必须声明标量变量 "@Script_ID"。 潜流带生物地球化学特征研究进展-《地球科学与环境学报》
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[1]苏小四,师亚坤,董维红*,等.潜流带生物地球化学特征研究进展[J].地球科学与环境学报,2019,41(03):337-351.
 SU Xiao-si,SHI Ya-kun,DONG Wei-hong*,et al.Review on Biogeochemical Characteristics of Hyporheic Zone[J].Journal of Earth Sciences and Environment,2019,41(03):337-351.
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《地球科学与环境学报》[ISSN:1672-6561/CN:61-1423/P]

卷:
第41卷
期数:
2019年第03期
页码:
337-351
栏目:
水资源与环境
出版日期:
2019-05-15

文章信息/Info

Title:
Review on Biogeochemical Characteristics of Hyporheic Zone
文章编号:
1672-6561(2019)03-0337-15
作者:
苏小四12师亚坤13董维红12*杨国强4王璜5
(1.吉林大学 水资源与环境研究所,吉林 长春 130021; 2.吉林大学 建设工程学院,吉林 长春 130021; 3.吉林大学 新能源与环境学院,吉林 长春 130021; 4.中国地质调查局南京地质调查中心,江苏 南京 210016; 5.中国地质调查局,北京 100037)
Author(s):
SU Xiao-si12 SHI Ya-kun13 DONG Wei-hong12* YANG Guo-qiang4 WANG Huang5
(1. Institute of Water Resources and Environment, Jilin University, Changchun 130021, Jilin, China; 2. Construction Engineering College, Jilin University, Changchun 130021, Jilin, China; 3. New Energy and Environment College, Jilin University, Changchun 130021, Jilin, China; 4. Nanjing Center, China Geological Survey, Nanjing 210016, Jiangsu, China; 5. China Geological Survey, Beijing 100037, China)
关键词:
潜流带 潜流交换量 生物地球化学 氧化-还原反应 数值模拟 原位监测 环境指标
Keywords:
hyporheic zone hyporheic exchange flux biogeochemistry oxidation-reduction reaction numerical modeling in-situ monitoring environmental indicator
分类号:
P641
DOI:
-
文献标志码:
A
摘要:
潜流带(即地表水-地下水交互作用带)是位于地表水和地下水之间发生物质和能量交换的,具有物理、化学、生物梯度的饱和含水带。潜流带内发生着强烈的生物地球化学过程,在改善水环境质量和维持水生态系统稳定中发挥着重要作用。潜流带生物地球化学特征主要受河床沉积物结构特征、水文特征、环境特征、生物群落格局、物质输入等因素的影响,潜流带内C、N、P元素以及有毒金属元素(Fe、Mn、As、Hg等)会发生氧化-还原、吸附与解吸、沉淀与溶解、生物催化等生物地球化学过程。原位监测、数值模拟、原位培养和地球物理探测等技术是潜流带中生物地球化学过程研究中常用的研究手段。未来针对潜流带的研究可以从监测和数值模拟技术、河床沉积物变化特征以及微生物生态系统的结构和功能等方面进一步开展。
Abstract:
The hyporheic zone, which exchanges matter and energy between surface water and groundwater, is a saturated zone with physical, chemical and biological gradients. Strong biogeochemical processes occur in the hyporheic zone, which plays an important role in improving the quality of the water environment and maintaining the stability of the water ecosystem. Because the biogeochemical characteristics of the hyporheic zone are mainly affected by factors such as structural characteristics of riverbed sediment, hydrological characteristics, environmental characteristics, biological communities patterns, and material input, the C, N, P and toxic metal elements(Fe, Mn, As, Hg, etc.)in the hyporheic zone mainly undergo biogeochemical processes such as oxidation-reduction, adsorption and desorption, precipitation and dissolution, and biocatalysis. In addition, the monitoring of biogeochemical processes in the hyporheic zone can utilize techniques such as in-situ monitoring, numerical simulation, in-situ culture, and geophysical exploration. The research on the hyporheic zone will be further carried out in terms of monitoring and numerical simulation techniques, characteristics of riverbed sediment changes, and the structure and function of microbial ecosystems.

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备注/Memo:
收稿日期:2018-12-19; 修回日期:2019-02-14 投稿网址:http://jese.chd.edu.cn/
基金项目:国家自然科学基金项目(41073054,41877178)
作者简介:苏小四(1971-),男,安徽巢湖人,教授,博士研究生导师,工学博士,博士后,E-mail:suxiaosi@jlu.edu.cn。
*通讯作者:董维红(1974-),女,河北保定人,教授,博士研究生导师,工学博士,E-mail:dongweihong@jlu.edu.cn。
更新日期/Last Update: 2019-05-20