dircet mineral cycling theory 直接矿物循环理论
Weathering and pedogenesis of rocks are important sources of mineral elements for ecological systems, and key processes of global biogeochemical cycling of mineral elements.
岩石风化成土作用是生态系统矿质元素的重要来源,也是全球矿质元素生物地球化学循环的重要环节。
Traditionally, silicon cycling is thought to be mainly controlled by rock weathering, subsequent mineral dissolution, and final aggradation in waters.
传统认为硅的循环主要受岩石风化、矿物溶解和水体沉积的影响。
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