E N D
1. 1
2. Units Hydraulic Conductivity (K)……[L/T]
Specific Storage (S) ……. [1/L]
Hydraulic Head
Elevation (h) ……[L]
Pressure head (P/?g) …….[L]
Velocity head (v2/2g) ……[L] negligible 2
3. 3
4. 4 DARCY’S LAW q = Darcy flux or hydraulic flux (L/T)
K = Saturated hydraulic conductivity (L/T)
dH = difference in total head (L)
dl = distance increment (L)
dH/dl = I = hydraulic gradient (unitless)
5. 5 Darcy’ Law
6. 6 Darcy’ Law
7. 7 DARCY’S LAW Q = total flow (L3/T)
A = total cross-sectional area (L2)
Q = qA
8. 8 DARCY’S LAW Actual water velocity is higher than q and called the pore water velocity, v.
v = q/n
n = porosity
9. 9 Example Consider measurements taken at two monitoring wells in an unconfined aquifer. The wells are located 200 m apart. The average K of the aquifer is 3.5 m/day. The observed values are 23.1 m and 24.2 m.
Find the total flow across the aquifer and the transmissivity.
10. 10
11. 11 Example q = -K dh/dx
Using consistent units of meters and days,
h1 = 23.1, h2=24.2, K=3.5
q = -K . (h2-h1)/(x2-x1)
= -3.5 . (24.2-23.1)/(200-0) = - 0.01925 m/day
12. 12 Since q is negative, flow is opposite to the direction of x. This is correct because flow occurs from high potential to low potential.
Q = qA = 0.01925 x 0.5(24.2+23.1)x1
= 0.455 m3/m-day
T = KD
D = 0.5(24.2+23.1) = 23.65 m
T = 3.5x23.65 = 82.8 m2/day
13. Deriving flow equations 13