Chapter 9: Problem 5
Consider one-dimensional flow through a confined porous aquifer of total thickness \(b\) and crosssectional area \(A\). Suppose the aquifer consists of \(N\) layers, each of thickness \(b_{i}(i=1, \ldots, N)\) and permeability \(k_{i}(i=1, \ldots, N) .\) Determine the total flow rate through the aquifer if all the layers are subjected to the same driving pressure gradient. What is the uniform permeability of an aquifer of thickness \(b\) that delivers the same flow rate as the layered aquifer when the two are subjected to the same pressure gradient?
Short Answer
Step by step solution
Understand the Problem
Set Up the Known Parameters
Equation for Flow Rate through a Layer
Calculate Total Flow Rate
Find Equivalent Uniform Permeability
Verify the Equation Dimensions
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Key Concepts
These are the key concepts you need to understand to accurately answer the question.
Permeability
Each layer in an aquifer has its unique permeability value, represented by the symbol \( k \). This parameter is crucial because it determines how much water can flow through the layer; higher permeability means the water moves more freely.
- Permeability is generally measured in units like darcies or millidarcies.
- It's directly proportional to the flow rate—higher permeability means a higher potential flow rate.
- In aquifers, knowing the permeability of each layer helps in predicting how water will travel through the subsurface.
Porous Media Flow
In the exercise, we explore the flow through a confined aquifer, emphasizing how water moves through each layer of sediment. Darcy’s Law becomes instrumental here as it provides a mathematical framework to describe and quantify this flow based on the permeability and pressure gradient.
- Porous media flow relies on the structure and connectedness of the pores, which influences how easily fluids can pass through.
- This kind of flow is characterized by slow movement, yet it's essential to the natural water cycle as it contributes to groundwater recharge.
Pressure Gradient
A uniform pressure gradient across the layers of a confined aquifer ensures that each layer contributes to the total flow rate. The gradient, often represented as \( abla P \), is crucial because:
- It's the difference in pressure that encourages the movement of water from high to low-pressure areas.
- The steeper the gradient, the faster the flow of fluid, assuming constant permeability.
Confined Aquifer
In our exercise, the aquifer consists of multiple layers, each contributing to overall distribution and flow. Key points about confined aquifers include:
- Water in confined aquifers is often under artesian pressure, meaning it can rise above the top of the aquifer layer when penetrated by a well.
- These aquifers are less susceptible to contamination from surface activities due to their protective spoil layers.
Hydraulic Conductivity
Given its role in Darcy's Law, hydraulic conductivity (often symbolized as \( K \)) is defined as a ratio involving both intrinsic permeability and the fluid's viscosity:
- It is expressed in units of velocity, often meters per second (m/s).
- A higher conductivity value indicates that water can flow more freely through the aquifer material.
- It takes into account both the permeability of the aquifer and the properties of the fluid, such as temperature and viscosity.