北京市典型城市河流(凉水河)沉积物耗氧污染特征

李延; 单保庆; 唐文忠; 陈静

doi:10.12030/j.cjee.201609081

环境工程学报

北京市典型城市河流(凉水河)沉积物耗氧污染特征

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李延, 单保庆, 唐文忠, 陈静. 北京市典型城市河流(凉水河)沉积物耗氧污染特征[J]. 环境工程学报, 2017, 11(9): 5065-5070. doi: 10.12030/j.cjee.201609081

引用本文:

李延, 单保庆, 唐文忠, 陈静. 北京市典型城市河流(凉水河)沉积物耗氧污染特征[J]. 环境工程学报, 2017, 11(9): 5065-5070. doi: 10.12030/j.cjee.201609081

LI Yan, SHAN Baoqing, TANG Wenzhong, CHEN Jing. Pollution characteristic of sediment oxygen demand in typical urban river (Liangshui River) of Beijing city, China[J]. Chinese Journal of Environmental Engineering, 2017, 11(9): 5065-5070. doi: 10.12030/j.cjee.201609081

Citation:

LI Yan, SHAN Baoqing, TANG Wenzhong, CHEN Jing. Pollution characteristic of sediment oxygen demand in typical urban river (Liangshui River) of Beijing city, China[J]. Chinese Journal of Environmental Engineering, 2017, 11(9): 5065-5070. doi: 10.12030/j.cjee.201609081

北京市典型城市河流(凉水河)沉积物耗氧污染特征

1.
北京市凉水河管理处, 北京 100054
2.
中国科学院生态环境研究中心环境水质学国家重点实验室, 北京 100085
基金项目:
国家水体污染控制与治理科技重大专项（2012ZX07203-006）

环境模拟与污染控制国家重点联合实验室专项经费（15L01ESPC）
中图分类号: X703

Pollution characteristic of sediment oxygen demand in typical urban river (Liangshui River) of Beijing city, China

1.
Liangshui River Management Office of Beijing, Beijing 100054, China
2.
State Key Laboratory of Environmental Aquatic Chemistry, Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences, Beijing 100085, China
Fund Project:

摘要: 针对北运河水系沉积物耗氧污染严重问题，选择凉水河上、中、下游作为研究对象，探讨了沉积物中NH4+-N、TOC、SOD的分布特征，初步判断了沉积物耗氧情况。结果表明凉水河表层沉积物中NH4+-N和TOC含量均较高。其中：NH4+-N在凉水河上游最高，均值为114.38 mg·kg，中游最低，均值为54.06 mg·kg-1；TOC在凉水河上、中、下游依次降低，均值分别为3.64%、3.36%和1.81%。凉水河表层沉积物SOD较高，且变化范围较大，沉积物耗氧污染较为严重。其中：凉水河中游SOD最高，均值为1.012 g·（m2·d）-1；上游最低，均值为0.939 g·（m2·d）-1。
- 城市河流 /
- 沉积物 /
- 沉积物耗氧 /
- 溶解氧
Abstract: Based on oxygen demand pollution in the typical urban rivers of Beiyun River Basin, Liangshui River was selected for this study. The distribution characteristics of NH4+-N, TOC, and sediment oxygen demand (SOD) in the sediments from the upstream, middle and downstream of Liangshui River were investigated. The results showed that the contents of NH4+-N and TOC in the sediment samples were high. NH4+-N contents were higher in the upstream (mean value 114.38 mg·kg-1), and lower in the midstream (mean value 54.06 mg·kg-1).TOC contents were 3.64%, 3.36% and 1.81% in the upstream, middle and downstream of Liangshui River, respectively. SOD in the middle of Liangshui River was highest (mean value 1.012 g·(m2·d)-1), and lowest in the upstream (mean value 0.939 g·(m2·d)-1).
- urban river /
- sediment /
- sediment oxygen demand (SOD) /
- DO

[1]	朱广伟,陈英旭.沉积物中有机质的环境行为研究进展[J]. 湖泊科学, 2001, 13(3):272-279
[2]	MA Z W, CHEN K, YUAN Z W, et al. Ecological risk assessment of heavy metals in surface sediments of six major Chinese freshwater lakes[J]. Journal of Environmental Quality, 2013, 42(2):341-350
[3]	聂新华, 郎印海, 贾永刚. 胶州湾河口沉积物中耗氧有机物的释放研究[J]. 海洋环境科学, 2006, 25(4):11-14
[4]	FU J, ZHAO C P, LUO Y P, et al. Heavy metals in surface sediments of the Jialu River, China:Their relations to environmental factors[J]. Journal of Hazardous Materials, 2014, 270:102-109
[5]	SENER S, DAVRAZ A, KARAGUZEL R. Assessment of trace metal contents in water and bottom sediments from Eğirdir Lake, Turkey[J]. Environment Earth Science, 2014, 71(6):1-13
[6]	蒋新,许士奋,MARTENS D,等. 长江南京段水、悬浮物及沉积物中多氯有毒有机污染物[J]. 中国环境科学, 2000, 20(3):193-197
[7]	谢婷, 张淑娟, 杨瑞强. 偏远高山湖泊沉积物中持久性有机污染物的沉积记录研究[J]. 环境化学, 2014, 33(10):1791-1801
[8]	马晓磊, 徐继荣, 张德民,等. 城市内河强还原性沉积物耗氧及相关因素研究[J]. 环境科学研究, 2010, 23(12):1499-1505
[9]	WALKER R, SNODGRASS W. Model for sediment oxygen demand in lakes[J].Journal of Environmental Engineering, 1986, 112(1):25-43
[10]	BELANGER T V. Benthic oxygen demand in lake Apopka, Flordia[J]. Water Research, 1981, 15(2):267-274
[11]	乔士斌, 林钦. 大鹏澳网箱养殖区沉积物耗氧的初步研究[J]. 南方水产, 2006, 2(3):32-39
[12]	PARR L, MASON C. Causes of low oxygen in a lowland, regulated eutrophic river in Eastern England[J]. Science of Total Environment, 2004, 321(1/2/3):273-286
[13]	HATCHER K J. Sediment oxygen demand:Processes, modeling, and measurement[D]. Athens, Georgia:University of Georgia Institute of Natural Resources, 1986
[14]	ZIADAT A H, BERDANIER B W. Stream depth significance during in-situ sediment oxygen demand measurements in shallow streams[J]. Journal of the American Water Resources Association, 2004, 40(3):631-638
[15]	JOSIAM R M, STEFAN H G. Effect of flow velocity on sediment oxygen demand:Comparison of theory and experiments[J]. Journal of the American Water Resources Association, 1999, 35(2):433-439
[16]	彭斌,黄金田,王资生.沿海滩涂养殖水体中溶解氧的变化及其影响因素[J]. 水生态学杂志, 2008, 29(5):97-99
[17]	郭婧, 荆红卫, 李金香,等. 北运河系地表水近10年来水质变化及影响因素分析[J]. 环境科学, 2012, 33(5):1511-1518
[18]	许晓伟, 刘德文, 车洪军,等. 北运河水环境调查与评价[J]. 海河水利, 2009(2):14-15
[19]	童保铭, 陈添, 徐谦, 等. 北京市北运河系水质有机污染时空变化研究[J]. 首都师范大学学报(自然科学版), 2009, 30(3):56-60
[20]	鲍士旦. 土壤农化分析[M].3版. 北京:中国农业出版社, 2013
[21]	CHAU K W. Field measurements of SOD and sediment nutrient fluxes in a land-locked embayment in Hong Kong[J]. Advances in Environmental Research, 2002, 6(2):135-142
[22]	臧家业, 庞雪辉, 冉祥滨,等. 底泥耗氧研究的主要技术手段及进展[J]. 海洋开发与管理, 2010, 27(11):36-40
[23]	RASMUSSEN H, JORGENSEN B B. Microelectrode studies of seasonal oxygen uptake in a coastal sediment:Role of molecular diffusion[J]. Marine Ecology Progress Series, 1992, 81(3):289-303
[24]	BERG P, RISGAARA P N, RYSGAARD S. Interpretation of measured concentration profiles in sediment pore water[J]. Limnology and Oceanography, 1998, 43(7):1500-1510
[25]	BERG P, RΦY H, JANSSEN F, et al. Oxygen uptake by aquatic sediments measured with a novel non-invasive eddy correlation technique[J]. Marine Ecology Progress, 2003, 261(8):75-83
[26]	BER P, RΦY H, WIBERG P. Eddy correlation flux measurements:The sediment surface area that contributes to the flux[J]. Limnology and Oceanography, 2007, 52(4):1672-1684

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李延, 单保庆, 唐文忠, 陈静. 北京市典型城市河流(凉水河)沉积物耗氧污染特征[J]. 环境工程学报, 2017, 11(9): 5065-5070. doi: 10.12030/j.cjee.201609081

引用本文:

李延, 单保庆, 唐文忠, 陈静. 北京市典型城市河流(凉水河)沉积物耗氧污染特征[J]. 环境工程学报, 2017, 11(9): 5065-5070. doi: 10.12030/j.cjee.201609081

Citation:

北京市典型城市河流(凉水河)沉积物耗氧污染特征

1. 北京市凉水河管理处, 北京 100054
2. 中国科学院生态环境研究中心环境水质学国家重点实验室, 北京 100085

收稿日期: 2016-10-23

基金项目:

国家水体污染控制与治理科技重大专项（2012ZX07203-006）

环境模拟与污染控制国家重点联合实验室专项经费（15L01ESPC）

关键词:

摘要: 针对北运河水系沉积物耗氧污染严重问题，选择凉水河上、中、下游作为研究对象，探讨了沉积物中NH4+-N、TOC、SOD的分布特征，初步判断了沉积物耗氧情况。结果表明凉水河表层沉积物中NH4+-N和TOC含量均较高。其中：NH4+-N在凉水河上游最高，均值为114.38 mg·kg，中游最低，均值为54.06 mg·kg-1；TOC在凉水河上、中、下游依次降低，均值分别为3.64%、3.36%和1.81%。凉水河表层沉积物SOD较高，且变化范围较大，沉积物耗氧污染较为严重。其中：凉水河中游SOD最高，均值为1.012 g·（m2·d）-1；上游最低，均值为0.939 g·（m2·d）-1。

English Abstract

Pollution characteristic of sediment oxygen demand in typical urban river (Liangshui River) of Beijing city, China

1. Liangshui River Management Office of Beijing, Beijing 100054, China
2. State Key Laboratory of Environmental Aquatic Chemistry, Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences, Beijing 100085, China

Received Date: 2016-10-23

Fund Project:

Keywords:

Abstract: Based on oxygen demand pollution in the typical urban rivers of Beiyun River Basin, Liangshui River was selected for this study. The distribution characteristics of NH4+-N, TOC, and sediment oxygen demand (SOD) in the sediments from the upstream, middle and downstream of Liangshui River were investigated. The results showed that the contents of NH4+-N and TOC in the sediment samples were high. NH4+-N contents were higher in the upstream (mean value 114.38 mg·kg-1), and lower in the midstream (mean value 54.06 mg·kg-1).TOC contents were 3.64%, 3.36% and 1.81% in the upstream, middle and downstream of Liangshui River, respectively. SOD in the middle of Liangshui River was highest (mean value 1.012 g·(m2·d)-1), and lowest in the upstream (mean value 0.939 g·(m2·d)-1).