A geochemist measures the concentration of salt dissolved in Lake Parsons and finds a concentration of 41.3 g·L *. The geochemist also -1 measures the concentration of salt in several nearby non-isolated lakes, and finds an average concentration of 4.3 g·L *. Assuming the salt concentration in Lake Parsons before it became isolated was equal to the average salt concentration in nearby non- isolated lakes, calculate the percentage of Lake Parsons which has evaporated since it became isolated.
A geochemist measures the concentration of salt dissolved in Lake Parsons and finds a concentration of 41.3 g·L *. The geochemist also -1 measures the concentration of salt in several nearby non-isolated lakes, and finds an average concentration of 4.3 g·L *. Assuming the salt concentration in Lake Parsons before it became isolated was equal to the average salt concentration in nearby non- isolated lakes, calculate the percentage of Lake Parsons which has evaporated since it became isolated.
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
Problem 1.1P
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Transcribed Image Text:A geochemist measures the concentration of salt dissolved in Lake Parsons and finds a concentration of 41.3 g L . The geochemist also
measures the concentration of salt in several nearby non-isolated lakes, and finds an average concentration of 4.3 g·L .
Assuming the salt concentration in Lake Parsons before it became isolated was equal to the average salt concentration in nearby non-
isolated lakes, calculate the percentage of Lake Parsons which has evaporated since it became isolated.
Be sure your answer has the correct number of significant digits.
x10
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