Gypsum is a relatively soft rock made of CaSO4. Rainwater percolates through gypsum, dissolves some of the rock, and eventually becomes saturated with Ca2+ ions and SO2- ions. A geochemist takes a sample of groundwater from a cave and finds that it contains 8.4 x 10-3 M SO2- and 5.8 x 10-3 M Ca²+. (The ratio is not 1:1 because other sulfate rock contributes some of the SO42- ions to the solution.) Use these data to determine the solubility product of CaSO4.

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Gypsum is a relatively soft rock made of CaSO4. Rainwater
percolates through gypsum, dissolves some of the rock, and
eventually becomes saturated with Ca2+ ions and SO²- ions. A
geochemist takes a sample of groundwater from a cave and finds
that it contains 8.4 x 10-3 M SO42- and 5.8 x 10-3 M Ca²+. (The
ratio is not 1:1 because other sulfate rock contributes some of the
SO42- ions to the solution.) Use these data to determine the
solubility product of CaSO4.
Transcribed Image Text:Gypsum is a relatively soft rock made of CaSO4. Rainwater percolates through gypsum, dissolves some of the rock, and eventually becomes saturated with Ca2+ ions and SO²- ions. A geochemist takes a sample of groundwater from a cave and finds that it contains 8.4 x 10-3 M SO42- and 5.8 x 10-3 M Ca²+. (The ratio is not 1:1 because other sulfate rock contributes some of the SO42- ions to the solution.) Use these data to determine the solubility product of CaSO4.
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