Which factors are known to affect the compressibility of soil?

The factors that affect the compressibility of soil include soil type, water content, confining pressure, and the arrangement of particles. Each of these elements plays a crucial role in determining how much a soil sample can be compacted under load.

Soil type shapes the intrinsic properties and behaviors of different soils; for example, clay soils tend to be more compressible compared to sandy soils due to their finer particles and greater porosity. Water content is also a significant factor; as water fills the voids in soil, it influences the effective stress and the soil's ability to compress. Higher water content generally reduces friction between particles, making the soil more susceptible to compression.

Confining pressure refers to the stress applied to the soil from all directions, which impacts the soil's structure and consequently its compressibility. Greater confining pressures can often lead to densification and reduced compressibility. Lastly, the arrangement of particles, or how they are organized in space, plays a critical role as well since a well-structured arrangement can resist deformation better than a disorganized one.

In contrast, while mineral composition and temperature might influence soil behavior to some extent, they are not as directly related to compressibility. Similarly, soil age and vegetation affect soil properties but