Step 1: Understanding the Concept:
Plant Available Water (PAW) is the portion of water in the soil that can be easily extracted by plant roots.
Key Formula or Approach:
The plant available water is calculated as:
\[ \text{Plant Available Water (PAW)} = \text{Field Capacity (FC)} - \text{Permanent Wilting Point (PWP)} \]
Step 2: Detailed Explanation:
Let us review the soil moisture constants:
- (B) Saturation moisture content: The soil pore space is completely filled with water, but some of this water drains away rapidly due to gravity (gravitational water) and is not available for plants.
- (A) Field capacity moisture content: The amount of water retained in the soil after excess gravitational water has drained away. This represents the upper limit of plant-available water.
- (D) Permanent wilting point: The soil moisture content at which plants can no longer extract water, leading to permanent wilting. This represents the lower limit of plant-available water.
- (C) Hygroscopic moisture content: Water held extremely tightly by soil particles as a thin film, which is completely unavailable to plants.
Thus, the available water is the water held between Field Capacity (A) and Permanent Wilting Point (D).
Step 3: Final Answer:
The correct combination is (A) and (D) only, which corresponds to Option (C).