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Volume 34 Issue 3
Jun.  2015
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Article Navigation >  CARSOLOGICA SINICA  > 2015  >  34(3): 247-253
HU Han, WANG Jian-li. Characteristics of hydrogen and oxygen isotopes in precipitation from october to december 2013 in Chongqing and analysis of moisture sources[J]. CARSOLOGICA SINICA, 2015, 34(3): 247-253. doi: 10.11932/karst20150307
Citation: HU Han, WANG Jian-li. Characteristics of hydrogen and oxygen isotopes in precipitation from october to december 2013 in Chongqing and analysis of moisture sources[J]. CARSOLOGICA SINICA, 2015, 34(3): 247-253. doi: 10.11932/karst20150307
shu

Characteristics of hydrogen and oxygen isotopes in precipitation from october to december 2013 in Chongqing and analysis of moisture sources

doi: 10.11932/karst20150307
  • 1.

    School of Geographical Sciences, Southwest University

  • 2.

    School of Geographical Sciences, Southwest University/Key Laboratory of the Three Gorges Reservoir Region’s Eco-Environment， Ministry of Education

  • Publish Date: 2015-06-25
    Abstract
  • Based on monitoring data and meteorological elements at School of Geographical Sciences，Southwest University of Chongqing，which were collected from October to December 2013, the LMWL of Chongqing is formulated as δD= 8.19δ18O+17.39，r=0.97（p<0.001). The influence of short-term weather factors accounts for the larger slope and intercept value of the LMWL. The characteristics of the hydrogen isotope and oxygen isotope and their relationships with temperature and precipitation were analyzed to reveal the moisture sources based on the statistics. The statistics shows that the relationships between hydrogen isotope and oxygen isotope are not obvious. Further study suggests that the co-existence of summer monsoon and winter monsoon during the transition span from October to December complicated isotope composition in precipitation. Then by virtue of HYSPLIT modeling，the vapor transport trajectories of every precipitation in Beibei of Chongqing during October to December 2013 are drawn.The resalts show that south-west monsoon was weak and the weather was affected mainly by westerlies in this period. The moisture sources of October and November 2013 were mainly from the Sanjiang drainage in the Hengduan Mountains，and there was moisture transport from tropical storm Haiyan in November. Different moisture sources have great influence to δD and δ18O,and the value of δD and δ18O have good respond to the different source.While moisture source of rain in December 2013 was mainly from local evaporation.

     

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    • References(49)
  • [1]
    Wang Bin, Ho Lin. Rainy Season of the Asian-Pacific Summer Monsoon ［J］. Journal of Climate, 2002, 15(4): 386-398.
    [2]
    Lawrence J R, D Gedzelman S, J Gamache. Stable isotope ratios: hurricane Olivia ［J］. Journal of atmospheric Chemistry, 2002, 41(1): 67-82.
    [3]
    孙玮玮, 毕春娟, 陈振楼, 等. 稳定性同位素示踪技术在环境领域的应用初探 ［J］. 环境科学与技术, 2009, 32(9): 88-92.
    [4]
    Vodila G, L Palcsu, I Futo, et al. A 9-year record of stable isotope ratios of precipitation in Eastern Hungary: Implications on isotope hydrology and regional palaeoclimatology ［J］. Journal of Hydrology, 2011, 1-2(400): 144-153.
    [5]
    Kumar U S, B Kumar, P Rai S, et al. Stable isotope ratios in precipitation and their relationship with meteorological conditions in the Kumaon Himalayas, India ［J］. Journal of Hydrology, 2010, 1-2(391): 1-8.
    [6]
    丁悌平, 高建飞, 石国钰, 等. 长江水氢、氧同位素组成的时空变化及其环境意义 ［J］. 地质学报, 2013, 87(5): 661-676.
    [7]
    葛源, 贺纪正, 郑袁明, 等. 稳定性同位素探测技术在微生物生态学研究中的应用 ［J］. 生态学报, 2006, 26(5): 1574-1582.
    [8]
    李忠义, 金显仕, 庄志猛, 等. 稳定同位素技术在水域生态系统研究中的应用 ［J］. 生态学报, 2005, 25(11): 260-268.
    [9]
    罗伦, 余武生, 万诗敏, 等. 植物叶片水稳定同位素研究进展 ［J］. 生态学报, 2013, 33(4): 1031-1041.
    [10]
    瞿思敏, 包为民, Donnell Jeffrey J. Mc, 等. 同位素示踪剂在流域水文模拟中的应用 ［J］. 水科学进展, 2008, 19(4): 587-596.
    [11]
    吴绍洪, 潘韬, 戴尔阜. 植物稳定同位素研究进展与展望 ［J］. 地理科学进展, 2006, 25(3): 1-11.
    [12]
    张应华, 仵彦卿, 温小虎, 等. 环境同位素在水循环研究中的应用 ［J］. 水科学进展, 2006, 17(5): 738-747.
    [13]
    章斌, 郭占荣, 高爱国, 等. 用氢氧稳定同位素评价闽江河口区地下水输入 ［J］. 水科学进展, 2012, 23(4): 539-548.
    [14]
    郑永飞. 稳定同位素体系理论模式及其矿床地球化学应用 ［J］. 矿床地质, 2001, 20(1): 57-70+85.
    [15]
    郑永飞, 徐宝龙, 周根陶. 矿物稳定同位素地球化学研究 ［J］. 地学前缘, 2000, 7(2): 299-320.
    [16]
    程海, 艾思本, 王先锋, 等. 中国南方石笋氧同位素记录的重要意义 ［J］. 第四纪研究, 2005, 25(2): 157-163.
    [17]
    冯慧文. 重庆羊口洞石笋记录的MIS3时期（51.3ka BP～37.8ka BP）古气候事件 ［D］; 西南大学, 2013.
    [18]
    侯书贵, 王叶堂, 庞洪喜. 南极冰盖雪冰氢、氧稳定同位素气候学:现状与展望 ［J］. 科学通报, 2013, 58(1): 27-40.
    [19]
    覃嘉铭, 袁道先, 程海, 等. 新仙女木及全新世早中期气候突变事件:贵州茂兰石笋氧同位素记录 ［J］. 中国科学(D辑:地球科学), 2004, 34(1): 69-74.
    [20]
    田立德, 姚檀栋, 余武生, 等. 青藏高原水汽输送与冰芯中稳定同位素记录 ［J］. 第四纪研究, 2006, 26(2): 145-152.
    [21]
    王建明, 王建力, 李廷勇. 洞穴石笋δ18O与δ13C气候意义研究 ［J］. 热带地理, 2008, 38(5): 395-399.
    [22]
    蓝江湖, 徐海, 刘斌, 等. 湖泊沉积中碳酸盐、有机质及其同位素的古气候意义 ［J］. 生态学杂志, 2013, 32(5): 1326-1334.
    [23]
    姚檀栋, 秦大河. Distribution of stable isotopes in Antarctic surface snow ［J］. Chinese Science Bulletin, 1995, 11): 921-925.
    [24]
    段旭, 距建华, 肖子牛, 等. 云南气候异常物理过程及预测信号的研究 ［M］. 北京: 气象出版社, 2000.
    [25]
    徐祥德, 陶诗言, 王继志, 等. 青藏高原——季风水汽输送“大三角扇型”影响域特征与中国区域旱涝异常的关系 ［J］. 气象学报, 2002, 60(3): 257-266.
    [26]
    Craig H. Isotopic variations in meteoric waters ［J］. Science, 1961, 133(3465): 1702-1703.
    [27]
    Yurtsever Y. Worldwide survey of stable isotopes in precipitation ［J］. Vienna: IAEA, 1975, 1040.
    [28]
    郑淑蕙, 侯发高, 倪葆龄. 我国大气降水的氢氧稳定同位素研究 ［J］. 科学通报, 1983, 13: 801-806.
    [29]
    章新平, 孙维贞, 刘晶淼. 西南水汽通道上昆明站降水中的稳定同位素 ［J］. 长江流域资源与环境, 2005, 14(5): 665-669.
    [30]
    章新平, 姚檀栋. 我国部分地区降水中氧同位素成分与温度和降水量之间的关系 ［J］. 冰川冻土, 1994, 16(1): 31-40.
    [31]
    刘进达, 赵迎昌, 刘恩凯, 等. 中国大气降水稳定同位素时-空分布规律探讨 ［J］. 勘察科学技术, 1997, 3: 34-39.
    [32]
    涂林玲, 王华, 冯玉梅. 桂林地区大气降水的D和18O同位素的研究 ［J］. 中国岩溶, 2004,23(4): 48-53.
    [33]
    王海波,李廷勇,袁娜,等.重庆金佛山羊口洞滴水δ庆和δ18O变化特征及其环境意义 ［J］. 中国岩溶, 2014, 33(2): 146-155.
    [34]
    李廷勇, 李红春, 沈川洲, 等. 2006～2008年重庆大气降水δ重和δ18O特征初步分析 ［J］. 水科学进展, 2010, 21(6): 757-764.
    [35]
    Jouzel J. Validity of the temperature reconstruction from water isotopes in ice cores. ［J］. J Geophys Res, 1997, 102(26): 471-426.
    [36]
    Araguás-Araguás L, Froehlich K,Rozanski K . Deuterium and oxygen-18 isotope composition of precipitation and atmospheric moisture ［J］. Hydrological Processes, 2000, 14 (8): 1341-1355.
    [37]
    Rietti-Shati M, Yam R , Karlen W , et al. Stable isotope composition of tropical high-altitude fresh waters on Mt.Kenya, Equatorial East Africa ［J］. Chemical Geology, 2000, 166: 341-350.
    [38]
    Yamanaka T, Tsujimura M , Oyunbaatar D, et al. sotopic variation of precipitation over eastern Mongolia and its implication for the atmospheric water cycle ［J］. Journal of Hydrology, 2007, 333: 21-34.
    [39]
    白志鹏, 张利文, 朱坦, 等. 稳定同位素在环境科学研究中的应用进展 ［J］. 同位素, 2007, 20(1): 57-64.
    [40]
    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.
    [41]
    吕俊梅, 张庆云, 陶诗言, 等. 亚洲夏季风的爆发及推进特征 ［J］. 科学通报, 2006, 51(3): 332-338.
    [42]
    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（3): 327-334.
    [43]
    卫克勤, 林瑞芬. 论季风气候对我国雨水同位素组成的影响 ［J］. 地球化学, 1994, 23(1): 33-41.
    [44]
    Draxler R R,D Hess G. An overview of the HYSPLIT 4 modeling system for trajectories,dispersion, and deposition ［J］. Australian Meteorological Magazine, 1998（47): 295-308.
    [45]
    黄健, 颜鹏, Draxler ROLAND R. 利用HYSPLIT-4模式分析珠海地面SO2浓度的变化规律 ［J］. 热带气象学报, 2002, 18(4): 407-414.
    [46]
    戚佳明. 基于HYSPLIT模型的大气CO2传输研究 ［D］.中国地质大学, 2014.
    [47]
    马京津, 高晓清. 华北地区夏季平均水汽输送通量和轨迹的分析 ［J］. 高原气象, 2006, 25(5): 893-899.
    [48]
    吴华武, 章新平, 关华德, 等. 不同水汽来源对湖南长沙地区降水中δD、δ18O的影响 ［J］. 自然资源学报, 2012, 27(8): 1404-1414.
    [49]
    Yaqiang Wang, Stein Ariel F, Draxler Roland R, et al. Global sand and dust storms in 2008: Observation and HYSPLIT model verification ［J］. Atmospheric environment, 2011, 45(35): 6368-6381.
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