The hydraulic gradient is  a rock that is porous and permeable enough to transmit water easily.  b the difference in hydraulic head between two points, divided by the distance between them.  c rock that is low in permeability so that water flows very slowly through it.  d a relationship of groundwater flow rate between two point to the difference in hydraulic head between them.

Structural Analysis
6th Edition
ISBN:9781337630931
Author:KASSIMALI, Aslam.
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Chapter2: Loads On Structures
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The hydraulic gradient is 

a

rock that is porous and permeable enough to transmit water easily. 

b

the difference in hydraulic head between two points, divided by the distance between them. 

c

rock that is low in permeability so that water flows very slowly through it. 

d

a relationship of groundwater flow rate between two point to the difference in hydraulic head between them. 

 
 

2. An artesian well is one in which

a

pressurized groundwater rises from a deep, unconfined aquifer.

b

water rises above the top of the confined aquifer without any pumping.

c

the well is horizontal and the water table is perched.

d

Paint colors are mixed.

e

the water is warm, fairly saline, and recharged by an affluent stream.

 
 
 

3. A cone of depression is 

 
a

a solid or hollow object which tapers from a circular or roughly circular base to a point.

b

the relationship of groundwater flow rate between two points to the difference in hydraulic head between them. 

c

an aquifer overlain by an aquitard or aquiclude. 

d

a large, cone-shaped lowering of the water table around a well when it is pumped. 

 
 
 

4. Karst is 

a

a terrain characterized by underground solution cavities that is usually made of limestone. 

b

a waxy solid hydrocarbon in oil shale. 

c

proportion of void space in rock, sediment or soil. 

d

a measure of how readily fluid can flow through a rock, sediment, or soil. 

 
 
 

5. The water table is the top of the zone of saturation. 

a True
b False
 
 
 
 

6. Pumping ancient groundwater faster than it can be replenished

a

is called groundwater mining.

b

is not a problem because of the enormous reserves of ancient groundwater.

c

is impossible.

d

forms aquicludes.

e

increases porosity in the intermediate zone.

 
 
 

7. Saltwater intrusion is 

a

the movement of groundwater from the subsurface to the surface.

b

a circular depression in the ground commonly caused by collapse of a cave.

c

a process by which salt water replaces fresh groundwater when the fresh water is being used more rapidly. It is most common by the shoreline. 

d

the processes of infiltration and migration by which groundwater is replenished. 

 

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