Please use this identifier to cite or link to this item: http://hdl.handle.net/11455/93619
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dc.contributor.authorBehzod Gaybullaeven_US
dc.contributor.authorSu-Chin Chenen_US
dc.contributor.other國立中興大學農學院zh_TW
dc.date2013-03-01en_US
dc.date.accessioned2016-04-18T06:56:10Z-
dc.date.available2016-04-18T06:56:10Z-
dc.identifier.urihttp://hdl.handle.net/11455/93619-
dc.description.abstractThe Amu Darya is the most important river in Central Asia, as the river water used for agricultural, industrial and domestic purposes. The Kelif, Kerki, Chardjow, Darganata, Kipchak, Takhiatash, and Samanbay gauging stations (g/s) are located in the Amu Darya River. The water salinity of the Amu Darya River at the Kelif, Chardjow, and Darganata g/s were decreased from 0.649-0.469, 0.823-0.614, and 0.99-0.696 g/ℓ to 1991-2010; at the Takhiatash, and Samanbay g/s has been raised from 1.218-1.562, and 1.126-1.46 g/ℓ to 1991-2000. We have predicted the seven gauging stations along the river water salinity from 2010 to 2020 used by the Holt's Linear Trend Forecasts Method, and the results are then applied in the prediction of water salinity. The forecast suggested that the Amu Darya river water salinity of the Kelif g/s will be increased to around 0.495 g/ℓ in 2020; of the Kerki, Chardjow, Darganata, Kipchak, Takhiatash, and Samanbay g/s will decreases to approximately 0.483, 0.602, 0.668, 0.484, 1.104, and 0.825 g/ℓ by 2020.en_US
dc.language.isoen_USen_US
dc.publisher臺中巿: 國立中興大學農學院zh_TW
dc.relation農林學報, Volume 62, Issue 1, Page(s) 1-13.zh_TW
dc.subjectAmu darya riveren_US
dc.subjectAral seaen_US
dc.subjectSalinityen_US
dc.titleWater Salinity Changes of the Gauging Stations along the Amu Darya Riveren_US
dc.typeJournal Articlezh_TW
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.languageiso639-1en_US-
item.grantfulltextopen-
item.cerifentitytypePublications-
item.openairetypeJournal Article-
item.fulltextwith fulltext-
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