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CivilSoil Mechanics
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The commonly used geophysical method for site exploration is ________

A

Gravitational method

B

Electrical resistivity

C

Magnetic method

D

All of the mentioned

Correct Answer

тЪЩя╕П TE тАв Technical Concept & PrincipleCivilSoil Mechanics
Option B

Electrical resistivity

Quick Summary:

The electrical resistivity method is the most widely used geophysical technique for soil exploration because it is non-destructive, cost-effective, and sensitive to soil moisture and clay content. It involves injecting an electrical current into the ground and measuring the potential drop between potential electrodes to determine the subsurface electrical resistivity.

тЪЩя╕ПTETechnical SolutionConcept & Principle
ЁЯТб Explanation

The electrical resistivity method is the most widely used geophysical technique for soil exploration because it is non-destructive, cost-effective, and sensitive to soil moisture and clay content. It involves injecting an electrical current into the ground and measuring the potential drop between potential electrodes to determine the subsurface electrical resistivity.

ЁЯФв Key Formulas

╧Бa=2╧АaVI\rho_a = 2\pi a \frac{V}{I}╧БaтАЛ=2╧АaIVтАЛ тАФ Apparent resistivity for Wenner configuration where 'a' is the uniform spacing between electrodes.

тЪЩя╕П Working Principle

The principle is based on Ohm's Law and the variation of resistivity among different soil types. An external current (I) is passed through two outer electrodes (A and B), and the potential difference (V) is measured between two inner potential electrodes (M and N). The apparent resistivity (╧Б\rho╧Б_a) is calculated using the measured V/I ratio and the specific geometry of the electrode arrangement, such as the Wenner or Schlumberger configuration.

ЁЯУМ Key Points
  • тЦ╕

    Resistivity depends on porosity, saturation, and clay content.

  • тЦ╕

    Clayey soils exhibit low resistivity compared to dry, granular soils.

  • тЦ╕

    The method is excellent for locating the water table and depth to bedrock.

  • тЦ╕

    It is categorized as an 'indirect' method of subsoil exploration.

тЬЕ Advantages
  • тЦ╕

    Non-invasive and non-destructive

  • тЦ╕

    Rapid data acquisition

  • тЦ╕

    Economical for large area surveys

тЭМ Disadvantages / Limitations
  • тЦ╕

    Sensitive to buried metallic objects and power lines

  • тЦ╕

    Ambiguity in interpretation of data

  • тЦ╕

    Effectiveness decreases with increasing depth

ЁЯЫая╕П Applications / Uses
  • тЦ╕

    Groundwater exploration

  • тЦ╕

    Mapping bedrock topography

  • тЦ╕

    Detection of pollution plumes in groundwater

ЁЯУД Additional Information
  • тЦ╕

    While gravitational and magnetic methods are used in deep geological prospecting (e.g., oil and mineral exploration), electrical resistivity is preferred for geotechnical shallow site exploration due to higher contrast sensitivity in soil materials.

  • тЦ╕

    The depth of investigation in resistivity surveys is approximately proportional to the electrode spacing.

ЁЯУК Diagram / Illustration
Apparent Resistivity Formula
╧Бa=2╧АaVI\rho_a = 2\pi a (V / I)╧БaтАЛ=2╧АaIVтАЛ
Where 'a' is electrode spacingI = Current Injection | V = Potential Drop | ╧БтВР = ApparentResistivity
тЬЕ

B is correct тАФ Electrical resistivity is the most common geophysical method for engineering site exploration due to its sensitivity to soil moisture and stratigraphy.

Core Concepts Used
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Geophysical Exploration Electrical Resistivity Tomography Soil Stratigraphy
ЁЯТб EXAM TIP

Always remember that geophysical methods are preliminary tools; they must be validated with direct methods like boreholes and standard penetration tests (SPT) for final engineering design.

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