Soil Bearing Capacity & Types
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Questions and Answers

What is the primary component of the earth's crust if organic matter is ignored?

  • Air
  • Water
  • Mineral matter (correct)
  • Gas
  • Which of the following describes well-graded sand?

  • Has no plasticity
  • Contains mostly finer particles
  • Contains a proportion of all sizes of sand particles (correct)
  • Is only found in dry environments
  • What characteristic defines stiff clay?

  • Feels greasy and smooth
  • Easily moulded with fingers
  • Requires a pick or pneumatic spade for removal (correct)
  • Can be removed with a spade
  • What is the particle size range for sand?

    <p>0.60 to 2mm</p> Signup and view all the answers

    Which type of soil is characterized by the largest particle size, typically over 2mm?

    <p>Gravel</p> Signup and view all the answers

    Which test determines the moisture content at which the soil ceases to be plastic?

    <p>Plastic limit test</p> Signup and view all the answers

    What is the primary use of cohesive soils in construction?

    <p>For foundations due to their strength</p> Signup and view all the answers

    What does the plasticity index measure?

    <p>The difference between liquid and plastic limits</p> Signup and view all the answers

    Which of the following is true about loose gravel and sand?

    <p>Can be removed by hand-shovelling only</p> Signup and view all the answers

    Which type of soil consists of the finest siliceous and aluminous products of rock weathering?

    <p>Clay</p> Signup and view all the answers

    In the Casagrande classification chart, what does the first letter 'G' represent?

    <p>Gravel</p> Signup and view all the answers

    Which method is considered to be more reliable for soil inspection and testing?

    <p>Test Pit method</p> Signup and view all the answers

    What happens to very soft clay when squeezed in the fist?

    <p>It extrudes between fingers</p> Signup and view all the answers

    What is a characteristic of a poorly graded sandy soil in terms of its group symbol?

    <p>SP</p> Signup and view all the answers

    What is a limitation of the Test Pit method?

    <p>High expense</p> Signup and view all the answers

    What is determined by the standard penetration and consolidation test?

    <p>Compressibility and shear strength</p> Signup and view all the answers

    What distinguishes clay particles from other soil constituents?

    <p>Particle shape</p> Signup and view all the answers

    Which of the following best describes silt?

    <p>Sediment finer than sand, with some plasticity</p> Signup and view all the answers

    In the presence of water, how do clayey soils behave?

    <p>They swell due to repulsive forces.</p> Signup and view all the answers

    What characteristic is typical of organic soils?

    <p>Dark color and strong odor of decay</p> Signup and view all the answers

    Which soil type is unsuitable for building foundations due to high compressibility?

    <p>Organic soil</p> Signup and view all the answers

    What method is primarily used to determine the particle size distribution in soils?

    <p>Sieve analysis through a nest of sieves</p> Signup and view all the answers

    What is the primary composition of peat found in organic soils?

    <p>Fully decayed plant matter</p> Signup and view all the answers

    How does the surface-area-to-volume ratio of clay particles compare to that of gravel or sand?

    <p>It is several hundred to a thousand times greater.</p> Signup and view all the answers

    Study Notes

    Soil Bearing Capacity

    • Soil is defined, in a construction context, as the part of the earth below topsoil and above rock, formed by erosion, water, atmospheric conditions, and intense pressure over thousands of years.
    • Organic matter, though present in small quantities, is usually disregarded in soil analysis.
    • Mineral matter, the majority component, is classified as rocks or soils.
    • Rocks have firmly bonded mineral particles, while soil particles are either individual particles or conglomerates of easily separable particles.
    • Soils are classified as cohesive and non-cohesive types.

    Non-Cohesive Soils

    • Gravel: A natural deposit of rock fragments in a matrix of finer, typically sandy material. Particles are mostly larger than 2mm.
    • Sand: A granular, mainly siliceous sediment from rock weathering. Gritty, lacks plasticity. Particles range between 0.06mm and 2.00mm.
    • Well-graded sand: Contains a proportion of all sand particle sizes, with a prevalence of coarser grades.
    • Compact gravel and sand: Requires tools like picks for removal due to high resistance to penetration.
    • Loose gravel and sand: Easily removable by hand tools.
    • Uniform or poorly graded sand: Particles mostly within a restricted size range.

    Cohesive Soils

    • Clay: A deposit mainly of fine, siliceous and aluminous products of rock weathering. Smooth, greasy texture, sticks to fingers, and dries slowly. Clay shrinks on drying and gains strength.
    • Stiff clay: Requires tools (like picks or pneumatic spades) for removal, and can't be molded at its natural moisture content.
    • Firm clay: Excavated with a spade, and moldable under substantial pressure at natural moisture content.
    • Very soft clay: Extrudes between fingers when squeezed at natural moisture content.
    • Soft clay: Readily excavated and moldable with fingers at natural moisture content.
    • Boulder clay: Unstratified, containing sub-angular stones of varying sizes.

    Silt

    • Silt: Finely graded material, smaller than sand. Most grains will pass through a 75-micron sieve. Exhibits some plasticity and notable cohesion when dry.

    Uniqueness of Clay

    • Clay particles are non-equidimensional (flat, plate-like), differing in shape from gravel, sand, and silt particles, which are mostly equidimensional.
    • Chemical weathering produces clay, contrasting with mechanical weathering that forms gravel, sand, and silt.
    • Clay's flat shape leads to a significantly higher surface area-to-volume ratio compared to other soil types.
    • Electrostatic forces between plate-like clay surfaces influence behaviour greatly. These forces are repulsive when water is present, causing swelling. As water decreases, clay shrinks.

    Organic Soils

    • Soil consisting primarily of organic matter is referred to as organic soil.
    • Organic soils primarily contain decomposed plant matter (peat), having little or no mineral matter.
    • Organic soils are highly compressible and are unsuitable for building foundations due to compressibility.
    • They are usually dark in color and have a distinctive decaying odor.
    • Additional characteristics may include a fibrous texture due to plant debris (bark, leaves, branches).
    • Organic soils often form the top layer of soil and are frequently removed before construction starts.

    Soil Identification and Classification Tests

    • Several tests are used to identify and classify soils.
    • Particle size distribution: Determines the proportion of gravel, sand, and clay in a soil sample.
    • Soils are dried, then sieved through a set of sieves.
    • The weight retained on each sieve is recorded to determine particle size distribution.
    • Liquid limit test: Determines moisture content at which soil transitions from plastic to liquid state.
    • Plastic limit test: Determines moisture content at which soil ceases to be plastic (can be rolled into a 3mm diameter thread without breaking).
    • Plasticity index: Difference between liquid and plastic limits.
    • Data from these tests is graphed. A graph defines the range of sand grain sizes (0.60mm-2mm), silt grain sizes (0.60mm-0.002mm), and clay grain sizes (less than 0.002mm).
    • Results are plotted on graphs to establish properties.

    Casagrande Classification Chart

    • The chart uses two-letter symbols to categorize soils.
    • The first letter indicates the particle size (e.g., G for gravel, S for sand, M for silt, C for clay, O for organic silts and clays).
    • The second letter describes the soil's properties (e.g., H for high compressibility, L for low compressibility, P for poorly graded, W for well-graded).

    Other Tests

    • Dry density tests: Determine dry soil density in a soil's natural position.
    • Standard penetration test and consolidation test: Determine soil compressibility and shear.
    • Triaxial compression soil test: Determines shear strength parameters, used to establish allowable bearing pressure.

    Test methods

    • Test Pit Method: Involves digging pits/trenches, allowing for visual soil inspection and sample collection for laboratory tests (considered reliable). Limitations include cost and depth restrictions by a high water table.
    • Test Boring Method: Uses a power-driven drilling system (hollow stem fitted with a bit) to collect soil samples. A split-spoon or Shelby tube is used to remove the sample core.

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    Description

    Explore the concepts of soil bearing capacity and its different classifications in construction. This quiz covers both cohesive and non-cohesive soils, including gravel and sand types. Test your knowledge on how these soils affect construction practices.

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