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Oxygen and Hydrogen Isotopes of Waters in the Ordos Basin, China: Implications for Recharge of Groundwater in the North of Cretaceous Groundwater Basin
Author(s) -
YANG Yuncheng,
SHEN Zhaoli,
WENG Dongguang,
HOU Guangcai,
ZHAO Zhenhong,
WANG Dong,
PANG Zhonghe
Publication year - 2009
Publication title -
acta geologica sinica ‐ english edition
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.444
H-Index - 61
eISSN - 1755-6724
pISSN - 1000-9515
DOI - 10.1111/j.1755-6724.2009.00012.x
Subject(s) - groundwater recharge , groundwater , geology , meteoric water , precipitation , structural basin , isotopes of oxygen , δ18o , stable isotope ratio , hydrology (agriculture) , plateau (mathematics) , aquifer , geochemistry , geomorphology , geography , mathematical analysis , physics , geotechnical engineering , mathematics , quantum mechanics , meteorology
Hundreds of precipitation samples collected from meteorological stations in the Ordos Basin from January 1988 to December 2005 were used to set up a local meteoric water line and to calculate weighted average isotopic compositions of modern precipitation. Oxygen and hydrogen isotopes, with averages of –7.8‰ and –53.0‰ for δ 18 O and δD, respectively, are depleted in winter and rich in spring, and gradually decrease in summer and fall, illustrating that the seasonal effect is considerable. They also show that the isotopic difference between south portion and north portion of the Ordos Basin are not obvious, and the isotope in the middle portion is normally depleted. The isotope compositions of 32 samples collected from shallow groundwater (less than a depth of 150 m) in desert plateau range from –10.6‰ to –6.0‰ with an average of –8.4‰ for δ 18 O and from –85‰ to –46‰ with an average of –63‰ for δD. Most of them are identical with modern precipitation. The isotope compositions of 22 middle and deep groundwaters (greater than a depth of 275 m) fall in ranges from –11.6‰ to –8.8‰ with an average of –10.2‰ for δ 18 O and from –89‰ to –63‰ with an average of –76‰ for δD. The average values are significantly less than those of modern precipitation, illustrating that the middle and deep groundwaters were recharged at comparatively lower air temperatures. Primary analysis of 14 C shows that the recharge of the middle and deep groundwaters started at late Pleistocene. The isotopes of 13 lake water samples collected from eight lakes define a local evaporation trend, with a relatively flat slope of 3.77, and show that the lake waters were mainly fed by modern precipitation and shallow groundwater.