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Oxygen and hydrogen isotopic ratios and chemistry in semiarid land river water, Southwest Victoria, Australia

II, Hiroyuki, Sherwood, John, Stagnitti, Frank, Turoczy, Nicholas, Hirata, Tatemasa and Nishikawa, Masataka 2002, Oxygen and hydrogen isotopic ratios and chemistry in semiarid land river water, Southwest Victoria, Australia, Journal of the Japan Society of Civil Engineers, vol. 791, pp. 1-9.

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Title Oxygen and hydrogen isotopic ratios and chemistry in semiarid land river water, Southwest Victoria, Australia
Author(s) II, Hiroyuki
Sherwood, John
Stagnitti, Frank
Turoczy, Nicholas
Hirata, Tatemasa
Nishikawa, Masataka
Journal name Journal of the Japan Society of Civil Engineers
Volume number 791
Start page 1
End page 9
Publisher Doboku Gakkai
Place of publication Tokyo, Japan
Publication date 2002
ISSN 0021-468X
Summary Salt in a salt lake accumulated as a result of perfect evaporation of inflow water during the dry season. Water in a salt lake had a high salinity and its isotope indicated a little evaporation in the wet season because precipitation replenished the salt lake and there was no residual water during evaporation process in salt lake. In a marsh, both perfect and partial disappearance of water by repeated evaporation and water supply from upstream contributed to high salinity and high isotopic ratios because residual water had high isotopic ratios and dried areas accumulated salt. On the other hand, salinity and isotopic ratios depended on ratio of evaporation and water supply during evaporation excluding perfect disappearance of water.
Language eng
Field of Research 079901 Agricultural Hydrology (Drainage, Flooding, Irrigation, Quality, etc)
HERDC Research category C1.1 Refereed article in a scholarly journal
Persistent URL http://hdl.handle.net/10536/DRO/DU:30009497

Document type: Journal Article
Collection: School of Ecology and Environment
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