What does 'consistence' measure in soil?

Consistence in soil refers to the soil's ability to hold together and resist deformation under pressure. It describes how the soil particles interact with one another and how they respond to mechanical stress, making it an important characteristic in terms of soil stability and structure. When assessing soil consistence, evaluators often consider how the soil behaves when squeezed, rolled, or pressed, which helps determine its suitability for various uses, such as agriculture or construction.

The measurement of consistence is pivotal for understanding soil compaction, stability, and its general handling properties, particularly under load. Soils with high consistence tend to resist deformation better than those with low consistence. This property is crucial for farmers, engineers, and builders, as it affects how water, air, and roots can penetrate the soil, impacting plant growth and structural integrity.

While other factors, like soil fertility, temperature response, and water retention, are vital attributes of soil, they are not directly tied to the concept of consistence, further highlighting the specific nature of this property in evaluating soil characteristics.