Physical Processes
Pedogenesis
PEE-doh-JEN-ih-sis
Also Known As Soil Formation
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Pedogenesis is the formation of soil from weathered rock and organic matter into the layered profile of horizons a mature soil shows. Five factors classically govern the outcome: climate, the organisms present, the relief of the land, the parent material weathering supplies, and the time available, which for a fully developed profile is measured in decades to several thousand years.
Facts
Process Type TimescaleDecades to several thousand years for a mature soil profile to develop. 1 First Proposed Year Cross-Tradition Connections
Demonstrated By
The Daintree's ancient, heavily leached tropical soils are a textbook case of rapid organic-matter cycling paired with deep chemical weathering.
Sources
1. Pedogenesis (Wikipedia)
Wikimedia FoundationDefinition sectionQuote, Definition section
Soil formation, also known as pedogenesis, is the process of soil genesis as regulated by the effects of place, environment, and history.
View the Source 1. Pedogenesis (Wikipedia)
Wikimedia FoundationFactors section, process-typeQuote, Factors section, process-type
Climate is the dominant factor in soil formation, and soils show the distinctive characteristics of the climate zones in which they form.
View the Source 1. Pedogenesis (Wikipedia)
Wikimedia FoundationFactors section, timescaleQuote, Factors section, timescale
It takes decades to several thousand years for a soil to develop a profile, although the notion of soil development has been criticized.
View the Source 2. Vasily Dokuchaev (Wikipedia)
Wikimedia FoundationBiography sectionQuote, Biography section
He arrived at his theory after extensive field studies on Russian soils in 1883. His most famous work is Russian Chernozem (1883).
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