Phosphorus(P) species in surface sediments from a shallow,hypertrophic lake,Lake Dianchi,China,were investigated by P fractionation and ^(31)P nuclear magnetic resonance(NMR) spectroscopy during a regional algal bloom.In addition,their potential contributions to the overlying water were also evaluated.Labile fractions of P extracted by NH_4C1,bicarbonate dithionite and NaOH ranged from 340.6 to 1,725.8 mg kg^(-1),accounting for20.5%-67.2%of the total P.A two-step extraction method refinement of P recovery was performed before the^(31)P NMR analysis.Recovery rates of sedimentary TP and organic P,by combining EDTA pretreatment and NaOH or mixed reagents,ranged from 31.8%to 69.3%and from19.8%to 51.7%.^(31)P NMR results showed that ortho-P and monoester-P were the most abundant P components in the sediment extractable P of sediments,followed by diester-P and pyro-P.Spatial distribution of the sum of ortho-P,diester-P and pyro-P detected by P NMR corresponded well with the labile P concentration determined by fractionation.Both exhibited a significant positive correlation with the total P in the water column,suggesting that internal loading may be an important source of P for the lake ecosystem.Biogenic P other than ortho-P may contribute to phytoplankton growth,with the relative proportion being 4.4%-18.7%.The release of labile P fractions fueled algal bloom,and the decay of organic matter,following the bloom events,consumed oxygen and elevated the pH value.This co-dependence might lead to a vicious cycle.Transformation mechanisms of various P species remain ambiguous and are worthy of further investigation.
The distribution characteristics of phosphorus （P） forms in the sediment profile of Lake Erhai, in southwestern China has been investigated by sequential extraction and 31p nuclear magnetic resonance spectroscopy （NMR） of NaOH extracts to understand P dynamics and its potential contribution to lake eutrophication. Contents of P fractions varied in the order of NH4C1 extracted P （NH4C1- P） 〈 bicarbonate-dithionite extracted P （BD-P） 〈 HC1-P, Residual-P 〈 NaOH extracted P （NaOH-P）. The highly available NH4C1-P represented less than 1% of total P （TP）. BD-P and NaOH extracted reactive P （NaOH-rP） averaged 39%, while the ratio of Fe/P was higher than 15, indicating low P release from the sediments under permanent oxic condition. The less bio-available HC1-P, NaOH extracted nonreactive P （NaOH-nrP） and residual-P contributed 61% of TP. Regression analysis revealed that BD-P, NaOH-rP and HC1-P were positively correlated with the contents of Fe and Mn, A1 and Fe, and Ca, respectively. The investigation of P compound groups in NaOH extracts by 31p NMR showed that ortho-P and monoester-P were the largest two constituents of the P pool, followed by diester-P, phosphonate and pyro-P. A comparison of vertical variations of P groups in the sediment profile suggested that these compounds were involved in the P recycling to different extents in Lake Erhai. In particular, the lake exhibits high potential for labile P release from the surface sediments, which should be taken into consideration even after the outsourced P runoff ceased.
磷是地表水体中的关键性营养盐,在水生生态系统的物质循环与能量流动方面发挥着重要作用,研究水体中磷的来源、转化与归趋对于了解水环境的演变过程与科学保护具有重要意义.近年来,磷酸盐氧同位素(δ18 O P)技术已逐渐应用于淡水环境中磷的来源示踪与生物地球化学循环研究,其样品前处理主要沿用海水方法体系.相比而言,淡水样品中PO 3-4浓度通常较低,有机质和干扰离子含量却较高,复杂的样品前处理过程极大地制约了δ18 O P分析在淡水环境体系的广泛应用.为此,本研究针对现有海水样品δ18 O P前处理方法在地表淡水环境的适用性加以检验,并进行了三点优化改进:①将MAGIC沉淀步骤使用的MgCl 2替换为Mg(NO 3)2,避免了Cl-的干扰,减少AgCl杂质的生成;②调节生成Ag3PO4溶液pH值为8.0,保证Ag3PO4沉淀快速完全;③对Ag3PO4沉淀过程采用避光处理,降低了AgNO 3及Ag3PO4可能的光解影响,提高了Ag3PO4的纯度,使δ18 O P的测试结果更为准确.本改进方法为后续利用δ18 O P技术深入探究淡水环境中磷的生物地球化学循环与生态环境效应提供了有益的方法借鉴.
