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Characteristics, distribution and ecological risk assessment of phosphorus in surface sediments from different ecosystems in Eastern China: A P-31-nuclear magnetic resonance study

机译:中国东部不同生态系统表层沉积物中磷的特征,分布及生态风险评估:P-31核磁共振研究

摘要

Surface sediments in different ecosystems (lake, river, reservoir, estuary and wetland) in Eastern China were extracted with NaOH-EDTA, and the extracts were analyzed by P-31-NMR to reveal the phosphorus (P) species distribution. The P release risk was also assessed by sorption experiments. The river sediments accumulated significant amounts of P compared with other sediments. The organic phosphorus (Po) concentration in the estuarine sediment was lower than that in other sediments. Two P compounds classes (phon-P and mono-P) and five P compounds were detected in the sediments. Ortho-P (83.3-97.6%) was the dominant P compounds and mono-P (1.1-18.0%) were the dominant Po compounds classes, while smaller amounts of DNA-P (0-4.1%), pyro-P (0-4.0%) and lipid-P (0-0.8%) were found in the surface sediment. Poly-P and phon-P were detected only in site 11 (wetland), site 10 (wetland) and 11, respectively. The ERI values, as a measure of eutrophication risk, were different in the various sediments, being greater than 25% in sites 1 (river), 3 (estuary) and 4 (estuary), and with values of 26, 59 and 83%, respectively. The Xm and ERI values fitted a power function (RXm-ERI = 0.89, p0.01) and a positive correlation between Xm and OM in the sediment (RXm-OM = 0.84, p0.01) indicated that the chemical-physical conditions play a vital role in controlling P sorption and desorption. (C) 2014 Elsevier B.V. All rights reserved.
机译:用NaOH-EDTA提取中国东部不同生态系统(湖泊,河流,水库,河口和湿地)的表层沉积物,并通过P-31-NMR分析提取物,揭示磷(P)的物种分布。还通过吸附实验评估了磷释放的风险。与其他沉积物相比,河流沉积物中积累了大量的P。河口沉积物中的有机磷(Po)浓度低于其他沉积物中。在沉积物中检测到2种P化合物类别(phon-P和mono-P)和5种P化合物。主要的P化合物为Ortho-P(83.3-97.6%),主要的Po化合物为mono-P(1.1-18.0%),而较少的DNA-P(0-4.1%),pyro-P(0 -4.0%)和脂质-P(0-0.8%)被发现在表面沉积物中。仅在站点11(湿地),站点10(湿地)和11中分别检测到Poly-P和phon-P。不同沉积物的ERI值(作为富营养化风险的度量标准)不同,在站点1(河流),站点3(河口)和站点4(河口)大于25%,分别为26、59和83% , 分别。 Xm和ERI值符合幂函数(RXm-ERI = 0.89,p <0.01),并且沉积物中Xm和OM之间呈正相关关系(RXm-OM = 0.84,p <0.01)表明化学物理条件在起作用在控制磷的吸附和解吸中起着至关重要的作用。 (C)2014 Elsevier B.V.保留所有权利。

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