The finer material holds more water. The granular size of Clay, Silt and Sand are in this order (smallest to largest):
So Clay holds the most water, then Silt, Then Sand.
This can be disproved if one is dry and the other is wet or other variations of this idea obviously.
*This is one of those question where I wish wiki Answers would allow commas.
Sand is more permeable than silt because sand particles are larger with more spaces between them, allowing water to flow more easily through them. Silt particles are smaller and more compact, resulting in lower permeability.
Sand is more permeable than loam. Sand has larger particles with more space between them, allowing water to flow through more easily, while loam has a mix of sand, silt, and clay particles which slows down the movement of water.
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.
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 soil is the least permeable because it has smaller particles that are closely packed together, reducing the spaces for water to flow through. Silt and loam soils have larger particles and more pore spaces, making them more permeable than clay soil.
Clay is not more porous than sand. Porous means permeable by fluids, so, sand is more porous than clay.
Sand is more permeable than silt because sand particles are larger with more spaces between them, allowing water to flow more easily through them. Silt particles are smaller and more compact, resulting in lower permeability.
Sand is more permeable than loam. Sand has larger particles with more space between them, allowing water to flow through more easily, while loam has a mix of sand, silt, and clay particles which slows down the movement of water.
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.
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 soil is the least permeable because it has smaller particles that are closely packed together, reducing the spaces for water to flow through. Silt and loam soils have larger particles and more pore spaces, making them more permeable than clay soil.
The percentage of sand, silt, and clay in soil determines its texture. Soil with more than 50% sand is classified as sandy, more than 50% clay is classified as clayey, and more than 50% silt is classified as silty. The ideal soil texture for plant growth is loam, which has a relatively equal mix of sand, silt, and clay.
gravel,coarse,fine sand,silt and clay
Silt is typically considered impermeable, meaning water has difficulty passing through it. Silt particles are smaller than sand but larger than clay, allowing for limited water infiltration.
clay
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.
Lome is contained by equal amounts of sand, silt, clay, and organic matter.