Step 1: Identifying the Goal:
The objective is to analyze how the soil suction head (\(S\)) and hydraulic conductivity (\(K\)) behave when the moisture content (\(w\)) of a soil sample is raised.
Step 2: Analysis of Soil Properties:
Soil Suction Head (S):
Soil suction represents the intensity with which soil particles attract and hold water. In dry soil, water is tightly bound within small pores by strong surface tension and adsorptive forces, creating high suction.
- As water content (\(w\)) increases, these capillary forces are satisfied and the water is held more loosely in larger pores. This causes the tension (suction head) to drop. Thus, \(S\) decreases as \(w\) increases.
Hydraulic Conductivity (K):
This property indicates the soil's ability to transmit water. In unsaturated or dry soil, air bubbles block the flow paths, resulting in low conductivity.
- When moisture content (\(w\)) increases, the air-filled voids are replaced by water, creating more continuous and wider channels for flow. This significantly improves the soil's ability to conduct water. Thus, \(K\) increases as \(w\) increases.
Step 3: Conclusion:
Since increasing the moisture content leads to a reduction in suction head and an increase in hydraulic conductivity, option (D) is the correct choice.