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the longer the soil partical the coarser it will be
Correct. Soil particles are categorized as sand, silt, and clay, with sand being the largest, followed by silt and then clay. The larger the particle size, the coarser the soil texture will be.
The bigger the particle size, the more drainage the soil would have. The smaller the particle sizer, the less drainage the soil would have. ITS EASY
Yes, soil texture can influence particle density. Soil particles in sandy soils are larger and less tightly packed, resulting in lower particle density. In contrast, clay soils have smaller particles that are more closely packed, leading to higher particle density.
Soil particle size influences filtration by affecting the pore size and distribution within the soil. Larger particles create larger pores, allowing water to flow more freely through the soil. Conversely, smaller particles create smaller pores, leading to slower water movement and potential clogging in the soil.
Smaller particle sizes generally result in faster percolation rates because there is less resistance to the flow of liquids through the smaller spaces between the particles. Larger particles create more void spaces and can slow down the percolation rate as the liquid has to travel through these larger spaces. Therefore, finer particles allow liquid to flow more quickly compared to coarser particles.
Capillary action increases as soil particle size decreases because smaller particles have higher surface area that enhances water retention and movement between them. Smaller particles create a tighter network of capillaries, allowing water to move more readily through the soil.
Silt is a type of soil particle that is finer than sand but coarser than clay. It is beneficial to soil fertility because it has good water retention properties and provides aeration for plant roots. Silt also contains essential nutrients that can help support plant growth.
Sandy soil will allow more water to percolate compared to clayey soil. This is because sandy soil has larger particle sizes with more space between them, allowing water to flow through more easily. Clayey soil has smaller particle sizes with less space between them, leading to slower water percolation.
Clay soil has fine particles, which are smaller than coarse particles such as sand. Clay particles are smaller than 0.002 mm in size, making the soil dense and able to retain moisture well due to its small particle size.
Smaller particle size increases the surface area available for chemical reactions to occur, thus accelerating the rate of weathering. This is because smaller particles provide more opportunities for water and chemicals to interact with the mineral surfaces. As a result, finer-grained rocks tend to weather more rapidly than coarser-grained rocks.
TRUE