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利用KOC*值判别杭州市地面水中多环芳烃污染来源
引用本文:陈宝梁,朱利中,王静,高彦征,杨坤,沈红心. 利用KOC*值判别杭州市地面水中多环芳烃污染来源[J]. 环境科学, 2004, 25(1): 107-110
作者姓名:陈宝梁  朱利中  王静  高彦征  杨坤  沈红心
作者单位:浙江大学环境科学系,杭州,310028
基金项目:国家自然科学基金重点项目(40031010);浙江省科技计划项目(001103156);浙江省自然科学基金人才项目(RC99032)
摘    要:测定了2002年12月杭州市钱塘江和运河杭州段地面水、底泥和土壤中10种多环芳烃的含量,计算了底泥和土壤中PAHs富集倍数K和有机碳标化表观分配系数KOC*.结果表明,地面水中PAHs总浓度范围为1.104~9.663μg·L-1,底泥中为132.7~7343μg·kg-1(干重),土壤为59.71~219.5μg·kg-1(干重),污染较为严重.钱塘江底泥PAHs的K值随水流而降低,而运河杭州段则增大.钱塘江底泥和土壤的KOC*比值接近1,PAHs主要来自土壤淋溶输入,污染历史不长.运河在城区(如拱宸桥和卖鱼桥)的KKOC*比值远大于1,地面径流输入少,而工业排放输入多,且污染历史较长.

关 键 词:地面水  多环芳烃  污染源判别  有机碳标化表观分配系数KOC*
收稿时间:2003-02-12
修稿时间:2003-04-10

Survey Sources of Polycyclic Aromatic Hydrocarbons in Surface Water of Hangzhou by KOC* Values
CHEN Bao-liang,ZHU Li-zhong,WANG Jing,GAO Yan-zheng,YANG Kun and SHEN Hong-xin. Survey Sources of Polycyclic Aromatic Hydrocarbons in Surface Water of Hangzhou by KOC* Values[J]. Chinese Journal of Environmental Science, 2004, 25(1): 107-110
Authors:CHEN Bao-liang  ZHU Li-zhong  WANG Jing  GAO Yan-zheng  YANG Kun  SHEN Hong-xin
Affiliation:Department of Environmental Science, Zhejiang University, Hangzhou 310028, China.
Abstract:Ten polycyclic aromatic hydrocarbons (PAHs) were simultaneously measured in 9 surface water samples of Qiantang River and Hangzhou Canal in Hangzhou, China, in December of 2002. It was observed that the sum of PAHs concentrations ranged from 1.104 to 9.663 microg x L(-1) in surface water, from 132.7 to 7343 microg x kg(-1) dry sediments, and from 59.71 to 219.5 microg x kg(-1) dry soils. The accumulative coefficients of PAHs in sediments and soils (K) and apparent partition coefficients normalized by solid organic carbon contents (K(OC)*) were calculated. In Hangzhou Canal, K and K(OC)* values in sediments increased with downstream, and ratio of K(OC)* on sediment to K(OC)* on soil were much larger than 1. Those indicated that Hangzhou Canal was heavily polluted by PAHs released from factory wastewater and PAHs in sediment were mainly sources of PAHs in surface water. In Qiantang River, K and K(OC)* values in sediments decreased with the downstream, and the ratio of K(OC)* on sediment to K(OC)* on soil near 1, and ratio fOC of sediment to fOC of soil approximate to 1, which showed that PAHs in Qiantang River were attributed to soil runoff.
Keywords:surface water  PAHs  sources survey  organic carbon normalized apparent partition coefficient
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