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A sedimentation process is to be used to separate pulverized coal from slate. A suspension of finely divided particles of galena (lead sulfide, SG = 7.44) in water is prepared. The overall specific gravity of the suspension is 1.48. (a) Four hundred kilograms of galena and a quantity of water are loaded into a tank and stirred to obtain a uniform suspension with the required specific gravity. Draw and label the flowchart (label both the masses and volumes of the galena and water), do the degree-of-freedom analysis, and calculate how much water ( \(\mathrm{m}^{3}\) ) must be fed to the tank. (b) A mixture of coal and slate is placed in the suspension. The coal rises to the top and is skimmed off, and the slate sinks. What can you conclude about the specific gravities of coal and slate? (c) The separation process works well for several hours, but then a region of clear liquid begins to form at the top of the cloudy suspension and the coal sinks to the bottom of this region, making skimming more difficult. What might be happening to cause this behavior and what corrective action might be taken? Now what can you say about the specific gravity of coal?

Short Answer

Expert verified
To create a suspension with a specific gravity of 1.48, approximately 466 cubic meters of water will be necessary. Based on the behavior in the suspension, the specific gravity of coal is less than 1.48 and the specific gravity of slate is more than 1.48. If a region of clear liquid forms at the top of the suspension causing coal to sink, this could be due to a decrease in the specific gravity of the suspension, which could be addressed by stirring to resuspend solids or adding more galena.

Step by step solution

01

Understanding the Principles Involved

The principle of specific gravity (SG) will be used extensively throughout this problem. The first step involves understanding that the overall specific gravity (\(SG_o\)) of a suspension is calculated from its components by the formula \(SG_o = \frac{SG_{Galena}*m_{Galena}+SG_{water}*v_{water}}{m_{Galena}+v_{water}}\). This formula implies that the overall specific gravity is the weighted average of the specific gravities of the components.
02

Calculate volume of water needed

Rearranging the formula to solve for the volume of water (\(v_{water}\)) gives \(v_{water} = \frac{SG_o*(m_{Galena}+v_{water}) - SG_{Galena}*m_{Galena}}{SG_{water}}\). Initial substitution of known values gives \(v_{water} = \frac{1.48*(400Kg+v_{water}) - 7.44*400Kg}{1}\). Now, the expression can be solved iteratively as it involves \(v_{water}\) on both sides of the equation. Assuming a starting guess value of \(v_{water}\) as 0 and working through iterations until a sufficiently accurate value is calculated.
03

Compare SG for coal and slate

As the coal rises, its specific gravity must be less than the specific gravity of the suspension. Similarly, as the slate sinks, its specific gravity must be higher than that of the suspension. Therefore \(SG_{coal}< 1.48 < SG_{slate}\).
04

Analyze the change in process

The formation of a layer of clear liquid and the sinking of coal suggest that the specific gravity of the suspension has decreased. Possible causes may include solids settling out or evaporation of the water. Corrective action may include stirring to resuspend solids or adding more galena to increase the specific gravity. The specific gravity of the coal is still less than the suspension so \(SG_{coal}< SG_{new suspension}\).

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Key Concepts

These are the key concepts you need to understand to accurately answer the question.

Degree-Of-Freedom Analysis
When designing a separation process like the sedimentation of coal from slate, engineers use a degree-of-freedom analysis to understand whether they have enough information to solve for the unknowns. This technique is essential in determining the feasibility of reaching a solution without additional data.

Degree-of-freedom (DOF) refers to the number of independent variables that can be changed without affecting the others. In this case, the specific gravities of coal and slate, the mass of galena, and the volume of water compose the known variables. However, the exact amount of water needed to achieve a specific gravity of 1.48 in the suspension is unknown.

The formula used to calculate the volume of water needed is derived from the principle of specific gravity and mass balance. The flowchart, in essence, should reflect these balances. We calculate the DOF by taking the number of equations available (mass balances for galena and water, and the specific gravity formula) and subtracting the number of unknowns (volume of water in this case). If the DOF equals zero, the system is solvable without further input. In our exercise, knowing the mass of galena and the desired overall specific gravity allows us to solve for the volume of water, confirming that our system is well-defined with zero degrees of freedom.
Suspension Properties
Understanding the suspension properties is crucial in the sedimentation process. A suspension in this context is a heterogeneous mixture containing solid particles that are substantially larger than molecules or ions and can be affected by the force of gravity.

The overall specific gravity of the suspension is a vital property as it determines the behavior of particles when mixed. This value, 1.48 in the case of our exercise, lies between that of galena and water. By using the defined specific gravity, we can infer the relative buoyancy of particles in the mixture. As coal floats and slate sinks, their specific gravities also act as a qualitative indicator of their relative densities compared to the suspension.

It is also essential to consider the settling rate, the viscosity of the fluid, and the particle size distribution within the suspension. These properties can affect the 'clarity' of the suspension over time and the efficiency of separation. For instance, if a clear layer forms on top of the mixture, it could signal that the solid particles have settled, indicating changes in the suspension properties over time.
Sedimentation Process
The sedimentation process is a method of separating particles based on their density by allowing them to settle out of a fluid. It leverages gravity to remove suspended solids from a mixture or to separate liquids with different densities.

Sedimentation is influenced by several factors: the size and density of the particles, the viscosity of the fluid, and the depth of the liquid. These factors combine to determine the settling rate of the particles. In the sedimentation process described in the exercise, galena is used to increase the specific gravity of the suspension to a point where coal can be separated from slate due to differences in their buoyancies.

As mentioned in the exercise solution, when the coal stops floating, it implies that there has been a change in the suspension's density, or possible settling of the heavier particles has occurred. Corrective actions might include stirring to keep the particles in suspension or adjusting the specific gravity to ensure coal remains buoyant. The challenge of maintaining a consistent suspension profile highlights the need for continuous monitoring and adjustment in any sedimentation process.

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Most popular questions from this chapter

A stream of humid air containing 1.50 mole \(\% \mathrm{H}_{2} \mathrm{O}(\mathrm{v})\) and the balance dry air is to be humidified to a water content of 10.0 mole\% \(\mathrm{H}_{2} \mathrm{O}\). For this purpose, liquid water is fed through a flowmeter and evaporated into the air stream. The flowmeter reading, \(R\), is \(95 .\) The only available calibration data for the flowmeter are two points scribbled on a sheet of paper, indicating that readings \(R=15\) and \(R=50\) correspond to flow rates \(\dot{V}=40.0 \mathrm{ft}^{3} / \mathrm{h}\) and \(\dot{V}=96.9 \mathrm{ft}^{3} / \mathrm{h},\) respectively. (a) Assuming that the process is working as intended, draw and label the flowchart, do the degree-offreedom analysis, and estimate the molar flow rate (lb-mole/h) of the humidified (outlet) air if (i) the volumetric flow rate is a linear function of \(R\) and (ii) the reading \(R\) is a linear function of \(\dot{V}^{0.5}\) (b) Suppose the outlet air is analyzed and found to contain only \(7 \%\) water instead of the desired \(10 \%\) List as many possible reasons as you can think of for the discrepancy, concentrating on assumptions made in the calculation of Part (a) that might be violated in the real process.

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