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The value of the maximum weathering rate and the precise soil thickness at which it occurs depend on several environmental variables, including precipitation regime, soil inundation, vegetation characteristics, and rate of groundwater drainage.
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Consequently, the weathering rate maximum occurs at intermediate soil thickness.
It increased the weathering rate rather definitely," he notes.
These weathering profiles generally develop under both stable geodynamic conditions (weathering rate ≫ erosion rate) and a hydrolysing climate.
Similarly, Hathorne and James [ 41] used Li isotopes in seawater as a tracer for silicate weathering and showed that between 16 and approximately 8 Ma silicate weathering rate has increased, while weathering intensity has decreased.
These factors support high chemical weathering rates and intense leaching.
A number of methods exist for estimating mineral weathering rates.
The weathering rates based on denudation since moraine deposition are comparable or smaller than weathering rates assuming steady-state denudation.
The weathering rates and ages of weathering profiles are discussed as a function of processes that run at the top and at the bottom of weathering mantles.
Chemical weathering rates for landscapes are difficult to quantify because the timescales over which weathering occurs are often unknown.
Chemical weathering rates are highest at the sites with rapid denudation rates, consistent with strong coupling between rates of chemical weathering and mineral supply from breakdown of rock.
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