石羊河流域降水稳定同位素变化的区域差异

Abstract
Figure/Table
References (42)
Related Citation (15)

Download: PDF (3492 KB) HTML (1 KB)
Export: BibTeX | EndNote (RIS)

Abstract

In order to better understand the changing process of precipitation stable isotope and its influencing factors in arid inland river basins, based on the oxyhydrogen stable isotope data and corresponding meteorological data of 497 precipitation samples from 8 stations in desert area, oasis area and mountain area of Shiyang river basin from July 2013 to July 2014, the spatiotemporal change, environmental effect and water vapor source of precipitation stable isotope of Shiyang river basin were studied. The slope and intercept of the local atmospheric water line in Shiyang river basin showed the trend of low in summer and high in winter. The stable isotope of precipitation showed the trend of high in summer and low in winter, the value of stable isotope decreased with the increase of altitude from desert area, oasis area to mountain area, and the altitude effect was -0.22‰/100m, which was another manifestation of the temperature effect. The stable isotopes of precipitation in the basin showed significant temperature effect with a variation range of 0.43‰/℃, and the precipitation effect was shown under the influence of monsoon water vapor and precipitation washing process on the weather scale. The source of precipitation in the basin was mainly controlled by the west wind water vapor, summer and winter will also be affected respectively by the monsoon water vapor and the polar air mass.

Key words： inland river basin Shiyang river precipitation stable isotope moisture source

Received: 18 March 2020

PACS:

X131.2

	Service

	E-mail this article
	Add to my bookshelf
	Add to citation manager
	E-mail Alert
	RSS
	Articles by authors
	YUAN Rui-feng
	JIA Wen-xiong
	LI Zong-xing
	XU Xiu-ting
	ZHANG Zhi-yuan
	SHI Yang
	YANG Le
	XIONG Hui

Cite this article:

YUAN Rui-feng,JIA Wen-xiong,LI Zong-xing等. Precipitation stable isotope regional difference in Shiyang River basin[J]. CHINA ENVIRONMENTAL SCIENCECE, 2020, 40(11): 4945-4956.

URL:

http://www.zghjkx.com.cn/EN/ OR http://www.zghjkx.com.cn/EN/Y2020/V40/I11/4945

[1]	康尔泗.西北干旱区内陆河流域SVAT系统和表层过程研究的一些进展[C]//中国地理学会学术年会暨海峡两岸地理学术研讨会, 2004:79-80. Kang E S. Advances in research on SVAT system and surface processes in the continental river basin in the arid area of Northwest China[C]//Academic Annual Meeting of The Geographical Society of China and Cross-Strait Geography Symposium, 2004:79-80.
[2]	Pang Z H, Kong Y Y, Froehlich K, et al. Processes affecting isotopes in precipitation of an arid region[J]. Tellus B, 2011,63(3):352-359.
[3]	Clark I D, Fritz P. Environmental isotopes in hydrogeology[M]. Boca Raton:CRC press, 1997.
[4]	Tian L D, Yao T D, MacClune K, et al. Stable isotopic variations in west China:A consideration of moisture sources[J]. Journal of Geophysical Research:Atmospheres, 2007,112(D10):1-12.
[5]	Yao T D, Masson-Delmotte V, Gao J, et al. A review of climatic controls on δ18O in precipitation over the Tibetan Plateau:Observations and simulations[J]. Reviews of Geophysics, 2013,51(4):525-548.
[6]	Dansgaard W. Stable isotopes in precipitation[J]. Tellus, 1964,16(4):436-468.
[7]	Dansgaard W. The abundance of 18O in atmospheric water and water vapor[J]. Tellus, 1953,5(4):461-469.
[8]	Gordon L. Deuterium and oxygen 18variations in the ocean and the marine atmosphere[A]. In:Tongiorgi E.Stable Isotopes in Oceanographic Studies and Paleotemperatures[M]. Pisa, Italy:CNR-Laboratorio di Geologia Nucleare, 1965:9-130.
[9]	黄天明,聂中青,袁利娟.西部降水氢氧稳定同位素温度及地理效应[J]. 干旱区资源与环境, 2008,22(8):76-81. Huang T M, Nie Z Q, Yuan L J. Temperature and geographical effects of hydrogen and oxygen isotopes in precipitation in West of China[J]. Journal of Arid Land Resources and Environment, 2008,22(8):76-81.
[10]	郭小燕,冯起,李宗省,等.敦煌盆地降水稳定同位素特征及水汽来源[J]. 中国沙漠, 2015,35(3):715-723. Guo X Y, Feng Q, Li Z X, et al. Variation of stable isotopes and moisture sources in precipitation at the Dunhuang basin in Northwest China[J]. Journal of Desert Research, 2015,35(3):715-723.
[11]	顾慰祖.同位素水文学[M]. 北京:科学出版社, 2011. Gu W Z. Isotope hydrology[M]. Beijing:Science Press, 2011.
[12]	冯芳,李忠勤,金爽,等.天山乌鲁木齐河流域山区降水δ18O和δD特征及水汽来源分析[J]. 水科学进展, 2013,24(5):634-641. Feng F, Li Z Q, Jin S, et al. Characteristics of the δ18O and δD in precipitation and its water vapor sources in the upper Urumqi River basin, Eastern Tianshan[J]. Advances in Water Science, 2013,24(5):634-641.
[13]	孙从建,张子宇,陈伟,等.亚洲中部高山降水稳定同位素空间分布特征[J]. 干旱区研究, 2019,36(1):22-31. Sun C J, Zhang Z Y, Chen W, et al. Spatial distribution of precipitation stable isotopes in the alpine zones in central asia[J]. Arid Zone Research, 2019,36(1):22-31.
[14]	Li Z X, Feng Q, Wang Q J, et al. Contributions of local terrestrial evaporation and transpiration to precipitation using δ18O and D-excess as a proxy in Shiyang inland river basin in China[J]. Global and Planetary Change, 2016,146:140-151.
[15]	Wang S J, Zhang M J, Hughes C E, et al. Meteoric water lines in arid Central Asia using event-based and monthly data[J]. Journal of hydrology, 2018,562:435-445.
[16]	Ma J Z, Zhang P, Zhu G F, et al. The composition and distribution of chemicals and isotopes in precipitation in the Shiyang River system, northwestern China[J]. Journal of Hydrology, 2012,436:92-101.
[17]	王宁练,张世彪,蒲健辰,等.黑河上游河水中δ18O季节变化特征及其影响因素研究[J]. 冰川冻土, 2008,30(6):914-920. Wang N L, Zhang S B, Pu J C, et al. Seasonal variation of δ18O in river water in the upper reaches of Heihe River basin and its influence factors[J]. Journal of Glaciology and Geocryology, 2008,30(6):914-920.
[18]	Jia W X, Ma X G, Xu X T, et al. Composition of stable isotope in precipitation and its influences by different vapor sources in the eastern Qilian Mountains[J]. Journal of Mountain Science, 2018, 15(10):122-132.
[19]	钟秀玲.石羊河流域径流特征分析[J]. 甘肃水利水电技术, 2011, 47(4):8-10. Zhong X L. Analysis of runoff characteristics in Shiyang River basin[J]. Gansu Water Conservancy and Hydropower Technology, 2011, 47(4):8-10.
[20]	Zhang W G, Cheng B, Hu Z B, et al. Using stable isotopes to determine the water sources in alpineecosystems on the east Qinghai-Tibet plateau, China[J]. Hydrological Process, 2010,24(22):3270-3280.
[21]	Niu L, Ye B S, Li J, et al. Effect of permafrost degradation on hydrological processes in typical basins with various permafrost coverage in Western China[J]. Science in China Series D:Earth Sciences, 2011,54(4):615-624.
[22]	王兴梅,张勃,王海军,等.石羊河流域近50年最高最低气温变化分析[J]. 干旱区地理, 2010,33(6):879-888. Wang X M, Zhang B, Wang H J, et al. Maximum and minimum temperature changes in Shiyang River basin in the last 50years[J]. Arid Land Geography, 2010,33(6):879-888.
[23]	文星,王涛,薛娴,等.1975~2010年石羊河流域绿洲时空演变研究[J]. 中国沙漠, 2013,33(2):478-485. Wen X, Wang T, Xue X, et al. Spatial-temporal evolution of the oasis in Shiyanghe River basin in 1975~2010[J]. Journal of Desert Research, 2013,33(2):478-485.
[24]	袁瑞丰,李宗省,蔡玉琴,等.干旱内陆河流域降水稳定同位素的时空特征及环境意义[J]. 环境科学, 2019,40(5):2122-2131. Yuan R F, Li Z X, Cai Y Q, et al.Space-time characteristics and environmental siginificance of stable isotopes in precipitation at an arid inland river basin[J]. Environmental Sciences, 2019,40(5):2122-2131.
[25]	侯典炯,秦翔,吴锦奎,等.乌鲁木齐大气降水稳定同位素与水汽来源关系研究[J]. 干旱区资源与环境, 2011,25(10):136-142. Hou D J, Qin X, Wu J K, et al. Characteristics of stable isotopes in precipitation and the water vapor sources in Urumqi[J]. Journal of Arid Land Resources and Environment, 2011,25(10):136-142.
[26]	Zhao L J, Yin L, Xiao H L, et al. Isotopic evidence for the moisture origin and composition of surface runoff in the headwaters of the Heihe River basin[J]. Chinese Science Bulletin, 2011,56(4/5):406-416.
[27]	Li Z X, Feng Q, Liu W, et al. Study on the contribution from cryosphere to runoff in the cold alpine basin:a case study of Hulugou River basin in the Qilian Mountains[J]. Global and Planetary Change, 2014,122:345-361.
[28]	郭小燕.基于稳定同位素和水化学的疏勒河流域水文过程研究.[D]. 兰州:中国科学院寒区旱区环境与工程研究所, 2015. Guo X Y. Study on the hydrological processes in Shule River basin by using isotopic tracers and hydro-chemical method[D]. Lanzhou, Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, 2015.
[29]	Wu J K, Ding Y J, Ye B S. Spatio-temporal variation of stable isotopes in precipitation in the Heihe River basin, Northwestern China[J]. Environmental Earth Sciences, 2010,61(6):1123-1134.
[30]	Liu J S, Xie J, Gong T L, et al. Impacts of winter warming and permafrost degradation on water variability, upper Lhasa River, Tibet[J]. Quaternary International, 2011,244(2):178-184.
[31]	高前兆,李小雁,仵彦卿,等.河西内陆河流域水资源转化分析[J]. 冰川冻土, 2004,26(1):48-54. Gao Q Z, Li X Y, Wu Y Q, et al. Analysis of water cycle in inland river basins in Hexi Region[J]. Journal of Glaciology and Geocryology, 2004,26(1):48-54.
[32]	刘忠方,田立德,姚檀栋,等.中国大气降水中δ18O的空间分布[J]. 科学通报, 2009,54(6):804-811. Liu Z F, Tian L D, Yao T D, et al. Spatial distribution of δ18O in precipitation over China (in Chinese)[J]. Chinese Sci Bull (Chinese Ver), 2009,54(6):804-811.
[33]	Bowen G J, Wilkinson B. Spatial distribution of δ18O in meteoric precipitation[J]. Geology, 2002,30(4):315-318.
[34]	Gonfiantini R, Roche M A, Olivry J C, et al. The altitude effect on isotopic composition of tropical rains[J]. Chemical Geology, 2001, 181(1-4):147-167.
[35]	Yao T D, Thompson L G, Jiao Keqin. Recent warming as recorded in the Qinghai Tibetan cryosphere[J]. Annals of Glaciology, 1995,21:196-200.
[36]	Li Z X, Gao Y, Wang Y M, et al. Can monsoon moisture arrive Qilian Mountains in summer?[J]. Quaternary international, 2015,358:113-125.
[37]	Yu T F, Feng Q, Si J H, et al. Hydraulic redistribution of soil water by roots of two desert riparian phreatophytes in northwest China's extremely arid region[J]. Plant and Soil, 2013,372(1/2):297-308.
[38]	孟玉川,刘国东.长江流域降水稳定同位素的云下二次蒸发效应[J]. 水科学进展, 2010,21(3):327-334. Meng Y C, Liu G D. Effect of below-cloud secondary evaporation on the stable isotopes in precipitation over the Yangtze River basin[J]. Advances In Water Science, 2010,21(3):327-334.
[39]	王圣杰.天山地区降水稳定同位素特征及其再水循环过程中的指示意义[D]. 兰州:西北师范大学, 2015. Wang S J. Stable hydrogen and oxygen isotopes in precipitation of the Tianshan Mountains and their significance in hydrological cycle[D]. Lanzhou:Northwest Normal University, 2015.
[40]	Zhao W, Ma J Z, Gu C J, et al. Distribution of isotopes and chemicals in precipitation in Shule River basin, northwestern China:an implication for water cycle and groundwater recharge[J]. Journal of Arid Land, 2017,8(2):318-318.
[41]	Wang S J, Zhang M J, Crawford J, et al. The effect of moisture source and synoptic conditions on precipitation isotopes in arid central Asia[J]. Journal of Geophysical Research:Atmospheres, 2017,122(5):2667-2682.
[42]	Karl J K, Cameron P W, Vladimir B A, et al. Seasonal deuterium excess in a Tien Shan ice core:Influence of moisture transport and recycling in Central Asia[J].Geophysical Research Letters, 2003, 30(18):1-4.