6.50. A correlation for methane solubility in seawater"3 is given by the equation In ß = -67.1962 + 99.1624 T T +27.9015 In| 100 T +s-0.072909 + 0.041674( 100 0.0064603 100 where ß is volume of gas in mL at STP per unit volume (mL) of water when the partial pressure of methane is 760 mm Hg, T is temperature in Kelvin, and S is salinity in parts per thousand (ppt) by weight. At conditions of interest, the average salinity is 35 ppt, the temperature is 42°F, and the average density of seawater is 1.027 g/cm. 12R. H. Perry and D. W. Green, Eds., Perry's Chemical Engineers' Handbook, 8th Edition, McGraw-Hill, New York, 2008, Pp. 2-91, 2-92, and 2-104. 13S. Yamamoto, J. B. Alcauskas, and T. E. Crozier, J. Chem. Eng. Data, 21, 78(1976). hase Systems (a) Estimate the mole fraction of methane in seawater for equilibrium at the given conditions. Use a mean molecular weight of 18.4 g/mol for seawater. What is the Henry's law constant at this temperature and salinity? (b) What does the above equation say about the effect of S on methane solubility? (e) Use the Henry's law constant from Part (a) to estimate methane solubility at the given temperature and salinity, but 5000 ft below the ocean surface. (Hint: Estimate the pressure at that depth.) Exploratory Exercise-Research and Discover (d) Atthe low temperatures and high pressures associated with the depths described in Part (c), methane can combine with water to form methane hydrates, which may affect both energy availability and the environment. Explain (i) how such behavior would influence the results in Part (c) and (ii) how dissolution of methane in seawater might affect energy availability and the environment.

Introduction to Chemical Engineering Thermodynamics
8th Edition
ISBN:9781259696527
Author:J.M. Smith Termodinamica en ingenieria quimica, Hendrick C Van Ness, Michael Abbott, Mark Swihart
Publisher:J.M. Smith Termodinamica en ingenieria quimica, Hendrick C Van Ness, Michael Abbott, Mark Swihart
Chapter1: Introduction
Section: Chapter Questions
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6.50. A correlation for methane solubility in seawater"3 is given by the equation
In ß = -67.1962 + 99.1624
T
T
+27.9015 In|
100
T
+s-0.072909 + 0.041674(
100
0.0064603
100
where ß is volume of gas in mL at STP per unit volume (mL) of water when the partial pressure of
methane is 760 mm Hg, T is temperature in Kelvin, and S is salinity in parts per thousand (ppt) by
weight. At conditions of interest, the average salinity is 35 ppt, the temperature is 42°F, and the
average density of seawater is 1.027 g/cm.
12R. H. Perry and D. W. Green, Eds., Perry's Chemical Engineers' Handbook, 8th Edition, McGraw-Hill, New York, 2008,
Pp. 2-91, 2-92, and 2-104.
13S. Yamamoto, J. B. Alcauskas, and T. E. Crozier, J. Chem. Eng. Data, 21, 78(1976).
hase Systems
(a) Estimate the mole fraction of methane in seawater for equilibrium at the given conditions. Use a
mean molecular weight of 18.4 g/mol for seawater. What is the Henry's law constant at this
temperature and salinity?
(b) What does the above equation say about the effect of S on methane solubility?
(e) Use the Henry's law constant from Part (a) to estimate methane solubility at the given temperature
and salinity, but 5000 ft below the ocean surface. (Hint: Estimate the pressure at that depth.)
Exploratory Exercise-Research and Discover
(d) Atthe low temperatures and high pressures associated with the depths described in Part (c), methane
can combine with water to form methane hydrates, which may affect both energy availability and the
environment. Explain (i) how such behavior would influence the results in Part (c) and (ii) how
dissolution of methane in seawater might affect energy availability and the environment.
Transcribed Image Text:6.50. A correlation for methane solubility in seawater"3 is given by the equation In ß = -67.1962 + 99.1624 T T +27.9015 In| 100 T +s-0.072909 + 0.041674( 100 0.0064603 100 where ß is volume of gas in mL at STP per unit volume (mL) of water when the partial pressure of methane is 760 mm Hg, T is temperature in Kelvin, and S is salinity in parts per thousand (ppt) by weight. At conditions of interest, the average salinity is 35 ppt, the temperature is 42°F, and the average density of seawater is 1.027 g/cm. 12R. H. Perry and D. W. Green, Eds., Perry's Chemical Engineers' Handbook, 8th Edition, McGraw-Hill, New York, 2008, Pp. 2-91, 2-92, and 2-104. 13S. Yamamoto, J. B. Alcauskas, and T. E. Crozier, J. Chem. Eng. Data, 21, 78(1976). hase Systems (a) Estimate the mole fraction of methane in seawater for equilibrium at the given conditions. Use a mean molecular weight of 18.4 g/mol for seawater. What is the Henry's law constant at this temperature and salinity? (b) What does the above equation say about the effect of S on methane solubility? (e) Use the Henry's law constant from Part (a) to estimate methane solubility at the given temperature and salinity, but 5000 ft below the ocean surface. (Hint: Estimate the pressure at that depth.) Exploratory Exercise-Research and Discover (d) Atthe low temperatures and high pressures associated with the depths described in Part (c), methane can combine with water to form methane hydrates, which may affect both energy availability and the environment. Explain (i) how such behavior would influence the results in Part (c) and (ii) how dissolution of methane in seawater might affect energy availability and the environment.
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