Chapter 9: Problem 13
Why does water rise in an artesian well? A) a pump C) heat B) erosion D) pressure
Short Answer
Expert verified
Water rises in an artesian well due to natural pressure (option D).
Step by step solution
01
Understanding the Context
Before solving, let's understand what an artesian well is. An artesian well taps into an aquifer that is confined under pressure. The water within the aquifer is under pressure greater than atmospheric pressure.
02
Identifying the Correct Principle
Artesian wells work due to the natural pressure in the aquifer. This pressure is caused by the weight of water at a higher elevation or other natural confinements, which pushes the water up the well without needing a pump or additional energy.
03
Eliminating Incorrect Options
Examine each option:
- A pump requires external energy, which isn't needed here.
- Heat is not relevant to the mechanism of artesian wells.
- Erosion affects landforms, not the pressure in an aquifer.
- Pressure, due to water elevation and confinement, is the correct principle causing water to rise.
04
Conclusion
Therefore, the rising of water in an artesian well is driven by natural pressure in the aquifer, answering option D.
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Key Concepts
These are the key concepts you need to understand to accurately answer the question.
Aquifer Pressure
The term 'aquifer pressure' refers to the force exerted within a saturated layer of earth or rock, where groundwater is stored. In particular, for artesian wells, this pressure is higher than atmospheric pressure, pushing water up naturally without the need for pumps.
This pressure arises due to the weight of the overlying layers of water in the aquifer, which can be thought of as a giant, underground natural water reservoir. Because the aquifer is confined, the water has nowhere else to go but up when tapped, which is why artesian wells can operate without external assistance. Additionally, the geographical features around the aquifer, such as rock formations and clay layers, help in maintaining the pressure by providing confinement.
This confined pressure is pivotal in understanding how artesian wells function and why they deliver water to the surface so effectively.
This pressure arises due to the weight of the overlying layers of water in the aquifer, which can be thought of as a giant, underground natural water reservoir. Because the aquifer is confined, the water has nowhere else to go but up when tapped, which is why artesian wells can operate without external assistance. Additionally, the geographical features around the aquifer, such as rock formations and clay layers, help in maintaining the pressure by providing confinement.
This confined pressure is pivotal in understanding how artesian wells function and why they deliver water to the surface so effectively.
Natural Pressure
Natural pressure in an aquifer is crucial for moving groundwater without mechanical energy. This pressure is created by the difference in elevation between the water table and the surface of the aquifer. In a confined aquifer, where the water is trapped between impermeable layers, this pressure can be significantly high.
When an artesian well is drilled, it taps into this pre-existing natural pressure. The water is then inclined to rise to the surface or even above ground level, if the pressure is strong enough. This self-sufficiency of artesian wells demonstrates how natural systems can be harnessed to provide water without energy consumption.
Understanding this natural pressure helps comprehend how artesian wells utilize earth’s natural forces to deliver sustainable groundwater solutions.
When an artesian well is drilled, it taps into this pre-existing natural pressure. The water is then inclined to rise to the surface or even above ground level, if the pressure is strong enough. This self-sufficiency of artesian wells demonstrates how natural systems can be harnessed to provide water without energy consumption.
Understanding this natural pressure helps comprehend how artesian wells utilize earth’s natural forces to deliver sustainable groundwater solutions.
Groundwater Flow
Groundwater flow refers to the movement of water through subsurface environments in aquifers. This flow is primarily determined by the pressure gradient, permeability of the materials through which it moves, and the gravity pulling it.
In artesian wells, groundwater flow is significantly directed by human intervention—drilling a well—into a confined aquifer. This allows for efficient extraction of water, thanks to the pressure naturally present in the aquifer system.
The study of groundwater flow is important as it helps predict the sustainability of water extraction from artesian wells and ensures minimal impact on the surrounding environment.
In artesian wells, groundwater flow is significantly directed by human intervention—drilling a well—into a confined aquifer. This allows for efficient extraction of water, thanks to the pressure naturally present in the aquifer system.
The study of groundwater flow is important as it helps predict the sustainability of water extraction from artesian wells and ensures minimal impact on the surrounding environment.
Confined Aquifer
A confined aquifer is a groundwater storage area trapped between layers of low permeability rock or sediment, like clay, that restricts the flow of water into or out of the aquifer. This confinement ensures that any water entering the aquifer is pressurized.
The pressure within a confined aquifer is what allows artesian wells to function. When a well taps into a confined aquifer, it utilizes the built-up pressure to move water upward without mechanical aids. The confinement not only maintains pressure but also protects the quality of the water by keeping it isolated from external contaminants.
The concept of a confined aquifer is central to understanding how artesian wells can sustainably provide water by taking advantage of natural geological formations.
The pressure within a confined aquifer is what allows artesian wells to function. When a well taps into a confined aquifer, it utilizes the built-up pressure to move water upward without mechanical aids. The confinement not only maintains pressure but also protects the quality of the water by keeping it isolated from external contaminants.
The concept of a confined aquifer is central to understanding how artesian wells can sustainably provide water by taking advantage of natural geological formations.