首页> 外文期刊>Applied Geochemistry: Journal of the International Association of Geochemistry and Cosmochemistry >Natural and anthropogenic factors affecting geochemistry of the Jialing and Yangtze Rivers in urban Chongqing, SW China
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Natural and anthropogenic factors affecting geochemistry of the Jialing and Yangtze Rivers in urban Chongqing, SW China

机译:中国重庆市嘉陵和长江地球化学地球化学的自然和人为因素

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Owing to the complex relationship between natural factors and anthropogenic activities, rivers passing through urban areas present special challenges to geochemists attempting to understand geochemical conditions and fluxes. Research here on a river impacted by urban development, influenced by both natural and anthropogenic factors, helps to understand the mechanisms of the processes that cause changes in water quality. In this study, we collected water samples weekly at three sampling sites from the Jialing and Yangtze Rivers in the urban area of Chongqing. To explore the evolutionary processes and factors influencing surface water quality, we used stoichiometry and principle component analysis (PCA). Results show that the samples belonged to the HCO3 center dot SO4-Ca hydrochemical facies. The hydrochemical characteristics of the two rivers were mainly controlled by rock weathering. Carbonate mineral weathering exhibited the largest contribution. Sulfuric acid was involved in carbonate mineral weathering reactions, but gypsum dissolution had little effect on surface water chemistry. PCA revealed that rock weathering, soil erosion, domestic sewage, and agricultural activities contribute to the dissolved chemical load in the Jialing and Yangtze Rivers. The chemical characteristics of the Yangtze River mainstream exhibited changes due to recharge from the Jialing River. Compared with historical data (1959-1990), we found that river water in our study area was more acidic because of coal emissions from industrial activities in Sichuan and Guizhou Provinces. As a result of urbanization and the increase in domestic sewage, the average Cl-/Na+ molar ratio at the sampling sites is approximately 50% greater than historical background data. Furthermore, NO3- was sensitive to agricultural activities, indicating that agricultural activities have an effect on the Jialing and Yangtze Rivers in the urban Chongqing.
机译:由于自然因素与人为活动之间的关系,通过城市地区的河流对地球化学家试图了解地球化学条件和助势的特殊挑战。在这里研究了城市发展影响的河流,受天然和人为因素影响,有助于了解导致水质变化的过程的机制。在这项研究中,我们每周在重庆市区的嘉陵和长江河中每周收集水样。为了探索影响地表水质的进化过程和因素,我们使用了化学计量和原理分量分析(PCA)。结果表明,样品属于HCO3中心DOT SO4-CA水化学领域。两条河流的水化学特征主要由岩石风化控制。碳酸盐矿物风化呈现最大的贡献。硫酸涉及碳酸盐矿物风化反应,但石膏溶解对地表水化学作用不大。 PCA透露,岩石风化,土壤侵蚀,国内污水和农业活动有助于嘉陵和长江河的溶解化学载荷。长江主流的化学特征由于嘉陵江而导致的变化。与历史数据(1959-1990)相比,我们发现我们的研究区河水更加酸性,因为四川和贵州省的工业活动煤炭排放量更为酸性。由于城市化和国内污水的增加,采样网站的平均Cl- / Na +摩尔比大约比历史背景数据大约50%。此外,NO3-对农业活动敏感,表明农业活动对重庆市镇嘉陵和长江河流有影响。

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