基于多级表征的杞麓湖水体有机质粒径分异与季节动态研究

Study on size differentiation and seasonal dynamics of aquatic organic matter in Qilu Lake based on multi-level characterization

  • 摘要: 湖泊水体有机质在全球碳循环中扮演关键角色,尤其在高富营养化水体中,其宏观分布与微观组成的关联机制尚不明确。以重度富营养化高原封闭湖泊杞麓湖为研究对象,通过物理粒径分级-三维荧光-高分辨质谱联用技术,解析有机质粒径分布、季节动态及分子组成,揭示杞麓湖有机质从宏观分布到分子组成的迁移规律。结果表明:杞麓湖水体中有机质以颗粒态为主,100~250 μm粒径区间的有机质浓度最高,对化学需氧量(CODCr)贡献率达15.4%;枯水期以粒径大于10 μm的颗粒态有机质为主导,丰水期转向粒径0.05~5 μm的组分为主。枯水期风力扰动使底泥中较大粒径的颗粒再悬浮,10~250 μm组分腐殖化程度高,而丰水期雨热同期引起藻类暴发,小于0.05 μm组分的溶解性有机质(DOM)微生物源特征增强。PARAFAC解析出DOM中类蛋白组分占优势,高分辨质谱技术证实小于0.45 μm的DOM以木质素类化合物为主,小于0.05 μm的DOM相较大于0.05 μm区间含硫化合物比例增加,推测分别是10年内沉水植物大量死亡残留以及换水周期长导致的入湖农业面源污染累积所致。杞麓湖水体有机质组成具有粒径分异与季节动态特征,受陆源输入及内源微生物活动共同影响,与湖泊封闭性、农业面源污染及藻华高发相关。研究从杞麓湖有机质的粒径分级入手,揭示其从生态系统尺度到分子水平的迁移规律,结果可为理解富营养化高原湖泊碳循环提供参考。

     

    Abstract: Organic matter in lake water plays a key role in the global carbon cycle, especially in highly eutrophic water bodies, yet the linkage between its macroscopic distribution and molecular composition remains unclear. Taking Lake Qilu, a severely eutrophic enclosed plateau lake, as a case study, we employed a combined approach of physical particle size fractionation, three-dimensional fluorescence spectroscopy, and high-resolution mass spectrometry to analyze the particle size distribution, seasonal dynamics, and molecular composition of organic matter. The study revealed the transport patterns of organic matter from macroscopic distribution to molecular composition in Lake Qilu. The results showed that particulate organic matter dominated the lake water, with the highest concentration in the 100-250 μm size fraction, contributing 15.4% to the chemical oxygen demand (CODCr). During the dry season, organic matter larger than 10 μm prevailed, whereas during the wet season, the 0.05-5 μm fraction became dominant. Due to wind-induced resuspension of larger sediment particles during the dry season, the 10-250 μm fraction exhibited a high degree of humification. In contrast, the warm and rainy wet season triggered algal blooms, possibly enhancing the microbial source characteristics of dissolved organic matter (DOM) in the <0.05 μm fraction. PARAFAC analysis reveals that protein-like components dominate in dissolved organic matter (DOM). High-resolution mass spectrometry confirms that DOM smaller than 0.45 μm is primarily composed of lignin-like compounds, while DOM smaller than 0.05 μm has an increased proportion of sulfur-containing compounds compared to that larger than 0.05 μm. This is presumed to be caused by the large-scale mortality of submerged plants over a decade and the accumulation of agricultural non-point source pollution due to prolonged water exchange cycles. The organic matter composition in Lake Qilu exhibits particle size differentiation and seasonal dynamics, influenced by both terrigenous inputs and endogenous microbial activity, which are closely related to the lake’s enclosure, agricultural NPS pollution, and frequent algal blooms. Starting from particle size fractionation of organic matter in Lake Qilu, this study revealed its transport patterns from the ecosystem scale to the molecular level, providing a reference for understanding the carbon cycle in eutrophic plateau lakes.

     

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