Intro to Geotechnical Science

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Cohesive

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Intro to Geotechnical Science

Definition

Cohesive refers to the property of soil that enables it to stick together due to the attractive forces between the particles. This characteristic is particularly significant in clayey soils, where fine particles have strong intermolecular forces that contribute to the soil's ability to retain shape and resist shear stress. Understanding cohesiveness is essential in evaluating how soils behave under load and how they interact with water, which are crucial for construction and engineering applications.

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5 Must Know Facts For Your Next Test

  1. Cohesive soils typically have high water retention capabilities, which can lead to increased stability when properly managed.
  2. The degree of cohesion in soil affects its compaction and overall strength, making it critical in the design of foundations and earth structures.
  3. Cohesive properties are often measured using tests like the unconfined compressive strength test, providing valuable data on the soil's load-bearing capacity.
  4. Cohesion decreases with increasing moisture content in clayey soils, as excess water can weaken the attractive forces between particles.
  5. In contrast to granular soils, cohesive soils are more susceptible to changes in water content, which can significantly alter their engineering properties.

Review Questions

  • How does the cohesiveness of clay affect its engineering applications?
    • The cohesiveness of clay is crucial in engineering because it affects how clay behaves under load and during construction processes. High cohesion provides better stability for structures like foundations, while low cohesion can lead to instability and potential failure. Engineers must consider these factors when designing structures on or with clay soils, ensuring proper analysis of shear strength and compaction characteristics.
  • Discuss the relationship between Atterberg limits and soil cohesiveness.
    • Atterberg limits are key indicators of soil behavior, specifically its plasticity and consistency, which directly relate to cohesiveness. The liquid limit represents the point at which soil transitions from a plastic to a liquid state, while the plastic limit indicates the moisture content where soil maintains its shape. These limits help identify cohesive soils' characteristics, influencing construction methods and material selection for various projects.
  • Evaluate the implications of changing moisture content on cohesive soils and their engineering performance.
    • Changing moisture content in cohesive soils significantly impacts their performance in engineering contexts. As moisture levels rise, cohesion can decrease due to increased pore water pressure, leading to a reduction in shear strength and stability. Conversely, low moisture can enhance cohesion but also increase brittleness. Understanding these dynamics is essential for engineers when designing safe structures that rely on cohesive soils, as they must anticipate potential fluctuations in moisture due to environmental conditions or construction activities.

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