Final Flashcards

(38 cards)

1
Q

Define Area of Influence

A

The land surface overlaying the cone of depression.

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2
Q

Define Artesian Aquifer

A

occurs when there is positive hydraulic head in the aquifer, when an aquifer’s recharge area is higher in elevation than the drainage point. This allows the porous aquifer to have a positive pressure and possibly even flow water to the ground.

When an aquifer is confined by an impermeable bed, a well penetrating this aquifer will have a water level higher than the aquifer, reflecting the pressure within the aquifer which is > than atmospheric

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3
Q

Define Bail Test

A

The removal of water from a well at regular timed intervals, using a long cylindrical container or bailer.

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4
Q

Define Baseflow

A

Steady input of groundwater that sustains streamflow over long periods of time.

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5
Q

Define Bedrock

A

A common term for consolidated rock underlaying soils and subsoils, a relatively solid rock or rick with significant contrast in hydraulic conductivity.

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6
Q

Define Capacity

A

The rate at which a well can produce on a continuous long-erm basis.

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7
Q

Define Cave

A

A natural underground space, created by the movement of groundwater.

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8
Q

Define Capillary Fringe

A

The subsurface layer in which groundwater seeps up from a water table by capillary action to fill pores. Pores at the base of the capillary fringe are filled with water due to tension saturation. Height of the capillary fringe is related to pore size.

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9
Q

Define Catchment

A

An area over which water falling on the surface will drain into a river or lake. Refers only to surface waters.

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10
Q

Define Condensation

A

an air mass is not 100% saturated with water vapour, but as the air temperature drops and the concentration of the air mass reaches 100% (the dew point), water will condense and drop out of the air (precipitation).

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11
Q

Define Compaction

A

to the process by which a sediment progressively loses its porosity due to the effects of loading. This forms part of the process of lithification. When a layer of sediment is originally deposited, it contains an open framework of particles with the pore space being usually filled with water. As more sediment is deposited above the layer, the effect of the increased loading is to increase the particle-to-particle stresses resulting in porosity reduction primarily through a more efficient packing of the particles and to a lesser extent through elastic compression and pressure solution.

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12
Q

Define Cone of Depression

A

The lowering of the water table near a well, an inverted cone-shaped surface of the water levels in the vicinity of a pumping well, caused by a decrease in pressure in the aquifer due to pumping.

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13
Q

Define Darcy’s Law

A

Flow rate is proportional to the rate of change in hydraulic head.

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14
Q

Define Differential Subsidence

A

When a subsiding rock unit has varying mechanical properties, portions of the unit may subside more quickly relative to the rest of the unit.

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15
Q

Define Drainage Basin

A

An area over which water falling on the surface will drain into a river or a lake, refers only to surface waters.

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16
Q

Define Drawdown

A

The lowering of the water level (hydraulic head) in the well due to pumping

17
Q

Define Funicular Groundwater

A

Water that is maintained in the vadose through the adhesive property of water, i.e. the water is adhering to the individual grains of soil or clasts of sediment.

18
Q

Define Hydraulic Conductivity

A

The permeability of soil for water. A property of both fluid and porous media.

19
Q

Define Hydraulic Head

A

elevation + pressure head

is a specific measurement of liquid pressure above a geodetic datum (sea level)

It is usually measured as a liquid surface elevation, expressed in units of length, at the entrance (or bottom) of a piezometer.

In an aquifer, it can be calculated from the depth to water in a piezometric well given the information of the piezometer’s elevation and screen depth.

Hydraulic head can similarly be measured in a column of water using a standpipe piezometer by measuring the height of the water surface in the tube relative to a common datum.

The hydraulic head can be used to determine a hydraulic gradient between two or more points.

The distribution of hydraulic head through an aquifer determines where groundwater will flow. Where the hydraulic head is constant, there is no flow. However, if there is a difference in hydraulic head from the top to bottom, the water will flow downward, due to the difference in head, also called the hydraulic gradient

20
Q

Define Piezometer

A

Any device used to measure hydraulic head.

21
Q

Define Residence Time

A

The average time required to replace an entire volume with new water.

22
Q

Define Slug Test

A

A controlled field experiment in which water level in a control well is caused to change (rise or fall) instantaneously and the subsequent water-level response (displacement or change from static) is measured in the control well and one more surrounding observation wells through time.

23
Q

Define Stratigraphic log

A

The description of the nature and thickness of geologic formations penetrated by a borehole.

24
Q

Define Subsidence

A

The motion of a surface as it shifts downward relative to a datum such as sea-level. This may be a response to groundwater removal, e.g. San Joaquin Valley

25
What path will water take while traveling through aquifers or aquitards?
Water takes the path of least resistance. Horizontally through aquifers, vertically through aquitards.
26
What is rate of flow controlled by?
Storativity, Transmissivity, and Hydraulic head.
27
What does hydraulic head measure?
Measures the ease with which groundwater is transmitted by an aquifer or other hydrogeologic unit.
28
A drop in what results in a release of water from storage by an actual dewatering of pores as the water table declines?
head
29
Pressure in an unconfined aquifer is equal to atmospheric pressure, true or false?
True
30
Pressure drops created by pumping of wells can create what in the water table?
Cone of depression.
31
What is the related time for each flow designation in sequence for Local flow, Intermediate flow, and regional flow?
Days for local, months for intermediate, and years for regional.
32
Discharge areas are generally what percentage of the bottom of a hill?
30%
33
Groundwater flow is the source of nearly all baseflow except for water draining from what?
Lakes, wetlands, and delayed interflow.
34
What are the three boundaries to flow called?
No Flow, Constant Head, Water Table Boundary.
35
What is a no flow boundary and what causes it?
something that allows no groundwater to flow across the boundary. An aquiclude, or groundwater divide. In which case flow lines run parallel.
36
Contribution of baseflow is the basis for the classification of streams. What are the three classifications?
Perennial - Always baseflow. Intermediate - Seasonal baseflow (usually gaining). Ephemeral - Event streams (usually loosing)
37
In relation to groundwater, streams may be?
Gaining (effluent) Losing (influent) Flow through (gaining on one bank, loosing on the other)
38
The driver of groundwater flow is?
Hydraulic Head