Art F. White

TL;DR: In this paper, the authors evaluated the effect of weathering on chemical weathering by correlating variations on solute concentrations and fluxes with temperature, precipitation, runoff, and evapotranspiration (ET) for a worldwide distribution of sixty-eight watersheds underlain by granitoid rock types.

TL;DR: In this article, the correlation between decreasing reaction rates of silicate minerals and increasing duration of chemical weathering was investigated for both experimental and field conditions, and it was shown that intrinsic surface area, which increases with the duration of weathering, was responsible for a third of the exponential decrease in the weathering rate.

TL;DR: Lee et al. as discussed by the authors presented a SEM image of a naturally weathered (001) cleavage surface of an al kal i felds par from gravels formed from the granite at Shap, northern England.

TL;DR: In this article, the authors evaluated the effect of climate on chemical weathering by correlating variations in solute con- centrations and fluxes with temperature, precipitation, runoff, and evapotranspiration (ET) for a worldwide distribution of sixty-eight watersheds underlain by granitoid rock types.