Study on Hydrogen and Oxygen Stable Isotopes in Precipitation in Wolong Nature Reserve,Sichuan Province

XU Qing; LIU Shi-rong; AN Shu-qing; JIANG Chun-qian; LIU Xing-liang

Volume 19 Issue 6

Article Contents

Turn off MathJax

Article Navigation > Forest Research > 2006 > 19(6): 679-686

Citation:

Study on Hydrogen and Oxygen Stable Isotopes in Precipitation in Wolong Nature Reserve,Sichuan Province

1.
Institute of Forest Ecology, Environment and Protection, CAF
2.
Key Laboratory of Forest Ecology and Environment, State Forestry Administration, Beijing 100091, China
3.
Laboratory of Forest Ecology and Global Changes, School of Life Science, Nanjing University, Nanjing 210093
4.
Jiangsu, China

Received Date: 2006-05-16

Abstract

This paper assayed the contents of stable isotope δD and δ18O in precipitation in Wolong Nature Reserve of Sichuan Province from July 2003 to June 2005.The equation of meteoric water line(MWL) and snow water line were δD= 9.443 δ18O+28.658(r=0.943,n =74,p18O+33.245(r=0.959,n =31,p18O+9.480(r=0.961,n=29,p18O of precipitation in summer had a significant amount effect,and temperature effect was withheld by monsoon climate.
- hydrogen and oxygen isotope,
- meteoric water line,
- excess deuterium,
- Wolong area,
- water vapor source

References

[R].IAEA. Vienna, 1981: 103～142
[2]	Craig H. Isotop ic variations in meteoric water[J]. Science, 1961,133: 1702～1703
[3]	Yurtsever Y, Gat J R. Atmospheric waters [A]. In: Stable IsotopeHydrology . Deuter2ium and OxygeN₂18 in the Water Cycle
[4]	尹观,倪师军,张其春. 氘过量参数及其水文地质学意义———以四川九寨沟和勒水文地质研究为例[J]. 成都理工学院学报,2001, 28 (3) : 251～254
[5]	Dansgard W. Stable isotope in p recip itation [J]. Tellus, 1964, 16(4) : 436～468
[6]	Merlivat L, Jouzel J. Global climate interp retation of the deuteriumoxygen 18 relationship for p recip itation[J]. Geophys Res, 1979, 84:5029～5033
[7]	Jouzel J,MerlivatL. Deuterium and oxygen-18 in p recip itation of theistope effects during snow formation [J]. Geophys Res, 1984, 89(D7) : 11749～11757
[8]	DansgaardW. The abundance of¹⁸O in atmospheric water and watervapor[J]. Tellus, 1953, 5 (4) : 461～469
[9]	章新平,田立德,刘晶,等. 沿三条水汽输送路径的降水中δ¹⁸O 变化特征[J]. 地理科学, 2005, 25 (2) : 190～196
[10]	章新平,施雅风,姚檀栋. 青藏高原东北部降水中δ¹⁸O 的变化特征[J]. 中国科学, 1995, 25 (5) : 540～547
[11]	宁爱凤,尹观,刘天仇. 拉萨河地区的大气降水同位素分布特征[J]. 矿物岩石, 2000, 20 (3) : 95～99
[12]	章新平,姚檀栋. 我国降水中δ¹⁸O 的分布特点[J]. 地理学报,1998, 53 (4) : 356～363
[13]	韩庆之,曾克峰,梁杏,等. 川西南雷泼地区降水的D 和¹⁸O 同位素研究[J]. 地质科技情报, 1998, 17 (增刊) : 106～110
[14]	尹观,范晓,郭建强,等. 四川九寨沟水循环系统的同位素示踪[J]. 地理学报, 2000, 55 (4) : 487～494
[15]	林光辉,柯渊. 稳定同位素技术与全球变化研究[A]. 见:李博.现代生态学讲座[M]. 北京:科学出版社, 1995: 161～188
[16]	石辉,刘世荣,赵晓广. 稳定性氢氧同位素在水分循环中的应用[J]. 水土保持学报, 2003, 17 (2) : 163～166
[17]	徐庆,安树青,刘世荣,等. 四川卧龙亚高山暗针叶林降水分配过程的氢稳定同位素特征[J]. 林业科学, 2005, 41 (4) : 7～12
[18]	徐庆,刘世荣,安树青,等. 川西亚高山暗针叶林降水分配过程中氧稳定同位素特征[J]. 植物生态学报, 2006, 30 (1) : 83～89
[19]	尹观. 同位素水文地球化学[M]. 成都:成都科技大学出版社,1988: 84～85
[20]	Craig H, Gordon L I, Horibe Y. Isotop ic exchange effects in the evaporation of water, low temperature experiment results [J]. Geophys J Res, 1963, 68: 50～79
[21]	郑淑蕙,候发高,倪葆龄. 我国大气降水的氢氧稳定同位素研究[J]1科学通报, 1983 (13) : 39～41
[22]	卧龙自然保护区管理局. 卧龙植被及资源植物[M]. 成都:四川科学技术出版社, 1987: 8～10
[23]	姚檀栋,丁良福,蒲建辰,等. 青藏高原唐古拉山地区降雪中δ¹⁸O特征及其与水汽来源的关系[J]. 科学通报, 1991 (20) : 1570～1573
[24]	田立德,姚檀栋,孙维贞. 青藏高原南北降水中δD 和δ¹⁸O 关系及水汽循环[J]. 中国科学, 2001, 31 (3) : 214～220
[25]	郭其蕴. 中国季风降水与赤道东太平洋海温的关系[J]. 地理研究, 1990, 9 (4) : 49～59
[26]	刘相超,宋献方,夏军,等. 东台沟实验流域降水氧同位素特征与水汽来源[J]. 地理研究, 2005, 24 (2) : 196～205
[27]	姚檀栋,孙维贞,蒲健辰,等. 内陆河流域系统降水中的稳定同位素———乌鲁木齐河流域降水中δ¹⁸O 与温度关系研究[J]. 冰川冻土, 2000, 22 (1) : 15～20
[28]	卫克勤,林瑞芬,王志祥. 西藏羊八井地热水的氢、氧稳定同位素组成及氘含量[J]. 地球化学, 1983 (4) : 338～345

Proportional views

通讯作者: 陈斌, bchen63@163.com

1.
沈阳化工大学材料科学与工程学院沈阳 110142

Get Citation

PDF

XML

Article views(3744) PDF downloads(1580) Cited by()

Proportional views

Study on Hydrogen and Oxygen Stable Isotopes in Precipitation in Wolong Nature Reserve,Sichuan Province

1. Institute of Forest Ecology, Environment and Protection, CAF

2. Key Laboratory of Forest Ecology and Environment, State Forestry Administration, Beijing 100091, China

3. Laboratory of Forest Ecology and Global Changes, School of Life Science, Nanjing University, Nanjing 210093

4. Jiangsu, China

Received Date: 2006-05-16

Abstract: This paper assayed the contents of stable isotope δD and δ18O in precipitation in Wolong Nature Reserve of Sichuan Province from July 2003 to June 2005.The equation of meteoric water line(MWL) and snow water line were δD= 9.443 δ18O+28.658(r=0.943,n =74,p18O+33.245(r=0.959,n =31,p18O+9.480(r=0.961,n=29,p18O of precipitation in summer had a significant amount effect,and temperature effect was withheld by monsoon climate.

HTML

Reference (28)

[1]	[R].IAEA. Vienna, 1981: 103～142
[2]	Craig H. Isotop ic variations in meteoric water[J]. Science, 1961,133: 1702～1703
[3]	Yurtsever Y, Gat J R. Atmospheric waters [A]. In: Stable IsotopeHydrology . Deuter2ium and OxygeN₂18 in the Water Cycle
[4]	尹观,倪师军,张其春. 氘过量参数及其水文地质学意义———以四川九寨沟和勒水文地质研究为例[J]. 成都理工学院学报,2001, 28 (3) : 251～254
[5]	Dansgard W. Stable isotope in p recip itation [J]. Tellus, 1964, 16(4) : 436～468
[6]	Merlivat L, Jouzel J. Global climate interp retation of the deuteriumoxygen 18 relationship for p recip itation[J]. Geophys Res, 1979, 84:5029～5033
[7]	Jouzel J,MerlivatL. Deuterium and oxygen-18 in p recip itation of theistope effects during snow formation [J]. Geophys Res, 1984, 89(D7) : 11749～11757
[8]	DansgaardW. The abundance of¹⁸O in atmospheric water and watervapor[J]. Tellus, 1953, 5 (4) : 461～469
[9]	章新平,田立德,刘晶,等. 沿三条水汽输送路径的降水中δ¹⁸O 变化特征[J]. 地理科学, 2005, 25 (2) : 190～196
[10]	章新平,施雅风,姚檀栋. 青藏高原东北部降水中δ¹⁸O 的变化特征[J]. 中国科学, 1995, 25 (5) : 540～547
[11]	宁爱凤,尹观,刘天仇. 拉萨河地区的大气降水同位素分布特征[J]. 矿物岩石, 2000, 20 (3) : 95～99
[12]	章新平,姚檀栋. 我国降水中δ¹⁸O 的分布特点[J]. 地理学报,1998, 53 (4) : 356～363
[13]	韩庆之,曾克峰,梁杏,等. 川西南雷泼地区降水的D 和¹⁸O 同位素研究[J]. 地质科技情报, 1998, 17 (增刊) : 106～110
[14]	尹观,范晓,郭建强,等. 四川九寨沟水循环系统的同位素示踪[J]. 地理学报, 2000, 55 (4) : 487～494
[15]	林光辉,柯渊. 稳定同位素技术与全球变化研究[A]. 见:李博.现代生态学讲座[M]. 北京:科学出版社, 1995: 161～188
[16]	石辉,刘世荣,赵晓广. 稳定性氢氧同位素在水分循环中的应用[J]. 水土保持学报, 2003, 17 (2) : 163～166
[17]	徐庆,安树青,刘世荣,等. 四川卧龙亚高山暗针叶林降水分配过程的氢稳定同位素特征[J]. 林业科学, 2005, 41 (4) : 7～12
[18]	徐庆,刘世荣,安树青,等. 川西亚高山暗针叶林降水分配过程中氧稳定同位素特征[J]. 植物生态学报, 2006, 30 (1) : 83～89
[19]	尹观. 同位素水文地球化学[M]. 成都:成都科技大学出版社,1988: 84～85
[20]	Craig H, Gordon L I, Horibe Y. Isotop ic exchange effects in the evaporation of water, low temperature experiment results [J]. Geophys J Res, 1963, 68: 50～79
[21]	郑淑蕙,候发高,倪葆龄. 我国大气降水的氢氧稳定同位素研究[J]1科学通报, 1983 (13) : 39～41
[22]	卧龙自然保护区管理局. 卧龙植被及资源植物[M]. 成都:四川科学技术出版社, 1987: 8～10
[23]	姚檀栋,丁良福,蒲建辰,等. 青藏高原唐古拉山地区降雪中δ¹⁸O特征及其与水汽来源的关系[J]. 科学通报, 1991 (20) : 1570～1573
[24]	田立德,姚檀栋,孙维贞. 青藏高原南北降水中δD 和δ¹⁸O 关系及水汽循环[J]. 中国科学, 2001, 31 (3) : 214～220
[25]	郭其蕴. 中国季风降水与赤道东太平洋海温的关系[J]. 地理研究, 1990, 9 (4) : 49～59
[26]	刘相超,宋献方,夏军,等. 东台沟实验流域降水氧同位素特征与水汽来源[J]. 地理研究, 2005, 24 (2) : 196～205
[27]	姚檀栋,孙维贞,蒲健辰,等. 内陆河流域系统降水中的稳定同位素———乌鲁木齐河流域降水中δ¹⁸O 与温度关系研究[J]. 冰川冻土, 2000, 22 (1) : 15～20
[28]	卫克勤,林瑞芬,王志祥. 西藏羊八井地热水的氢、氧稳定同位素组成及氘含量[J]. 地球化学, 1983 (4) : 338～345

Study on Hydrogen and Oxygen Stable Isotopes in Precipitation in Wolong Nature Reserve,Sichuan Province

Abstract

References

Proportional views

通讯作者: 陈斌, bchen63@163.com

Proportional views

Study on Hydrogen and Oxygen Stable Isotopes in Precipitation in Wolong Nature Reserve,Sichuan Province

HTML

Catalog

Export File

Citation

Format

Content