Field capacity, Available water, Permanent wilting point, Ultimate wilting point, Saturation capacity
Available water, Saturation capacity, Permanent wilting point, Field capacity, Ultimate wilting point
Saturation capacity, Field capacity, Permanent wilting point, Ultimate wilting point, Available water
Saturation capacity, Field capacity, Available water, Permanent wilting point, Ultimate wilting point
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The Correct Option isD
Solution and Explanation
Concept:
After a heavy rainfall, soil moisture gradually decreases with time because of:
• Gravitational drainage
• Evaporation
• Plant uptake
Different soil moisture conditions occur sequentially as water content reduces.
The important soil moisture constants are:
• Saturation capacity
• Field capacity
• Available water
• Permanent wilting point
• Ultimate wilting point
These occur in a descending order of moisture content.
Step 1: Understanding Saturation Capacity.
Immediately after heavy rainfall:
• All soil pores become filled with water
• Both macro-pores and micro-pores contain water
This condition is known as:
\[
\boxed{
\text{Saturation Capacity}
}
\]
This is the maximum moisture condition of soil.
Step 2: Understanding Field Capacity.
After some time:
• Excess gravitational water drains away
• Soil retains only useful moisture
This stage is called:
\[
\boxed{
\text{Field Capacity}
}
\]
Field capacity represents optimum moisture for plant growth.
Step 3: Understanding Available Water.
Plants then begin extracting moisture from the soil.
The water available between:
\[
\text{Field Capacity and Permanent Wilting Point}
\]
is known as:
\[
\boxed{
\text{Available Water}
}
\]
This moisture can be utilized by plants.
Step 4: Understanding Permanent Wilting Point.
As soil dries further:
• Plants cannot recover from wilting
• Water becomes unavailable to roots
This condition is called:
\[
\boxed{
\text{Permanent Wilting Point}
}
\]
Step 5: Understanding Ultimate Wilting Point.
With additional drying:
• Soil becomes extremely dry
• Practically no usable water remains
This final stage is:
\[
\boxed{
\text{Ultimate Wilting Point}
}
\]
Step 6: Writing the correct sequence.
Thus the correct sequence after heavy rain is:
\[
\boxed{
\text{Saturation Capacity}
\rightarrow
\text{Field Capacity}
\rightarrow
\text{Available Water}
\rightarrow
\text{Permanent Wilting Point}
\rightarrow
\text{Ultimate Wilting Point}
}
\]
Step 7: Comparing with options carefully.
Option (A):
Incorrect arrangement because saturation capacity should come first.
\[
\boxed{
\text{Option (A) is incorrect}
}
\]
Option (B):
Incorrect sequence.
\[
\boxed{
\text{Option (B) is incorrect}
}
\]
Option (C):
Available water should come before permanent wilting point.
\[
\boxed{
\text{Option (C) is incorrect}
}
\]
Option (D):
Correct sequence.
\[
\boxed{
\text{Option (D) is correct}
}
\]
Final Conclusion:
The correct order of soil moisture constants after heavy rainfall is:
\[
\boxed{
\text{Saturation Capacity}
\rightarrow
\text{Field Capacity}
\rightarrow
\text{Available Water}
\rightarrow
\text{Permanent Wilting Point}
\rightarrow
\text{Ultimate Wilting Point}
}
\]
Hence the correct answer is:
\[
\boxed{
(D)
}
\]
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