Construct · 1 fields · 1 citations

field-laboratory weathering rate discrepancy: a standalone construct

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Soil chemistry

the finding that silicate minerals weather orders of magnitude more slowly in the field than in laboratory experiments, linked to mineral age and solution saturation.

In soil chemistry, field-laboratory weathering rate discrepancy refers to the finding that silicate minerals weather orders of magnitude more slowly in the field than in laboratory experiments, linked to mineral age and solution saturation. This meaning comes from White (2003) in Chemical Geology.[1]

Unit
Recovery means
Measured by

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field3 fields · 5 citationsjingle · one word, three constructs magnitude4 fields · 5 citationsjingle · one word, four constructs saturation4 fields · 4 citationsjingle · one word, four constructs

References

White, A. F., & Brantley, S. L. (2003). The effect of time on the weathering of silicate minerals: why do weathering rates differ in the laboratory and field? Chemical Geology, 202(3-4), 479-506. https://doi.org/10.1016/j.chemgeo.2003.03.001

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