depending on the dung they use to make the fertilizer soil
A piece of soil is commonly referred to as a soil particle or soil grain. These individual particles can vary in size, shape, and composition.
Black soil is a visual classification and the composition of black soils will vary,
Small particles of soil are called "soil particles" or "soil grains." These particles can vary in size from sand particles to silt and clay particles.
It will vary from leaching, weathering, and accumulation of organic matter.
The answer depends on how tighly the soil is packed.
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Loam soil typically contains around 2-3% organic matter. This percentage can vary depending on the location and management practices. Organic matter in soil is important for fertility, nutrient retention, and soil structure.
Soil properties can vary with depth due to factors like organic matter content, texture, nutrient levels, and pH. Generally, surface soil layers (topsoil) tend to have more organic matter and nutrients, while deeper layers may have different physical and chemical characteristics based on factors like weathering processes and root activity. The depth of the soil profile can also affect water retention, nutrient availability, and root growth.
The equivalent of 100 grams of soil in cups can vary depending on the soil density. On average, 100 grams of soil is approximately equal to 0.45 cups.
Iraq's soil is primarily composed of three main types: clay soil, loamy soil, and sandy soil. These soils vary in their composition and characteristics, with clay soil being dominant in the central and southern regions, loamy soil in the north, and sandy soil in desert areas. These soils support a range of agricultural activities in the country.
The vertical sequence of soil layers is called a soil profile. This profile typically consists of distinct layers, or horizons, that vary in color, texture, and composition. It is important for understanding the different properties and characteristics of the soil.
In the Philippines, there are various types of soil, including clayey soil, sandy soil, loamy soil, and volcanic soil. These soils can vary in texture, fertility, and composition, depending on the region and geological history of the area. Each type of soil has its own characteristics that can affect agricultural productivity and land use.