河岸带潜流层动态过程与生态修复

夏继红; 陈永明; 王为木; 韩玉玲; 刘海洋; 胡玲

高级搜索

全国中文核心期刊
中国科技核心期刊
美国工程索引（EI）收录期刊

留言板

尊敬的读者、作者、审稿人, 关于本刊的投稿、审稿、编辑和出版的任何问题, 您可以本页添加留言。我们将尽快给您答复。谢谢您的支持!

姓名
邮箱
手机号码
标题
留言内容
验证码

河岸带潜流层动态过程与生态修复

夏继红, 陈永明, 王为木, 韩玉玲, 刘海洋, 胡玲

文章导航 > 水科学进展 > 2013 > 24(4): 589-597

夏继红, 陈永明, 王为木, 韩玉玲, 刘海洋, 胡玲. 河岸带潜流层动态过程与生态修复[J]. 水科学进展, 2013, 24(4): 589-597.

引用本文:

夏继红, 陈永明, 王为木, 韩玉玲, 刘海洋, 胡玲. 河岸带潜流层动态过程与生态修复[J]. 水科学进展, 2013, 24(4): 589-597.

XIA Jihong, CHEN Yongming, WANG Weimu, HAN Yuling, LIU Haiyang, HU Ling. Dynamic processes and ecological restoration of hyporheic layer in riparian zone[J]. Advances in Water Science, 2013, 24(4): 589-597.

Citation:

XIA Jihong, CHEN Yongming, WANG Weimu, HAN Yuling, LIU Haiyang, HU Ling. Dynamic processes and ecological restoration of hyporheic layer in riparian zone[J]. Advances in Water Science, 2013, 24(4): 589-597.

河岸带潜流层动态过程与生态修复

1.
河海大学水利水电学院, 江苏南京 210098;
2.
National Center for Computational Hydroscience and Engineering, the University of Mississippi, MS Oxford 38655 USA;
3.
浙江省河道管理总站, 浙江杭州 310009

基金项目: 国家自然科学基金资助项目(40871050);浙江省水利科技重大项目(RA1104)

详细信息

作者简介:
夏继红(1970-),男,江苏如皋人,副教授,博士,主要从事生态河岸带及河流生态修复研究。E-mail:syjhxia@hhu.edu.cn

中图分类号: TV122

Dynamic processes and ecological restoration of hyporheic layer in riparian zone

1.
College of Water Conservancy and Hydropower, Hohai University, Nanjing 210098, China;
2.
National Center for Computational Hydroscience and Engineering, University of Mississippi, MS Oxford 38655, USA;
3.
Department of River Management of Zhejiang Province, Hangzhou 310009, China

Funds: The study is financially supported by the National Natural Science Foundation of China (No.40871050).

摘要: 河岸带潜流层是河岸带内地表水与地下水相互作用的生态交错带,在水文地理学、生态学、环境学上含义不尽相同。河岸带潜流层具有复杂的垂向、横向、纵向结构特征,其边缘效应显著,表现为泥沙、水流、生物、环境化学因子之间的复杂动态过程,主要包括水动力动态过程、生态学过程、溶质循环与化学过程等。水动力动态过程是驱动条件,氧气浓度是生态过程、溶质循环和化学过程的决定性因素。在各动态过程的驱动下,河岸带潜流层具有调蓄洪水、削减污染、净化缓冲环境和提供适宜栖息地等功能。针对河岸带潜流层功能退化的问题,需开展健康诊断,明确致病机理,实施适宜的生态修复。未来中国在开展河岸带潜流层研究时,应根据中国河岸带特点,采用示踪试验、数值模拟等方法,集成GIS等现代技术手段,研究多尺度下,水文条件、地形变化、土壤渗透系数、河岸带建设方式、植被分布等对河岸带潜流层水文、热传导、生化、生态等的影响机制,准确界定河岸带潜流层区域范围,制定适宜的生态修复策略。
- 河岸带 /
- 潜流 /
- 潜流生物 /
- 边缘效应 /
- 生态修复
Abstract: Hyporheic layer of riparian zone is an active transition zone and ecotone between river and groundwater in riparian zone, which can be denoted respectively from hydrogeography, ecology and environment. Due to its unique structure properties in vertical, lateral and longitudinal directions, hyporheic layer of riparian zone was characterized to have some edge-effects and dynamic processes, including flow dynamics, ecological and chemical processes, which were driven by interactions among sediments, flow, communities, organic matters, solutes and environmental factors. As the three dynamic processes have affected each other and ecological and chemical processes have depended on flow dynamics driving and oxygen concentration, it has resulted that hyporheic layer in riparian zone could have stored floods and supplied suitable habitats and removed pollution. However, some of these functions were being weakened due to human and natural actions. In order to conserve the ecological balance and keep the sustainable development in riparian zone, it should be necessary to diagnose health status and verify weakening mechanism and practice ecological restoration. In future, according to the complex properties of riparian zones in our countries, it should be very important to investigate the responses of the hydrological, heat transportation, biochemical and ecological mechanisms to variation of hydrology, geomorphology, permeability, vegetation and riparian construction, and quantify the range of hyporheic layer and design the ecological restoration.
- riparian zone /
- hyporheic /
- hyporheos /
- edge effect /
- ecological restoration

[1]	夏继红, 窦传彬, 蔡旺炜, 曾灼, 余根听. 河岸带蜿蜒性与植被密度对潜流驻留时间的复合效应 . 水科学进展, 2020, 31(3): 433-440. doi: 10.14042/j.cnki.32.1309.2020.03.013
[2]	陈孝兵, 郑春阳, 袁越. 河床沉积物非均质性影响下的潜流交换数值模拟 . 水科学进展, 2019, 30(2): 220-229. doi: 10.14042/j.cnki.32.1309.2019.02.007
[3]	任杰, 程嘉强, 杨杰, 程琳. 潜流交换温度示踪方法研究进展 . 水科学进展, 2018, 29(4): 597-606. doi: 10.14042/j.cnki.32.1309.2018.04.016
[4]	高建平, 潘俊奎, 谢义昌. 生物滞留带结构层参数对道路径流滞蓄效应影响 . 水科学进展, 2017, 28(5): 702-711. doi: 10.14042/j.cnki.32.1309.2017.05.007
[5]	刘东升, 赵坚, 吕辉. 大坝下游河岸带冬夏季水热交换特征对比 . 水科学进展, 2017, 28(1): 124-132. doi: 10.14042/j.cnki.32.1309.2017.01.014
[6]	钱进, 沈蒙蒙, 王沛芳, 王超, 侯俊, 李昆, 刘晶晶. 河岸带土壤磷素空间分布及其对水文过程响应 . 水科学进展, 2017, 28(1): 41-48. doi: 10.14042/j.cnki.32.1309.2017.01.005
[7]	李英玉, 赵坚, 吕辉, 陈斌. 河岸带潜流层温度示踪流速计算方法 . 水科学进展, 2016, 27(3): 423-429. doi: 10.14042/j.cnki.32.1309.2016.03.010
[8]	于靖, 张华. 城市小型河流水动力弥散和潜流交换过程 . 水科学进展, 2015, 26(5): 714-721. doi: 10.14042/j.cnki.32.1309.2015.05.013
[9]	张维, 唐翔宇, 鲜青松. 紫色土坡地泥岩裂隙潜流中的胶体迁移 . 水科学进展, 2015, 26(4): 543-549. doi: 10.14042/j.cnki.32.1309.2015.04.011
[10]	陈孝兵, 赵坚, 李英玉, 陈力. 床面形态驱动下潜流交换试验 . 水科学进展, 2014, 25(6): 835-841.
[11]	林俊强, 严忠民, 夏继红. 弯曲河岸侧向潜流交换试验 . 水科学进展, 2013, 24(1): 118-124.
[12]	孙艳伟, 王文川, 魏晓妹, POMEROY C A, 王富强. 城市化生态水文效应 . 水科学进展, 2012, 23(4): 569-574. doi: CNKI:32.1309.P.20120614.2251.013
[13]	鲁程鹏, 束龙仓, 陈洵洪. 河床地形影响潜流交换作用的数值分析 . 水科学进展, 2012, 23(6): 789-795. doi: CNKI: 32.1309.P.20121101.1759.015
[14]	钱进, 王超, 王沛芳, 侯俊, 艾小榆. 河岸带表土层氮素非饱和入渗运移规律模拟 . 水科学进展, 2011, 22(4): 568-573.
[15]	段学花, 王兆印. 生物栖息地隔离对河流生态影响的试验研究 . 水科学进展, 2009, 20(1): 86-91.
[16]	金光球, 李凌. 河流中潜流交换研究进展 . 水科学进展, 2008, 19(2): 285-293.
[17]	田伟君, 王超, 翟金波, 董洁. 入湖河道生态修复工程对水流流速的影响研究 . 水科学进展, 2006, 17(4): 502-506.
[18]	陈锦年, 吕新艳, 胡敦欣. 赤道太平洋潜流变化特征及其与异常海温东传 . 水科学进展, 2005, 16(6): 792-798.
[19]	夏继红, 严忠民, 蒋传丰. 河岸带生态系统综合评价指标体系研究 . 水科学进展, 2005, 16(3): 345-348.
[20]	肖羽堂, 许建华, 吴鸣. 天然水温对生物修复污染水源除NH₄⁺-N效果的影响研究 . 水科学进展, 2002, 13(2): 201-205.

点击查看大图

计量

文章访问数: 6
HTML全文浏览量: 3
PDF下载量: 1161
被引次数: 0

河岸带潜流层动态过程与生态修复

1. 河海大学水利水电学院, 江苏南京 210098;

2. National Center for Computational Hydroscience and Engineering, the University of Mississippi, MS Oxford 38655 USA;

3. 浙江省河道管理总站, 浙江杭州 310009

基金项目: 国家自然科学基金资助项目(40871050);浙江省水利科技重大项目(RA1104)

作者简介:
夏继红(1970-),男,江苏如皋人,副教授,博士,主要从事生态河岸带及河流生态修复研究。E-mail:syjhxia@hhu.edu.cn

收稿日期: 2012-08-07
刊出日期: 2013-07-25

中图分类号: TV122

关键词:

河岸带 /

潜流 /

潜流生物 /

边缘效应 /

生态修复

摘要: 河岸带潜流层是河岸带内地表水与地下水相互作用的生态交错带,在水文地理学、生态学、环境学上含义不尽相同。河岸带潜流层具有复杂的垂向、横向、纵向结构特征,其边缘效应显著,表现为泥沙、水流、生物、环境化学因子之间的复杂动态过程,主要包括水动力动态过程、生态学过程、溶质循环与化学过程等。水动力动态过程是驱动条件,氧气浓度是生态过程、溶质循环和化学过程的决定性因素。在各动态过程的驱动下,河岸带潜流层具有调蓄洪水、削减污染、净化缓冲环境和提供适宜栖息地等功能。针对河岸带潜流层功能退化的问题,需开展健康诊断,明确致病机理,实施适宜的生态修复。未来中国在开展河岸带潜流层研究时,应根据中国河岸带特点,采用示踪试验、数值模拟等方法,集成GIS等现代技术手段,研究多尺度下,水文条件、地形变化、土壤渗透系数、河岸带建设方式、植被分布等对河岸带潜流层水文、热传导、生化、生态等的影响机制,准确界定河岸带潜流层区域范围,制定适宜的生态修复策略。

English Abstract

Dynamic processes and ecological restoration of hyporheic layer in riparian zone

1. College of Water Conservancy and Hydropower, Hohai University, Nanjing 210098, China;

2. National Center for Computational Hydroscience and Engineering, University of Mississippi, MS Oxford 38655, USA;

3. Department of River Management of Zhejiang Province, Hangzhou 310009, China

Funds: The study is financially supported by the National Natural Science Foundation of China (No.40871050).

Received Date: 2012-08-07
Publish Date: 2013-07-25

Keywords:

Abstract: Hyporheic layer of riparian zone is an active transition zone and ecotone between river and groundwater in riparian zone, which can be denoted respectively from hydrogeography, ecology and environment. Due to its unique structure properties in vertical, lateral and longitudinal directions, hyporheic layer of riparian zone was characterized to have some edge-effects and dynamic processes, including flow dynamics, ecological and chemical processes, which were driven by interactions among sediments, flow, communities, organic matters, solutes and environmental factors. As the three dynamic processes have affected each other and ecological and chemical processes have depended on flow dynamics driving and oxygen concentration, it has resulted that hyporheic layer in riparian zone could have stored floods and supplied suitable habitats and removed pollution. However, some of these functions were being weakened due to human and natural actions. In order to conserve the ecological balance and keep the sustainable development in riparian zone, it should be necessary to diagnose health status and verify weakening mechanism and practice ecological restoration. In future, according to the complex properties of riparian zones in our countries, it should be very important to investigate the responses of the hydrological, heat transportation, biochemical and ecological mechanisms to variation of hydrology, geomorphology, permeability, vegetation and riparian construction, and quantify the range of hyporheic layer and design the ecological restoration.

夏继红, 陈永明, 王为木, 韩玉玲, 刘海洋, 胡玲. 河岸带潜流层动态过程与生态修复[J]. 水科学进展, 2013, 24(4): 589-597.

引用本文:

夏继红, 陈永明, 王为木, 韩玉玲, 刘海洋, 胡玲. 河岸带潜流层动态过程与生态修复[J]. 水科学进展, 2013, 24(4): 589-597.

Citation:

全文HTML

下载: 全尺寸图片幻灯片

返回文章

用微信扫码二维码

分享至好友和朋友圈

留言板

河岸带潜流层动态过程与生态修复

作者简介: 夏继红(1970-),男,江苏如皋人,副教授,博士,主要从事生态河岸带及河流生态修复研究。E-mail:syjhxia@hhu.edu.cn

Dynamic processes and ecological restoration of hyporheic layer in riparian zone

计量

出版历程

河岸带潜流层动态过程与生态修复

1. 河海大学水利水电学院, 江苏南京 210098; 2. National Center for Computational Hydroscience and Engineering, the University of Mississippi, MS Oxford 38655 USA; 3. 浙江省河道管理总站, 浙江杭州 310009

作者简介: 夏继红(1970-),男,江苏如皋人,副教授,博士,主要从事生态河岸带及河流生态修复研究。E-mail:syjhxia@hhu.edu.cn

English Abstract

Dynamic processes and ecological restoration of hyporheic layer in riparian zone

1. College of Water Conservancy and Hydropower, Hohai University, Nanjing 210098, China; 2. National Center for Computational Hydroscience and Engineering, University of Mississippi, MS Oxford 38655, USA; 3. Department of River Management of Zhejiang Province, Hangzhou 310009, China

全文HTML

目录

作者简介:
夏继红(1970-),男,江苏如皋人,副教授,博士,主要从事生态河岸带及河流生态修复研究。E-mail:syjhxia@hhu.edu.cn

1. 河海大学水利水电学院, 江苏南京 210098;

2. National Center for Computational Hydroscience and Engineering, the University of Mississippi, MS Oxford 38655 USA;

3. 浙江省河道管理总站, 浙江杭州 310009

作者简介:
夏继红(1970-),男,江苏如皋人,副教授,博士,主要从事生态河岸带及河流生态修复研究。E-mail:syjhxia@hhu.edu.cn

1. College of Water Conservancy and Hydropower, Hohai University, Nanjing 210098, China;

2. National Center for Computational Hydroscience and Engineering, University of Mississippi, MS Oxford 38655, USA;

3. Department of River Management of Zhejiang Province, Hangzhou 310009, China