Research on the hydrologic cycle characteristics using stable isotopes of oxygen and hydrogen in the Jinxiuchuan Basin

Wang, T., Xu, Z., Zhang, S., Zhang, L., & Zhao, Z. (MarchApril, 2017). Research on the hydrologic cycle characteristics using stable isotopes of oxygen and hydrogen in the Jinxiuchuan Basin. Water Technology and Sciences (in Spanish), 8(2), 105-115. Stable isotopes of oxygen (δ18O) and hydrogen...

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Main Authors: Wang Tong, Xu Zhenghe, Zhang Shengdong, Zhang Lizhi, Zhao Zhiqiang
Format: Article
Language:English
Published: Instituto Mexicano de Tecnología del Agua 2017-08-01
Series:Tecnología y ciencias del agua
Subjects:
Online Access:https://www.revistatyca.org.mx/ojs/index.php/tyca/article/view/1311
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author Wang Tong
Xu Zhenghe
Zhang Shengdong
Zhang Lizhi
Zhao Zhiqiang
author_facet Wang Tong
Xu Zhenghe
Zhang Shengdong
Zhang Lizhi
Zhao Zhiqiang
author_sort Wang Tong
collection DOAJ
description Wang, T., Xu, Z., Zhang, S., Zhang, L., & Zhao, Z. (MarchApril, 2017). Research on the hydrologic cycle characteristics using stable isotopes of oxygen and hydrogen in the Jinxiuchuan Basin. Water Technology and Sciences (in Spanish), 8(2), 105-115. Stable isotopes of oxygen (δ18O) and hydrogen (δD) in water were used as important indicators to research the hydrologic cycle or processes. To study the hydrologic cycle characteristics of the Jinxiuchuan basin, the isotope labelling and the industrial salt tracing method were used in this research. Sixty-seven samples of different water bodies were collected at different sampling sites from July 2011 to July 2012. The stable hydrogen and oxygen isotopes in water samples were measured by using Liquid Water Isotope Analyzer (LWIA-24d) to study the conversion relationship among precipitation, river water, soil water, and groundwater of the Jinxiuchuan basin in Jinan. The results show that δD and δ18O varied from 35.6 ‰ to 128.3 ‰ and from 5.3 ‰ to 17.5‰, respectively. A meteoric water line of δD = 7.16δ18O + 4.35‰, which was in accordance with the global meteoric water line and the meteoric water line of China, was established in the Jinxiuchuan basin. The deuterium excess values vary with time and space, ranging from 5.1 to 22.3‰, and increase gradually from the southeast to the northwest. In addition, the exchange of different water bodies was determined preliminarily, the rates of precipitation transforming into river water, soil water, and groundwater are 43.76%, 21.91% and 6.84%, and the remaining is 27.49% returned to the atmosphere. The results indicated the hydrologic cycle characteristics in the Jinxiuchuan basin. It may provide the references for precipitation isotopes research in semi-humid regions.
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spelling doaj.art-f4d2db90d0d241d1a4baa18ae57b48df2023-12-14T17:15:06ZengInstituto Mexicano de Tecnología del AguaTecnología y ciencias del agua0187-83362007-24222017-08-018210511510.24850/j-tyca-2017-02-101198Research on the hydrologic cycle characteristics using stable isotopes of oxygen and hydrogen in the Jinxiuchuan BasinWang Tong0Xu Zhenghe1Zhang Shengdong2Zhang Lizhi3Zhao Zhiqiang4University of Jinan, ChinaUniversity of Jinan, ChinaBeijing Zhongshui Runke Certification Co., Ltd., ChinaUniversity of Jinan, ChinaUniversity of Jinan, ChinaWang, T., Xu, Z., Zhang, S., Zhang, L., & Zhao, Z. (MarchApril, 2017). Research on the hydrologic cycle characteristics using stable isotopes of oxygen and hydrogen in the Jinxiuchuan Basin. Water Technology and Sciences (in Spanish), 8(2), 105-115. Stable isotopes of oxygen (δ18O) and hydrogen (δD) in water were used as important indicators to research the hydrologic cycle or processes. To study the hydrologic cycle characteristics of the Jinxiuchuan basin, the isotope labelling and the industrial salt tracing method were used in this research. Sixty-seven samples of different water bodies were collected at different sampling sites from July 2011 to July 2012. The stable hydrogen and oxygen isotopes in water samples were measured by using Liquid Water Isotope Analyzer (LWIA-24d) to study the conversion relationship among precipitation, river water, soil water, and groundwater of the Jinxiuchuan basin in Jinan. The results show that δD and δ18O varied from 35.6 ‰ to 128.3 ‰ and from 5.3 ‰ to 17.5‰, respectively. A meteoric water line of δD = 7.16δ18O + 4.35‰, which was in accordance with the global meteoric water line and the meteoric water line of China, was established in the Jinxiuchuan basin. The deuterium excess values vary with time and space, ranging from 5.1 to 22.3‰, and increase gradually from the southeast to the northwest. In addition, the exchange of different water bodies was determined preliminarily, the rates of precipitation transforming into river water, soil water, and groundwater are 43.76%, 21.91% and 6.84%, and the remaining is 27.49% returned to the atmosphere. The results indicated the hydrologic cycle characteristics in the Jinxiuchuan basin. It may provide the references for precipitation isotopes research in semi-humid regions.https://www.revistatyca.org.mx/ojs/index.php/tyca/article/view/1311stable isotopes of hydrogen and oxygenprecipitationdeuterium excessjinxiuchuan basin
spellingShingle Wang Tong
Xu Zhenghe
Zhang Shengdong
Zhang Lizhi
Zhao Zhiqiang
Research on the hydrologic cycle characteristics using stable isotopes of oxygen and hydrogen in the Jinxiuchuan Basin
Tecnología y ciencias del agua
stable isotopes of hydrogen and oxygen
precipitation
deuterium excess
jinxiuchuan basin
title Research on the hydrologic cycle characteristics using stable isotopes of oxygen and hydrogen in the Jinxiuchuan Basin
title_full Research on the hydrologic cycle characteristics using stable isotopes of oxygen and hydrogen in the Jinxiuchuan Basin
title_fullStr Research on the hydrologic cycle characteristics using stable isotopes of oxygen and hydrogen in the Jinxiuchuan Basin
title_full_unstemmed Research on the hydrologic cycle characteristics using stable isotopes of oxygen and hydrogen in the Jinxiuchuan Basin
title_short Research on the hydrologic cycle characteristics using stable isotopes of oxygen and hydrogen in the Jinxiuchuan Basin
title_sort research on the hydrologic cycle characteristics using stable isotopes of oxygen and hydrogen in the jinxiuchuan basin
topic stable isotopes of hydrogen and oxygen
precipitation
deuterium excess
jinxiuchuan basin
url https://www.revistatyca.org.mx/ojs/index.php/tyca/article/view/1311
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AT zhanglizhi researchonthehydrologiccyclecharacteristicsusingstableisotopesofoxygenandhydrogeninthejinxiuchuanbasin
AT zhaozhiqiang researchonthehydrologiccyclecharacteristicsusingstableisotopesofoxygenandhydrogeninthejinxiuchuanbasin