On the variation of water resource structure in the Lower Yellow River
In view of river functions and the Minimum Water Demand for River Ecosystem (MWDRE), the water resources in the Lower Yellow River is further divided into three portions, i.e. water available for ecosystem (WE), water exploitable for socioeconomic purposes (WS) and excess flood water (WF). Correspon...
Gespeichert in:
Veröffentlicht in: | Science China. Technological sciences 2004, Vol.47 (8), p.127-141 |
---|---|
1. Verfasser: | |
Format: | Artikel |
Sprache: | eng |
Schlagworte: | |
Online-Zugang: | Volltext |
Tags: |
Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
|
container_end_page | 141 |
---|---|
container_issue | 8 |
container_start_page | 127 |
container_title | Science China. Technological sciences |
container_volume | 47 |
creator | NI, Jinren |
description | In view of river functions and the Minimum Water Demand for River Ecosystem (MWDRE), the water resources in the Lower Yellow River is further divided into three portions, i.e. water available for ecosystem (WE), water exploitable for socioeconomic purposes (WS) and excess flood water (WF). Corresponding conceptions and practical significances are expounded in details. The annual amount of the three portions of water resources from 1950 to 2001 is worked out on the basis of the daily hydrologic data, and the division of different portions is discussed. The results indicate that although the essential water demand for river functions is considered preferentially, the amount of the WE has decreased dramatically while its proportion increased gradually since the 1950s, and the shortage to the MWDRE increased markedly; both the amount and the proportion of the WS decreased notably. Since the 1990s, the actual water consumption for socioeconomic purposes in the lower reaches of the river basin has already exceeded the maximum amount of the WS and has to take over the WE which is already insufficient, hence not only the normal river functions are further disturbed and the river course shrinks greatly, but also the proportion and potential danger of the WF show no decreasing tendency in spite of the sharp decrease of upstream runoff. |
doi_str_mv | 10.1360/04ez0011 |
format | Article |
fullrecord | <record><control><sourceid>wanfang_jour_proqu</sourceid><recordid>TN_cdi_wanfang_journals_zgkx_ee2004z1011</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><wanfj_id>zgkx_ee2004z1011</wanfj_id><sourcerecordid>zgkx_ee2004z1011</sourcerecordid><originalsourceid>FETCH-LOGICAL-c319t-c21c5f7177f081bea0edb6676a05870f7df5f2d2b337d218e1d00efe4a18f883</originalsourceid><addsrcrecordid>eNpdkE9LAzEQxYMoWKvgRwgI4mV1kuxuskcpVoVCQXrxFNLdSd3abmqy29V-eiP1D3iaGebHmzePkHMG10zkcAMp7gAYOyADpvIiYQXAYewB8qQQnB2TkxCWcQLO0wEZTxvaviDdGl-btnYNdZb2pkVPPQbX-RJpaH1Xtp1HWu_hievj_hlXK9fTp3qL_pQcWbMKePZdh2Q2vpuNHpLJ9P5xdDtJSsGKNik5KzMrmZQWFJujAazmeS5zA5mSYGVlM8srPhdCVpwpZBUAWkwNU1YpMSRXe9neNNY0C72MDpt4UO8Wr-8akQOkOxbfj-jlHt1499ZhaPW6DmW0bBp0XdBcCchyVUTw4h_4K8qlkrlQIoW_y6V3IXi0euPrtfEfmoH-Cl7_BC8-AU-idEI</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>2787638340</pqid></control><display><type>article</type><title>On the variation of water resource structure in the Lower Yellow River</title><source>Alma/SFX Local Collection</source><source>SpringerLink Journals - AutoHoldings</source><creator>NI, Jinren</creator><creatorcontrib>NI, Jinren</creatorcontrib><description>In view of river functions and the Minimum Water Demand for River Ecosystem (MWDRE), the water resources in the Lower Yellow River is further divided into three portions, i.e. water available for ecosystem (WE), water exploitable for socioeconomic purposes (WS) and excess flood water (WF). Corresponding conceptions and practical significances are expounded in details. The annual amount of the three portions of water resources from 1950 to 2001 is worked out on the basis of the daily hydrologic data, and the division of different portions is discussed. The results indicate that although the essential water demand for river functions is considered preferentially, the amount of the WE has decreased dramatically while its proportion increased gradually since the 1950s, and the shortage to the MWDRE increased markedly; both the amount and the proportion of the WS decreased notably. Since the 1990s, the actual water consumption for socioeconomic purposes in the lower reaches of the river basin has already exceeded the maximum amount of the WS and has to take over the WE which is already insufficient, hence not only the normal river functions are further disturbed and the river course shrinks greatly, but also the proportion and potential danger of the WF show no decreasing tendency in spite of the sharp decrease of upstream runoff.</description><identifier>ISSN: 1006-9321</identifier><identifier>ISSN: 1674-7321</identifier><identifier>EISSN: 1869-1900</identifier><identifier>DOI: 10.1360/04ez0011</identifier><language>eng</language><publisher>Heidelberg: Springer Nature B.V</publisher><subject>Floodwater ; Hydrologic data ; Hydrology ; River basins ; Water consumption ; Water demand ; Water resources</subject><ispartof>Science China. Technological sciences, 2004, Vol.47 (8), p.127-141</ispartof><rights>Science in China Press 2004.</rights><rights>Copyright © Wanfang Data Co. Ltd. All Rights Reserved.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c319t-c21c5f7177f081bea0edb6676a05870f7df5f2d2b337d218e1d00efe4a18f883</citedby></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Uhttp://www.wanfangdata.com.cn/images/PeriodicalImages/zgkx-ee/zgkx-ee.jpg</thumbnail><link.rule.ids>314,780,784,4023,27922,27923,27924</link.rule.ids></links><search><creatorcontrib>NI, Jinren</creatorcontrib><title>On the variation of water resource structure in the Lower Yellow River</title><title>Science China. Technological sciences</title><description>In view of river functions and the Minimum Water Demand for River Ecosystem (MWDRE), the water resources in the Lower Yellow River is further divided into three portions, i.e. water available for ecosystem (WE), water exploitable for socioeconomic purposes (WS) and excess flood water (WF). Corresponding conceptions and practical significances are expounded in details. The annual amount of the three portions of water resources from 1950 to 2001 is worked out on the basis of the daily hydrologic data, and the division of different portions is discussed. The results indicate that although the essential water demand for river functions is considered preferentially, the amount of the WE has decreased dramatically while its proportion increased gradually since the 1950s, and the shortage to the MWDRE increased markedly; both the amount and the proportion of the WS decreased notably. Since the 1990s, the actual water consumption for socioeconomic purposes in the lower reaches of the river basin has already exceeded the maximum amount of the WS and has to take over the WE which is already insufficient, hence not only the normal river functions are further disturbed and the river course shrinks greatly, but also the proportion and potential danger of the WF show no decreasing tendency in spite of the sharp decrease of upstream runoff.</description><subject>Floodwater</subject><subject>Hydrologic data</subject><subject>Hydrology</subject><subject>River basins</subject><subject>Water consumption</subject><subject>Water demand</subject><subject>Water resources</subject><issn>1006-9321</issn><issn>1674-7321</issn><issn>1869-1900</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2004</creationdate><recordtype>article</recordtype><recordid>eNpdkE9LAzEQxYMoWKvgRwgI4mV1kuxuskcpVoVCQXrxFNLdSd3abmqy29V-eiP1D3iaGebHmzePkHMG10zkcAMp7gAYOyADpvIiYQXAYewB8qQQnB2TkxCWcQLO0wEZTxvaviDdGl-btnYNdZb2pkVPPQbX-RJpaH1Xtp1HWu_hievj_hlXK9fTp3qL_pQcWbMKePZdh2Q2vpuNHpLJ9P5xdDtJSsGKNik5KzMrmZQWFJujAazmeS5zA5mSYGVlM8srPhdCVpwpZBUAWkwNU1YpMSRXe9neNNY0C72MDpt4UO8Wr-8akQOkOxbfj-jlHt1499ZhaPW6DmW0bBp0XdBcCchyVUTw4h_4K8qlkrlQIoW_y6V3IXi0euPrtfEfmoH-Cl7_BC8-AU-idEI</recordid><startdate>2004</startdate><enddate>2004</enddate><creator>NI, Jinren</creator><general>Springer Nature B.V</general><general>Institute of Hydraulic Research,Yellow River Conservancy Commission,Zhengzhou 450003,China</general><general>The Key Laboratory of Water and Sediment Sciences, Ministry of Education,Beijing 100871,China</general><general>Department of Environmental Engineering, Peking University</general><scope>AAYXX</scope><scope>CITATION</scope><scope>8FD</scope><scope>FR3</scope><scope>KR7</scope><scope>2B.</scope><scope>4A8</scope><scope>92I</scope><scope>93N</scope><scope>PSX</scope><scope>TCJ</scope></search><sort><creationdate>2004</creationdate><title>On the variation of water resource structure in the Lower Yellow River</title><author>NI, Jinren</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c319t-c21c5f7177f081bea0edb6676a05870f7df5f2d2b337d218e1d00efe4a18f883</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2004</creationdate><topic>Floodwater</topic><topic>Hydrologic data</topic><topic>Hydrology</topic><topic>River basins</topic><topic>Water consumption</topic><topic>Water demand</topic><topic>Water resources</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>NI, Jinren</creatorcontrib><collection>CrossRef</collection><collection>Technology Research Database</collection><collection>Engineering Research Database</collection><collection>Civil Engineering Abstracts</collection><collection>Wanfang Data Journals - Hong Kong</collection><collection>WANFANG Data Centre</collection><collection>Wanfang Data Journals</collection><collection>万方数据期刊 - 香港版</collection><collection>China Online Journals (COJ)</collection><collection>China Online Journals (COJ)</collection><jtitle>Science China. Technological sciences</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>NI, Jinren</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>On the variation of water resource structure in the Lower Yellow River</atitle><jtitle>Science China. Technological sciences</jtitle><date>2004</date><risdate>2004</risdate><volume>47</volume><issue>8</issue><spage>127</spage><epage>141</epage><pages>127-141</pages><issn>1006-9321</issn><issn>1674-7321</issn><eissn>1869-1900</eissn><abstract>In view of river functions and the Minimum Water Demand for River Ecosystem (MWDRE), the water resources in the Lower Yellow River is further divided into three portions, i.e. water available for ecosystem (WE), water exploitable for socioeconomic purposes (WS) and excess flood water (WF). Corresponding conceptions and practical significances are expounded in details. The annual amount of the three portions of water resources from 1950 to 2001 is worked out on the basis of the daily hydrologic data, and the division of different portions is discussed. The results indicate that although the essential water demand for river functions is considered preferentially, the amount of the WE has decreased dramatically while its proportion increased gradually since the 1950s, and the shortage to the MWDRE increased markedly; both the amount and the proportion of the WS decreased notably. Since the 1990s, the actual water consumption for socioeconomic purposes in the lower reaches of the river basin has already exceeded the maximum amount of the WS and has to take over the WE which is already insufficient, hence not only the normal river functions are further disturbed and the river course shrinks greatly, but also the proportion and potential danger of the WF show no decreasing tendency in spite of the sharp decrease of upstream runoff.</abstract><cop>Heidelberg</cop><pub>Springer Nature B.V</pub><doi>10.1360/04ez0011</doi><tpages>15</tpages></addata></record> |
fulltext | fulltext |
identifier | ISSN: 1006-9321 |
ispartof | Science China. Technological sciences, 2004, Vol.47 (8), p.127-141 |
issn | 1006-9321 1674-7321 1869-1900 |
language | eng |
recordid | cdi_wanfang_journals_zgkx_ee2004z1011 |
source | Alma/SFX Local Collection; SpringerLink Journals - AutoHoldings |
subjects | Floodwater Hydrologic data Hydrology River basins Water consumption Water demand Water resources |
title | On the variation of water resource structure in the Lower Yellow River |
url | https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-01-08T13%3A48%3A57IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-wanfang_jour_proqu&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=On%20the%20variation%20of%20water%20resource%20structure%20in%20the%20Lower%20Yellow%20River&rft.jtitle=Science%20China.%20Technological%20sciences&rft.au=NI,%20Jinren&rft.date=2004&rft.volume=47&rft.issue=8&rft.spage=127&rft.epage=141&rft.pages=127-141&rft.issn=1006-9321&rft.eissn=1869-1900&rft_id=info:doi/10.1360/04ez0011&rft_dat=%3Cwanfang_jour_proqu%3Ezgkx_ee2004z1011%3C/wanfang_jour_proqu%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_pqid=2787638340&rft_id=info:pmid/&rft_wanfj_id=zgkx_ee2004z1011&rfr_iscdi=true |