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全球温室效应正在缓慢地进行。本文首次探讨气候变暖对岩溶发育环境［温度（Ｔ），ＣＯ２分压（Ｐ）和大气降水］的影响，并预测了大气ＣＯ２浓度加倍时中国南北方碳酸盐岩化学溶蚀速率
The global warming is slowing down. This paper first explores the effects of climate warming on the developmental environments of karst [temperature (T), partial pressure of CO2 (P) and precipitation in the atmosphere) and predicts the chemical dissolution rates of carbonate rocks in northern and southern China when the atmospheric CO2 concentration is doubled