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Darcys law

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By comparison with N-S.E solution for simple cases it was concluded that: ... Constant head permeameter. Falling head permeameter. Example ... – PowerPoint PPT presentation

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Title: Darcys law


1
Lecture 5 6
  • Darcys law its applications

2
Darcys observation Law
  • One form of Darcy law

By comparison with N-S.E solution for simple
cases it was concluded that
3
Estimating the hydraulic conductivity
Kozney-Carman Equation
Fair and Hatch Equation
4
Example (Bear 1972)
  • 1 darcy 9.8697 x 10-9 cm2
  • a porous media has a permeability of 1 darcy.
  • a) What is the hydraulic conductivity of this
    medium for water (? 0.013 cm2/s)
  • b) What is the hydraulic conductivity of this
    medium for oil (? 1.8 cm2/s)

5
Simple Applications
  • Flow in confined, homogeneous constant thickness
  • What if we allow K to be a given function
  • What if we allow b to be variable
  • Range of DL validity (NRqd/v less than 10)

6
Determination of Flow Direction (horizontal flow)
7
Problem 2.2.4 TEXT
8
Constant head permeameter
9
Falling head permeameter
10
Example
A long narrow reservoir (area 1.5 km2)is
hydraulically connected to a stream though a 7 m
thick sand body. To keep the water level
constant, (25 m above the stream level), a flow
of 4.2 m3/min is added to the reservoir. a)
calculate K for the sand. b) If the inflow is
stopped, neglect evaporation and calculate how
much time is required to drop the water level by
3 m c) If a layer of silt (K0.003 m/d) 0.5 m
thick is formed on the face of the aquifer
calculate the reduction of seepage.
11
Equivalent K for Layered Media
12
Anisotropy
13
Example on anisotropy
  • x and y are principal axis and Kx 25 m/d, Ky
    5 m/d estimate the flow direction if the head
    gradient I has a magnitude of 0.01 and makes an
    angle of 50 with the x-axis, estimate the
    magnitude and direction of the Darcy velocity.

14
Refraction of q
Flow across boundary is equal Pressure at
interface is the same in both PMs
15
Example
  • Downward seepage occurs from a shallow pond
    to a water table. A conservative traces is
    introduced at point A. Calculate the location of
    tracer appearance at the water table and the time
    it takes. Neglect dispersion, diffusion and
    assume subsurface fully saturated.

16
K for fractured PMsection 2.2.4 text
Example 2.2.2 Fracture thickness 0.01
cm Fracture spacing 220 cm Q (total) Q (pm)
Q (fracture)
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