Analysis on the evolution trend of water resources and water environment in Xiangjiang River basin
According to the daily flow data collected by three representative hydrological stations in the Xiangjiang River basin which are the Guiyang station in the upstream section, the Hengshan station in the midstream section, and the Xiangtan station in the downstream section, and the water environment d...
Ausführliche Beschreibung
Autor*in: |
Xu Xingyi [verfasserIn] Xiao Chuqiu [verfasserIn] Hu Chunyan [verfasserIn] Li Guiyuan [verfasserIn] Gao Xiang [verfasserIn] He Huaiguang [verfasserIn] Wang Xinkui [verfasserIn] Pan Yuqi [verfasserIn] |
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E-Artikel |
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Sprache: |
Englisch ; Französisch |
Erschienen: |
2018 |
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Übergeordnetes Werk: |
In: MATEC Web of Conferences - EDP Sciences, 2013, 246, p 02030(2018) |
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Übergeordnetes Werk: |
volume:246, p 02030 ; year:2018 |
Links: |
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DOI / URN: |
10.1051/matecconf/201824602030 |
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Katalog-ID: |
DOAJ053385233 |
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10.1051/matecconf/201824602030 doi (DE-627)DOAJ053385233 (DE-599)DOAJ9b13f27c22c6423b9e194a7751afb910 DE-627 ger DE-627 rakwb eng fre TA1-2040 Xu Xingyi verfasserin aut Analysis on the evolution trend of water resources and water environment in Xiangjiang River basin 2018 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier According to the daily flow data collected by three representative hydrological stations in the Xiangjiang River basin which are the Guiyang station in the upstream section, the Hengshan station in the midstream section, and the Xiangtan station in the downstream section, and the water environment data collected from the Hunan Water Resources Bulletin, Mann-Kendal method was used to analyze the changes of the annual average flow of the Xiangjiang River basin in the past 20 years as well as the variation of water environment quality in the whole year, flood season and non-flood season. Based on these analysis, the evolution trend of water resources and water environment in the Xiangjiang River basin is further forecasted. The results show that the annual runoff of the upper reaches of the Xiangjiang River basin tends to be stable, and the runoff of the middle and lower reaches is decreasing. The water quality of the Xiangjiang River basin got deteriorated from 1996 to 2010. A sudden change occurred around 2012, and the water quality of the basin gradually improved. Engineering (General). Civil engineering (General) Xiao Chuqiu verfasserin aut Hu Chunyan verfasserin aut Li Guiyuan verfasserin aut Gao Xiang verfasserin aut He Huaiguang verfasserin aut Wang Xinkui verfasserin aut Pan Yuqi verfasserin aut In MATEC Web of Conferences EDP Sciences, 2013 246, p 02030(2018) (DE-627)720166209 (DE-600)2673602-0 2261236X nnns volume:246, p 02030 year:2018 https://doi.org/10.1051/matecconf/201824602030 kostenfrei https://doaj.org/article/9b13f27c22c6423b9e194a7751afb910 kostenfrei https://doi.org/10.1051/matecconf/201824602030 kostenfrei https://doaj.org/toc/2261-236X Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ SSG-OLC-PHA GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2014 GBV_ILN_2055 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 246, p 02030 2018 |
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10.1051/matecconf/201824602030 doi (DE-627)DOAJ053385233 (DE-599)DOAJ9b13f27c22c6423b9e194a7751afb910 DE-627 ger DE-627 rakwb eng fre TA1-2040 Xu Xingyi verfasserin aut Analysis on the evolution trend of water resources and water environment in Xiangjiang River basin 2018 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier According to the daily flow data collected by three representative hydrological stations in the Xiangjiang River basin which are the Guiyang station in the upstream section, the Hengshan station in the midstream section, and the Xiangtan station in the downstream section, and the water environment data collected from the Hunan Water Resources Bulletin, Mann-Kendal method was used to analyze the changes of the annual average flow of the Xiangjiang River basin in the past 20 years as well as the variation of water environment quality in the whole year, flood season and non-flood season. Based on these analysis, the evolution trend of water resources and water environment in the Xiangjiang River basin is further forecasted. The results show that the annual runoff of the upper reaches of the Xiangjiang River basin tends to be stable, and the runoff of the middle and lower reaches is decreasing. The water quality of the Xiangjiang River basin got deteriorated from 1996 to 2010. A sudden change occurred around 2012, and the water quality of the basin gradually improved. Engineering (General). Civil engineering (General) Xiao Chuqiu verfasserin aut Hu Chunyan verfasserin aut Li Guiyuan verfasserin aut Gao Xiang verfasserin aut He Huaiguang verfasserin aut Wang Xinkui verfasserin aut Pan Yuqi verfasserin aut In MATEC Web of Conferences EDP Sciences, 2013 246, p 02030(2018) (DE-627)720166209 (DE-600)2673602-0 2261236X nnns volume:246, p 02030 year:2018 https://doi.org/10.1051/matecconf/201824602030 kostenfrei https://doaj.org/article/9b13f27c22c6423b9e194a7751afb910 kostenfrei https://doi.org/10.1051/matecconf/201824602030 kostenfrei https://doaj.org/toc/2261-236X Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ SSG-OLC-PHA GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2014 GBV_ILN_2055 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 246, p 02030 2018 |
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10.1051/matecconf/201824602030 doi (DE-627)DOAJ053385233 (DE-599)DOAJ9b13f27c22c6423b9e194a7751afb910 DE-627 ger DE-627 rakwb eng fre TA1-2040 Xu Xingyi verfasserin aut Analysis on the evolution trend of water resources and water environment in Xiangjiang River basin 2018 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier According to the daily flow data collected by three representative hydrological stations in the Xiangjiang River basin which are the Guiyang station in the upstream section, the Hengshan station in the midstream section, and the Xiangtan station in the downstream section, and the water environment data collected from the Hunan Water Resources Bulletin, Mann-Kendal method was used to analyze the changes of the annual average flow of the Xiangjiang River basin in the past 20 years as well as the variation of water environment quality in the whole year, flood season and non-flood season. Based on these analysis, the evolution trend of water resources and water environment in the Xiangjiang River basin is further forecasted. The results show that the annual runoff of the upper reaches of the Xiangjiang River basin tends to be stable, and the runoff of the middle and lower reaches is decreasing. The water quality of the Xiangjiang River basin got deteriorated from 1996 to 2010. A sudden change occurred around 2012, and the water quality of the basin gradually improved. Engineering (General). Civil engineering (General) Xiao Chuqiu verfasserin aut Hu Chunyan verfasserin aut Li Guiyuan verfasserin aut Gao Xiang verfasserin aut He Huaiguang verfasserin aut Wang Xinkui verfasserin aut Pan Yuqi verfasserin aut In MATEC Web of Conferences EDP Sciences, 2013 246, p 02030(2018) (DE-627)720166209 (DE-600)2673602-0 2261236X nnns volume:246, p 02030 year:2018 https://doi.org/10.1051/matecconf/201824602030 kostenfrei https://doaj.org/article/9b13f27c22c6423b9e194a7751afb910 kostenfrei https://doi.org/10.1051/matecconf/201824602030 kostenfrei https://doaj.org/toc/2261-236X Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ SSG-OLC-PHA GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2014 GBV_ILN_2055 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 246, p 02030 2018 |
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10.1051/matecconf/201824602030 doi (DE-627)DOAJ053385233 (DE-599)DOAJ9b13f27c22c6423b9e194a7751afb910 DE-627 ger DE-627 rakwb eng fre TA1-2040 Xu Xingyi verfasserin aut Analysis on the evolution trend of water resources and water environment in Xiangjiang River basin 2018 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier According to the daily flow data collected by three representative hydrological stations in the Xiangjiang River basin which are the Guiyang station in the upstream section, the Hengshan station in the midstream section, and the Xiangtan station in the downstream section, and the water environment data collected from the Hunan Water Resources Bulletin, Mann-Kendal method was used to analyze the changes of the annual average flow of the Xiangjiang River basin in the past 20 years as well as the variation of water environment quality in the whole year, flood season and non-flood season. Based on these analysis, the evolution trend of water resources and water environment in the Xiangjiang River basin is further forecasted. The results show that the annual runoff of the upper reaches of the Xiangjiang River basin tends to be stable, and the runoff of the middle and lower reaches is decreasing. The water quality of the Xiangjiang River basin got deteriorated from 1996 to 2010. A sudden change occurred around 2012, and the water quality of the basin gradually improved. Engineering (General). Civil engineering (General) Xiao Chuqiu verfasserin aut Hu Chunyan verfasserin aut Li Guiyuan verfasserin aut Gao Xiang verfasserin aut He Huaiguang verfasserin aut Wang Xinkui verfasserin aut Pan Yuqi verfasserin aut In MATEC Web of Conferences EDP Sciences, 2013 246, p 02030(2018) (DE-627)720166209 (DE-600)2673602-0 2261236X nnns volume:246, p 02030 year:2018 https://doi.org/10.1051/matecconf/201824602030 kostenfrei https://doaj.org/article/9b13f27c22c6423b9e194a7751afb910 kostenfrei https://doi.org/10.1051/matecconf/201824602030 kostenfrei https://doaj.org/toc/2261-236X Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ SSG-OLC-PHA GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2014 GBV_ILN_2055 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 246, p 02030 2018 |
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10.1051/matecconf/201824602030 doi (DE-627)DOAJ053385233 (DE-599)DOAJ9b13f27c22c6423b9e194a7751afb910 DE-627 ger DE-627 rakwb eng fre TA1-2040 Xu Xingyi verfasserin aut Analysis on the evolution trend of water resources and water environment in Xiangjiang River basin 2018 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier According to the daily flow data collected by three representative hydrological stations in the Xiangjiang River basin which are the Guiyang station in the upstream section, the Hengshan station in the midstream section, and the Xiangtan station in the downstream section, and the water environment data collected from the Hunan Water Resources Bulletin, Mann-Kendal method was used to analyze the changes of the annual average flow of the Xiangjiang River basin in the past 20 years as well as the variation of water environment quality in the whole year, flood season and non-flood season. Based on these analysis, the evolution trend of water resources and water environment in the Xiangjiang River basin is further forecasted. The results show that the annual runoff of the upper reaches of the Xiangjiang River basin tends to be stable, and the runoff of the middle and lower reaches is decreasing. The water quality of the Xiangjiang River basin got deteriorated from 1996 to 2010. A sudden change occurred around 2012, and the water quality of the basin gradually improved. Engineering (General). Civil engineering (General) Xiao Chuqiu verfasserin aut Hu Chunyan verfasserin aut Li Guiyuan verfasserin aut Gao Xiang verfasserin aut He Huaiguang verfasserin aut Wang Xinkui verfasserin aut Pan Yuqi verfasserin aut In MATEC Web of Conferences EDP Sciences, 2013 246, p 02030(2018) (DE-627)720166209 (DE-600)2673602-0 2261236X nnns volume:246, p 02030 year:2018 https://doi.org/10.1051/matecconf/201824602030 kostenfrei https://doaj.org/article/9b13f27c22c6423b9e194a7751afb910 kostenfrei https://doi.org/10.1051/matecconf/201824602030 kostenfrei https://doaj.org/toc/2261-236X Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ SSG-OLC-PHA GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2014 GBV_ILN_2055 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 246, p 02030 2018 |
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Analysis on the evolution trend of water resources and water environment in Xiangjiang River basin |
abstract |
According to the daily flow data collected by three representative hydrological stations in the Xiangjiang River basin which are the Guiyang station in the upstream section, the Hengshan station in the midstream section, and the Xiangtan station in the downstream section, and the water environment data collected from the Hunan Water Resources Bulletin, Mann-Kendal method was used to analyze the changes of the annual average flow of the Xiangjiang River basin in the past 20 years as well as the variation of water environment quality in the whole year, flood season and non-flood season. Based on these analysis, the evolution trend of water resources and water environment in the Xiangjiang River basin is further forecasted. The results show that the annual runoff of the upper reaches of the Xiangjiang River basin tends to be stable, and the runoff of the middle and lower reaches is decreasing. The water quality of the Xiangjiang River basin got deteriorated from 1996 to 2010. A sudden change occurred around 2012, and the water quality of the basin gradually improved. |
abstractGer |
According to the daily flow data collected by three representative hydrological stations in the Xiangjiang River basin which are the Guiyang station in the upstream section, the Hengshan station in the midstream section, and the Xiangtan station in the downstream section, and the water environment data collected from the Hunan Water Resources Bulletin, Mann-Kendal method was used to analyze the changes of the annual average flow of the Xiangjiang River basin in the past 20 years as well as the variation of water environment quality in the whole year, flood season and non-flood season. Based on these analysis, the evolution trend of water resources and water environment in the Xiangjiang River basin is further forecasted. The results show that the annual runoff of the upper reaches of the Xiangjiang River basin tends to be stable, and the runoff of the middle and lower reaches is decreasing. The water quality of the Xiangjiang River basin got deteriorated from 1996 to 2010. A sudden change occurred around 2012, and the water quality of the basin gradually improved. |
abstract_unstemmed |
According to the daily flow data collected by three representative hydrological stations in the Xiangjiang River basin which are the Guiyang station in the upstream section, the Hengshan station in the midstream section, and the Xiangtan station in the downstream section, and the water environment data collected from the Hunan Water Resources Bulletin, Mann-Kendal method was used to analyze the changes of the annual average flow of the Xiangjiang River basin in the past 20 years as well as the variation of water environment quality in the whole year, flood season and non-flood season. Based on these analysis, the evolution trend of water resources and water environment in the Xiangjiang River basin is further forecasted. The results show that the annual runoff of the upper reaches of the Xiangjiang River basin tends to be stable, and the runoff of the middle and lower reaches is decreasing. The water quality of the Xiangjiang River basin got deteriorated from 1996 to 2010. A sudden change occurred around 2012, and the water quality of the basin gradually improved. |
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title_short |
Analysis on the evolution trend of water resources and water environment in Xiangjiang River basin |
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