| 沉积物-水界面的生物地球化学作用 |
| |
| 引用本文： | 吴丰昌 万国江. 沉积物-水界面的生物地球化学作用[J]. 地球科学进展, 1996, 11(2): 191-197. DOI: 10.11867/j.issn.1001-8166.1996.02.0191 |
| |
| 作者姓名： | 吴丰昌 万国江 |
| |
| 作者单位： | 中国科学院地球化学研究所环境地球化学国家重点实脸室 贵阳 550002 |
| |
| 基金项目： | 国家自然科学基金项目“云贵高原湖泊沉积地球化学过程及环境信息的提取气”（项目编号:49333040)和“湖泊季节性硫酸盐还原作用和环境效应研究”(项目编号:4950305的资助. |
| |
| 摘 要： | 沉积物－水界面是天然水体在物理、化学和生物特征等方面差异性最显著和负责水体和沉积物之间物质输送和交换的重要边界环境。对沉积物－水界面生物地球化学的定义、研究方法和它在水体微量物质循环中所起的作用、物质迁移方式、典型氧化还原敏感性元素转化反应（Ｃ、Ｏ、Ｎ）、界面扩散通量和表面扩散亚层的意义和估算等进行了讨论。
|
| 关 键 词： | 沉积物—水界面 生物地球化学作用 氧化还原反应 扩散作用 |
| 收稿时间： | 1995-07-03 |
| 修稿时间： | 1995-08-24 |
BIOGEOCHEMICAL PROCESSES AT THE SEDIMENT-WATER INTERFACE |
| |
| Wu Fengchang,Wan Guojiang,Cai Yurong. BIOGEOCHEMICAL PROCESSES AT THE SEDIMENT-WATER INTERFACE[J]. Advances in Earth Sciences, 1996, 11(2): 191-197. DOI: 10.11867/j.issn.1001-8166.1996.02.0191 |
| |
| Authors: | Wu Fengchang Wan Guojiang Cai Yurong |
| |
| Affiliation: | Institute of Geochemistry ,Chinese Academy of Sciences ,Guiyand 550002 |
| |
| Abstract: | Sediment-water interface is an important boundary,the greatest gradient in physics, chemistry and biology in natural water, responsible for transportation and exchange of chemical species between waters and sediments. All chemical processes occuring near the interface were involved in organic matter and micrical organic oxidation indirectly or directly in deep-water and oxic/anoxic interface environment,it’s typical biogeochemical process.Organic oxidation and the resulting redox process is the base of all chemical processes and transformation near the interface.The article discussed research methods,the contribution of interface processes to rare elements; cycling,mobile and transporting mechanisms,transformation of typical redox elements(C,N,O),and significance and calculation of diffusive fluxes and sublayers of the interface. |
| |
| Keywords: | Biogeochemistry Sediment-water interface Redox process Microbiological bacteria Diffusion. |
| 本文献已被 维普 等数据库收录！ |
| 点击此处可从《地球科学进展》浏览原始摘要信息 |
|
点击此处可从《地球科学进展》下载全文 |
