The deterioration of the surface water environment has become a serious challenge for water resources management due to increasing anthropogenic disturbance. Water resources protection requires control of potential po...The deterioration of the surface water environment has become a serious challenge for water resources management due to increasing anthropogenic disturbance. Water resources protection requires control of potential pollution sources. In this study, 99 water samples were collected from a river in a typical agricultural city of Anhui Province in eastern China, and these samples were analyzed in terms of pH, electrical conductivity, and the concentrations of F-, Cl-, SO42-, Na+, K+, Mg2+, Ca2+, As, Cr, Cu, Zn, and Pb. Cluster analysis, co-occurrence network analysis, and principal component analysis/factor analysis were conducted to qualitatively identify the potential sources of river water pollution in the study area. An absolute principal component score-multiple linear regression receptor model was used to quantitatively evaluate the contribution of each source to water quality parameters. The results showed that all observed water quality indices met the quality criteria specified in the Chinese drinking water standards, except for pH, ρ(F-), ρ(SO42-), and ρ(As). The heat map showed that the frequent recharge of pollutants from the tributaries during the wet season was the main reason for the deterioration of water quality. Five sources of river water pollution were identified, and their contribution ratios in a descending order were as follows: the geogenic process (24%) > agricultural activities (21%) > poultry farming sources (17%) > domestic pollution (9%) > transportation pollution (5%). Therefore, controlling pollution from agricultural activities, strengthening the regulation of livestock farming, and improving the sewage network are the recommended strategies for improving the quality of surface water resources in this area.展开更多
The dust source and transporting system are two indispensable aspects in the process of Ioess-palaeosol accumulation. It has been proved that the dust of the Loess Plateau mainly comes from the northwestern inland gob...The dust source and transporting system are two indispensable aspects in the process of Ioess-palaeosol accumulation. It has been proved that the dust of the Loess Plateau mainly comes from the northwestern inland gobi and desert, transported by the East Asia monsoon systems and westerlies. However, there are little researches with respect to the dust source and deposition dynamics of the upper reaches of the Huaihe River. In the present study, we investigated and collected the YPC section with high resolution in the upper reaches of the Huaihe River. The chronological frame was reconstructed by optically stimulated luminescence （QSL） dating and correlated with the published loess time series. By comparison of the magnetic susceptibility （MS） and grain size （GS） of loess-soil profile among YPC profile, XJN profile （western Loess Plateau） and the JYC profile （southern Loess Plateau）, we find similar climate change and pedogenic process between the upper reaches of the Huaihe River and the Loess Plateau, both experienced an extreme dry and the weakest pedogenesis during the last glacial, followed by a transitional episodes from the cold-dry last glacial to the warm-humid mid-Holocene and increased pedogenesis in the early Holocene, then a most humid-warm and strong pedogenesis in the mid-Holocene, and climate deterioration and decreased pedogenesis occurred during the late Holocene. But the MS of loess-soil profile sequences in the upper reaches of the Huaihe River was much lower than those in the Loess Plateau, and the GS was much coarser than those in the Loess Plateau. Comparison of GS for these three profiles revealed that there were different dust sources, which belonged to different aeolian transporting systems. The loess in the upper reaches of the Huaihe River was a wind blown deposition of near source, while the coarser dust mainly came from loose alluvial deposits of alluvial and proluvial fans of the Yellow River. The yield- ing and carrying dynamics of the dust in the Huaihe River is the northeast wind prevails in the winter half year.展开更多
淮河流域位于我国南北气候过渡带,其复杂多变的降水过程及水汽来源是导致流域洪旱灾害易发、多发的重要因素。以全球降水同位素监测网络(Global Network of Isotope in Precipitation,GNIP)监测的多年降水氢氧稳定同位素数据为基础,探...淮河流域位于我国南北气候过渡带,其复杂多变的降水过程及水汽来源是导致流域洪旱灾害易发、多发的重要因素。以全球降水同位素监测网络(Global Network of Isotope in Precipitation,GNIP)监测的多年降水氢氧稳定同位素数据为基础,探讨了淮河流域大气降水氢氧稳定同位素组成时空变化的驱动因素及其气候指示意义;通过分析氢氧稳定同位素组成(δ^(18)O、δ^(2)H、氘盈余)、大气降水线特征与流域气温、降水量的响应关系,解析流域不同季节大气降水水汽来源及气团移动路径。结果表明:①淮河流域大气降水氢氧稳定同位素组成能够指示南北气候过渡带特征;②同位素时空变化及异常低的大气降水线斜率、截距与局地降水环境关系不大,主要是由水汽来源差异及降水气团在移动过程中同位素分馏造成的。氘盈余示踪和HYSPLIT模型模拟结果进一步表明流域降水水汽来源及变化受季风活动的控制,冬季风和夏季风的交替进退使得淮河流域的降水氘盈余变化具有明显的“V”型特征。研究成果可为水资源调度管理、极端气候应对决策等提供科学依据。展开更多
基金supported by the 2021 Graduate Science Research Project of the Anhui Higher Education Institutions(Grant No.YJS20210375)the Natural Science Research Project of Universities in Anhui Province(Grant No.KJ2020ZD64)+2 种基金the Natural Science Foundation of Anhui Province(Grant No.2008085MD122)the Outstanding Young Talents in Higher Education Institutions of Anhui Province(Grant No.ZD2021134)the Research Development Foundation of Suzhou University(Grant No.2021fzjj28).
文摘The deterioration of the surface water environment has become a serious challenge for water resources management due to increasing anthropogenic disturbance. Water resources protection requires control of potential pollution sources. In this study, 99 water samples were collected from a river in a typical agricultural city of Anhui Province in eastern China, and these samples were analyzed in terms of pH, electrical conductivity, and the concentrations of F-, Cl-, SO42-, Na+, K+, Mg2+, Ca2+, As, Cr, Cu, Zn, and Pb. Cluster analysis, co-occurrence network analysis, and principal component analysis/factor analysis were conducted to qualitatively identify the potential sources of river water pollution in the study area. An absolute principal component score-multiple linear regression receptor model was used to quantitatively evaluate the contribution of each source to water quality parameters. The results showed that all observed water quality indices met the quality criteria specified in the Chinese drinking water standards, except for pH, ρ(F-), ρ(SO42-), and ρ(As). The heat map showed that the frequent recharge of pollutants from the tributaries during the wet season was the main reason for the deterioration of water quality. Five sources of river water pollution were identified, and their contribution ratios in a descending order were as follows: the geogenic process (24%) > agricultural activities (21%) > poultry farming sources (17%) > domestic pollution (9%) > transportation pollution (5%). Therefore, controlling pollution from agricultural activities, strengthening the regulation of livestock farming, and improving the sewage network are the recommended strategies for improving the quality of surface water resources in this area.
基金Key Project of National Natural Science Foundation of China, No.40830107 No.41030637
文摘The dust source and transporting system are two indispensable aspects in the process of Ioess-palaeosol accumulation. It has been proved that the dust of the Loess Plateau mainly comes from the northwestern inland gobi and desert, transported by the East Asia monsoon systems and westerlies. However, there are little researches with respect to the dust source and deposition dynamics of the upper reaches of the Huaihe River. In the present study, we investigated and collected the YPC section with high resolution in the upper reaches of the Huaihe River. The chronological frame was reconstructed by optically stimulated luminescence （QSL） dating and correlated with the published loess time series. By comparison of the magnetic susceptibility （MS） and grain size （GS） of loess-soil profile among YPC profile, XJN profile （western Loess Plateau） and the JYC profile （southern Loess Plateau）, we find similar climate change and pedogenic process between the upper reaches of the Huaihe River and the Loess Plateau, both experienced an extreme dry and the weakest pedogenesis during the last glacial, followed by a transitional episodes from the cold-dry last glacial to the warm-humid mid-Holocene and increased pedogenesis in the early Holocene, then a most humid-warm and strong pedogenesis in the mid-Holocene, and climate deterioration and decreased pedogenesis occurred during the late Holocene. But the MS of loess-soil profile sequences in the upper reaches of the Huaihe River was much lower than those in the Loess Plateau, and the GS was much coarser than those in the Loess Plateau. Comparison of GS for these three profiles revealed that there were different dust sources, which belonged to different aeolian transporting systems. The loess in the upper reaches of the Huaihe River was a wind blown deposition of near source, while the coarser dust mainly came from loose alluvial deposits of alluvial and proluvial fans of the Yellow River. The yield- ing and carrying dynamics of the dust in the Huaihe River is the northeast wind prevails in the winter half year.
文摘淮河流域位于我国南北气候过渡带,其复杂多变的降水过程及水汽来源是导致流域洪旱灾害易发、多发的重要因素。以全球降水同位素监测网络(Global Network of Isotope in Precipitation,GNIP)监测的多年降水氢氧稳定同位素数据为基础,探讨了淮河流域大气降水氢氧稳定同位素组成时空变化的驱动因素及其气候指示意义;通过分析氢氧稳定同位素组成(δ^(18)O、δ^(2)H、氘盈余)、大气降水线特征与流域气温、降水量的响应关系,解析流域不同季节大气降水水汽来源及气团移动路径。结果表明:①淮河流域大气降水氢氧稳定同位素组成能够指示南北气候过渡带特征;②同位素时空变化及异常低的大气降水线斜率、截距与局地降水环境关系不大,主要是由水汽来源差异及降水气团在移动过程中同位素分馏造成的。氘盈余示踪和HYSPLIT模型模拟结果进一步表明流域降水水汽来源及变化受季风活动的控制,冬季风和夏季风的交替进退使得淮河流域的降水氘盈余变化具有明显的“V”型特征。研究成果可为水资源调度管理、极端气候应对决策等提供科学依据。
