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Soil
Classification
Pedogenesis
Soil
formation (pedogenesis or genesis) can be illustrated using the
example of ecological theatre and the evolutionary play proposed
by Hutchinson
(1965). Soil forming factors can be envisioned as setting the
stage or conditions for soil formation – the ecological
theatre. The play that is enacted within the theatre is the
processes that interact over time to modify the original solum.
When we dig a soil pit, we peek into a moment taken from the
play and view the imprint of all that has occurred up to that
moment. Human intervention in the play can be either as actor or
co-director, re-defining the plot and changing the scope of the
theatre.
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Pedogenesis
is the relationship between soil forming factors
and processes
(modified from Hutchinson 1965)
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Soil
formation factors and processes combine to affect the overall
soil body, which is recognized and described as a pedon. The
resulting soil properties (thickness, color, texture, structure,
chemical properties of horizons) are used to classify the soil.
These properties, in combination with other land attributes and
economic considerations, may be used to interpret soil
suitability for particular uses. Monitoring soil changes through
selected attributes (so called soil quality indicators) should
be carried out periodically to determine soil quality and to
provide feedback into management practices, so that the role of
“director” in the evolutionary play is carried out
responsibly. Also review Soil
Quality.
Reference
Hutchinson
, G.E. 1965. The ecological theater and the evolutionary play.
Yale Univ. Press, New Haven , Connecticut .
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