黄河小浪底库区降水δD和δ~(18)O季节变化特征及水汽来源分析
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- 英文论文题名：Seasonalcharacteristics of δD and δ~(18)O in precipitation and its water vapor sources in the Xiaolangdi reservoir area of Yellow River
- 论文作者：田超 ; 孟平 ; 张劲松 ; 高峻 ; 郑宁 ; 何春霞
- 英文论文作者：Tian Chao ; Meng Ping ; Zhang Jinsong ; Gao Jun ; Zheng Ning ; He Chunxia ; Chinese Academy of forestry ; state Key Laboratory of Tree Genetics and Breeding ; Nanjing Forestry University
- 年：2015
- 作者机构：中国林业科学研究院林业研究所林木遗传育种国家重点实验室;南京林业大学南方现代林业协同创新中心;
- 论文关键词：δD ; δ~(18)O ; 大气降水线 ; 过量氘 ; 水汽来源 ; 黄河小浪底库区 ; 东部季风区
- 英文论文关键词：δD ; δ~(18)O ; meteoric water line ; d value ; water vapor source ; Xiaolangdi Reservoir Area ; eastern monsoon region
- 会议召开时间：2015-09-01
- 会议录名称：2015海峡两岸水土保持学术研讨会论文集（下）
- 英文会议录名称：Proceedings of Cross-strait Symposium on Soil and Water Conservation 2015
- 语种：中文
- 分类号：P426
- 学会代码：OGSJ
- 会议名称：2015海峡两岸水土保持学术研讨会
- 会议地点：中国山西太原
- 主办单位：中国水土保持学会、台湾中华水土保持学会
- 学会名称：中国水土保持学会
- 页数：10
- 文件大小：3900k
- 原文格式：O
- 会议级别：全国
摘要
根据2011~2014年4—10月在位于我国东部季风区的黄河小浪底库区收集降水样品及相应气象资料,分析该地区大气降水的δD和δ~(18)O季节变化规律及影响因素,建立不同季节大气降水线,揭示该地区不同季节水汽来源差异.结果表明,降水的δD和δ~(18)O值变化范围较大,具有明显的季节变化,春季降水的δD和δ~(18)O值较高,夏季次之,秋季最低.4一10月及秋季降水δD和δ~(18)O与降水量存在负相关关系,4—10月降水δD与温度成负相关关系,而季节性降水同位素与温度相关性不显著.夏季大气水线斜率及降水d值较小,而秋季最大.利用HYSPLIT气团轨迹模型,得出夏季水汽主要来自东南及西南海洋性季风输送,春秋季节降水受大陆和海洋性季风共同影响.
The seasonal characteristics of δD and δ~(18)O in precipitation and its influence factors were analyzed in the Xiaolangdi Reservoir area which located at the eastern monsoon region of China.The precipitation samples and the corresponding meteorological data were collected between April and October from the year 2011 to 2014.The Local Meteoric Water Line(LMWL) of different seasons were established,and water vapor source differences were revealed in different seasons.The results show that the δD and δ~(18)O in precipitation exhibited an extremely wide range and a distinct seasonal variation,and they were enriched in spring,and depleted in autumn.The δD and δ~(18)O values showed significant negative correlations with the precipitation from April to October and autumn,respectively.The δD values and the mean air temperature showed a significant negative correlation from April to October,but showed no significant correlation in seasons.Both the slope of the LMWL and d value of precipitation were the smallest in summer,and they were the biggest in autumn.The results of airmass back trajectories of seasonal precipitation with the HYSPLIT model indicate a dominant effect of southeast and southwest maritime monsoon air masses in summer and the co- influence of continental and oceanic monsoons air masses in spring and autumn in the study area.
The seasonal characteristics of δD and δ~(18)O in precipitation and its influence factors were analyzed in the Xiaolangdi Reservoir area which located at the eastern monsoon region of China.The precipitation samples and the corresponding meteorological data were collected between April and October from the year 2011 to 2014.The Local Meteoric Water Line(LMWL) of different seasons were established,and water vapor source differences were revealed in different seasons.The results show that the δD and δ~(18)O in precipitation exhibited an extremely wide range and a distinct seasonal variation,and they were enriched in spring,and depleted in autumn.The δD and δ~(18)O values showed significant negative correlations with the precipitation from April to October and autumn,respectively.The δD values and the mean air temperature showed a significant negative correlation from April to October,but showed no significant correlation in seasons.Both the slope of the LMWL and d value of precipitation were the smallest in summer,and they were the biggest in autumn.The results of airmass back trajectories of seasonal precipitation with the HYSPLIT model indicate a dominant effect of southeast and southwest maritime monsoon air masses in summer and the co- influence of continental and oceanic monsoons air masses in spring and autumn in the study area.
引文
[1]Zheng S-H(郑淑蕙),Hou F-G(侯发高),Ni B-L(倪葆龄).Studies on stable deuterium and oxygen-18 isotope composition of precipitation in China.Chinese Science Bulletin(科学通报),1983,28(13):801-806(in Chinese)
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[3]Vreca P,Bronic I K,Horvatincic N,el al.Isotopic characteristics of precipitation in Slovenia and Croatia:comparison of continental and maritime stations.Journal of Hydrology,2006,330(3):457-469
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[6]Zhang Y-H(张应华),Wu Y-Q(仵彦卿),Wen X-H(温小虎),et al.Application of environmental isotopes in water cycle.Advances in Water Science(水科学进展),2006,17(5):738-747(in Chinese)
[7]Qu S-M(瞿思敏),Bao W-M(包为民).McDonnell JJ,et al.Isotope tracer in watershed hydrological modeling.Advances in Water Science(水科学进展),2008,19(4):587-596(in Chinese)
[8]Dansgaard W.The abundance of 8180 in atmospheric water and water vapour.Tellus,1953,5(4):461-469
[9]Craig H.Isotopic variations in meteoric waters.Science,1961(133):1702-1703
[10]Zhang X-P(章新平),Yao T-D(姚檀栋).World spatial characteristics of oxygen isotope ratio in precipitation.Journal of Glaciology and Geocryology(冰川冻土),1994,16(3):202-210(in Chinese)
[11]Vodila G,Palcsu L,Futo I,et al.A 9-year record of stable isotope ratios of precipitation in Eastern Hungary:Implications on isotope hydrology and regional palaeoclimatology.Journal of Hydrology,2011,400(1):144-153
[12]Kumar US,Kumar B,Rai SP,et al.Stable isotope ratios in precipitation and their relationship with meteorological conditions in the Kumaon Himalayas,India.Journal of hydrology,2010,391(1):1-8
[13]Zhou S-Z(周淑贞),Zhang R-Y(张如一),Zhang C(张超).Meteorology and climatology[M].Higher Education Press(高等教育出版社),1979(in Chinese)
[14]Wei K-Q(卫克勤),Lin R-F(林瑞芬).The influence of the monsoon climate on the isotopic composition of precipitation in China.Geochimica(地球化学),1994,23(1):32-41(in Chinese)
[15]Pang H-X(庞洪喜),He Y-Q(何元庆),Zhang Z-L(张忠林).Correlation between 8180 in the monsoonal precipitation and some astronomy-atmosphere-ocean events.Journal of Glaciology and Geocryology(冰川冻土),2004,26:42-47(in Chinese)
[16]Liu J-R(柳鉴容),Song X-F(宋献方),Yuan G-F(袁国富),et al.Characteristics of 8180 in precipitation over eastern monsoon China and the water vapor sources.Chinese Science Bull(科学通报),2009,54(22):3521-3531(in Chinese)
[17]Li X-F(李小飞),Zhang M-J(张明军),Wang S-J(王圣杰),et al.Spatial and temporal variations of hydrogen and oxygen isotopes in precipitation in the Yellow River Basin and its environmental significance.Acta Geologica Sinica(地质学报),2013,87(2):269—277(in Chinese)
[18]Zhang M-J(张明军),Ma Q(马潜),Li Y-J(李亚举),el al.Research of isotopic characteristic in precipitation and water vapor origin at the edge of monsoon region-a case study of Lanzhou city.Journal of Northwest Normal Vniversityi.Natural Science)(西北师范大学学报:自然科学版),2012,47(6):80-86(in Chinese)
[19]Wang F-G(王福刚).The application of isotope techniques in the hydrological cycle of overground section(Henan section)of the lower reaches of Yellow River.Changchun;Jilin university,2006(in Chinese)
[20]Wang T(王涛),Zhang J-R(张洁茹),Liu X(刘笑),et al.Variations of stable isotopes in precipitation and water vapor sources in Nanjing area.Journal of China Hydrology(张洁茹),2013,33(4):25-31(in Chinese)
[21]Tu L-L(涂林玲),Wang H(王华),Feng Y-M(冯玉梅).Research on D and 180 isotope in the precipitation of Guilin.Carsologica Sinica(中国岩溶),2004,23(4):304-309(in Chinese)
[22]Chen F-L(陈粉丽).Zhang M-J(张明军),Ma Q(马潜),et al.Characteristics of 8180 in precipitation and water vapor sources in Lanzhou city and its surrounding area.Environmental Science(环境科学),2013,34(10):3755-3763(in Chinese)
[23]Wang R(王锐),Liu W-Z(刘文兆),Song X-F(宋献方).Characteristics of hydrogen and oxygen isotopes in precipitation on Changwu Tableland.Journal of Soil and Water Conservation(水土保护学报),2008,22(3):56-59(in Chinese)
[24]Hu K(胡可),Chen H-S(I^Sfe),Nie Y-P(聂云鹏),et al.Characteristics of seasonal variation of deuterium and oxygen-18 isotope composition of precipitation in karst peak-cluster depression area,northwest Guangxi of China.Transactions of the Chinese Society of Agricultural Engineering{Transactions of the CSAE)(农业工程学报),2013,29(5):53-62(in Chinese)
[25]Li G(李广),Zhang X-P(章新平),Wu H-W(吴华武),et al.Stable oxygen isotope in precipitation in relation to the meteorological factors and the moisture sources in Yunnan.Journal of Natural Resource(自然资源学报),2014,29(6):1043-1052(in Chinese)
[26]MiuQ-L(缪启龙),Wang Y(王勇).The four seasons division of China and its variation characteristics analysis.Chinese Meteorological Society-climate change in 2007.Beijing:Chinese Meteorological Society(中国气象学会2007年年会气候变化分会场论文集),2007:693-701(in Chinese)
[27]Sun S-J(孙守家),Meng P(孟平),Zhang J-S(张劲松),et al.Ecosystems water use patterns of Quercus variabilis and Grewia biloba based on stable hydrogen and oxygen isotopes in the south aspect of Taihang Mountains.Acta Ecologica Sinica(生态学报),2014,34(21):6317-6325(in Chinese)
[28]Yapp CJ.A model for the relationships between precipitation D/H ratios and precipitation intensity.Journal of Geophysical Research:Oceans(1978-2012),1982,87(C12):9614-9620
[29]Zhang XP,Yao TD,Liu JM,et al.Simulations of stable isotopic fractionation in mixed cloud in middle latitudes—taking the precipitation at Urumqi as an example.Advances in Atmospheric Sciences,2003,20(2):261-268
[30]Liu JR,Song XF,Yuan GF,et al.Characteristics of 8180 in precipitation over Eastern Monsoon China and the water vapor sources.Chinese Science Bulletin,2009,55(2):200-211
[31]Zhang X-P(章新平),Yao T-D(姚檀栋).Distributional features of 8180 inprecipitation in China.Acta geographica sinica(地理学报),1998,53(4):356-364(in Chinese)
[32]Zhang L(张琳),Chen Z-Y(陈宗宇),Nie Z-L(聂振龙),et al.Correlation betweenδ18O in precipitation and surface air temperature on different time-scale in China.Nuclear Techniques(核技术),2008,31(9):715-720(in Chinese)
[33]Liu J-R(柳鉴容),Song X-F(宋献方),Yuan G-F(袁国富),et al.Stable Isotope Evidence of Vapor Sources in Summer Monsoonal Precipitation over Southern China.Journal of Natural Resources(自然资源学报),2007,22(6):1004-1012.
[34]Zhang X-P(章新平),Sun W-Z(孙维贞),Liu J-M(刘晶淼).Stable isotopes in precipitation in the vapor transport path in Kunming of southwest China.Resources and Environment in the Yangtze Basin(长江流域资源与环境),2005,14(5):665-669(in Chinese)
[35]Tian H(田华),Duan Z-Y(段昭毅).Research on isotopes of the meteoric rainfall in the Guanzhong basin.Ground Water(地下水),2007,29(2):1-2(in Chinese)
[36]Merlivat L,Jouzel J.Global climatic interpretation of the deuterium-oxygen 18 relationship for precipitation.Journal of Geophysical Research;Oceans(1978-2012),1979,84(C8):5029-5033
[37]Gat JR.Oxygen and hydrogen isotopes in the hydrologic cycle.Annual Review of Earth and Planetary Sciences,1996,24(1):225-262
[38]Jouzel J,Froehlich K,Schotterer U.Deuterium and oxygen-18 in present-day precipitation:data and modelling.Hydrological Sciences Journal,1997,42(5):747-763
[39]Liu X-C(刘相超),Song X-F(宋献方),Xia J(夏军),et al.A study on oxygen isotope in precipitation of Dengtaigou basin in Chao and Bai river basin.Geographical Research(地理研究),2005,24(2),196-205(in Chinese)
[2]Li T-Y(李廷勇),Li H-C(李红春),Shen C-Z(沈川洲),et al.Study on the 8D and 8180 characteristics of meteoric precipitation during2006-2008 in Chongqing,China.Advances in Water Science(水科学进展),2010,21(6):757-764(in Chinese)
[3]Vreca P,Bronic I K,Horvatincic N,el al.Isotopic characteristics of precipitation in Slovenia and Croatia:comparison of continental and maritime stations.Journal of Hydrology,2006,330(3):457-469
[4]Dansgaard W.Stable isotopes in precipitation.Tellus,1964,16(4);436-468
[5]He YQ,Pang HX,Theakstone WH,et al.Isotopic variations in precipitation at Bangkok and their climatological significance.Hydrological processes,2006,20(13):2873-2884
[6]Zhang Y-H(张应华),Wu Y-Q(仵彦卿),Wen X-H(温小虎),et al.Application of environmental isotopes in water cycle.Advances in Water Science(水科学进展),2006,17(5):738-747(in Chinese)
[7]Qu S-M(瞿思敏),Bao W-M(包为民).McDonnell JJ,et al.Isotope tracer in watershed hydrological modeling.Advances in Water Science(水科学进展),2008,19(4):587-596(in Chinese)
[8]Dansgaard W.The abundance of 8180 in atmospheric water and water vapour.Tellus,1953,5(4):461-469
[9]Craig H.Isotopic variations in meteoric waters.Science,1961(133):1702-1703
[10]Zhang X-P(章新平),Yao T-D(姚檀栋).World spatial characteristics of oxygen isotope ratio in precipitation.Journal of Glaciology and Geocryology(冰川冻土),1994,16(3):202-210(in Chinese)
[11]Vodila G,Palcsu L,Futo I,et al.A 9-year record of stable isotope ratios of precipitation in Eastern Hungary:Implications on isotope hydrology and regional palaeoclimatology.Journal of Hydrology,2011,400(1):144-153
[12]Kumar US,Kumar B,Rai SP,et al.Stable isotope ratios in precipitation and their relationship with meteorological conditions in the Kumaon Himalayas,India.Journal of hydrology,2010,391(1):1-8
[13]Zhou S-Z(周淑贞),Zhang R-Y(张如一),Zhang C(张超).Meteorology and climatology[M].Higher Education Press(高等教育出版社),1979(in Chinese)
[14]Wei K-Q(卫克勤),Lin R-F(林瑞芬).The influence of the monsoon climate on the isotopic composition of precipitation in China.Geochimica(地球化学),1994,23(1):32-41(in Chinese)
[15]Pang H-X(庞洪喜),He Y-Q(何元庆),Zhang Z-L(张忠林).Correlation between 8180 in the monsoonal precipitation and some astronomy-atmosphere-ocean events.Journal of Glaciology and Geocryology(冰川冻土),2004,26:42-47(in Chinese)
[16]Liu J-R(柳鉴容),Song X-F(宋献方),Yuan G-F(袁国富),et al.Characteristics of 8180 in precipitation over eastern monsoon China and the water vapor sources.Chinese Science Bull(科学通报),2009,54(22):3521-3531(in Chinese)
[17]Li X-F(李小飞),Zhang M-J(张明军),Wang S-J(王圣杰),et al.Spatial and temporal variations of hydrogen and oxygen isotopes in precipitation in the Yellow River Basin and its environmental significance.Acta Geologica Sinica(地质学报),2013,87(2):269—277(in Chinese)
[18]Zhang M-J(张明军),Ma Q(马潜),Li Y-J(李亚举),el al.Research of isotopic characteristic in precipitation and water vapor origin at the edge of monsoon region-a case study of Lanzhou city.Journal of Northwest Normal Vniversityi.Natural Science)(西北师范大学学报:自然科学版),2012,47(6):80-86(in Chinese)
[19]Wang F-G(王福刚).The application of isotope techniques in the hydrological cycle of overground section(Henan section)of the lower reaches of Yellow River.Changchun;Jilin university,2006(in Chinese)
[20]Wang T(王涛),Zhang J-R(张洁茹),Liu X(刘笑),et al.Variations of stable isotopes in precipitation and water vapor sources in Nanjing area.Journal of China Hydrology(张洁茹),2013,33(4):25-31(in Chinese)
[21]Tu L-L(涂林玲),Wang H(王华),Feng Y-M(冯玉梅).Research on D and 180 isotope in the precipitation of Guilin.Carsologica Sinica(中国岩溶),2004,23(4):304-309(in Chinese)
[22]Chen F-L(陈粉丽).Zhang M-J(张明军),Ma Q(马潜),et al.Characteristics of 8180 in precipitation and water vapor sources in Lanzhou city and its surrounding area.Environmental Science(环境科学),2013,34(10):3755-3763(in Chinese)
[23]Wang R(王锐),Liu W-Z(刘文兆),Song X-F(宋献方).Characteristics of hydrogen and oxygen isotopes in precipitation on Changwu Tableland.Journal of Soil and Water Conservation(水土保护学报),2008,22(3):56-59(in Chinese)
[24]Hu K(胡可),Chen H-S(I^Sfe),Nie Y-P(聂云鹏),et al.Characteristics of seasonal variation of deuterium and oxygen-18 isotope composition of precipitation in karst peak-cluster depression area,northwest Guangxi of China.Transactions of the Chinese Society of Agricultural Engineering{Transactions of the CSAE)(农业工程学报),2013,29(5):53-62(in Chinese)
[25]Li G(李广),Zhang X-P(章新平),Wu H-W(吴华武),et al.Stable oxygen isotope in precipitation in relation to the meteorological factors and the moisture sources in Yunnan.Journal of Natural Resource(自然资源学报),2014,29(6):1043-1052(in Chinese)
[26]MiuQ-L(缪启龙),Wang Y(王勇).The four seasons division of China and its variation characteristics analysis.Chinese Meteorological Society-climate change in 2007.Beijing:Chinese Meteorological Society(中国气象学会2007年年会气候变化分会场论文集),2007:693-701(in Chinese)
[27]Sun S-J(孙守家),Meng P(孟平),Zhang J-S(张劲松),et al.Ecosystems water use patterns of Quercus variabilis and Grewia biloba based on stable hydrogen and oxygen isotopes in the south aspect of Taihang Mountains.Acta Ecologica Sinica(生态学报),2014,34(21):6317-6325(in Chinese)
[28]Yapp CJ.A model for the relationships between precipitation D/H ratios and precipitation intensity.Journal of Geophysical Research:Oceans(1978-2012),1982,87(C12):9614-9620
[29]Zhang XP,Yao TD,Liu JM,et al.Simulations of stable isotopic fractionation in mixed cloud in middle latitudes—taking the precipitation at Urumqi as an example.Advances in Atmospheric Sciences,2003,20(2):261-268
[30]Liu JR,Song XF,Yuan GF,et al.Characteristics of 8180 in precipitation over Eastern Monsoon China and the water vapor sources.Chinese Science Bulletin,2009,55(2):200-211
[31]Zhang X-P(章新平),Yao T-D(姚檀栋).Distributional features of 8180 inprecipitation in China.Acta geographica sinica(地理学报),1998,53(4):356-364(in Chinese)
[32]Zhang L(张琳),Chen Z-Y(陈宗宇),Nie Z-L(聂振龙),et al.Correlation betweenδ18O in precipitation and surface air temperature on different time-scale in China.Nuclear Techniques(核技术),2008,31(9):715-720(in Chinese)
[33]Liu J-R(柳鉴容),Song X-F(宋献方),Yuan G-F(袁国富),et al.Stable Isotope Evidence of Vapor Sources in Summer Monsoonal Precipitation over Southern China.Journal of Natural Resources(自然资源学报),2007,22(6):1004-1012.
[34]Zhang X-P(章新平),Sun W-Z(孙维贞),Liu J-M(刘晶淼).Stable isotopes in precipitation in the vapor transport path in Kunming of southwest China.Resources and Environment in the Yangtze Basin(长江流域资源与环境),2005,14(5):665-669(in Chinese)
[35]Tian H(田华),Duan Z-Y(段昭毅).Research on isotopes of the meteoric rainfall in the Guanzhong basin.Ground Water(地下水),2007,29(2):1-2(in Chinese)
[36]Merlivat L,Jouzel J.Global climatic interpretation of the deuterium-oxygen 18 relationship for precipitation.Journal of Geophysical Research;Oceans(1978-2012),1979,84(C8):5029-5033
[37]Gat JR.Oxygen and hydrogen isotopes in the hydrologic cycle.Annual Review of Earth and Planetary Sciences,1996,24(1):225-262
[38]Jouzel J,Froehlich K,Schotterer U.Deuterium and oxygen-18 in present-day precipitation:data and modelling.Hydrological Sciences Journal,1997,42(5):747-763
[39]Liu X-C(刘相超),Song X-F(宋献方),Xia J(夏军),et al.A study on oxygen isotope in precipitation of Dengtaigou basin in Chao and Bai river basin.Geographical Research(地理研究),2005,24(2),196-205(in Chinese)