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Lithology is a principle state factor of soil formation, interacting with climate, organisms, topography and time to define pedogenesis.
Here we use Hans Jenny's State Factor Equation as a flexible, integrative tool for understanding these effects.
Chronosequence studies in the region have improved our understanding of the temporal state factor associated with the development of this mineralogy.
Here we present the supporting rationale for the development of subaqueous soil resource inventories; and through a synthesis of geologic and pedologic principles and concepts, propose a new state factor equation to explain subaqueous soil genesis and distribution.
Formal arguments, framed in the context of the state factor model of soils and ecosystems, show that where the scales of the global and local components are sufficiently different, global or local dynamics can be discovered without considering the other.
We use the state factor approach to highlight the role of important aspects of climate, substrate, organisms, relief, and time in differentiating urban from non-urban areas, and for determining heterogeneity within spatially extensive metropolitan areas.
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These five "state factors" are parent material, topography, climate, organisms, and time.
Big Brown has never raced on a synthetic track and will have to ship to Colonel John's home state, factors that will be in Colonel John's favor.
What relationships among state factors does it change?
We then ask: What abiotic state factors does an engineer affect?
We describe how the state factors affecting soil formation affect the persistence and decomposition of SOC in buried soils.
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