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Flow through Soils ch7

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Head: convert each form of energy into the equivalent ... Slug test. Pumping test. In-situ testing. k a pore size. Hazen's Correlation ~ (pore diameter)2 ... – PowerPoint PPT presentation

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Title: Flow through Soils ch7


1
Flow through Soils(ch7)
2
Energies
Kinetic E (velocity) Strain E (fluid
pressure) Potential E (elevation) Head convert
each form of energy into the equivalent
potential energy and express it as the
corresponding height. units of LENGTH
3
Heads
hv velocity head (KE) hp pressure head
(SE) he elevation head (PE) h total head
hv hp he (Bernoulli) units of LENGTH
4
Heads in a tank of water
A
B
5
Head loss
Fluid flows from point of high total head to
point of low total head
head loss Dh h1 h2
6
Hydraulic gradient

Rate at which the total head changes along a
length
7
Heads in soils
Since velocity is slow through soils, we neglect
the velocity head. Thus,
8
Soil piezometer
A
The pore water pressure at A is
9
Pore water pressures

uhydrostatic uh due to hydrostatic condition
only
uexcess ue due to additional processes
10
Hydrostatic pore water pressure

11
One dimensional flow
Flow vectors parallel of equal magnitude

SOIL
Flow is in one direction
12
Flowrate through soil
What is the flowrate through a soil?

Concrete dam
Flowrate Q m3/sec
SOIL
13
Darcys Law
Assumptions flow is laminar soil
properties do not D with time

14
Finding k
Measure Q
Figure 7.11 (text)
15
k
Measure of a soil-fluid systems resistance to
flow
depends on
Void size Fabric (structure) Void
continuity Specific surface (drag)
Viscosity Mass density
16
k
Units are in cm/sec
but
k velocity
17
k
sands
10-3 100
silts
10-8 10-3
clays
10-10 10-6
Probably soils most varying parameter (largest
numerical range)
18
Lab testing
k1 10-2 k2 10-6
k precision is on the order of /- 50 or
more! Report values to one decimal place.
19
Lab testing (constant head test)
Measure Q
Figure 7.11 (text)
20
In-situ testing
Slug test Pumping test
21
Hazens Correlation
k a pore size
(pore diameter)2
(pore diameter) D10
For loose clean sands with 0.1mm lt D10 lt 3mm and
Cu lt 5
k cm/sec C Hazens coefficient 0.8 1.2
(typical 1) D10 mm
22
Example
Given ksand 4x10-2 cm/sec reservoir length
(into board) 1000 m
Compute seepage loss (Q) through the sand seam
23
Solution
Q kiA
k 4x10-2 cm/sec
i Dh/L (167.3m 165m) / 256m 0.009
A (3.2 m) (1000 m) 3200 m2
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