Shi Zhanyao, Du Yao, Liu Hongni, Xie Xianjun
Key Laboratory of Groundwater Quality and Health, China University of Geosciences, Ministry of Education, Wuhan 430078, China; School of Environmental Studies, State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan 430078, China; Hubei Key Laboratory of Yangtze Catchment Environmental Aquatic Science, China University of Geosciences, Wuhan 430078, China.
Key Laboratory of Groundwater Quality and Health, China University of Geosciences, Ministry of Education, Wuhan 430078, China; School of Environmental Studies, State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan 430078, China; Hubei Key Laboratory of Yangtze Catchment Environmental Aquatic Science, China University of Geosciences, Wuhan 430078, China.
Sci Total Environ. 2024 Nov 15;951:175647. doi: 10.1016/j.scitotenv.2024.175647. Epub 2024 Aug 20.
Anthropogenic and hydrological drivers are key factors influencing the fate of dissolved organic matter (DOM) and dissolved organic phosphorus (DOP) in river runoff. However, how anthropogenic disturbances and hydrological conditions jointly affect the composition and characteristics of DOM and DOP in river runoff remains unclear. This study used fluorescence spectroscopy, Fourier transform ion cyclotron resonance mass spectrometry, and the stable water isotopes to interpret the chemical composition and properties of DOM and DOP as well as their linkages to anthropogenic disturbances and hydrological conditions in a typical P-contaminated tributary to the central Yangtze River. The results show in the wet season, the average abundance of humic-like components in DOM exceeded 60 %, while the average abundance of tryptophan-like components in DOM exceeded 50 % in the dry season. During the dry season, hydrological conditions had a greater impact on highly unsaturated DOM compounds compared to anthropogenic disturbances because a decrease in precipitation reduced the transport of terrestrial DOM into aquatic systems and increased water retention time in the river, promoting the production of unsaturated compounds from photochemistry. The effects of the two factors were similar in the wet season because active agricultural activities and intense precipitation jointly facilitated the entry of exogenous humics into the runoff, leading to the similar relative abundance of highly unsaturated DOM compounds associated with both factors. Anthropogenic disturbances had a greater impact on aliphatic DOM and DOP than hydrological conditions, which was associated with intense human activities in the watershed, such as phosphate mining, agricultural cultivation, and domestic sewage discharge. This study provides new knowledge about the composition, properties and underlying mechanisms of DOM and DOP in the P-contaminated watershed runoff.
人为因素和水文驱动因素是影响河流径流中溶解有机物(DOM)和溶解有机磷(DOP)归宿的关键因素。然而,人为干扰和水文条件如何共同影响河流径流中DOM和DOP的组成及特性仍不清楚。本研究利用荧光光谱法、傅里叶变换离子回旋共振质谱法和稳定水同位素来解释长江中游典型磷污染支流中DOM和DOP的化学组成及性质,以及它们与人为干扰和水文条件的联系。结果表明,在雨季,DOM中类腐殖质成分的平均丰度超过60%,而在旱季,DOM中类色氨酸成分的平均丰度超过50%。在旱季,与人为干扰相比,水文条件对高度不饱和DOM化合物的影响更大,这是因为降水量减少降低了陆地DOM向水生系统的输送,并增加了河流中的水停留时间,促进了光化学产生不饱和化合物。在雨季,这两个因素的影响相似,因为活跃的农业活动和强降水共同促使外源腐殖质进入径流,导致与这两个因素相关的高度不饱和DOM化合物的相对丰度相似。人为干扰对脂肪族DOM和DOP的影响比水文条件更大,这与流域内强烈的人类活动有关,如磷矿开采、农业种植和生活污水排放。本研究为磷污染流域径流中DOM和DOP的组成、性质及潜在机制提供了新的认识。