In the case of chemical weathering control, soil moisture maintains greater rates of chemical alteration of saprolite, and physical disruption by creep and bioturbation is minimal on N-facing slopes.

High potential for weathering and climate effects of non-vascular vegetation in the Late Ordovician. Nature Communications , 2016; 7: 12113 DOI: 10.1038/ncomms12113 Cite This Page : ...