Silt is larger in particle size than clay and feels gritty when dry, while clay is finer in particle size and feels sticky when wet. Silt is more fertile than clay and drains better, while clay holds more water and nutrients.
Clay particles are smaller than silt particles. Clay particles are smaller than 0.002 mm in diameter, while silt particles range from 0.002 to 0.05 mm.
Clay is the most dense soil type, followed by silt and then sand. Clay particles are finer and more closely packed, which gives clay a higher density compared to silt and sand.
Clay is generally heavier than silt because clay particles are smaller and more densely packed together, resulting in a higher density. Silt particles are larger and less dense, making them lighter than clay particles.
Clay holds more water than sand and silt. Clay particles are smaller and create a denser structure that can hold water more effectively than the larger particles of sand and silt.
They are formed when rocks are weathered. They are found in the soil
It is more accurate to say it is formed from clay and silt.
clay
gravel,coarse,fine sand,silt and clay
Silt is larger in particle size than clay and feels gritty when dry, while clay is finer in particle size and feels sticky when wet. Silt is more fertile than clay and drains better, while clay holds more water and nutrients.
Clay particles are smaller than silt particles. Clay particles are smaller than 0.002 mm in diameter, while silt particles range from 0.002 to 0.05 mm.
Clay is the most dense soil type, followed by silt and then sand. Clay particles are finer and more closely packed, which gives clay a higher density compared to silt and sand.
Clay is generally heavier than silt because clay particles are smaller and more densely packed together, resulting in a higher density. Silt particles are larger and less dense, making them lighter than clay particles.
Clay holds more water than sand and silt. Clay particles are smaller and create a denser structure that can hold water more effectively than the larger particles of sand and silt.
suspensions
silt
The four main classes of soil are sand, silt, clay, and loam. Sand particles are the largest, silt particles are medium-sized, and clay particles are the smallest. Loam is a mixture of sand, silt, and clay, and is considered the most ideal soil type for plant growth.