在热带,岩石的风化强度取决于渗入岩石的大气降水和岩石所获得的热量。如果取消一种营力,岩石的风化强度就会显著降低。生物风化作用对岩石地球化学改造的方向影响重大。碳酸气和有机酸的量在很大程度上溴定着渗入岩石的大气降水的PH值和表生作用的水化学环境。硅、铝、铁、钙、镁和钾是原生矿物及风化次生矿物的主要组成 In the tropics, the intensity of weathering of a rock depends on the amount of heat that the rock infiltrates into the atmosphere and the heat it receives. If you cancel a camping force, rock weathering intensity will be significantly reduced. The biological weathering has a great influence on the direction of rock geochemical alteration. The amounts of carbon dioxide and organic acids are largely determined by the pH of the atmospheric precipitation that infiltrates the rock and the aquatic environment of the epiphytes. Silicon, aluminum, iron, calcium, magnesium and potassium are the major constituents of primary minerals and weathered secondary minerals