不同水体沉积物中磷的形态分析

屈森虎<sup>1</sup>; 王逊<sup>2</sup>; 陈媛<sup>3</sup>; 张明浩<sup>4</sup>

引用本文:	屈森虎,王逊,陈媛,张明浩.不同水体沉积物中磷的形态分析[J].环境监控与预警,2011,3(05):34-37
	.Different Forms of Phosphorus in Sediment[J].Environmental Monitoring and Forewarning,2011,3(05):34-37

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不同水体沉积物中磷的形态分析
屈森虎¹, 王逊², 陈媛³, 张明浩⁴
1.南京市建邺区环境监测站，江苏南京 210019;2.南京市环境保护科学研究院，江苏南京210013;3.江苏省环境监测中心，江苏南京 210036;4.南京市建邺区环保局，江苏南京 210019

摘要:

磷是生态系统中必不可少的的营养元素，其含量与水体的营养程度密切相关，过剩的磷会导致水体富营养化，使生态平衡遭到破坏。就不同水体沉积物中磷的形态进行了分类综述，归纳总结了不同水体沉积物中磷的形态以及分布特征，并且进一步概述了影响沉积物中磷向水体释放的因素。

关键词: 水体沉积物磷释放

DOI：

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Different Forms of Phosphorus in Sediment

Abstract:

Phosphorus is an essential nutritional element in ecological system, and its concentration is closely related to the content of the nutrient in water. Excess phosphorus can lead to eutrophication, and also can break the ecological balance. This paper discussed the forms of phosphorus in sediments and discussed its different forms and distribution characteristics in sediments. This study also provided an overview of the factors that effected phosphorus release.

Key words: water sediment phosphorus release