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土壤温度变化导致微生物群落组成及其活性产生变化；某些微生物群落成员在较高温度时有能力代谢那些在较低温度时不能被利用的基质；因此，土壤温度上升将影响土壤生态系统中的C、N、S 循环。大多数研究结果显示，温度对土壤溶液中的溶解态有机质和土壤有机磷组分有较大的影响。这些结论对预测全球气候变化对土壤的影响有重要的意义。
Changes in soil temperature lead to changes in the composition and activity of microbial communities; some microbial community members have the ability to metabolize matrices that can not be utilized at lower temperatures at higher temperatures; therefore, increasing soil temperature will affect soil microbial community composition C, N, S cycle. Most studies have shown that temperature has a greater impact on dissolved organic matter and soil organic phosphorus components in soil solutions. These conclusions are of great significance in predicting the impact of global climate change on the soil.