漓江流域δD和δ18O对蒸发的指示作用

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Abstract

The stable isotope compositon of water (δD and δ¹⁸O) were collected in November 2018 and March 2019 along the Lijiang River to estimate their indication of the evaporation. The results showed that:the δD and δ¹⁸O values had different composition characteristics among different sampling sietes in the the Lijiang River, the δD and δ¹⁸O values of groundwater was smaller than those of surface water, the δD and δ¹⁸O values in the wet season were easier to enrich than in the dry season; The variation trend of δ¹⁸O value was more obvious than d-excess under the increasing of water temperature. The elevation gradually decreased from the upstream to the downstream, and the slope and intercept of Lijaing River water line also gradually decreased; Underground river water line and Lijiang River water line were closely to local meteoric water line(LMWL), indicating that there was a close hydraulic connection between underground river, Lijiang River and precipitation in the study area. Due to the influence of temperature and humidity, the evaporation proportion of Lijiang River in wet season and dry season were 0.7%~9.1%,2.6%~9.7%, respectively; The evaporation proportion from upstream to downstream gradually increased in the study area, regardless of in wet season or dry season. The evaluated evaporation value based on isotope mass balance model in the study area was 959.40mm, which was less 43.11mm than the multi-year monitoring data, with the relative error of 4.70%; Using stable isotopes (δD and δ¹⁸O) is an essential method to study the hydrological cycle in a river basin, thus stable isotope still has a wide application space in hydrological cycle in Lijiang River Basin.

Key words： δD δ¹⁸O evaporation hydrologic process Lijiang River Basin

Received: 25 September 2019

PACS:	X522
	P339

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	Articles by authors
	REN Meng-meng
	HUANG Fen
	HU Xiao-nong
	CAO Jian-hua
	ZHANG Peng
	LIANG Jian-hong
	ZHANG Jin

Cite this article:

REN Meng-meng,HUANG Fen,HU Xiao-nong等. The composition characteristics of hydrogen and oxygenstable isotopes as an indicator of evaporation in the River Lijiang, China[J]. CHINA ENVIRONMENTAL SCIENCECE, 2020, 40(4): 1637-1648.

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http://www.zghjkx.com.cn/EN/ OR http://www.zghjkx.com.cn/EN/Y2020/V40/I4/1637

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