7. a). Barnett Reservoir, the north-west section was eroded much, adding limestone (CaCO3) to stabilize the bank, calculate pH of the water equilibrated with the atmosphere and bottom rock limestone. b). Barnett Reservoir, the east section is surrounded by regular mud soil, calculate pH of water equilibrated with the atmosphere. KCO2, henry constant: 3.38 x 10 2 M/atm, Ka1 for CO2 in water (CO2 +H20 HCO3 + H*), 4.45x 10-/; K for CaCO3 dissolution reaction CaCO3 (s) + CO2 (aq)+ H20 + Ca* + 2HCO3", 4.24x10-5. (Please show all work and include all steps!)

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
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7. a). Barnett Reservoir, the north-west section
was eroded much, adding limestone (CaCO3)
to stabilize the bank, calculate pH of the water
equilibrated with the atmosphere and bottom
rock limestone. b). Barnett Reservoir, the east
section is surrounded by regular mud soil,
calculate pH of water equilibrated with the
atmosphere. KCo2, henry constant: 3.38 x 10-
M/atm, Kal for CO2 in water (CO2 +H2O
2
HCO3 + H*), 4.45x 10; K for CaCO3
dissolution reaction CaCO3 (s) + CO2 (aq)+
H20 + Ca* + 2HCO3", 4.24x10-5. (Please
show all work and include all steps!)
Transcribed Image Text:7. a). Barnett Reservoir, the north-west section was eroded much, adding limestone (CaCO3) to stabilize the bank, calculate pH of the water equilibrated with the atmosphere and bottom rock limestone. b). Barnett Reservoir, the east section is surrounded by regular mud soil, calculate pH of water equilibrated with the atmosphere. KCo2, henry constant: 3.38 x 10- M/atm, Kal for CO2 in water (CO2 +H2O 2 HCO3 + H*), 4.45x 10; K for CaCO3 dissolution reaction CaCO3 (s) + CO2 (aq)+ H20 + Ca* + 2HCO3", 4.24x10-5. (Please show all work and include all steps!)
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