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河流与湖泊沉积物之间的沉积物特征、磷类型及磷释放速率

Sediment characteristics, phosphorus types and phosphorus release rates between river and lake sediments.

作者信息

Kim Lee-Hyung, Choi Euiso, Stenstrom Michael K

机构信息

Department of Civil and Environmental Engineering, 5714 Boelter Hall, University of California, Los Angeles, CA 90095-1593, USA.

出版信息

Chemosphere. 2003 Jan;50(1):53-61. doi: 10.1016/s0045-6535(02)00310-7.

Abstract

The Han river is 469.7 km long with 26219-km2 area watershed, and is the primary drinking water source for the 20 million people that live in Seoul, Kangwon-Do and Kyunggi-Do, Korea. Phosphorus release from sediments impacts water quality, and is endangering the beneficial use of the river. This research measures phosphorus release and predicts future releases from bottom sediments of two tributary areas (Chungpyung Lake (CPL) and Jamsil submerged dam (JSD) area in the Han river). Sediment samples were taken over a 4-year period from four points in the Jamsil dam area and from 92 points in CPL. The sediments were analyzed for total phosphorus, the form of the phosphorus and release rates under different conditions to the water column. Sediment phosphorus distribution from CPL was 3-5% adsorbed-P (Ads-P), 15-20% non-apatite-P (NAI-P), 25-30% apatite-P (A-P) and 45-57% residual-P (R-P). In the JSD area, the phosphorus distribution ranges were 1-3% Ads-P, 22-39% NAI-P, 26-40% A-P and 30-39% R-P. Laboratory experiments showed that phosphorus release rates from 60 to 80 mg/m2 week in JSD area and ranged from 25 to 40 mg/m2 week in CPL sediments.

摘要

汉江全长469.7公里,流域面积26219平方公里,是韩国首尔、江原道和京畿道2000万人口的主要饮用水源。沉积物中的磷释放会影响水质,危及该河流的有益用途。本研究测量了磷的释放,并预测了汉江两个支流区域(清平湖(CPL)和蚕室潜坝(JSD)区域)底部沉积物未来的磷释放情况。在4年时间里,从蚕室坝区域的4个点以及清平湖的92个点采集了沉积物样本。对沉积物进行了总磷、磷的形态以及在不同条件下向水柱的释放速率分析。清平湖沉积物中的磷分布为3 - 5%吸附态磷(Ads - P)、15 - 20%非磷灰石磷(NAI - P)、25 - 30%磷灰石磷(A - P)和45 - 57%残余磷(R - P)。在蚕室潜坝区域,磷的分布范围为1 - 3% Ads - P、22 - 39% NAI - P、26 - 40% A - P和30 - 39% R - P。实验室实验表明,蚕室潜坝区域的磷释放速率为60至80毫克/平方米·周,清平湖沉积物中的释放速率为25至40毫克/平方米·周。

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