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The coefficient of transmissibility is defined as the rate of flow of water through a horizontal strip of unit width and full saturation height under unit hydraulic gradient.
- a)True
- b)False
Correct answer is option 'B'. Can you explain this answer?
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The coefficient of transmissibility is defined as the rate of flow of ...
For a fully saturated soil mass of unit width extending to depth infinity, the discharge through it is known as the coefficient of transmissibility when the hydraulic gradient is unity.
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The coefficient of transmissibility is defined as the rate of flow of ...
Explanation:
Coefficient of Transmissibility:
- The coefficient of transmissibility is not defined as the rate of flow of water through a horizontal strip of unit width and full saturation height under unit hydraulic gradient.
- The correct definition of the coefficient of transmissibility is the rate of flow of water through a unit width of an aquifer under a unit hydraulic gradient with full saturation.
- It is a measure of the ability of an aquifer to transmit water.
Clarification:
- The coefficient of transmissibility is an important parameter in hydrogeology and is used to characterize the hydraulic conductivity of an aquifer.
- It is usually denoted by the symbol T and has units of length squared per unit time (e.g., m^2/day).
Importance:
- The coefficient of transmissibility is crucial in determining the flow of groundwater through an aquifer and is used in various hydrogeological calculations.
- It helps in understanding the movement of contaminants in groundwater and in designing effective groundwater management strategies.
Conclusion:
- The coefficient of transmissibility is not defined as stated in the question but plays a significant role in hydrogeology and groundwater studies.
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The coefficient of transmissibility is defined as the rate of flow of water through a horizontal strip of unit width and full saturation height under unit hydraulic gradient.a)Trueb)FalseCorrect answer is option 'B'. Can you explain this answer?
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