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干湿交替对南四湖潮间带有机磷动态和沉积物特征的影响。

Effects of wet-dry alternation on organic phosphorus dynamics and sediment characteristics in the intertidal zone of Nansi Lake.

机构信息

School of Municipal and Environmental Engineering, Shandong Jianzhu University, Jinan 250101, China; Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences, Beijing 100085, China.

School of Municipal and Environmental Engineering, Shandong Jianzhu University, Jinan 250101, China.

出版信息

Ecotoxicol Environ Saf. 2024 Aug;281:116668. doi: 10.1016/j.ecoenv.2024.116668. Epub 2024 Jul 3.

Abstract

The study of the fractions and distribution characteristics of organic phosphorus in the sediment of the water level fluctuating zone of Nansi Lake is conducive to revealing the transformation of phosphorus in the lake, and has important scientific significance for controlling the eutrophication of Nansi Lake. Based on the sediment of the water level fluctuation zone of Nansi Lake. The improved Hedley continuous grading extraction, ultraviolet-visible spectroscopy and three-dimensional fluorescence spectroscope were used to characterize the structural characteristics and stability of organic molecules in the sediment, and to reflect the differences in the structure and stability of organophosphate in the water level fluctuating zone. Principal component analysis (PCA), Redundancy analysis (RDA) and correlation heat map analysis were used to analyze the correlation between phosphorus and physicochemical index. The results showed that the alternation between wet-dry conditions was more favorable for the release of phosphorus from sediment, compared to continuous inundation conditions. Moreover, the higher the frequency of wet-dry alternations, the greater the release of phosphorus in different forms from the sediment. Wet-dry alternation resulted in a reduction of substituent on the aromatic rings of sediment DOM (dissolved organic matter), and the continuous drying would increase the molecular weight and humidification degree of DOM in the sediment. Correlation analysis showed that NaOH-P content in sediment was significantly negatively correlated with TP, IP, OP and various organophosphorus forms, indicating a close transformation relationship between phosphorus forms in sediment. The results can provide a scientific basis for controlling the release of endogenous phosphorus and the risk of eutrophication in Nansi Lake.

摘要

研究南四湖消落带沉积物中有机磷的赋存形态及分布特征,有利于揭示湖泊磷的形态转化规律,对于控制南四湖富营养化具有重要的科学意义。本研究以南四湖消落带沉积物为研究对象,采用改进的 Hedley 连续分级提取法、紫外-可见分光光度法和三维荧光光谱法,对沉积物中有机分子的结构特征及稳定性进行了表征,反映了不同淹水条件下消落带有机磷的结构及稳定性差异,运用主成分分析(PCA)、冗余分析(RDA)和相关性热图分析等方法,分析了磷与理化指标的相关性。结果表明,干湿交替条件更有利于磷从沉积物中释放,相比于连续淹水条件。并且,干湿交替频率越高,沉积物中不同形态磷的释放量越大。干湿交替导致沉积物 DOM(溶解性有机质)芳香环上取代基减少,连续干燥会增加沉积物中 DOM 的分子量和湿润度。相关性分析表明,沉积物中 NaOH-P 含量与 TP、IP、OP 和各种有机磷形态呈显著负相关,表明了沉积物中磷形态之间存在密切的转化关系。研究结果可为控制南四湖内源磷释放和富营养化风险提供科学依据。

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