The difference between porosity and permeability and the examples of substances with high porosity and low permeability.

Question

Want to see more full solutions like this?

Answer 1

Question

Chapter 16, Problem 1RQ

To determine

The difference between porosity and permeability and the examples of substances with high porosity and low permeability.

Expert Solution & Answer

Answer to Problem 1RQ

Porosity depends only in the presence of pores whereas permeability depends upon the interconnections between the pores. Both are expressed in terms of percentages. Some examples of the substances with high porosity and low permeability are mud-stones, shale etc. The substances with high porosity and low permeability are known as aquitards.

Explanation of Solution

Any open space present within the rock sediment or a given volume of rock is known as porosity. The porosity is expressed as a percentage. When the pore spaces are present within a rock during its formation, it is known as primary porosity. The pores spaces here are developed because grains do not grow to fill all the spaces during crystallization or open spaces are not completely filled with cement. When the new pore spaced is produced after the formation of a rock due to fracturing or chemical effect of some fluids passing through the cementing material, it is known as secondary porosity.

When a pore filled with water is surrounded by the solid rock mass, the water cannot flow out. The movement of water from pore to pore is possible only with the interconnections or conduits between them. For the ground water to flow, the conduits must present between the pores. The permeability of a material depends on many factors such as number of available conduits, size of the conduits and straightness of the conduits.

Want to see more full solutions like this?

Subscribe now to access step-by-step solutions to millions of textbook problems written by subject matter experts!

Students have asked these similar questions

I need help with tracing part A could I get some help

Activity 12.3: Wave Refraction Pgs 202-203Figure 12.2 is a map view of a headland along a coastline. The water depths are shown by blue contour lines. As you complete the following questions, assume that waves with a wavelength of 60 feet are approaching the shoreline from the bottom left of the figure. 1. At approximately what water depth-10, 20, 30, or 40 feet-will the approaching waves begin to touch bottom and slow down? (Hint: Recall that this occurs when the water depth is one-half the wavelength.) Approximately the 30-foot depth line. 2. Using the wave shown in Figure 12.2 as a starting point, sketch a series of lines to illustrate the wave refraction that will occur as the wave approaches the shore by following these steps:Step 1: Mark the position on the 30-foot contour line where the wave front will first touch bottom.Step 2: Knowing that the section of the wave that touches bottom will slow down first, sketch the shape of the wave front when it reaches the 20-foot contour…

N Depth of water contour Advancing wave crest Beach HEADLAND -10'- 20'- -30- Land -40- -50'- 0 Beach Scale 200 feet

Answer 2

Question

Chapter 16, Problem 1RQ

To determine

The difference between porosity and permeability and the examples of substances with high porosity and low permeability.

Expert Solution & Answer

Answer to Problem 1RQ

Porosity depends only in the presence of pores whereas permeability depends upon the interconnections between the pores. Both are expressed in terms of percentages. Some examples of the substances with high porosity and low permeability are mud-stones, shale etc. The substances with high porosity and low permeability are known as aquitards.

Explanation of Solution

Any open space present within the rock sediment or a given volume of rock is known as porosity. The porosity is expressed as a percentage. When the pore spaces are present within a rock during its formation, it is known as primary porosity. The pores spaces here are developed because grains do not grow to fill all the spaces during crystallization or open spaces are not completely filled with cement. When the new pore spaced is produced after the formation of a rock due to fracturing or chemical effect of some fluids passing through the cementing material, it is known as secondary porosity.

When a pore filled with water is surrounded by the solid rock mass, the water cannot flow out. The movement of water from pore to pore is possible only with the interconnections or conduits between them. For the ground water to flow, the conduits must present between the pores. The permeability of a material depends on many factors such as number of available conduits, size of the conduits and straightness of the conduits.

Want to see more full solutions like this?

Subscribe now to access step-by-step solutions to millions of textbook problems written by subject matter experts!

Answer 3

Question

Chapter 16, Problem 1RQ

To determine

The difference between porosity and permeability and the examples of substances with high porosity and low permeability.

Expert Solution & Answer

Answer to Problem 1RQ

Porosity depends only in the presence of pores whereas permeability depends upon the interconnections between the pores. Both are expressed in terms of percentages. Some examples of the substances with high porosity and low permeability are mud-stones, shale etc. The substances with high porosity and low permeability are known as aquitards.

Explanation of Solution

Any open space present within the rock sediment or a given volume of rock is known as porosity. The porosity is expressed as a percentage. When the pore spaces are present within a rock during its formation, it is known as primary porosity. The pores spaces here are developed because grains do not grow to fill all the spaces during crystallization or open spaces are not completely filled with cement. When the new pore spaced is produced after the formation of a rock due to fracturing or chemical effect of some fluids passing through the cementing material, it is known as secondary porosity.

When a pore filled with water is surrounded by the solid rock mass, the water cannot flow out. The movement of water from pore to pore is possible only with the interconnections or conduits between them. For the ground water to flow, the conduits must present between the pores. The permeability of a material depends on many factors such as number of available conduits, size of the conduits and straightness of the conduits.

Want to see more full solutions like this?

Subscribe now to access step-by-step solutions to millions of textbook problems written by subject matter experts!

Answer 4

Question

Chapter 16, Problem 1RQ

To determine

The difference between porosity and permeability and the examples of substances with high porosity and low permeability.

Expert Solution & Answer

Answer to Problem 1RQ

Porosity depends only in the presence of pores whereas permeability depends upon the interconnections between the pores. Both are expressed in terms of percentages. Some examples of the substances with high porosity and low permeability are mud-stones, shale etc. The substances with high porosity and low permeability are known as aquitards.

Explanation of Solution

Any open space present within the rock sediment or a given volume of rock is known as porosity. The porosity is expressed as a percentage. When the pore spaces are present within a rock during its formation, it is known as primary porosity. The pores spaces here are developed because grains do not grow to fill all the spaces during crystallization or open spaces are not completely filled with cement. When the new pore spaced is produced after the formation of a rock due to fracturing or chemical effect of some fluids passing through the cementing material, it is known as secondary porosity.

When a pore filled with water is surrounded by the solid rock mass, the water cannot flow out. The movement of water from pore to pore is possible only with the interconnections or conduits between them. For the ground water to flow, the conduits must present between the pores. The permeability of a material depends on many factors such as number of available conduits, size of the conduits and straightness of the conduits.

Want to see more full solutions like this?

Subscribe now to access step-by-step solutions to millions of textbook problems written by subject matter experts!

Answer 5

Chapter 16, Problem 1RQ

To determine

The difference between porosity and permeability and the examples of substances with high porosity and low permeability.

Expert Solution & Answer

Answer to Problem 1RQ

Porosity depends only in the presence of pores whereas permeability depends upon the interconnections between the pores. Both are expressed in terms of percentages. Some examples of the substances with high porosity and low permeability are mud-stones, shale etc. The substances with high porosity and low permeability are known as aquitards.

Explanation of Solution

Any open space present within the rock sediment or a given volume of rock is known as porosity. The porosity is expressed as a percentage. When the pore spaces are present within a rock during its formation, it is known as primary porosity. The pores spaces here are developed because grains do not grow to fill all the spaces during crystallization or open spaces are not completely filled with cement. When the new pore spaced is produced after the formation of a rock due to fracturing or chemical effect of some fluids passing through the cementing material, it is known as secondary porosity.

When a pore filled with water is surrounded by the solid rock mass, the water cannot flow out. The movement of water from pore to pore is possible only with the interconnections or conduits between them. For the ground water to flow, the conduits must present between the pores. The permeability of a material depends on many factors such as number of available conduits, size of the conduits and straightness of the conduits.

Answer 6

Chapter 16, Problem 1RQ

To determine

The difference between porosity and permeability and the examples of substances with high porosity and low permeability.

Expert Solution & Answer

Answer to Problem 1RQ

Porosity depends only in the presence of pores whereas permeability depends upon the interconnections between the pores. Both are expressed in terms of percentages. Some examples of the substances with high porosity and low permeability are mud-stones, shale etc. The substances with high porosity and low permeability are known as aquitards.

Explanation of Solution

Any open space present within the rock sediment or a given volume of rock is known as porosity. The porosity is expressed as a percentage. When the pore spaces are present within a rock during its formation, it is known as primary porosity. The pores spaces here are developed because grains do not grow to fill all the spaces during crystallization or open spaces are not completely filled with cement. When the new pore spaced is produced after the formation of a rock due to fracturing or chemical effect of some fluids passing through the cementing material, it is known as secondary porosity.

When a pore filled with water is surrounded by the solid rock mass, the water cannot flow out. The movement of water from pore to pore is possible only with the interconnections or conduits between them. For the ground water to flow, the conduits must present between the pores. The permeability of a material depends on many factors such as number of available conduits, size of the conduits and straightness of the conduits.

Answer 7

Chapter 16, Problem 1RQ

To determine

The difference between porosity and permeability and the examples of substances with high porosity and low permeability.

Answer 8

Expert Solution & Answer

Answer to Problem 1RQ

Porosity depends only in the presence of pores whereas permeability depends upon the interconnections between the pores. Both are expressed in terms of percentages. Some examples of the substances with high porosity and low permeability are mud-stones, shale etc. The substances with high porosity and low permeability are known as aquitards.

Answer 9

Expert Solution & Answer

Answer 10

Expert Solution & Answer

Answer 11

Explanation of Solution

Any open space present within the rock sediment or a given volume of rock is known as porosity. The porosity is expressed as a percentage. When the pore spaces are present within a rock during its formation, it is known as primary porosity. The pores spaces here are developed because grains do not grow to fill all the spaces during crystallization or open spaces are not completely filled with cement. When the new pore spaced is produced after the formation of a rock due to fracturing or chemical effect of some fluids passing through the cementing material, it is known as secondary porosity.

When a pore filled with water is surrounded by the solid rock mass, the water cannot flow out. The movement of water from pore to pore is possible only with the interconnections or conduits between them. For the ground water to flow, the conduits must present between the pores. The permeability of a material depends on many factors such as number of available conduits, size of the conduits and straightness of the conduits.

Answer 12

Ch. 16.2 - Prob. 1QQ Ch. 16.3 - Prob. 1QQ Ch. 16.4 - Prob. 1DYEW Ch. 16.4 - Prob. 1QQ Ch. 16.5 - Prob. 1QQ Ch. 16.6 - Prob. 1QQ Ch. 16.7 - Prob. 1DYEW Ch. 16.7 - Prob. 1QQ Ch. 16 - Prob. 1RQ Ch. 16 - Prob. 2RQ

The difference between porosity and permeability and the examples of substances with high porosity and low permeability.

The difference between porosity and permeability and the examples of substances with high porosity and low permeability.

Answer to Problem 1RQ

Explanation of Solution

Want to see more full solutions like this?

Chapter 16 Solutions