洱海沉积物间隙水中溶解有机质的地球化学特性

Geochemical characteristics of dissolved organic matter in the sediment pore water of Erhai Lake

  • 摘要: 对洱海沉积物间隙水中溶解有机质(DOM)含量、紫外可见吸收、荧光以及分子量等的垂直分布特征进行了研究。结果表明,DOC含量在沉积物水界面明显富集,随后急剧下降,6cm处达到最小值,随后呈上升趋势。DOC与吸光度值、荧光发射光谱强度之间具有一定的线性相关关系。DOM的E3/E4值范围在1~6之间,绝大多数在1~35之间。表征DOM中腐殖质来源的指标荧光指数值处于148~159之间,说明DOM以陆源输入为主。此外,洱海沉积物间隙水DOM分子量分布呈多峰分布模式,重均分子量(Mw)值在1462~1953Da之间,数均分子量(Mn)值在547~900Da之间,多分散性系数ρ值在202~305之间。随着沉积深度增大,MwMn有略微的增大趋势,但变化不大。沉积物的氧化还原条件、微生物活动以及铁、锰氧化物等在沉积剖面的差异是控制间隙水中DOM各种地球化学特性的主要因素。

     

    Abstract: We study the DOC concentrations, the UV-Vis absorbance, fluorescence and the molecular weight of the dissolved organic matter in the sediment pore water of Erhai Lake.DOC concentration has a high value at the sediment-water interface, with a sharp decrease within the depth of 6 cm, and, then, increases later.The vertical distributions of a254, a280 and fluo-rescence intensity at Ex=335 nm are in agree with the distribution of DOC.The E3/E4 values range from.to 6 and most of the values are less than 3.5, which means that the DOM in sediment pore water has relatively high humification, aromaticity and molecular weight.f450/500 values range from 1.48 to 1.59, showing the terrestrial nature of the majority of the sediment pore water DOM.Through the HPSEC results, all the sediment pore water DOM show a multi-modal distribution of the molec-ular weight.Weight-average molecular weight (Mw), which ranges from 1462 to 1953 Da, and number-average molecular weight (Mn), which ranges from 547 to 900 Da, vary a little along the depth and mainly have a trend of increase.The poly-dispersity, ρ (the ration of Mw to Mn) ranges from 2.02 to 3.05, which suggests that the pore water DOM resides in a rela-tively wide size distribution.In general, the geochemical characteristics of sediment pore water DOM are attributed to the changes in redox chemistry occurrs as a function of the sediment depth, partial mineralization of particulate organic matter as a result of the biotic or abiotic reduction and the effect of metal oxide through the dissolution and formation process.

     

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