Soil formation, known as pedogenesis, is the process of soil genesis as regulated by the effects of place, environment, and history.
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Soil formation, known as pedogenesis, is the process of soil genesis as regulated by the effects of place, environment, and history.
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Soil formation is influenced by at least five classic factors that are intertwined in the evolution of a soil.
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The type and amount of precipitation influence soil formation by affecting the movement of ions and particles through the soil, and aid in the development of different soil profiles.
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Soil formation is the most speciose ecosystem on Earth, but the vast majority of organisms in soil are microbes, a great many of which have not been described.
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Soil formation animals, including soil macrofauna and soil mesofauna, mix soils as they form burrows and pores, allowing moisture and gases to move about, a process called bioturbation.
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Humans impact soil formation by removing vegetation cover through tillage, application of biocides, fire and leaving soils bare.
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Soil formation-forming factors continue to affect soils during their existence, even on stable landscapes that are long-enduring, some for millions of years.
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Russian geologist Vasily Dokuchaev, commonly regarded as the father of pedology, determined in 1883 that soil formation occurs over time under the influence of climate, vegetation, topography, and parent material.
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Soil formation demonstrated this in 1898 using the soil forming equation:.
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The empirical method is still mostly employed today, and soil formation can be defined by varying a single factor and keeping the other factors constant.
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