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抚仙湖悬浮颗粒物正构烷烃来源及季节特征
引用本文:袁红香,孙惠玲,段立曾,张虎才.抚仙湖悬浮颗粒物正构烷烃来源及季节特征[J].中国环境科学,2021,41(6):2812-2820.
作者姓名:袁红香  孙惠玲  段立曾  张虎才
作者单位:1. 云南师范大学地理学部, 云南省高原地理过程与环境变化重点实验室, 云南 昆明 650500;2. 云南大学资源环境与地球科学学院, 高原湖泊生态与污染治理研究院, 云南 昆明 650504
基金项目:国家自然科学基金资助项目(41761044,41971115);云南省领军人才项目(2015HA024)
摘    要:为了探究抚仙湖水体中有机质的正构烷烃来源和时空变化特征,对2016年4月~2017年3月抚仙湖水柱悬浮颗粒物中正构烷烃的分布特征、来源、季节变化特征及其与沉积物中正构烷烃的关系进行了研究.结果表明:抚仙湖水柱悬浮颗粒物中正构烷烃的碳数分布范围在C17~C33之间,呈现以优势峰C27和C29为主的单峰分布模式.在垂直梯度的空间分布上,正构烷烃在变温层和温跃层的浓度高于深水层,最大浓度出现在深20m水层,深层水体中正构烷烃浓度受沉积物再悬浮作用影响微弱;在季节变化上,正构烷烃含量存在明显的季节波动,在10月和4月呈现最高值;其中,中长链正构烷烃(C25、C27和C29)丰度与浮游植物生物量季节变化趋势一致,证明浮游植物是抚仙湖水柱中正构烷烃的主要来源,水温是限制抚仙湖水柱中正构烷烃时空分布的关键因子.浮游植物、流域表土和沉水植物的共同输入是抚仙湖沉积物中正构烷烃C29具有较高丰度的原因,沉积物中正构烷烃(C31和C23)来源相对单一,可以有效指示流域陆源植物和沉水植物输入.本文结果可多应用正构烷烃指标进行抚仙湖长序列钻孔古环境重建研究提供数据支持.

关 键 词:抚仙湖  悬浮颗粒物  正构烷烃  浮游植物  
收稿时间:2020-11-02

The sources and seasonal variation characteristics of n-alkanes in suspended particulate matter in Fuxian Lake
YUAN Hong-xiang,SUN Hui-ling,DUAN li-zeng,ZHANG Hu-cai.The sources and seasonal variation characteristics of n-alkanes in suspended particulate matter in Fuxian Lake[J].China Environmental Science,2021,41(6):2812-2820.
Authors:YUAN Hong-xiang  SUN Hui-ling  DUAN li-zeng  ZHANG Hu-cai
Institution:1. Yunnan Key Laboratory of Plateau Geographical Processes and Environmental Change, Faculty of Geography, Yunnan Normal University, Kunming 650500, China;2. Institute for Ecological Research and Pollution Control of Plateau Lakes, School of Resources, Environment and Earth Sciences, Yunnan University, Kunming 650504, China
Abstract:In order to investigate the sources and spatiotemporal variation characteristics of n-alkanes in organic matter in Fuxian Lake, the distribution characteristics, biological sources and seasonal variations of suspended particulate matter in water columns of Fuxian Lake from April 2016 to March 2017 were studied. The vertical distribution of n-alkanes demonstrated the relative abundance of n-alkanes above the thermocline was higher than that below the thermocline. The maximum concentration of n-alkanes occured in ~20m depth. The relative abundance of n-alkanes in water columns was weakly affected by sediment resuspension. The obvious seasonal fluctuation in n-alkanes with the highest values in October and April can be found. Furthermore, the seasonal variation trends of n-25, n-27, n-29 alkanes were consistent with that of phytoplankton biomass, which illustrated that the phytoplankton was the main source of n-alkanes in water columns of Fuxian Lake. Water temperature was one of the key factors to limit the spatial and temporal distribution of n-alkanes in water columns of Fuxian Lake. All the input from the phytoplanktons, surface soil and submerged plants played an important role for the high abundance of C29in the surface sediments. The n-alkanes (C31 and C23) in the sediments of Fuxian Lake could effectively indicate the input of terrestrial plants and submerged plants. The results were good foundation of paleo-environmental reconstruction in down core sediments based on n-alkanes in Fuxian Lake.
Keywords:Fuxian Lake  suspended particulate matter  n-alkanes  phytoplankton  
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