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Feb 17, 2023 · Found below the O horizon, it has a dark brown color as it contains the maximum organic matter of the soil. The A horizon or topsoil is thus also called the humus layer. The topsoil is the region of intense biological activity and has the most nutrients.
The horizon description system begins by splitting soil horizons into two distinct groups: organic and mineral horizons. Organic horizons are those that contain 17% or more organic carbon; mineral horizons have less than 17% organic carbon.
A soil horizon is a distinct layer within the soil profile that has unique physical and chemical properties, formed as a result of various processes such as weathering, organic matter accumulation, and biological activity.
The process of soil formation generally involves the downward movement of clay, water, and dissolved ions, and a typical result of that movement is the development of chemically and texturally different layers known as soil horizons.
Apr 27, 2024 · In some soils the B horizon is enriched with calcium carbonate in the form of nodules or as a layer. This occurs when the carbonate precipitates out of downward moving soil water or from capillary action. The diagram below illustrates the effect of climate on eluviation and illuviation.
A cut in the side of a hillside shows each of the different layers of soil. All together, these are called a soil profile (figure 1). The simplest soils have three horizons: topsoil (A horizon), subsoil (B horizon), and C horizon.
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Feb 19, 2022 · In some soils the B horizon is enriched with calcium carbonate in the form of nodules or as a layer. This occurs when the carbonate precipitates out of downward moving soil water or from capillary action. The diagram below illustrates the effect of climate on eluviation and illuviation.