Step 1: Understanding the Concept:
The storage capacity of a soil (also known as the available water depth) is the maximum depth of water that a soil can store in its pore spaces for crop uptake.
This water is held between two physical limits:
- Field Capacity (FC): The upper limit of water storage after excess gravitational water has drained.
- Permanent Wilting Point (PWP): The lower limit of water storage, below which plants can no longer extract water.
Key Formula or Approach:
The depth of available water ($d$) stored in the root zone is calculated using the formula:
\[ d = \text{As} \times d_{\text{root}} \times (FC - PWP) \]
where:
- $\text{As}$ is the apparent specific gravity (bulk density of soil divided by density of water, which is a dimensionless ratio).
- $d_{\text{root}}$ is the depth of the crop root zone (in $\text{cm}$).
- $FC$ is the field capacity (expressed as a decimal fraction).
- $PWP$ is the permanent wilting point (expressed as a decimal fraction).
Step 2: Detailed Explanation:
Let us identify the values provided:
- Apparent specific gravity ($\text{As}$) $= 1.5$
- Root zone depth ($d_{\text{root}}$) $= 100\text{ cm}$
- Field Capacity ($FC$) $= 22\% = 0.22$
- Permanent Wilting Point ($PWP$) $= 12\% = 0.12$
Substitute these values into the storage capacity equation:
\[ d = 1.5 \times 100\text{ cm} \times (0.22 - 0.12) \]
\[ d = 150 \times 0.10 \]
\[ d = 15\text{ cm} \]
Therefore, the total depth of available water that can be stored in the root zone is $15\text{ cm}$.
Step 3: Final Answer:
The storage capacity of the soil is $15\text{ cm}$.
Hence, the correct option is (B).