answersLogoWhite

0


Best Answer

The water table is affected by the amount of water going into it, and the amount of water taken out of it. The level in the water table is also affected to some degree by geology and what happens to the water that is "just sitting" in the water table. Some may be able to "escape" in some way through premeable layers or cracks in the geologic structure. Certainly earthquates and vulcanism can modify the manner in which the water is held in the water table. Cracks can be originated or propagated (from existing fractures) under different conditions.

User Avatar

Wiki User

16y ago
This answer is:
User Avatar
More answers
User Avatar

AnswerBot

4mo ago

The rate of movement of groundwater is controlled by factors such as the permeability of the material it is flowing through (such as soil or rock), the slope of the water table, the hydraulic gradient, and the presence of obstacles or barriers to flow like impermeable layers. Additionally, human activities like groundwater extraction can also influence the rate of movement.

This answer is:
User Avatar

User Avatar

Wiki User

11y ago

Ground water moves at a varying speeds depending on the nature of the material through which it is moving. Just to cite a couple of examples, consider sand and clay. Gravity acts to draw water down fairly quickly through sand, but a packed layer of clay will prevent water from moving through it very quickly, and can in many cases block the penetration of water completely. A review of the underground geology in a given area is required to plot or make estimates of (model) the speed at which ground water will move through it.

This answer is:
User Avatar

User Avatar

Wiki User

10y ago

Some of the factors that control the speed and movement of ground water include the soil topography and the type of the soil. Some rocks or soils are more permeable than others.

This answer is:
User Avatar

User Avatar

Wiki User

12y ago

Climate (precipitation, temperature)

Vegetation (plants)

Parent material (geological/organic)

Organisms (soil microbes/fauna)

Relief (configuration of surface)

This answer is:
User Avatar

User Avatar

Wiki User

16y ago

anything can affect soil erosion, chemicals, also types of fertilizers and the structure is it clay like or very rich soil, depends in area.

This answer is:
User Avatar

User Avatar

Wiki User

11y ago

The velocity at which water moves depends on the hydraulic head of the water and on the permeability of the material that the water is moving through.

This answer is:
User Avatar

User Avatar

Wiki User

12y ago

water

Cohesion of water molecules, osmotic potential, gravitation force and transpiration pull (in plants) etc.

This answer is:
User Avatar

User Avatar

Wiki User

14y ago

precipitation (rain, snow, etc.), lag time (diff between rainfall and when the water level goes back to normal), seasons, water pumping

This answer is:
User Avatar

User Avatar

Wiki User

13y ago

The two factors that determine the flow velocity of ground water are perembilty and the force of gravity pulling the water downward.

This answer is:
User Avatar

Add your answer:

Earn +20 pts
Q: What controls the rate of movement of groundwater?
Write your answer...
Submit
Still have questions?
magnify glass
imp
Related questions

What control the rate of movement of groundwater?

What controls the movement of groundwater


What controls the rate of movement of ground water?

The porosity and permeability of the soil or rock control the rate of movement of groundwater. Other factors such as hydraulic gradient, hydraulic conductivity, and gradient also influence the speed at which groundwater moves through the subsurface.


An area's rate of groundwater recharge exceeds it's rate groundwater discharge what can you conclude about the area's groundwater Supply?

If an area's rate of groundwater recharge exceeds its rate of groundwater discharge, it indicates that the groundwater supply in the area is being replenished at a faster rate than it is being used or lost. This is a positive sign for the sustainability of the groundwater supply in the area.


An areas rate of groundwater recharge exceeds its rate of groundwater discharge?

When the rate of groundwater recharge exceeds the rate of discharge in an area, it leads to the replenishment of groundwater reserves. This can result in increased water availability for wells, springs, and ecosystems dependent on groundwater. It may also help in mitigating issues related to groundwater depletion and subsidence.


What is the movement of underground water?

Groundwater flow.


What is the movement of water underground called?

Groundwater flow.


What body system senses pain and controls movement?

The nervous system senses pain and controls movement.


What is the difference between renewable groundwater and nonrenewable groundwater?

Renewable groundwater is replenished through natural processes at a rate that is sustainable for human use, while nonrenewable groundwater is not replenished, or is replenished at a very slow rate compared to human consumption. Nonrenewable groundwater is often fossil water that has been stored underground for thousands to millions of years and is not easily replenished.


WHAT force below accounts for the movement of groundwater?

The force that accounts for the movement of groundwater is primarily gravity, as water flows from areas of higher elevation to lower elevation through porous materials like soil and rock. Additionally, pressure gradients and capillary action also play a role in the movement of groundwater.


What controls lung movement?

The diaphragm controls lung movement. The rib cage also contributes to this.


What is the difference between throughflow and groundwater flow?

Through flow is the horizontal movement of water through the soil zone. Groundwater flow is the movement of water through the bedrock, which is typically an aquifer


What is groundwater overuse?

Groundwater overuse occurs when the rate of water removal from an aquifer exceeds the rate of water recharge. This can lead to depletion of the groundwater supply, causing lower water levels, reduced stream flow, and land subsidence. Groundwater overuse can also result in saltwater intrusion in coastal areas.