The image shows a one dimensional problem where water is entering and leaving a soil column that is Z m deep, has a volumetric water content of 0 and porosity o. Water enters as precipitation P [m/day], and leaves as evaporation E [m/day] and deep drainage D [m/day]. Which of the following equations for 0, the relative water content, is a sensible water balance equation (assuming constant density) for this problem? TE S,0 D P. N
The image shows a one dimensional problem where water is entering and leaving a soil column that is Z m deep, has a volumetric water content of 0 and porosity o. Water enters as precipitation P [m/day], and leaves as evaporation E [m/day] and deep drainage D [m/day]. Which of the following equations for 0, the relative water content, is a sensible water balance equation (assuming constant density) for this problem? TE S,0 D P. N
Chapter2: Loads On Structures
Section: Chapter Questions
Problem 1P
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![The image shows a one dimensional problem where water is entering and leaving a soil column that is Z m deep, has a
volumetric water content of 0 and porosity p. Water enters as precipitation P [m/day], and leaves as evaporation E
[m/day] and deep drainage D [m/day].
Which of the following equations for 0, the relative water content, is a sensible water balance equation (assuming
constant density) for this problem?
TE
s,0
P.](/v2/_next/image?url=https%3A%2F%2Fcontent.bartleby.com%2Fqna-images%2Fquestion%2F7b8aaa98-c6af-42c4-95e0-38c9d5feb90d%2F6754b224-39ae-4b25-8ed7-44a5d07fa079%2Fi32gwme_processed.jpeg&w=3840&q=75)
Transcribed Image Text:The image shows a one dimensional problem where water is entering and leaving a soil column that is Z m deep, has a
volumetric water content of 0 and porosity p. Water enters as precipitation P [m/day], and leaves as evaporation E
[m/day] and deep drainage D [m/day].
Which of the following equations for 0, the relative water content, is a sensible water balance equation (assuming
constant density) for this problem?
TE
s,0
P.
Transcribed Image Text:a. de
- =P – E - D
dt
b.
de
pZ –=P- E– D
dt
O c. de
: (Р-Е-D)ф
dt
O d.
de
Z==P- E-D
— Р—
dt
ds
фZ—-Р-Е-D
dt
е.
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