MIDTERM Flashcards

(41 cards)

1
Q

Symbols meaning

A

ι = Hydraulic Gradient
h = loss of head from A to B
L = length of flow over A to B
V = discharge velocity
K = hydraulic conductivity or coefficient of permeability
q = Flow rate
A = cross sectional area
Vs = seepage Velocity
n = porosity
e = void ratio
Q = Volume of water collected
t = duration of water collected
h = constant head between inlet and outlet
a = area of standpipe
h1 h2 = heads
r1 = smaller
r2 = larger or away
D10= effective size
c = constant that varies from 10 to 50mm2
h = capillary rise in mm

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2
Q

Known as Darcy slope (determines quantity of Darcy flux or discharge)

vector gradient between 2 or more hydraulic head measurements over the length of the flow path

A

Hydraulic Gradient

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3
Q

is a measure of a given porous medium ability to permit fluid flow through its voids

Interconnected voids that permits water to pass through under gradient force.

A

Permeability

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4
Q

The ability of an aquifer to transmit water through its entire thickness

A

Transmissivity or transmissibility

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5
Q

Ground-water reservoir, underground layer of water-bearing permeable rock, rock fractures, or unconsolidated materials where groundwater can be extracted using a water well.

A

Aquifer

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6
Q

Is the rate of flow of water through porous medium per unit cross-sectional area.

Used to solve for coefficient of permeability

A

Discharge Velocity

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7
Q

Represents the average velocity of flowing groundwater within pores of a porous medium.

Actual velocity (?)

flow of water through soil

A

Seepage Velocity

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8
Q

Use to determine the coefficient of permeability of coarse-grained soil

A

Constant Head Test

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9
Q

Who made the Darcy’s Law or Darcy’s permeability of soil

A

Henry Darcy

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10
Q

Hydraulic Gradient formula

A

ι =h/L

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11
Q

Discharge Velocity Formula

A

V=K ι
V=Q/At
Q=AV

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12
Q

Flow Rate Formula

A

Q=K ι A

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13
Q

Seepage Velocity Formula

A

Vs=V/n

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14
Q

Porosity Formula

A

n=e/1+e

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15
Q

Constant Head formula

A

K=QL/Aht

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16
Q

Falling Head Test

A

K=(aL/At) ln (h1/h2)

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17
Q

Area formula

18
Q

mm-m
cm-m
mm-cm

A

1/1000
1/100
1/10

19
Q

Unconfined Aquifer Formula

A

Q ln (r1/r2) / π(h1^2 - h2^2)

20
Q

Confined Aquifer formula

A

K= Q ln (r1/r2) / 2πt (h1-h2)

21
Q

Transmissibility formula

A

K= Q ln (r1/r2) / 2π (z1-z2)

22
Q

Total Stress Formula

23
Q

Pore water pressure formula

24
Q

Effective Stress Formula

25
Capillary Stress formula
c=S(δ w) (h)
26
Capillary Rise formula
h= c/eD10
27
Gamma dry
δ d= Gs δ w / 1+e
28
Gamma moist
(Gs+Se) δ w / 1+e
29
Gamma sat
δ sat= (Gs+e) δ w / 1+e
30
Porosity formula
e / 1+e
31
Describes how fast water flows through the soil voids.
Hydraulic Conductivity
32
Sponge term, ratio of volume of voids to the total volume of soil
Porosity
33
Ratio of empty spaces in soil
Void Ratio
34
Meaning of r
distance from test well to observation well r1 is the nearest
35
Meaning of z
water level dropped, should be subtracted to height z1 is for h1
36
Movement of pore water from lower elevation to higher elevation, experiencing upward pull
Capillary Rise
37
The pressure transmitted through particles' contact with each other. (grain-to-grain interaction). Deformation of soil.
Effective Stress
38
It is the pressure of grounwater or fluids in the pore space of rock
Pore Water Pressure
39
Have a layer of impenetrable rock or clay above them, usually deeper than unconfined aquifer
Confined Aquifer
40
Lie below the permeable layer of soil, being recharged by rainwater or snow melt.
Unconfined Aquifer
41
Used to determine the coefficient of permeability of sands/silts/clays
Falling Head Test