Step 1: Understanding the Concept:
Water erosion is governed by the interaction between the erosive agent (rainfall) and the material being eroded (soil).
Soil conservation scientists use the terms "erosivity" and "erodibility" to distinguish between these active and passive forces.
Step 2: Detailed Explanation:
Let us evaluate Statement (I):
Rainfall erosivity (the R-factor in USLE) is the potential ability of rain to cause soil erosion.
It is determined by the physical characteristics of the rainfall, including raindrop size, terminal velocity, total kinetic energy, and maximum 30-minute intensity (\( I_{30} \)).
Erosivity is purely a climatic factor and is independent of soil properties.
Thus, Statement (I) is correct.
Let us evaluate Statement (II):
Soil erodibility (the K-factor in USLE) represents the soil's inherent susceptibility or vulnerability to detachment and transport by erosive agents.
It depends entirely on the soil's physical properties, including texture (sand, silt, clay ratios), organic matter content, soil structure, and permeability.
For example, soils rich in silt and very fine sand are highly erodible, whereas high clay and organic matter content reduce erodibility by binding soil particles together.
Thus, Statement (II) is correct.
Step 3: Final Answer:
Both Statement (I) and Statement (II) are correct.