Loam soil is more fertile than silt because it has a balanced mixture of sand, silt, and clay particles, which provides good drainage, moisture retention, and nutrient availability for plant growth. Silt soil has smaller particles that compact easily, leading to poor drainage and limited nutrient availability, reducing its fertility compared to loam.
Lome is contained by equal amounts of sand, silt, clay, and organic matter.
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 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.
Loam particles are typically between 0.002-0.02 millimeters in size. They are larger than clay particles but smaller than silt and sand particles, giving loam soil a balanced combination of water retention and drainage characteristics.
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.
Lome is contained by equal amounts of sand, silt, clay, and organic matter.
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 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.
Loam particles are typically between 0.002-0.02 millimeters in size. They are larger than clay particles but smaller than silt and sand particles, giving loam soil a balanced combination of water retention and drainage characteristics.
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.
Loam soil holds more water than clay soil. This is because loam soil is a mixture of sand, silt, and clay, which allows for better drainage and moisture retention compared to pure clay soil, which tends to compact and hold water tightly.
There are many different types of loam soils, each with slightly different characteristics, and with some draining liquids more efficiently than others. Different proportions of sand, silt, and clay give rise to types of loam soils: sandy loam, silty loam, clay loam, sandy clay loam, silty clay loam, and loam.[1] A soil dominated by one or two of the three particle size groups can behave like loam if it has a strong granular structure, promoted by a high content of organic matter.
Silt soil is composed of fine particles that are smaller than sand but larger than clay. It has good water retention properties and is fertile for agriculture. However, silt soil can be prone to compaction and erosion if not managed properly.
Types of SoilGeologists classify soils into more categories than seven, but there are six soil types that non-geologists use. They are: Clay, Silt, Sandy, Chalky, Peat, and Loam.
Bhangar contains more sand and less loam (balanced mix of sand, silt and clay) and is usually deposited away from flood plains (as these are coarse) thus lacking fertility but khadar is more loamy therefore it is more fertile (found mostly in lower flood plains). I hope it will satisfy you if not you can further ask !
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.
Sand is generally heavier than silt because sand particles are larger and more dense than silt particles. The larger size and higher density of sand particles make them weigh more than silt particles.