高分子
土壤水分
生物地球化学循环
风化作用
环境化学
化学
溶解有机碳
化学工程
地质学
土壤科学
地球化学
生物化学
工程类
作者
Satish C. B. Myneni,John T. Brown,Gustavo A. Martı́nez,W. Meyer‐Ilse
出处
期刊:Science
[American Association for the Advancement of Science]
日期:1999-11-12
卷期号:286 (5443): 1335-1337
被引量:279
标识
DOI:10.1126/science.286.5443.1335
摘要
Humic substances (HSs) are the natural organic polyelectrolytes formed from the biochemical weathering of plant and animal remains. Their macromolecular structure and chemistry determine their role in biogeochemical processes. In situ spectromicroscopic evidence showed that the HS macromolecular structures (size and shape) vary as a function of HS origin (soil versus fluvial), solution chemistry, and the associated mineralogy. The HSs do not simply form coils in acidic or strong electrolyte solutions and elongated structures in dilute alkaline solutions. The macromolecular structural changes of HSs are likely to modify contaminant solubility, biotransformation, and the carbon cycle in soils and sediments.
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