The three primary particles that make up soil are sand, silt, and clay. Sand particles are larger and provide good drainage, silt particles are intermediate in size and improve soil fertility, while clay particles are the smallest and help retain water and nutrients. The proportion of these three particles determines soil texture and quality.
soil texture is some what the same there are soils with coarse or rough texture and there those with fine smooth texture . soil texture is due to the size of the particles that make it up. there are 3 main types of soil particle :-sand, with coarser or larger particles-silt, with medium sized particles-clay, with the finest or smallest particles
Three types of soil textures are sandy (large particles), loamy (equal parts of sand, silt, and clay), and clayey (small particles). These textures influence properties like drainage, water holding capacity, and nutrient availability in the soil.
Texture, structure, and pH are three characteristics used to describe soil. Texture refers to the size of soil particles, structure relates to how particles are arranged and aggregated, and pH indicates the acidity or alkalinity of the soil.
The three main types of soil texture are sand, silt, and clay. Sand particles are the largest, silt particles are medium-sized, and clay particles are the smallest. Soil texture influences properties like water retention, drainage, and nutrient availability.
Clay soil: has small particles that hold water and nutrients well, but can become compacted and have poor drainage. Sandy soil: has large particles that drain quickly and are low in nutrients, making it prone to drought and leaching. Loam soil: a balanced mix of sand, silt, and clay particles that provides good drainage, water retention, and nutrient content for plant growth.
clay, sand, and silt make up inorganic material in soil
Soil texture is identified on its particles. The particles are classified into 3 groups called soil separates which are the sand, silt, and the clay.
soil texture is some what the same there are soils with coarse or rough texture and there those with fine smooth texture . soil texture is due to the size of the particles that make it up. there are 3 main types of soil particle :-sand, with coarser or larger particles-silt, with medium sized particles-clay, with the finest or smallest particles
Three types of soil textures are sandy (large particles), loamy (equal parts of sand, silt, and clay), and clayey (small particles). These textures influence properties like drainage, water holding capacity, and nutrient availability in the soil.
The 3 most used nutrients in soil are Nitrogen, Potassium and Phosphorus. The others are Calcium, Magnesium and Sulfur.
Texture, structure, and pH are three characteristics used to describe soil. Texture refers to the size of soil particles, structure relates to how particles are arranged and aggregated, and pH indicates the acidity or alkalinity of the soil.
Detachment:soil particles are detached from the soil mass due to rain splash. Transport: deposition
i think the carbon oxgen and water :P
The three main types of soil texture are sand, silt, and clay. Sand particles are the largest, silt particles are medium-sized, and clay particles are the smallest. Soil texture influences properties like water retention, drainage, and nutrient availability.
The three basic particles that make up atoms are protons, neutrons, and electrons. Protons carry a positive charge, neutrons have no charge, and electrons carry a negative charge. Together, these particles form the structure of an atom.
These particles are: neutron, proton, electron.
every atom is made up of 3 particles and these are: 1) Electron- negatively charged 2) Proton-positively charged 3)Neutron_electrically neutral