Situation 3: Consider the following shrinkage limit test using mercury. Mass of moisture can: 16.5 g 72.3 g Mass of wet soil and moisture can: Mass of dish: Mass of dish and displaced mercury: Mass of dry soil and moisture can: Volume of wet soil: 132.4 g 486.1 g 58.2 g 32.4 cm³ 3a. What is the volume of the dried soil particle? 3b. What is the shrinkage limit? 3c. If the liquid limit is 48% and the plasticity index is 18%. what is the liquidity index of the soil considering a natural water content of 16.4%? 3d. What is the consistency index? 3e. What is the shrinkage ratio? 3f. What is the specific gravity of the soil?

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Sediment transport

Sediment transport or Soil transport is the movement of solid particles, usually due to the combination of gravitational forces acting on the sediment, and the movement of the liquid at which the sediment enters. Soil erosion occurs in natural systems where the particles are sandstones (sand, rocks), mud, or clay; the liquid is air, water, or ice; and the gravitational force that works to move particles to the landing surface. Sediment transportation or soil migration due to the movement of liquids occurs in rivers, lakes, lakes, oceans, and other bodies of water as a result of currents and waves. Transportation is also caused by glaciers as they flow, and to places on earth under the influence of wind. Soil erosion due to gravity alone is possible in most sloping areas, including hills, scarves, cliffs, and the continental shelf — the continental boundary of the slope.