.10 Average, 2 -7 percent 0.10 -0.15 St eep, 7 percent 0.15 -0.20
Lawns, heav y soil Flat, 2 percent 0.13 -0.17
Ave rage, 2 -7 percent 0.18 -0.22 St eep, 7 percent 0.25 -0.35
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Rainfall Intensity, Duration & Recurrence Interval
To find the correct
value for rainfall
intensity from the
chart, the time of
concentration must
be known.
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Time of Concentration (TOC)
The time of concentration for a watershed is defined as the timerequired for water to flow from the most remote point of the
watershed to the outlet.
The peak rate will occur when the entire watershed contributes
to the runoff.
The time of concentration is a function of drainageway lengthand slope.
Tables are available for TOC.
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Area
The area used is the number of acres in the watershed above the
outlet.
Watershed area can bedifficult to determine.
When a map is
available a planimeter
can be is used for this
purpose.
Another method is placing a grid over the map and counting
squares.
If the map is digital, mapping software can calculate area.
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Rational Method Example
Determine the peak runoff for a1- 1/2 acre lot that has grass
planted on heavy soil with an average slope of 3%. The client saysa 50 year reoccurrence interval is appropriate. The drainageway is
850 feet long and has a slope of 1.25 %.
Q = CIAThe first step is
determining the C
value.
Character o f surface Runoff Coe ffic ient CPavement Asphaltic and concre te 0.70 -0 .95 Brick 0.70 -0.85
Roofs 0.75 -0 .95 Lawns, sandy soil
Flat, 2 percent 0.05 -0.10 Average, 2 -7 percent 0.10 -0.15 St eep, 7 percent 0.15 -0.20
Lawns, heav y soilFlat, 2 percent 0.13 -0.17
Ave rage, 2 -7 percent 0.18 -0.22 Steep, 7 percent 0.25 -0.35
C = 0.18 to 0.22
Use 0.22
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Example--cont.
The next step is todetermine anappropriate value forthe rainfall intensity.
The time of concentration is used
to determine theintensity.
Time of concentration for small wat ersheds (min).
Drainage way gradient (slope), %
Maximum lengt hofflow (ft) 0.05 0.10 0.50 1.00 2.00 5.00
500 18 13 7 6 4 3
1,000 30 23 11 9 7 5
2,000 51 39 20 16 12 9
4,000 86 66 33 27 21 15
6,000 119 91 46 37 29 20
8,000 149 114 57 47 36 25
10,000 175 134 67 55 42 30
7 min
This example shows one of the problems of using tabular data.
What do you do when the data falls in between columns and/or
rows?
In this case the lower number was used knowing that this willcause the calculated peak flow to be slightly higher.
A drainageway of 850 feet at 1.25% slope =
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Example--cont.
With a TOC of7 minutes
and a 50 year interval, the
IDR graph can be used to
estimate rainfall intensity.
I = 10 in/hr
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Example--cont.
Solving for peak runoff:
Q = CI
= 22 x 10 x 1.25
= 275 cfs
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Mixed Watershed
The previous example assumed that the entire watershed hadthe same surface and slope.
This seldom happens, therefore the equation must be modified
to accommodate mixed watersheds.
This is accomplished by calculating a Weighted C.
Cw=
C1x A
1 C2 x A2 ...Cn An A
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Mixed Watershed Example
Determine the peak runoff for a watershed that consists of .75
acres of impervious surface, 3.4 acres of lawn at 1.8 % slopeand sandy soil and 2.2 acres of lawn at 0.75% slope and heavy
soil. The drainageway is 400 feet long with a slope of 1.2%.
The first step is to determine the weighted C.
Cw =0.70 x 0.75
0.06 x 3.4
0.15 x 2.2 0.75
3.4
2.2
Cw =5.25 + 0.204 + 0.33
0.75 + 3.4 + 2.2=
1.059
6.35= 0.167
r ct r f s rf c ff ffici tt
s ltic c cr t 0.70-0.95rick 0.70-0.85
Roofs 0.75-0.95Lawns, sandy soil
lat, 2 rc nt 0.05-0.10rage, 2-7 ercent 0.10-0.15
teep, 7 percent 0.15-0.20Lawns, eavy soil
lat, 2 percent 0.13-0.17verage, 2-7 percent 0.18-0.22teep, 7 percent 0.25-0.35
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Mixed Watershed Example--cont.
With a drainageway length of 400 feet and a slope of 1.2% the best
number for TOC is 6 minutes.
Time of concentration for small watersheds (min).
rainage way gradient (slope), %Maximum lengthof flow (ft)
0.05 0.10 0.50 1.00 2.00 5.00
500 18 13 7 6 4 3
1,000 30 23 11 9 7 5
2,000 51 39 20 16 12 9
The next step is to determine the time of concentration and rainfallintensity.
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Mixed Watershed Example--cont.
With a TOC of6 minutesand a reoccurrence
interval of 100 years, the
rainfall intensity can be
determined from the
chart.
Rainfall intensity = 12
in/hour
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Mixed Watershed Example--cont.
The peak runoff rate from the mixed watershed is:
Q = CIA
= 0.167 x 12 x 6.35
= 12.72.. or 12.7 cfs
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Questions?