Soil Moisture The evapotranspiration index I is a measure of soil moisture. An article on 10- to 14-year-old heath vegetation described the rate of change of I with respect to W, the amount of water available, by the equation dl = 0.088(2.4 - 1). MP Source: Australian Journal of Botany. (a) According to the article, I has a value of 1 when W = 0. Solve the initial value problem. (b) What happens to I as W becomes larger and larger?

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Soil Moisture The evapotranspiration index I is a measure of
soil moisture. An article on 10- to 14-year-old heath vegetation
described the rate of change of I with respect to W, the amount
of water available, by the equation
dl
= 0.088(2.4 - 1).
MP
Source: Australian Journal of Botany.
(a) According to the article, I has a value of 1 when W = 0.
Solve the initial value problem.
(b) What happens to I as W becomes larger and larger?
Transcribed Image Text:Soil Moisture The evapotranspiration index I is a measure of soil moisture. An article on 10- to 14-year-old heath vegetation described the rate of change of I with respect to W, the amount of water available, by the equation dl = 0.088(2.4 - 1). MP Source: Australian Journal of Botany. (a) According to the article, I has a value of 1 when W = 0. Solve the initial value problem. (b) What happens to I as W becomes larger and larger?
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