subsurface flow Flashcards

1
Q

Is a geologic formation,

sediment, or rock that is

surrounded by sediment

beneath the ground and

contains a body of water

that has been contained by

at least one confining layer.

A

CONFINED AQUIFERS

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2
Q

L a y e r t h a t

s l o w s b u t d o e s

n o t c o m p l e t e l y

s t o p s w a t e r

f r o m p a s s i n g

t h r o u g h

A

AQUITARD

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3
Q

L a y e r t h a t i s

i m p e r m e a b l e o r

d o e s n o t a l l o w

a n y a m o u n t o f

w a t e r t o p a s s

t h r o u g h

A

AQUILUDE

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4
Q

Is a body of water that is not

silt or rock and is close

beneath the surface. During

rain and snowfall, this

aquifer receives direct

penetration from the

surface. The saturated

zone’s surface is known as

the water table.

A

UNCONFINED

AQUIFER

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5
Q

A fundamental principle in fluid mechanics
that describes the flow of a fluid through a
porous medium.

A

DARCY’S LAW

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6
Q

An aquifer below the land surface that is saturated by water.

A

Confined Aquifer

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7
Q

The level to which the water rises is called ____________________

A

potentiometric surface

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8
Q

is where water flows of the borehole under pressure.

A

Artesian flow

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9
Q

defined as a body of water formed from groundwater, rain water runoff and stream with its water table or upper surface open to the atmosphere.

A

Unconfined Aquifer

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10
Q

How an unconfined aquifers recharge?

A

-via infiltration or snowmelt
-rain or stream of water
-human activities

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11
Q

How an unconfined aquifer discharge

A

through natural discharge via springs, seepage, evapotranspiration, and artificial extraction such as wells and drainage system.

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12
Q

is normally used to assess flow towards a pumping well in unconfined aquifers under steady-state conditions.

A

The Dupuit-Thiem

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13
Q

It describes the
movement of
groundwater
towards or away
from a point (such
as a well) in a radial
direction

A

RADIAL GROUNDWATER FLOW

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14
Q

The time interval between
recharge and discharge points is
defined as the __________________

A

travel time of
groundwater flow

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15
Q

is used in several
applications, such as
designing exploitation and
monitoring systems, identifying
areas affected by
contaminant migration and
assessing the potential for
natural attenuation of
pollutants.

A

Travel time

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16
Q

The left-hand boundary is
impermeable (flow divide), and
flow discharges through the
right-hand fixed-head boundary.
The travel time is calculated
between the two arbitrary
points: xi(the departure point at
the water table) and x.

A

Aquifer system with a no-flow boundary and fixed head boundary condition and
constant groundwater recharge

17
Q

The system is bound
by two fixed-head
boundary conditions
and contains a flow
divide between
these two
boundaries.

A

Aquifer system with two fixed head boundary conditions, a flow divide within the system and
constant groundwater recharge

18
Q

A velocity of __ foot per
day or greater is a high
rate of movement for
ground water, and
ground-water velocities
can be as low as ___ foot
per year or __ foot per
decade.

A

1

19
Q

Flow
rates in aquifers are
commonly measured in
____ per day.

A

feet

20
Q

The system is bound by two
fixed-head boundary
conditions and contains a flow
divide outside of these two
boundaries. Flow is
unidirectional between the
constant head boundaries.

A

Aquifer system with two fixed head boundary conditions,
a flow divide outside of the system and constant
groundwater recharge