[1]刘澄静,角媛梅*,刘志林,等.哈尼梯田区降水稳定氢氧同位素的旱雨季变化特征及其影响因素[J].山地学报,2018,(04):519-526.[doi:10.16089/j.cnki.1008-2786.000348]
　LIU Chengjing,JIAO Yuanmei*,LIU Zhilin,et al.Seasonal Variations of Precipitation Stable Hydrogen and Oxygen Isotope in Hani Rice Terraces and Its Influencing Factors[J].Mountain Research,2018,(04):519-526.[doi:10.16089/j.cnki.1008-2786.000348]
点击复制

哈尼梯田区降水稳定氢氧同位素的旱雨季变化特征及其影响因素()
分享到：

《山地学报》[ISSN:1008-2186/CN:51-1516]

卷:
期数:
2018年04期
页码:
519-526
栏目:
山地环境
出版日期:
2018-07-30

文章信息/Info

Title:
Seasonal Variations of Precipitation Stable Hydrogen and Oxygen Isotope in Hani Rice Terraces and Its Influencing Factors
文章编号:
1008-2786-(2018)4-519-08
作者:
刘澄静; 角媛梅*; 刘志林; 刘 歆; 高 璇
云南师范大学 旅游与地理科学学院,昆明 650500
Author(s):
LIU Chengjing;  JIAO Yuanmei*;  LIU Zhilin;  LIU Xin;  GAO Xuan
School of Tourism and Geographical Sciences Yunnan Normal University, Kunming 650500, China
关键词:
哈尼梯田区;  降水;  氢氧同位素;  旱雨季;  相关性分析
Keywords:
Hani Rice Terraces;  precipitation;  hydrogen and oxygen isotope;  dry and wet season;  correlation analysis
分类号:
P426.6
DOI:
10.16089/j.cnki.1008-2786.000348
文献标志码:
A
摘要:
水的稳定同位素(D 和O)是水文过程的重要示踪剂。本文以哈尼梯田文化景观遗产核心区全福庄河扇形小流域为研究对象,通过采集流域内雨季和旱季的大气降水样品,并测定和分析氢氧同位素值(D和δ18O),得出以下结论:(1)研究区全年大气降水线方程为:δD=8.35δ18O+22.41(R2=0.98,n=48),但年内旱季和雨季降水线方程的斜率和截距差异明显。(2)研究区大气降水中氢氧稳定同位素组成具有明显季节差异,雨季降水中氢氧同位素贫化,d值偏低; 旱季降水氢氧同位素值相对偏正,d值偏高,这与我国季风区旱雨季水汽来源差异有关。(3)根据相关分析可知,温度、降水和相对湿度3个要素的变化是研究区降水同位素值变化的主要影响因素,但在不同的时间尺度下影响降水同位素变化的环境因素存在差异。(4)在年尺度下降水和相对湿度是主要的影响因素; 在旱雨季尺度下,温度是雨季降水同位素值变化的主要因素,而温度、降水量和相对湿度对旱季降水同位素值变化的影响则不显著,旱季降水同位素δ18O值变化为三因素共同作用的结果。
Abstract:
The stable isotopes of water(D and O)are important tracers for hydrological processes.In this paper it took a fan-shaped watershed of the Quanfuzhuang River located at the core zone of the cultural landscape heritage of Hani Rice Terraces in Yunnan, China as the research object, where 48 atmospheric precipitation samples in this basin were collected in rainy seasons and dry seasons separately, and then they were tested and analyzed for hydrogen and oxygen isotopes(δD and δ18O)comparison.Conclusions were drawn:(1)The meteoric water line equation for a year was: δD=8.35δ18O+22.41(R2=0.98, n=48), and graphically the slopes and intercepts of the equation for dry season were quite different from those for rainy season.(2)There was an obvious seasonal variation in the composition of precipitation hydrogen and oxygen stable isotope.During the rainy season they were lean with low d values, whereas in the dry seasons they were relatively positive with higher d values, suggesting that the differences were ascribable to the seasonal changes in the moisture sources of China monsoon regions.(3)Correlation analysis revealed that temperature, precipitation, and relative humidity were the main three factors affecting the changes in precipitation isotope values, but they changed in response to different time scales.At an annual scale they were precipitation and relative humidity, but in rainy season it was only temperature significant.As for a dry season they were attributed to a combination of all the three factors.

参考文献/References:

[1] 顾慰祖,庞忠和,王全九,等.同位素水文学[M].北京:科学出版社,2011:105-144 [GU Weizu, PANG Zhonghe, WANG Quanjiu, et al.Isotope hydrology[M].Beijing: Science Press, 2011:105-144]
[2] 李晖,周宏飞.乌鲁木齐地区大气降水中δD和δ18O的变化特征[J].干旱区资源与环境, 2007,21(09):46-50 [LI Hui, ZHOU Hongfei.Variation characteristics of δD and δ18O stable isotope in the precipitation of Urumqi[J].Journal of Arid Land Resources and Environment, 2007,21(09): 46-50]
[3] KOSTER R D, JOUZEL J, SUOZZO R, et al.Global sources of local precipitation as determined by the NASS/GISS GCM[J].Geophysical Research Letters, 1986, 13(2):121-124
[4] 李亚举,张明军,王圣杰,等.我国大气降水中稳定同位素研究进展[J].冰川冻土, 2011,33(3):624-633 [LI Yaju, ZHANG Mingjun, WANG Shengjie, et al.Progress of the research of stable isotope in precipitation in China: a review[J].Journal of Glaciology and Geocryology, 2011,33(3):624-633]
[5] 庞朔光,赵诗坤,文蓉,等.海河流域大气降水中稳定同位素的时空变化[J].科学通报, 2015,60(13):1218-1226 [ PANG Shuoguang, ZHAO Shikun, WEN Rong, et al.Spatial and temporal variation of stable isotopes in precipitation in the Haihe River basin.Chinese Science Bulletin, 2015, 60(13): 1218-1226]
[6] 刘鑫,宋献方,夏军,等.黄土高原岔巴沟流域降水氢氧同位素特征及水汽来源初探[J].资源科学,2007,29(3):29-66 [ LIU Xin, SONG Xianfan, XIA Jun, et al.Characteristics of hydrogen and oxygen isotopes and preliminary analysis of vapor source for precipitation in Chabagou Catchment of the Loess Plateau[J].Resources Science,2007,29(3):29-66]
[7] ARAGUASARAGUAS L, FROEHLICH K, ROZANSKI K.Stable isotope composition of precipitation over southeast Asia[J].Journal of Geophysical Research,1998,130(D22): 28721-28742
[8] JOHNSON K R, INGRAM B L.Spatial and temporal variability in the stable isotope systematics of modern precipitation in China: implications for paleoclimate reconstructions[J].Earth and Planetary Science Letters, 2004,220(3):365-377
[9] LIU Z, TIAN L, CHAI X, et al.A model-based determination of spatial variation of precipitation δ18O over China[J].Chemical Geology, 2008,249(1-2): 203-212
[10] 郭政昇,王娟,赵培.珠江流域大气降水稳定性氢氧同位素特征[J].水文,2017,37(02):78-82 [GUO Zhengsheng, WANG Juan, ZHAO Pei.Characteristics of hydrogen and oxygen stable isotopes in precipitation in Pearl River Basin[J].Journal of China Hydrology,2017,37(02): 78-82]
[11] 柳鉴容,宋献方,袁国富,等.中国东部季风区大气降水δ18O的特征及水汽来源[J].科学通报,2009,54(22):3521-3531 [LIU Jianrong, SONG Xianfang, YUAN Guofu, et al.Characteristics of δ18O in precipitation over Eastern Monsoon China and the water vapor sources [J].Chinese Sci Bull,2009,54(22):3521-3531]
[12] 角媛梅.哈尼梯田自然与文化景观生态研究[M].北京:中国环境科学出版社,2009:1-12 [JIAO Yuanmei.Natural and cultural landscape ecology of Hani Rice Terraces[M].Beijing: Chinese Environmental Science Press.2009:1-12]
[13] 张贵玲,角媛梅,刘澄静,等.哈尼梯田麻栗寨河流域雨季大气降水氢氧同位素特征及影响因素[J].冰川冻土,2016,38(06):1701-1709 [ZHANG Guiling, JIAO Yuanmei, LIU Chengjing,et al.Hydrogen and oxygen isotopic of precipitation during the rainy season of the Malizhai River basin in Hani terraces: characteristics and impact factors[J].Journal of Glaciology and Geocryology,2016,38(06):1701-1709]
[14] 刘澄静,角媛梅,张贵玲,等.哈尼梯田麻栗寨河流域泉水氢氧同位素的海拔效应[J].冰川冻土,2016,38(05):1404-1410 [LIU Chengjing, JIAO Yuanmei, ZHANG Guiling, et al.Altitude effect of hydrogen and oxygen isotopes in spring water of the Malizhai River basin, Hani terrace[J].Journal of Glaciology and Geocryology,2016,38(05): 1404-1410]
[15] 角媛梅,刘澄静,刘歆,等.哈尼梯田区优势景观类型对泉水氢氧同位素效应的影响[J].应用生态学报,2017,28(07):2299-2306 [JIAO Yuanmai, LIU Chengjing, LIU Xin, et al.Impacts of dominated landscape types on hydrogen and oxygen isotope effects of spring water in the Hani Rice Terraces[J].Chinese Journal of Applied Ecology,2017,28(07): 2299-2306]
[16] 章新平,关华德,孙治安,等.云南降水中稳定同位素变化的模拟和比较[J].地理科学,2012,32(01):121-128 [ZHANG Xinping, GUAN Huade, SUN Zhian, et al.Simulations of stable isotopic variations in precipitation and comparison with measured values in Yunnan Province,China[J].Scientia Geographica Sinica,2012, 32(01):121-128]
[17] 庞洪喜,何元庆,卢爱刚,等.天气尺度下丽江季风降水中δ18O变化[J].科学通报,2006,51(10):1218-1224 [PANG Hongxi, HE Yuanqing, LU Aigang, et al.Synoptic-scalevariation of δ18O in summer monsoon rainfall at Lijiang, China[J].Chinese Science Bulletin,2006,51(10): 2897-2904]
[18] 陈曦,李志,程立平,等.黄土塬区大气降水的氢氧稳定同位素特征及水汽来源[J].生态学报,2016,36(01):98-106 [CHEN Xi, LI Zhi, CHENG Liping, et al.Analysis of stable isotopic composition and vapor source of precipitation at the Changwu Loess Tableland[J].Acta Ecologica Sinica, 2016,36(01):98-106]
[19] 林光辉.稳定同位素生态学[M].北京:高等教育出版社,2013:58-75 [LIN Guanghui.Stable isotope ecology[M].Beijing: Higher Education Press, 2013:58-75]
[20] 于静洁,宋献方,刘相超,等.基于δ(D)和δ(O18)及水化学的永定河流域地下水循环特征解析[J].自然资源学报.2007,22(3):415-421[ YU Jingjie, SONG Xianfang, LIU Xiangchao, et al.A Study of groundwater cycle in Yongding River Basin by using d δD, δ18O and Hydrochemical Data[J].Journal of Natural Resources.2007,22(3):415-421]
[21] 庞洪喜,何元庆,张忠林.新德里季风降水中过量氘与季风水汽来源[J].冰川冻土,2005,27(06):876-880 [PANG Hongxi, HE Yuanqing, ZHANG Zhonglin.Correlation between deuterium excess in monsoon precipitation of New Delhi and the origin of precipitation[J].Journal of Glaciology and Geocryology,2005,27(06): 876-880]
[22] 胡海英,黄华茂,杨健文.香港地区降水氢氧同位素多尺度演变特征分析[J].武汉大学学报(工学版),2014,47(05):577-584,620 [HU Haiying, HUANG Huamao, YANG Jianwen.Multi time scale variation of hydrogen and oxygen in precipitation under changing environment in Hong Kong area[J].Engineer Journal of Wuhan University,2014,47(05):577-584,620]
[23] 刘忠方,田立德,姚檀栋,等.雅鲁藏布江流域降水中δ18O的时空变化[J].地理学报,2007,62(05):510-517 [LIU Zhongfang, TIAN Lide,YAO Tandong, et al.Variations of δ18O in precipitation of the Yarlung Zangbo River Basin[J].Acta Geographica Sinica,2007,62(05):510-517
[24] 张琳,陈宗宇,聂振龙,等.我国不同时间尺度的大气降水氧同位素与气温的相关性分析[J].核技术,2008,31(09):715-720 [ZHANG Lin, CHEN Zongyu, NIE Zhenlong, et al.Correlation between δ18O in precipitation and surface air temperature on different time-scale in China[J].Nuclear Techniques,2008,31(09):715-720]

相似文献/References:

[1]沈志强,卢 杰*,华 敏,等.西藏拉萨达孜夏季降水日变化特征[J].山地学报,2016,(04):409.[doi:10.16089/j.cnki.1008-2786.000145]
　SHEN Zhiqiang,LU Jie,HUA Min,et al.Diurnal Variation of Precipitation in Summer in Dazi County of Tibet[J].Mountain Research,2016,(04):409.[doi:10.16089/j.cnki.1008-2786.000145]
[2]宋海凤,张 胜*.杨柳科植物随环境变化的性别响应差异[J].山地学报,2017,(05):645.[doi:10.16089/j.cnki.1008-2786.000263]
　SONG Haifeng,ZHANG Sheng.Sex-Related Responses to Environmental Changes in Salicaceae[J].Mountain Research,2017,(04):645.[doi:10.16089/j.cnki.1008-2786.000263]
[3]王 涛,白红英*.秦岭山地植被NDVI对气候变化与人类活动的响应[J].山地学报,2017,(06):778.[doi:10.16089/j.cnki.1008-2786.000278]
　WANG Tao,,et al.Variation of Vegetation NDVI in Response to Climate Changesand Human Activities in Qinling Mountains[J].Mountain Research,2017,(04):778.[doi:10.16089/j.cnki.1008-2786.000278]
[4]徐 飞,贾仰文*,牛存稳,等.横断山区气温和降水年季月变化特征[J].山地学报,2018,(02):171.[doi:10.16089/j.cnki.1008-2786.000313]
　XU Fei,JIA Yangwen*,et al.Variation Character of Annual, Seasonal and Monthly Temperature and Precipitation[J].Mountain Research,2018,(04):171.[doi:10.16089/j.cnki.1008-2786.000313]
[5]梅 静,王 建,何 亮,等.川西甘孜州1961-2015年气温和降水时空变化特征研究[J].山地学报,2019,(02):161.[doi:10.16089/j.cnki.1008-2786.000410]
　MEI Jing,WANG Jian,HE Liang,et al.Spatio-temporal Variations of Temperature and Precipitation in Ganzi of Western Sichuan in China during 1961-2015[J].Mountain Research,2019,(04):161.[doi:10.16089/j.cnki.1008-2786.000410]
[6]陈 志a,杨志全b*,刘传秋.云南省麻栗坡县猛硐河“9.02”泥石流调查[J].山地学报,2019,(04):631.[doi:10.16089/j.cnki.1008-2786.000454]
　CHEN Zhia,YANG Zhiquan b*,LIU Chuanqiu.Investigation of the “9.02” Debris Flows in Mengdong River,Malipo County, Yunnan, China[J].Mountain Research,2019,(04):631.[doi:10.16089/j.cnki.1008-2786.000454]
[7]周苏娥,张明军*,王圣杰,等.甘肃夏季降水同位素云下二次蒸发效应[J].山地学报,2019,(6):808.[doi:10.16089/j.cnki.1008-2786.000471]
　ZHOU Su'e,ZHANG Mingjun*,WANG Shengjie,et al.Sub-cloud Secondary Evaporation in Summer Precipitation Isotope in Gansu, China[J].Mountain Research,2019,(04):808.[doi:10.16089/j.cnki.1008-2786.000471]
[8]张闻多,熊东红*,张宝军,等.1980—2018年拉萨河径流泥沙变化[J].山地学报,2022,(5):670.[doi:10.16089/j.cnki.1008-2786.000702]
　ZHANG Wenduo,XIONG Donghong*,ZHANG Baojun,et al.Runoff and Related Sediment Migration in the Lhasa River of China from 1980 to 2018[J].Mountain Research,2022,(04):670.[doi:10.16089/j.cnki.1008-2786.000702]
[9]杨 霞,何 清,赵克明,等.基于加密探空资料的塔里木东风低空急流特征[J].山地学报,2023,(6):836.[doi:10.16089/j.cnki.1008-2786.000791]
　YANG Xia,HE Qing,ZHAO Keming,et al.Characteristics of Easterly Low-Level Jet over Tarim Based on Encrypted Radiosonde Observations[J].Mountain Research,2023,(04):836.[doi:10.16089/j.cnki.1008-2786.000791]

备注/Memo

备注/Memo:
收稿日期(Received date):2017-10-24; 改回日期(Accepted date):2018-05-04
基金项目(Foundation item):国家自然科学基金项目(41271203,41761115)。[National Natural Science Foundation of China(41271203, 41761115)]
作者简介(Biography):刘澄静(1994-),男,云南宾川人,硕士研究生,主要研究方向:稳定同位素生态学。 [LIU Chengjing(1994-), male, born in Binchuan, Yunnan province, M.Sc.candidate, research on stable isotope ecology] E-mail: 18487101130@163.com
*通讯作者(Corresponding author):角媛梅(1972-),女,博士,教授,主要研究方向:景观生态学。[JIAO Yuanmei(1972-), female, Ph.D., professor, specialized in landscape] E-mail: ymjiao@sina.com.
更新日期/Last Update: 2018-07-30