Step 1: Understanding the Concept:
Soil is a complex porous medium consisting of irregular solid particles and interconnected pore spaces.
When water or gases flow through soil, they cannot travel in a straight line; instead, they must wind through an irregular, twisted path around the soil particles.
Step 2: Key Formula or Approach:
The tortuosity ($T$) of a porous medium is defined as:
\[ T = \frac{L_e}{L} \]
where $L_e$ is the actual, curved path length traveled by a fluid molecule through the pores, and $L$ is the straight-line distance across the soil column.
Step 3: Detailed Explanation:
Let us analyze the geometry of fluid flow path:
Because the pore channels in soil are winding and non-linear, the actual path length ($L_e$) that water or gas must travel is always greater than the straight-line thickness of the soil sample ($L$).
Mathematically, because $L_e > L$, the ratio:
\[ T = \frac{L_e}{L} > 1 \]
This means the tortuosity value of any real soil must always be greater than $1$.
A completely straight, parallel capillary tube would have a tortuosity value of exactly $1$, which represents the minimum limit.
Higher tortuosity values indicate highly compacted soils or soils rich in plate-like clay minerals, which increase the flow path length and reduce the soil's hydraulic conductivity and gas diffusion rates.
Step 4: Final Answer:
The value of tortuosity in soil is always $>1$.
Therefore, the correct option is (C).