长江流域资源与环境 >> 2022, Vol. 31 >> Issue (2): 414-425.doi: 10.11870/cjlyzyyhj202202015

• 生态环境 • 上一篇    下一篇

旱雨季抚仙湖及其入湖河流有色可溶性有机物的吸收与组成

杨炫1,2,陈乐2,3,李凯迪1,3,万国帅1,段立曾1,周起超1,3*   

  1. (1. 云南大学生态与环境学院高原湖泊生态与治理研究院,云南 昆明 650500; 2. 云南大学国际河流与生态安全研究院,云南 昆明 650500; 3. 云南省生态环境科学研究院云南省高原湖泊流域污染过程与管理重点实验室,云南 昆明 650034)
  • 出版日期:2022-02-20 发布日期:2022-03-21

Spectral Absorption and Composition of Chromophoric Dissolved Organic Matter in Lake Fuxian and Its Inflowing Rivers during the Dry and Rainy Seasons

YANG Xuan1,2,CHEN Le2,3,LI Kai-di1,3,WAN Guo-shuai1,DUAN Li-zeng1,ZHOU Qi-chao1,3   

  1. (1. Institute for Ecological Research and Pollution Control of Plateau Lakes, School of Ecology and Environmental Sciences,
     Yunnan University, Kunming 650500, China; 2. Institute of International River and Eco-security, Yunnan University, 
    Kunming 650500, China; 3. Yunnan Key Laboratory of Pollution Process and Management of Plateau Lake-Watershed, 
    Yunnan Research Academy of Eco-environmental Sciences, Kunming 650034, China)
  • Online:2022-02-20 Published:2022-03-21

摘要: 基于2018年旱季(2月)和雨季(7月)对抚仙湖及其主要入湖河流有色可溶性有机物(CDOM)光谱吸收和三维荧光光谱的测定,研究了该湖CDOM的来源组成与时空变化特征。结果表明:抚仙湖湖体CDOM丰度处于较低水平,a(254)范围为3.58~4.66 m-1。抚仙湖及其入湖河流的荧光指数FI为1.51~1.89、自生源指数BIX为0.81~1.24、新鲜度指数β/α为0.76~1.14,腐殖化指数HIX除雨季HD7、HD13外均小于4,表明其CDOM以生物源为主、腐殖化程度不高。平行因子分析得到5种荧光组分,包括两个类腐殖质组分(C1、C2)、两个类酪氨酸组分(C3、C4)和一个类色氨酸组分(C5)。旱季入湖河流、近岸与远岸湖水的CDOM均表现出类蛋白质类酪氨酸荧光特性,雨季入湖河流表现出类腐殖质荧光特性,旱季的内源荧光组分C3、C4及其占比显著大于雨季,雨季的外源荧光组分占比及HIX显著升高,表明旱季到雨季CDOM有从内源为主向外源为主转变的趋势;但由于光辐射强、蓄水量大、水力停留时间长及其次生效应(如微生物作用强),使该湖雨季的内源荧光组分占比仍达45%,河流输入对该湖CDOM丰度的直接贡献小。此外,入湖河流、近岸湖水与远岸湖水的BIX、β/α、M的旱雨季差异不同,表明不同研究区域CDOM荧光特性受季节变化影响有异。

Abstract: In February (dry season) and July (wet season) 2018, the spectral absorption and three-dimensional fluorescence spectrometry analysis of chromophoric dissolved organic matter (CDOM) in Lake Fuxian and its inflowing rivers have been performed to clarify the CDOM’s sources, composition and their spatiotemporal characteristics.The values of a(254) ranged from 3.58 to 4.66 m-1, indicatinglow CDOM abundance. The fluorescence index FI (1.51-1.89), biological autochthonous index BIX (0.81-1.24), freshness index β/α (0.76-1.14) and the humification index HIX (all less than 4 except for HD7 and HD13 during thewet season) of Lake Fuxian and its inflowing rivers,indicated that the CDOMwas mainly autochthonous with a low degree of humification.Five CDOM components were identified by using the parallel factor analysis, including two humus-like components (C1, C2), two tyrosine-like components (C3, C4) and one tryptophan-like component (C5). The CDOM of the inflowing rivers, nearshore and offshore areas of Lake Fuxian during the dry season showed tyrosine-like fluorescence characteristics. However, the CDOM of the inflowing rivers during thewet season showed humus-like fluorescence characteristics.During the dry season, the autochthonous components and their proportion (C3+C4) of Lake Fuxian had larger values. However, in wet season, the allochthonous components (C1+C2+C5) and the HIX were larger. These results indicated the sources of CDOM transformed to allochthonous during the wet seasons. River inputs had few direct contributions on the CDOM abundances of the lake. Due to the strong light radiation, large water storage, long hydraulic retention time and its secondary effects (e.g., microbial actions), CDOM autochthonous components of Lake Fuxian was still up to 45% in the wet season. Furthermore, the varies of BIX、β/α、M in different areas of Lake Fuxian implied that the influences of seasonality on CDOM had spatial heterogeneity.

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