摘要
溶解性有机质(DOM)是湖泊生态系统重要组成部分,其性质和结构决定了其在污染物(例如汞)环境行为中扮演着重要角色。本研究选取三峡库区内陆腹地典型水库型湖泊———长寿湖,采用吸收光谱表征方法,通过1年时间对 DOM 地球化学变化规律进行了定性定量分析,并结合汞观测数据,讨论了 DOM 对不同形态汞浓度的影响。结果表明,和1月相比,长寿湖4~11月 DOC 差异性低于 CDOM,4~11月间差异性不显著。有色组分变化是解释 DOM 季节性变化的重要原因。 DOM 中主要生色团仍然来自于大分子量的芳香性组分。而 CDOM 三波长模型可较好对 DOC 的年际观测进行反演。同时,SUVA254和S 275~295季节性变化特征较明显,1月芳香性和分子量均最小,4月上升。与其他类型湖泊相比,长寿湖水体 DOM 芳香性和分子量大小均低于森林湖泊,但高于高原湖泊。周边生态系统和土地利用类型对湖泊 DOM 差异影响明显。另外,SUVA254和 DOC与各形态 Hg 无明显相关性,但水体生色组分和分子量大小是控制溶解态和活性汞的重要因素;而湖区甲基汞变化可能与湖泊初级生产力导致的有机质富集和迁移关系密切。
Dissolved organic matter (DOM) is an important component in lake eco-systems. It plays a crucial role in the environmental fate of pollutants such as mercury ( Hg), because of its specific characteristics and functional structures. In this study, a typical reservoir lake from inland of Three Gorges Reservoir areas, Changshou Lake was selected to track the changes of DOM geochemical properties for one year by using UV-Vis absorption spectroscopy technique. Meanwhile, based on observed Hg data in Changshou Lake, it further validated the key environmental implications of DOM for Hg distributions in lake. The results showed that as compared to January, other months including April, June and September had significantly higher CDOM, but also higher DOC with a slightly decreasing significance. Dynamics of chromphoric component is an important reason to explain the seasonal changes of DOM concentration in Changshou Lake. Chromphores of DOM were mainly derived from high molecular weight (MW) materials with high aromaticity. Also, three wavelengths fitting model of CDOM could be used for inversion of DOC concentration in annual monitoring. Meanwhile, seasonal differences of SUVA254 and S275-295 were significant. Lowest aromaticity and MW size were observed in January following an obvious increase from April. In contrast to other types of lakes, DOM aromaticity and MW size in Changshou Lake were lower than forest lakes, but higher than plateau lakes. Eco-system and land use types surrounding lakes could have a heavily impact on the heterogeneous properties of DOM. Importantly, no clear differences between concentrations of Hg species and SUVA254 and DOC respectively were observed, however chromphoric component and MW size controlled the dissolved Hg and reactive Hg in lake. Additionally, enrichment and migration of organic matter resulted from primary productivity in lake may be a substantial reason to explain the methylmercury changes.
出处
《环境科学》
EI
CAS
CSCD
北大核心
2016年第6期2073-2081,共9页
Environmental Science
基金
国家重点基础研究发展计划(973)项目(2013CB430004)
国家自然科学基金项目(41403079
41373113)
重庆市科委基础与前沿研究计划项目(cstc2015jcyjA20021)
中央高校基本科研业务费专项基金重点项目(XDJK2015B035)
重庆市博士后科研项目(Xm2014023)
关键词
三峡库区
长寿湖
溶解性有机质
天然有机质
吸收光谱
汞
甲基汞
Three Gorges Reservoir Areas
Changshou Lake
dissolved organic matter (DOM)
natural organic matter
absorption spectrum
mercury
methylmercury