Quantifying denudation rates under different climatic and tectonic settings is fundamental to
understanding landscape evolution. Carbonate rocks may respond differently to climatic and …

For the estimation of global karst carbon sink, a few conventional methods usually require
the parameters that are difficult to measure, resulting in the big cost. Moreover, under the …

Rock weathering is a key component of the rock cycle that transforms rocks in sediments,
soils and/or dissolves minerals to ions, and plays an important role in landforms …

This study introduces an improved method to assess land capability in the rural
environment. Land capability, also defined as natural use, is a powerfull asset in land use …

Aquifer recharge may depend mainly on the difference between precipitation and
evapotranspiration. Hydrological models used to estimate groundwater reserves use …

Carbonate rocks are highly reactive and can have higher ratios of chemical weathering to
total denudation relative to most other rock types. Their chemical reactivity affects the first …

Hilltop curvature (CHT) can record erosional responses to tectonic forces and/or climate
change. Although CHT has a linear relationship with the erosion rate, which is a significant …

The rates of carbonate rock weathering affect the global carbon cycle over timescales of
hundreds to thousands of years. While field measurements show that the rate of carbonate …

Tectonic plate motion, and the resulting change in land surface elevation, has been shown
to have a fundamental impact on landscape morphology. Changes to uplift rates can drive a …

The development of a karst landscape results from complex interactions between lithology,
climate, hydrology, soil, vegetation and tectonics. Weathering and erosion of carbonate …