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Consequently, the weathering rate maximum occurs at intermediate soil thickness.
In this study, we investigate the influence of physical erosion on soil profile weathering rate calculations.
These weathering profiles generally develop under both stable geodynamic conditions (weathering rate ≫ erosion rate) and a hydrolysing climate.
To reduce the weathering rate of natural building stones, a wide variety of water repellents and consolidants are commercially available.
Weathering rate models designed for watersheds combine chemical data of discharging waters with morphologic and hydrologic parameters of the catchments.
The effect of climate, rock type and land management is illustrated by different combinations of weathering rate and erosive diffusivity.
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These factors support high chemical weathering rates and intense leaching.
The weathering rates based on denudation since moraine deposition are comparable or smaller than weathering rates assuming steady-state denudation.
A number of methods exist for estimating mineral weathering rates.
Long-term chemical weathering rates range from 0 to 173 t·km−2 year−1, in several cases exceeding the highest granitic weathering rates on record from previous work.
Weathering rates are related to the mass, elevation, and exposure of bedrock.
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