关于巴丹吉林沙漠湖泊形成机制的初步看法

郭永海; 王海龙; 董建楠; 刘淑芬; 李亚伟; 季瑞利

doi:10.3799/dqkx.2012.029

Volume 37 Issue 2

Mar. 2012

Turn off MathJax

Article Contents

Article Navigation > Earth Science > 2012 > 37(2): 276-282

GUO Yong-hai, WANG Hai-long, DONG Jian-nan, LIU Shu-fen, LI Ya-wei, JI Rui-li, 2012. The Primary Opinion on the Formation Mechanisms of Megadunes and Lakes in the Badain Jaran Desert. Earth Science, 37(2): 276-282. doi: 10.3799/dqkx.2012.029

Citation:

GUO Yong-hai, WANG Hai-long, DONG Jian-nan, LIU Shu-fen, LI Ya-wei, JI Rui-li, 2012. The Primary Opinion on the Formation Mechanisms of Megadunes and Lakes in the Badain Jaran Desert. Earth Science, 37(2): 276-282. doi: 10.3799/dqkx.2012.029

Citation:

GUO Yong-hai, WANG Hai-long, DONG Jian-nan, LIU Shu-fen, LI Ya-wei, JI Rui-li, 2012. The Primary Opinion on the Formation Mechanisms of Megadunes and Lakes in the Badain Jaran Desert. Earth Science, 37(2): 276-282. doi: 10.3799/dqkx.2012.029

PDF( 628 KB)

The Primary Opinion on the Formation Mechanisms of Megadunes and Lakes in the Badain Jaran Desert

doi: 10.3799/dqkx.2012.029

Beijing Research Institute of Uranium Geology, Beijing 100029, China

Received Date: 2011-09-15
Publish Date: 2012-03-15

Abstract

Abstract

Badain Jaran desert is well-known for its distribution of many megadunes and lakes. However, opinions about the formation of these megadunes and lakes vary from person to person until recently. Actually, their formation is directly related to the circulation and alternation of the groundwater in this area. According to the previous research, combining with the current hydro-geological investigation in the study area, this article discusses the formation mechanisms of megadunes and lakes in Badain Jaran desert. It is found that lakes in the desert formed mainly as a result of the lateral recharge of groundwater both from Yabulai Mountain and megadunes. The formation of megadunes is closely related with the rainfall and groundwater in the area. The formation and coexistent relationship between megadunes and lakes are as follows: the megadunes formed firstly, and then the lakes appeared. That means megadunes are a necessary condition for the formation of lakes there.
- megadune,
- lake,
- formation,
- Badain Jaran desert,
- environmental impact,
- hydrogeology

FullText(HTML)

References(30)

References

Chen, J.S., Li, L., Wang, J.Y., et al., 2004. Groundwater maintains dune landscape. Nature, 432(7016): 459-460. doi: 10.1038/432459a

Chen, J.S., Wang, J.Y., 2004. The impact of a underground reservoir found in Badain Jaran desert on the water transferring plan in Northwest China. Journal of Economics of Water Resources, 22(3): 28-32 (in Chinese with English abstract).

Chen, J.S., Wang, J.Y., 2005. Adverse impact of Altun fault's strong water delivery on nuclear disposal field of Beishan Mount. Journal of Economics of Water Resources, 23(1): 9-13 (in Chinese with English abstract). http://d.wanfangdata.com.cn/Periodical/sljj200501002

Chen, J.S., Wang, J.Y., Zhao, X., et al., 2004. Study of groundwater supply of the confined aquifers in the Ejin basin based on isotopic methods. Geological Review, 50(6): 649-658 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DZLP200406014.htm

Chen, J.S., Zhao, X., Sheng, X.F., et al., 2006. Formation mechanisms of megadunes and lakes in the Badain Jaran desert, Inner Mongolia. Chinese Science Bulletin, 51(23): 2789-2796 (in Chinese with English abstract). doi: 10.1360/csb2006-51-23-2789

Edmunds, W.M., Wright, E.P., 1979. Groundwater recharge and paleoclimate in the Sirte and Kufra basins, Libya. Journal of Hydrology, 40(3-4): 215-241. doi: 10.1016/0022-1694(79)90032-5

Gates, J.B., Edmunds, W.M., Darling, W.G., et al., 2008. Conceptual model of recharge to southeastern Badain Jaran desert groundwater and lakes from environmental tracers. Applied Geochemistry, 23(12): 3519-3534. doi: 10.1016/j.apgeochem.2008.07.019

Gu, W.Z., Chen, J.S., Wang, J.Y., et al., 2004. Challenge from the appearance of vadose water within the surface iayer of megadunes, Badain-Jaran dune desert, Inner Mongolia. Advances in Water Science, 15(6): 695-699 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-SKXJ200406002.htm

Guo, H.D., Liu, H., Wang, X.Y., et al., 2000. Subsurface old drainage detection and paleoenvironment analysis using spaceborne radar images in Alxa plateau. Science in China (Ser. D), 43(4): 439-448. doi: 10.1007/BF02959455

Huang, T.M., Pang, Z.H., 2007. Groundwater recharge in Badain Jaran desert and Gurinai Oasis based on environmental tracers. Geoscience, 21(4): 624-631 (in Chinese with English abstract). http://www.zhangqiaokeyan.com/academic-journal-cn_geoscience_thesis/0201254378102.html

Li, B.X., 1964. The hydrogeological characteristics of drought and desert regions in China. Research on treatment to desert (6th). Science Press, Beijing, 1-32 (in Chinese).

Ma, J.Z., Li, D. Zhang, J.W., et al., 2003. Groundwater recharge and climatic change during the last 1 000 years from unsaturated zone of SE Badain Jaran desert. Chinese Science Bulletin, 48(14): 1469-1474. doi: 10.1360/02wd0262

Sun, P.S., Sun, D.Q., 1964. The study on hydrogeology in the west area in Inner Mongolian. Research on treatment to desert (6th). Science Press, Beijing, 245-317 (in Chinese).

Yan, M.C., Wang, G.Q., Dong, G.R., et al., 2001. Study on mega dunes development and environmental change in Badain Jaran desert. Journal of Desert Research, 21(4): 361-366 (in Chinese with English abstract). http://www.researchgate.net/publication/312973938_Study_on_mega_dunes_development_and_environmental_change_in_Badain_Jaran_Desert

Yang, X., 2001. Late quarternary evolution and paleoclimates, western Alashan plateau, Inner Mongolia, China. Zeitschrift fur Geomorphologie, 45(1): 1-16. doi: 10.1127/zfg/45/2001/1

Yang, X.P., 2000. Landscape evolution and precipitation changes in the Badain Jaran desert during the last 30000 years. Chinese Science Bulletin, 45(4): 428-434(in Chinese). doi: 10.1360/csb2000-45-4-428

Yang, X.P., Liu, T.S., Xiao, H.L., 2003. Evolution of megadunes and lakes in the Badain Jaran desert, Inner Mongolia, China during the last 31, 000 years. Quaternary International, 104: 99-112. doi: 10.1016/S1040-6182(02)00138-6

Zhang, W.M., Wang, T., 2005. Approach to formation and evolution of megadunes in Badain Jaran desert. Journal of Desert Research, 25(2): 281-286 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-ZGSS20050200I.htm

陈建生, 汪集旸, 2004. 试论巴丹吉林沙漠地下水库的发现对西部调水计划的影响. 水利经济, 22(3): 28-32. doi: 10.3969/j.issn.1003-9511.2004.03.013

陈建生, 汪集旸, 2005. 阿尔金断裂中地下河对北山修建核废物库的不利影响. 水利经济, 23(1): 9-13. doi: 10.3969/j.issn.1003-9511.2005.01.002

陈建生, 汪集旸, 赵霞, 等, 2004. 用同位素方法研究额济纳盆地承压含水层地下水的补给. 地质论评, 50(6): 649-658. doi: 10.3321/j.issn:0371-5736.2004.06.017

陈建生, 赵霞, 盛雪芬, 等, 2006. 巴丹吉林沙漠湖泊群与沙山形成机理研究. 科学通报, 51(23): 2789-2796. doi: 10.3321/j.issn:0023-074X.2006.23.014

顾慰祖, 陈建生, 汪集旸, 等, 2004. 巴丹吉林高大沙山表层孔隙水现象的疑义. 水科学进展, 15(6): 695-699. doi: 10.3321/j.issn:1001-6791.2004.06.002

黄天明, 庞忠和, 2007. 应用环境示踪剂探讨巴丹吉林沙漠及古日乃绿洲地下水补给. 现代地质, 21(4): 624-631. doi: 10.3969/j.issn.1000-8527.2007.04.006

李宝兴, 1964. 中国干旱-沙漠地区水文地质特征. 治沙研究(6). 北京: 科学出版社, 1-32.

孙培善, 孙德钦, 1964. 内蒙古高原西部水文地质初步研究. 治沙研究(6). 北京: 科学出版社, 245-317.

阎满存, 王光谦, 董光荣, 等, 2001. 巴丹吉林沙漠沙山发育与环境演变研究, 中国沙漠, 21(4): 361-366. doi: 10.3321/j.issn:1000-694X.2001.04.008

杨小平, 2000. 近3万年来巴丹吉林沙漠的景观发育与雨量变化. 科学通报, 45(4): 428-434. doi: 10.3321/j.issn:0023-074X.2000.04.020

张伟民, 王涛, 2005. 巴丹吉林沙漠高大沙山形成演化初步探讨, 中国沙漠, 25(2): 281-286. doi: 10.3321/j.issn:1000-694X.2005.02.019

朱震达, 吴正, 刘恕, 等, 1980. 中国沙漠概论. 北京: 科学出版社, 73-78.

Relative Articles

Supplements(0)

Cited By

Proportional views

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

Figures(2) / Tables(2)

Get Citation

PDF

XML

Article views (3100) PDF downloads(75)

The Primary Opinion on the Formation Mechanisms of Megadunes and Lakes in the Badain Jaran Desert

doi: 10.3799/dqkx.2012.029

Abstract

References

Proportional views

Catalog

通讯作者: 陈斌, bchen63@163.com

Proportional views

Export File

Citation

Format

Content