环境同位素在识别伊犁河谷地下水补给来源中的指示作用

doi:10.13686/j.cnki.dzyzy.2022.04.012

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Abstract This study analyzes the distribution characteristics of δD and δ¹⁸O in phreatic water, shallow confined water, spring water and surface water, as well as the δ¹³C of five groups of groundwater samples from hydrologic drilling wells. The results show that both groundwater and surface water originate from the local meteoric water. The phreatic water and shallow confined water, belonging to the same aquifer system, have a strong hydraulic connection. The age of deep confined water is about 20 ka, older than the shallow confined water, belonging to sedimentary buried water, with weak hydraulic relation between the two. The δ¹³C values of phreatic water and shallow confined water are close to each other, approximating that of atmospheric CO₂(-7‰) which serves as the main source of carbon in groundwater of the study area.

Key words： environmental isotope aquifer system δD-δ¹⁸O relation δ¹³C Ili River Valley Xinjiang

Received: 06 May 2021

PACS:

P641.3

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	Articles by authors
	SHAO Jie
	LI Ying
	LI Shu-cai
	TENG Chao
	YANG Xin-jie
	CAO Jun
	CHEN Xi-qing

Cite this article:

SHAO Jie,LI Ying,LI Shu-cai等. INDICATION OF ENVIRONMENTAL ISOTOPES IN IDENTIFYING THE GROUNDWATER RECHARGE SOURCES IN ILI RIVER VALLEY[J]. GEOLOGY AND RESOURCES, 2022, 31(4): 547-552.

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http://manu25.magtech.com.cn/Jweb_dzyzy/EN/10.13686/j.cnki.dzyzy.2022.04.012 OR http://manu25.magtech.com.cn/Jweb_dzyzy/EN/Y2022/V31/I4/547

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