pedogenesis process成壤过程
pedogenesis characteristics发生特性
pedogenesis Å成土酌
pedogenesis E成土酌
pedogenesis ĥ成土酌
Anthropic Pedogenesis人为成土过程
pedogenesis environment成壤环境
pedogenesis diagenesis成土成岩作用
weathering pedogenesis风化成土作用
Soil chronosequences are valuable tools for investigating rates and directions of soil evolution and their modeling as well as for testing theories of pedogenesis.
土壤时间序列在研究土壤演化速率与方向、建立土壤发生演化模型上具有重要的价值,并且能为土壤发生学理论的验证提供宝贵的信息。
参考来源 - 土壤时间序列的构建及其在土壤发生研究中的意义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。
参考来源 - 中国黄土磁学与古气候(英文) CHINESE LOESS MAGNETISM AND PALEOCLIMATEIn the warmer and wetter climate conditions, the paleosol layer grows with strong pedogenesis and abundant rainfall. The content of CaCO3 strongly affected by leaching.
黄土层发育时气候较为干冷,成壤作用弱；古土壤层发育时气候温湿,降水丰富,成壤作用较强,CaCO3含量受淋滤强烈。
参考来源 - 陕西洛川离石黄土下部土层渗透率与含水条件研究