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滇池福保湾沉积物磷的形态及其与间隙水磷的关系
  • ISSN号:1003-5427
  • 期刊名称:湖泊科学
  • 时间:0
  • 页码:1393-1397
  • 语言:中文
  • 分类:X524.02[环境科学与工程—环境工程]
  • 作者机构:[1]中国科学院南京地理与湖泊研究所湖泊与环境国家重点实验室,南京210008, [2]中国科学院研究生院,北京100049, [3]西安建筑科技大学,西安710055
  • 相关基金:国家高技术研究发展计划(863)项目(2005AA601010050201)、国家自然科学基金项目(20577053,40601087)和中国科学院知识创新工程项(KZCX3.SW.348)联合资助.
  • 相关项目:浅水湖泊沉积物重金属垂向分布的高分辨研究及其界面源/汇转化规律
中文摘要:

研究了滇池福保湾沉积物中磷的地球化学形态及间隙水中PO4^3- -p含量的垂向分布特征.福保湾沉积物磷形态空间差异大,河口区TP高达(5630.59±424.25)mg/kg,东两沿岸区TP只有200—300mg/kg,无机磷(I-P)是TP的主要部分,占TP的55%-74%,铁/铝结合态磷(Fe/A1.P)是I-P的主要组成部分,约占I-P的90%,不稳定性磷(L-P)含量很低,只占TP含量的0.5%.福保湾沉积物具有极高的Fe/A1-P含量,说明湾内具有很高的内源磷负荷,这与福保湾水体严重富营养化和藻类暴发关系密切.湖湾沉积磷的垂向分布规律较复杂,但基本上是随深度增加而减小,说明福保湾周边区域近几年人类活动作用加强,福保湾污染有加重的趋势在湾内不同区域应用Peeper(渗吸膜式)技术,获得了问隙水中PO4^3- -p的垂向分布特征,PO4^3- -p浓度自上覆水向下层间隙水呈先升后降,反映它们有自间隙水向上覆水扩散的趋势.福保湾间隙水PO4^3- -p浓度同沉积物L-P含量具有显著正相关性(d=0.05),但Fe/A1-P、Ca-P、org-P和TP含量未发现有明显的相关关系

英文摘要:

This paper presents investigations on geochemical species of phosphorus in sediments and vertical distributions of PO4^3- -p in interstitial waters of Fubao Bay in Lake Dianchi. The sediments of Fubao Bay had high TP contents, with the maximum value of (5630.59 ± 424.25)mg/kg. I-P(inorganic phosphorus) was the major part of TP, which was about 55%-74%of TP. Fe/A1-P (P bound to A1, Fe and Mn oxides and hydroxides) was the major part of I-P, which was about 90% of I-E The contents of L-P(labile phosphorus) were very low, which was about 0.5%of TP. The Fe/A1-P contents in sediments were very high, which were highly correlated with high eutrophication phenomenon and algae blooming events in Fubao Bay, implying a strong diffusion trend for sediment phosphorus in Fubao Bay. Vertical distributions of sediment phosphorus species were complicated, exhibiting a little disorder in both increased and decreased trends with the depth. This feature was related to the ecosystem conditions, pollutant discharge and sediment dynamic conditions in Fubao Bay. Peeper technique (in situ dialysis membrane samplers) was used to sample interstitial waters in sediments, and vertical distributions of PO4^3- -p were achieved in the waters. The results showed that concentrations of PO4^3- -p in interstitial waters had general increases followed by decreases with the depth, reflecting a possible diffusion trend for PO4^3- -p fi-om interstitial waters to overlying waters. Regression analyses showed that concentrations of PO4^3- -p in the interstitial waters were positively correlated with L-P contents.

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期刊信息
  • 《湖泊科学》
  • 北大核心期刊(2011版)
  • 主管单位:中国科学院
  • 主办单位:中国科学院南京地理与湖泊研究所 中国海洋湖沼学会
  • 主编:沈吉
  • 地址:南京市北京东路73号
  • 邮编:210008
  • 邮箱:jlakes@niglas.ac.cn
  • 电话:025-86882041 86882040
  • 国际标准刊号:ISSN:1003-5427
  • 国内统一刊号:ISSN:32-1331/P
  • 邮发代号:28-201
  • 获奖情况:
  • 中国科技核心期刊,中国期刊方阵“双效”期刊
  • 国内外数据库收录:
  • 俄罗斯文摘杂志,美国化学文摘(网络版),美国工程索引,美国地质文献预评数据库,美国剑桥科学文摘,美国生物科学数据库,英国动物学记录,日本日本科学技术振兴机构数据库,中国中国科技核心期刊,中国北大核心期刊(2004版),中国北大核心期刊(2008版),中国北大核心期刊(2011版),中国北大核心期刊(2014版)
  • 被引量:16668