『Abstract
　Concentrations of weathering products in streams often show relatively little variation compared to changes in discharge, both at event and annual scales. In this study, several hypothesized mechanisms for this “chemostatic behavior” were evaluated, and the potential for those mechanisms to influence relations between climate, weathering fluxes, and CO2 consumption via mineral weathering was assessed. Data from Loch Vale, an alpine catchment in the Colorado Rocky Mountains, indicates that cation exchange and seasonal precipitation and dissolution of amorphous or poorly crystalline aluminosilicates are important processes that help regulate solute concentrations in the stream; however, those processes have no direct effect on CO2 consumption in catchments. Hydrograph separation analyses indicate that almost one-half of annual fluxes of Na and SiO2 in the stream; thus, flushing of old water by new water (snowmelt) is an important component of chemostatic behavior. Hydrologic flushing of subsurface materials further induces chemostatic behavior by reducing mineral saturation indices and increasing reactive mineral surface area, which stimulate mineral weathering rates. CO2 consumption by carbonic acid mediated mineral weathering was quantified using mass-balance calculations; results indicated that silicate mineral weathering was responsible for approximately two-thirds of annual CO2 consumption, and carbonate weathering was responsible for the remaining one-third. CO2 consumption was strongly dependent on annual precipitation and temperature; these relations were captured in a simple statistical model that accounted for 71％ of the annual variation in CO2 consumption via mineral weathering in Loch Vale.

Keywords: Mineral; Weathering; Carbon; CO2; Sequestration』
1. Introduction
　1.1. Description of study site
2. Methods
　2.1. Sample collection and analyses
　2.2. Solute flux calculations
　2.3. Geochemical modeling
　2.4. Experimental methods
3. Results
　3.1. Concentration-discharge relations and weathering fluxes
　3.2. Cation exchange
　3.3. Flushing of subsurface waters
　3.4. Seasonal precipitation/dissolution of amorphos aluminosilicates
　3.5. Chemical affinity
　3.6. Variations in reactive mineral surface area
　3.7. Laboratory experiments
4. Discussion
　4.1. Implications for consumption of CO2 by chemical weathering
5.Summary and conclusions
Acknowledgements
References