生物地球化学循环
生态系统
有机质
环境科学
环境化学
土壤有机质
陆地生态系统
土壤水分
生物多样性
生态学
地球科学
化学
土壤科学
生物
地质学
作者
Panming Huang,Ming-Kuang Wang,Chih‐Yu Chiu
出处
期刊:Pedobiologia
[Elsevier BV]
日期:2005-08-18
卷期号:49 (6): 609-635
被引量:174
标识
DOI:10.1016/j.pedobi.2005.06.006
摘要
Soils are the central organizer of the terrestrial ecosystem. Their colloidal and particulate constituents, be they minerals, organic matter, and microorganisms, are not separate entities; rather, they are constantly interacting with each other. Interactions of these components control biogeochemical reactions, namely, the formation of short-range-ordered metal oxides, catalysis of humic substance formation, enzymatic stability and activity, mineral transformation, aggregate turnover, biogeochemical cycling of C, N, P, and S, and the fate and transformation of organic and inorganic pollutants. Furthermore, the impacts of mineral–organic matter–microorganism interactions and associated biogeochemical reactions and processes on biodiversity, species composition, and sustainability of the terrestrial ecosystem deserve close attention for years to come. This paper integrates the frontiers of knowledge on this subject matter, which is essential to uncovering the dynamics and mechanisms of terrestrial ecosystem processes and to developing innovative management strategies to sustain ecosystem health on the global scale.
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