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CivilSoil Mechanics
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Specific gravity of soil mass is the ratio of

A

╬│╬│w\frac{\gamma}{\gamma_w}╬│wтАЛ╬│тАЛ

B

╬│w╬│s\frac{\gamma_w}{\gamma_s}╬│sтАЛ╬│wтАЛтАЛ

C

╬│s╬│w\frac{\gamma_s}{\gamma_w}╬│wтАЛ╬│sтАЛтАЛ

D

╬│w╬│\frac{\gamma_w}{\gamma}╬│╬│wтАЛтАЛ

Correct Answer

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

╬│s╬│w\frac{\gamma_s}{\gamma_w}╬│wтАЛ╬│sтАЛтАЛ

Quick Summary:

The specific gravity (GGG) of soil solids is defined as the ratio of the unit weight of soil solids (╬│s\gamma_s╬│sтАЛ) to the unit weight of distilled water (╬│w\gamma_w╬│wтАЛ) at a standard temperature, typically 4┬░C4┬░C4┬░C. It is a dimensionless quantity that reflects the density of the soil particles relative to water.

тЪЩя╕ПTETechnical SolutionConcept & Principle
ЁЯТб Explanation

The specific gravity (GGG) of soil solids is defined as the ratio of the unit weight of soil solids (╬│s\gamma_s╬│sтАЛ) to the unit weight of distilled water (╬│w\gamma_w╬│wтАЛ) at a standard temperature, typically 4┬░C4┬░C4┬░C. It is a dimensionless quantity that reflects the density of the soil particles relative to water.

ЁЯФв Key Formulas

G=╬│s╬│wG = \frac{\gamma_s}{\gamma_w}G=╬│wтАЛ╬│sтАЛтАЛ тАФ Definition of specific gravity of soil solids

G=MsVsтЛЕ╬│wG = \frac{M_s}{V_s \cdot \gamma_w}G=VsтАЛтЛЕ╬│wтАЛMsтАЛтАЛ тАФ Mass-volume relationship form

тЪЩя╕П Working Principle

The principle relies on Archimedes' buoyancy and density definitions. By determining the mass of a known volume of dry soil particles using a pycnometer and comparing it to the mass of an equal volume of water, the specific gravity is calculated, which serves as a fundamental index property for classifying soil and calculating void ratios.

ЁЯУМ Key Points
  • тЦ╕

    Specific gravity is a dimensionless quantity.

  • тЦ╕

    For most inorganic soils, GGG typically ranges between 2.60 and 2.80.

  • тЦ╕

    The value is essential for determining void ratio (eee) using the relationship e=GтЛЕ╬│w╬│dтИТ1e = \frac{G \cdot \gamma_w}{\gamma_d} - 1e=╬│dтАЛGтЛЕ╬│wтАЛтАЛтИТ1.

  • тЦ╕

    It is usually determined in the laboratory using a pycnometer or density bottle.

тЬЕ Advantages
  • тЦ╕

    Useful in calculating the void ratio and degree of saturation.

  • тЦ╕

    Assists in identifying mineralogical composition of soil.

тЭМ Disadvantages / Limitations
  • тЦ╕

    Does not account for the influence of organic matter (which lowers GGG).

  • тЦ╕

    Experimental measurement requires precise temperature control.

ЁЯЫая╕П Applications / Uses
  • тЦ╕

    Soil classification and index property determination.

  • тЦ╕

    Calculation of dry density and unit weight relations in geotechnical engineering.

ЁЯУД Additional Information
  • тЦ╕

    The value of GGG is generally taken as 2.65 for quartz-based sands.

  • тЦ╕

    Option A is incorrect as it represents the bulk unit weight ratio, Option B is inverted, and Option D is the reciprocal of specific gravity.

ЁЯУК Diagram / Illustration
Specific Gravity of Soil (G)
╬│s\gamma_s╬│sтАЛ (Unit weight of soil solids)
╬│w\gamma_w╬│wтАЛ (Unit weight of water)
тЬЕ

C is correct тАФ Specific gravity of soil solids is defined as the ratio of the unit weight of soil solids to the unit weight of distilled water.

Core Concepts Used
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Phase Relationships Index Properties of Soil Unit Weight Principles
ЁЯТб EXAM TIP

Remember that specific gravity of solids (GsG_sGsтАЛ) is distinct from bulk specific gravity (GmG_mGmтАЛ); always check if the question specifies 'soil mass' or 'soil solids'.

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