Chapter 7 Ground water Flashcards

1
Q

A water table is defined as

A

the surface on which the fluid pressure in the pores of a porous medium is exactly atmospheric.

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2
Q

a ……………………often existed above………………………

A

saturated capillary fringe

the water table

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3
Q

a hydrologic system is often divided into

A
  1. unsaturated zone
  2. capillary fringe (sometimes also called tension-saturated zone)
  3. saturated zone.
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4
Q

The following figure represents

A

Hydrologic system zones

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5
Q

A represents

A

Unsaturated zone

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6
Q

B represents

A

capillary fringe

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7
Q

C represents

A

Saturated zone

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8
Q

D represent

A

Water table

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9
Q

If one places a well a few feet or so below the water table, the water in that well will

A

rise to the elevation of the water table at the location of the well.

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10
Q

The water table often follows

A

topography

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11
Q

although the relief of the water table is ……………….. than the topography, ……………………………. generally flows from topographic ………………….to topographic …………….., and discharges at ……………………………..

A

less - Groundwater - highs - lows - the topographic low spots.

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12
Q

The capillary fringe

A

subsurface layer in which ground water seeps up from a water table by capillary action to fill pores.

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13
Q

Pores at the base of the capillary fringe are……………………………… due to ………………

A

filled with water due to tension saturation

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14
Q

This saturated portion of the capillary fringe is ………………than total capillary rise because of ……………………………………….

A

less

the presence of a mix in pore size.

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15
Q

If pore size is small and relatively uniform, it is …………………………………………..

A

possible that soils can be completely saturated with water for several feet above the water table.

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16
Q

If pore size is small and relatively uniform, it is possible that soils can be completely saturated with water for several feet above the water table. Alternately, the saturated portion will

A

extend only a few inches above the water table when pore size is large.

17
Q

aquifer

A

geologic unit that can store and transmit water at sufficient rates to supply wells.

18
Q

Unconfined aquifers

A

water seeps from the ground surface directly above the aquifer.

19
Q

Confined aquifers

A

an impermeable dirt/rock layer exists that prevent water from seeping into the aquifer from the ground surface located directly above. Instead, water seeps into confined aquifers from farther away where the impermeable layer doesn’t exist.

20
Q

Confining layers are subdivided into

A

aquifuges (absolutely impermeable) and aquitards (impermeable relative to the adjacent units).

21
Q

unconfined aquifers

A

Water table aquifers, those with no confining layer above

22
Q

confined aquifers

A

Aquifers overlain by a confining layer

23
Q

A represents

A

Recharge

24
Q

B represents

A

confined aquifier

25
Q

C represent

A

confining layer

26
Q

Aquifers are

A

underground layers of very porous water-bearing soil or sand.

27
Q

Aquitards

A

compacted layers of clay, silt or rock that retard water flow underground; that is, they act as a barrier for groundwater.

28
Q

Aquitards ………………………………..and ………………………………….

A

separate aquifers

partially disconnect the flow of water underground.

29
Q

Aquitards separate aquifers and partially disconnect the flow of water underground. Also known as

A

cap rocks

30
Q

aquitards …………………… and …………………….the surface water which ………………………. and ……………………..

A

limit and direct

seeps down and replenishes aquifers.

31
Q

aquiclude

A

geological material through which zero flow occurs.

32
Q

Groundwater flow

A

part of stream flow that has infiltrated the ground, has entered the phreatic zone, and has been discharged into a stream channel, via springs or seepage water

33
Q

Groundwater is water that is found ……………………… in …………………………….

A

underground in cracks and spaces in the soil, sand and rocks.

34
Q

Groundwater is water that is found underground in cracks and spaces in the soil, sand and rocks. ………………………………………………….is called a ………………………. or saturated zone.

A

An area where water fills these spaces

phreatic zone

35
Q

The rate of groundwater flow depends on

A
  1. on the permeability (the size of the spaces in the soil or rocks and how well the spaces are connected)
  2. hydraulic head (water pressure).