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德州引黄灌区主要河流沉积物各形态磷分布研究
引用本文:张芳,常春平,李发东,李静,宋帅,赵广帅,蔡文静.德州引黄灌区主要河流沉积物各形态磷分布研究[J].农业环境保护,2012(11):2223-2229.
作者姓名:张芳  常春平  李发东  李静  宋帅  赵广帅  蔡文静
作者单位:[1]中国科学院地理科学与资源研究所生态系统网络观测与模拟重点实验室,北京100101 [2]河北师范大学资源与环境科学学院,石家庄050091 [3]中国科学院研究生院,北京100049
基金项目:中国科学院“百人计划”项目
摘    要:对河流沉积物中各形态磷(P)的研究有助于认识沉积物中P的行为特征、水-沉积物界面上P的迁移、转化、可利用性以及水体营养状态。以德州引黄灌区为例,采用改进的RuttenbergSEDEX分级连续提取方法,分析了漳卫新河、马颊河和德惠新河表层沉积物中主要赋存形态磷的含量,以期为评价该地区水环境质量,探究水体污染来源以及制定相应的治理措施提供科学依据。结果表明,河流表层沉积物中总磷(TP)的含量为437.4~1197.0mg.kg-1,无机磷(IP)的含量为373.8~1136.4mg.kg-1,占TP的64.3%~98.5%。IP又分为弱吸附态磷(Lsor-P)、铁结合态磷(Fe-P)、自生磷和碎屑磷(Au-P&De-P),含量分别为26.4~415.2mg.kg-1、6.3~331.2mg.kg-1和302.3~563.6mg.kg-1,分别占TP的5.2%~54.3%、0.8%~31.5%、35.7%~80.9%。有机磷(OP)的含量为9.0~413.4mg.kg-1,占TP含量的1.55%~35.68%。三条河流沉积物中不同形态P含量的变化趋势不同,空间变异性大;从上游到下游,漳卫新河底泥中的TP呈下降趋势,马颊河底泥中TP变化幅度不大,德惠新河底泥中TP呈现出先增高后降低的趋势,变化幅度较大。相关分析表明黄河下游引黄灌区沉积物中部分形态P之间存在显著的相关性,表明这些形态的P可能来源相同或者在某些特定的条件下会相互转化。最后,提出了控制P排放来源、加强污水处理、提高农业P的利用效率以及加强相关的研究等建议。

关 键 词:黄河下游  引黄灌区  沉积物  磷含量  磷形态

Phosphorus Fractions in Sediments Along Three Major Rivers of Irrigation Districts of Yellow River in Dezhou City
ZHANG Fang,CHANG Chun-ping,LI Fa-dong,LI Jing,SONG Shuai,ZHAO Guang-shuai,CAI Wen-jing.Phosphorus Fractions in Sediments Along Three Major Rivers of Irrigation Districts of Yellow River in Dezhou City[J].Agro-Environmental Protection,2012(11):2223-2229.
Authors:ZHANG Fang  CHANG Chun-ping  LI Fa-dong  LI Jing  SONG Shuai  ZHAO Guang-shuai  CAI Wen-jing
Institution:1.Key Laboratory of Ecosystem Network Observation and Modeling,Institute of Geographic Sciences and Natural Resources Research,Chinese Academy of Sciences,Beijing 100101,China;2.College of Resource and Environment Sciences,Hebei Normal University,Shijiazhuang 050091,China;3.Graduate University of Chinese Academy of Sciences,Beijing 100049,China)
Abstract:Studies on phosphorus fractions in river sediments is helpful to recognize the behavioral character of P,to understand the migration,transformation,availability of P that on the water-sediment interface,and to master nutritional status of water bodies.As a case study in Dezhouirrigation distric(t115°45'-117°36'E,36°24'-38°0'N)of the Yellow River in China,the concentrations of phosphorus fractions in the sediments along Zhangweixin River,Majia River,and Dehuixin River were determined by the modified sequential extraction method(Ruttenberg SEDEX).It is expected to provide a scientific basis for evaluating the water quality,exploring the phosphorus sources of water pollution,and finding appropriate management actionin this area.The results showed that the concentrations of total phosphorus(TP),inorganic phosphorus(IP),and organic phosphorus(OP)ranged from 437.4 to 1197.0 mg.kg-1,373.8 to 1136.4 mg.kg-1,and 9.0 to 413.4 mg.kg-1,respectively.Sediment samples were characterized by a dominance of the inorganic fraction(64.32%~98.53%).For OP,however,it is 1.55%~ 35.68%.IP was also divided into three fractions:loosely adsorbed phosphorus(Lsor-P),iron-bound phosphorus(Fe-P),authigenic phosphorus and detritalphosphorus(Au-PDe-P)which were mainly associated Au-PDe-P(35.67%~80.89%),Lsor-P and Fe-P accounted for5.21% ~54.27% and 0.77% ~31.54%,respectively.The distribution trends and large spatial variation of phosphorus fractions along three rivers were found.From up to down stream,the concentrations of TP in the Zhangweixin River,Majia River and Dehuixin River showed decreasing trend,smooth variation,and choppy change,respectively.The correlation between some kinds of phosphorus fractions along these rivers were significant,which suggested these fractions of phosphorus should derive from the same sources or transform into each other under certain conditions.Some advises,such as controlling phosphorus drainage sources,setting-up more sewage factories,improving the phosphorus use efficiency,and supporting more relative studies,were suggested.
Keywords:irrigation district of the Yellow River  sediment  concentration of phosphorus  phosphorus fractions
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