在碳酸盐岩地区，流域侵蚀过程中硫酸是否参与，对于我们正确理解流域化学风化速率，以及流域侵蚀对大气co2的消耗和全球碳循环等都有重要的意义。
It is important to ascertain the role of sulfuric acid in carbonate weathering so as to understand the chemical weathering rate carbonate rocks, CO2 consumption and global carbon cycle.
由于非连续特性，化学风化可增大水岩界面，提升矿物溶解反应的规模及速率。
Because of discontinuity, chemical weathering can add water-rock interface and raise mineral dissolution rate.
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