『Abstract
　Rock weathering by carbonic acid has played a substantial role in both the global carbon cycle and related climate change. Carbonic acid as the major weathering agent has been accepted, whereas the importance of other acid (sulfuric, nitric or organic acids) as an agent is gradually recognized. Here, we examine sulfate dual-isotopic evidence (δ³⁴SSO4, δ¹⁸OSO4) and water chemistry from the Jialing River (Sichuan Basin, Southwest China) to identify dissolved sulfate sources and the role of sulfuric acid in carbonate weathering. A survey was carried our at 29 sites where surface water was sampled during the rainy (July, 2008) and dry (February, 2009) seasons in the Jialing River. The chemical composition of river water was characterized by a dominance of Ca²⁺, Mg²⁺ and HCO3^-, and SO4^2-, which accounted for more than 90％ of the total ion concentrations. Water chemistry varied greatly in time and space, particularly for Na⁺, Cl^-, and SO4^2-. This variation was a result of anthropogenic influences, such as acid deposition and domestic sewage inputs. Co-variation of the equivalent ratios of [Ca²⁺ + Mg²⁺] and [SO4^2- + HCO3^-] indicate that it required significant additional SO4^2- to achieve ionic balance, which implied that sulfuric acid might play a relatively important role in carbonate weathering of this river basin. Water samples from the Jialing River were significantly rich in SO4^2-, and increased almost two times from 274μM in the period of 1958-1990 to 499μM in this study. The use of co-variations of δ³⁴SSO4 vs.δ¹⁸OSO4 and of δ¹⁸OSO4 vs. δ¹⁸OH2O allowed us to demonstrate that most of the sulfate in the waters of the Jialing River was derived from sulfide oxidation and atmospheric inputs by high sulfur-content coal combustion while the contribution of sulfate from domestic and industrial wastewater could be important in the dry season. Thus, the contribution of sulfuric acid, produced by such sulfide oxidation and the oxidation of atmospheric SO2 emitted from coal combustion, as a weathering agent is also confirmed.

Keywords: Jialing River; Sulfate isotopic composition; Carbonate weathering; Sulfide oxidation; Sulfuric acid』

1. Introduction
2. Natural setting
　2.1. Topography and geology
　2.2. Climate and soil
3. Methodology
　3.1. Water samples
　3.2. Analytical methods
4. Results and discussion
　4.1. General characteristics of Jialing River water
　4.2. Carbonate dissolution and abundant sulfate in river water
　　4.2.1. Carbonate dissolution
　　4.2.2. Abundant sulfate in river water
　4.3. Sulfate sources
　　4.3.1. Long-term variation of sulfate concentration
　　4.3.2. Spatial and seasonal changes of SO4^2- concentration and dual-isotopic values
　　4.3.3. Contributions from different sulfate sources
5. Conclusions
Acknowledgments
References