土壤有机质和粘粒含量显著地影响土壤团聚体的“原始稳定性”和“崩解速率”，是影响土壤团聚体抗蚀性的主要内在因素。
The soil organic and clay influence remarkably the soil aggregate "original stability" and "collapse velocity", they are the mostly intrinsic factor to soil aggregate erosion.
研究还显示，芳烃的甲基化和甲基重排作用受原始可溶有机质丰度、来源和演化程度的控制。
In addition, methylation and methyl rearrangement of arenes were mainly controlled by the abundance, source and evolution degree of soluble organic matter.
未成熟-低成熟阶段到高成熟阶段，有机质丰度明显降低，需要进行原始有机碳含量的恢复。
The abundance of organic matter lowers significantly from immature-low mature stage to high mature stage, thus the original TOC should be restituted.
同时，成烃动力学的研究在确定有机质类型、热史恢复、原始生烃潜力恢复等方面均有较高的实际应用价值。
Moreover, the kinetics of organic matter generating hydrocarbon is worthy of ascertaining type of organic matter, resuming hot history and evaluating.
同时，成烃动力学的研究在确定有机质类型、热史恢复、原始生烃潜力恢复等方面均有较高的实际应用价值。
Moreover, the kinetics of organic matter generating hydrocarbon is worthy of ascertaining type of organic matter, resuming hot history and evaluating.
应用推荐