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一种用于确定海水中和海洋表层沉积物中磷分布的连续萃取法。

A sequential extraction to determine the distribution of phosphorus in the seawater and marine surface sediment.

作者信息

Aydin Isil, Aydin Firat, Saydut Abdurrahman, Hamamci Candan

机构信息

Dicle University, Science and Art Faculty, Chemistry Department, Diyarbakir, Turkey.

出版信息

J Hazard Mater. 2009 Sep 15;168(2-3):664-9. doi: 10.1016/j.jhazmat.2009.02.095. Epub 2009 Feb 25.

Abstract

The distribution of phosphorus species among environmental compartments (e.g., between water and sediment), significantly affects the bioavailability of these species to organisms. The eastern Mediterranean Sea is one of the most extreme oligotrophic oceanic regions on earth in terms of nutrient concentrations and primary productivity. The paper presents the results of inorganic and organic forms in surface sediment and seawater from NE Mediterranean Sea (Burclar Bay, Erdemli, South Anatolia of Turkey) in May 2007. Speciation of phosphorus in seawater and surface sediment using inductively coupled plasma-atomic emission spectrometer (ICP-AES) has been reported here. The method is based on sequential extractions of the seawater and sediment each releasing four forms of inorganic phosphorus: loosely sorbed phosphorus, phosphorus bound to aluminium (P-Al), phosphorus bound to iron (P-Fe) and phosphorus bound to calcium (P-Ca). The most abundant form of inorganic phosphorus in the seawater and surface sediment is calcium-bound phosphorus. Relative abundances of the remaining phosphorus forms in sediment follow the order: P-Al>P-Fe>loosely bound-P and in seawater follow the order P-Fe>P-Al>loosely bound-P.

摘要

磷在不同环境介质(如水体与沉积物之间)中的分布,显著影响了这些形态的磷对生物体的生物可利用性。就营养盐浓度和初级生产力而言,地中海东部是地球上最极端的贫营养海洋区域之一。本文展示了2007年5月采集自地中海东北部(土耳其南安纳托利亚的布尔克拉湾、埃尔德姆利)表层沉积物和海水中无机磷和有机磷的研究结果。本文报道了使用电感耦合等离子体原子发射光谱仪(ICP-AES)对海水和表层沉积物中磷形态的分析。该方法基于对海水和沉积物的连续萃取,每种样品均释放出四种无机磷形态:松散吸附态磷、铝结合态磷(P-Al)、铁结合态磷(P-Fe)和钙结合态磷(P-Ca)。海水中和表层沉积物中最丰富的无机磷形态是钙结合态磷。沉积物中其余磷形态的相对丰度顺序为:P-Al>P-Fe>松散结合态-P,海水中的顺序为P-Fe>P-Al>松散结合态-P。

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