State Key Laboratory of Lake Science and Environment, Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences, 73 East Beijing Road, Nanjing 210008, China.
Environ Pollut. 2009 Aug-Sep;157(8-9):2507-13. doi: 10.1016/j.envpol.2009.03.018. Epub 2009 Apr 5.
Organic phosphorus (P) fractions in surface sediments from a large shallow, eutrophic Lake Taihu, China, were extracted with 0.1 M NaOH after pre-treatment of the sediments with a solution composed of 0.1 M EDTA and 2% (w/v) Na(2)S(2)O(4). Composition of organic P in the extracts was then characterized by (31)P nuclear magnetic resonance spectroscopy ((31)P NMR). Several P species, including phosphonates, orthophosphate, orthophosphate monoesters, phospholipids, DNA, pyrophosphate and polyphosphate, were detected in the NaOH extracts. The proportion of extracted organic P to total P in sediments was negatively correlated with total P in the water column, as were the proportions for orthophosphate monoesters and DNA. This implies that the majority of organic P in surface sediments is likely stabilized in some way, and does not directly contribute to the internal loading of P from sediments.
采用 0.1 M EDTA 和 2%(w/v)Na₂S₂O₄ 的混合溶液对沉积物进行预处理后,用 0.1 M NaOH 从中国大浅型富营养化太湖表层沉积物中提取有机磷(P)组分。采用 ³¹P 核磁共振波谱法(³¹P NMR)对提取物中的有机 P 组成进行了表征。在 NaOH 提取物中检测到了几种 P 物质,包括膦酸酯、正磷酸盐、正磷酸盐单酯、磷脂、DNA、焦磷酸盐和多磷酸盐。沉积物中提取的有机 P 与水柱中总 P 的比例与正磷酸盐单酯和 DNA 的比例呈负相关。这意味着表层沉积物中大部分有机 P 可能以某种方式稳定下来,不会直接导致沉积物中 P 的内部负荷增加。