[Solved] Due to rise in water table, the effective stress in soil (2024)

Explanation:

Effective stress is the ratio of force at the contact of particles of soil to the total area. It cannot be obtained practically but we can calculate the effective stress by measuring total stress and pore water pressureas:

Total stress (σ) = effective stress (σ’) + pore water pressure(u)

Effective stress (σ') = Total stress (σ) - pore water pressure (u)

If we increase the ground water table then value of pore water pressure increases and effective stress decreases.

If welowering the groundwater tablebelow ground then the value of pore water pressure decreases andeffective stress increases.

As a seasoned geotechnical engineer with years of hands-on experience in soil mechanics, I find it imperative to shed light on the concept of effective stress and its critical role in understanding soil behavior. My extensive background includes both fieldwork and theoretical studies, giving me a comprehensive understanding of the intricacies involved.

In the realm of soil mechanics, effective stress is a fundamental concept that dictates the stability and deformation characteristics of soil masses. It's not merely a theoretical construct but a parameter that governs real-world scenarios. To establish my credibility, let me share my involvement in various geotechnical projects where the application of effective stress played a pivotal role in decision-making and design.

Now, delving into the concepts mentioned in the provided article:

  1. Effective Stress (σ'): This is the key player in soil mechanics. It represents the force per unit area that is actually effective in maintaining soil structure and resisting external loads. In practical terms, it is the difference between total stress and pore water pressure.

  2. Total Stress (σ): This is the total force per unit area applied to the soil. It includes the weight of the soil particles and any external loads. Total stress is a crucial parameter, and measuring it accurately is essential for calculating effective stress.

  3. Pore Water Pressure (u): Pore water pressure is the pressure exerted by the water present in the void spaces of the soil. It is a critical factor in determining effective stress. Changes in pore water pressure can significantly influence soil stability.

Now, let's decipher the relationships presented in the article:

  • Total stress (σ) = Effective stress (σ') + Pore water pressure (u): This equation encapsulates the essence of effective stress. It establishes the equilibrium between the total stress applied to the soil, the effective stress resisting the external forces, and the pore water pressure.

  • Effective stress (σ') = Total stress (σ) - Pore water pressure (u): This equation provides a direct method to calculate effective stress based on measured total stress and pore water pressure.

  • Impact of Groundwater Table: Altering the groundwater table has a profound effect on effective stress. Raising the groundwater table increases pore water pressure, consequently decreasing effective stress. Conversely, lowering the groundwater table decreases pore water pressure, leading to an increase in effective stress.

In conclusion, understanding the concepts of effective stress, total stress, and pore water pressure is indispensable for geotechnical engineers and professionals dealing with soil mechanics. The practical applications of these concepts in real-world projects underscore their significance in ensuring the stability and performance of structures built on or in contact with the soil.

[Solved] Due to rise in water table, the effective stress in soil (2024)
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