Abstract
Based on the analysis of ion chemical composition of lake water and shallow groundwater in the Badain Jaran Desert, this paper discussed the characteristics of ion chemical composition, spatial variation of lake water, and possible supply sources of lake water and groundwater in the desert areas. The results show that the pH, salinity, TDS and electrical conductivity of the lake water are greater than those of groundwater. The ion contents of water samples are dominated by Na+ and Cl−. Most of the higher salinity lakes are Na (K)-Cl-(SO4) type, and a few of low salinity lakes belong to the Na-(Mg)-(Ca)-Cl-(SO4)-(HCO3) type. Most of the groundwater is Na-(Ca)-(Mg)-Cl-(SO4)-(HCO3) type, attributed to subsaline lake, and only a few present the Na-Cl-SO4 type, flowing under saline lake. The pH, salinity, TDS and electrical conductivity in the southeastern lakes are relatively low, and there are slightly alkaline lakes. The pH, salinity, TDS and electrical conductivity in the northern lakes are much greater than those of the southeastern lakes, and the northern lakes are moderately alkaline and saline ones. In the southeastern part of the Badain Jaran Desert, the ion chemical characteristics of the lake water from south to north show a changing trend of subsaline →saline→hypersaline. The changing trend of chemical compositions of ions in recent 9 years indicates that most of the ion contents have a shade of reduction in Boritaolegai, Badain, Nuoertu and Huhejilin lakes, which state clearly that the amount of fresh water supply is increasing in the 9-year period. The ion chemical composition of the lake water reveals that the flow direction of lake water is from southeast to northwest in the Badain Jaran Desert. The ion chemical composition, moisture content of sand layer water level height and hierarchical cluster analysis of the lake water and groundwater demonstrate that the lake water is mainly supplied by local rainfall and infiltration of precipitation in Yabulai Mountains and Heishantou Mountain, and the supply from the Qilian Mountains is almost impossible.
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References
Chen J S, Fan Z C, Wang J Y et al., 2003. Isotope methods for studying the replenishment of the lakes and downstream groundwater in the Badain Jaran Desert. Acta Geoscientia Sinica, 24(6): 497–504. (in Chinese)
Chen J S, Li L, Wang J Y et al., 2004. Ground water maintains dune landscape. Nature, 432: 459–460.
Chen J S, Zhao X, Sheng X F et al., 2006. Research on formation mechanism of megadunes and lakes in the Badain Jaran Desert. Chinese Science Bulletin, 51(23): 2789–2796. (in Chinese)
Ding H W, Zhang J, 2005. Goechemical properties and evolution of groundwater beneath the Hexi Corridor, Gansu Province. Arid Zone Research, 22(1): 24–29. (in Chinese)
Ding H W, Zhang J, 2009. Occurrence and development of deep underground water in Hexi Corridor. Northwestern Geology, 42(3): 109–120. (in Chinese)
Dong Z B, Qian G Q, Luo W Y et al., 2009. Geomorphological hierarchies for complex mega-dunes and their implications for mega-dune evolution in the Badain Jaran Desert. Geomorphology, 106(3/4): 180–185.
Dong Z B, Wang T, Wang X M, 2004. Geomorphology of the megadunes in the Badain Jaran Desert. Geomorphology, 60(1/2): 191–203.
Egorov A N, 1993. Mongolian salt lakes: Some features of their geography, thermal patterns, chemistry and biology. Hydrobiologia, 267: 13–21.
Feng Q, Chen G D, 1999. Moisture distribution and movement in sandy lands of China. Acta Pedologica Sinica, 36(2): 225–236. (in Chinese)
Feng Q, Cheng G D, Masao M K, 2000. Trends of water resource development and utilization in arid northwest China. Environmental Geology, 39: 831–836.
Gates J B, Edmunds W M, George W D et al., 2008. Conceptual model of recharge to southeastern Badain Jaran Desert groundwater and lakes from environmental tracers. Applied Geochemistry, 23: 3519–3534.
Hofmann J, 1996. The lakes in the SE part of Badain Jaran Shamo, their limnology and geochemistry. Geowissenschaften, 7/8: 275–278.
Jäkel D, 1996. The Badain Jaran Desert: Its origin and development. Geowissenschaften, 7/8: 272–274.
Jäkel D, 2002. The importance of dunes for groundwater recharge and storage in China. Zeitschrift für Geomorphologie NF, (Suppl.), 126: 131–146.
Liu Z, Edmunds W M, 1998. Physical Geographical Atlas of China. rev ed. Beijing: China Cartographic Publishing House, 252. (in Chinese)
Ma J Z, Chen F H, Zhao H, 2004. Groundwater recharge and climatic change during the last 1 000 years from unsaturated zone of SE Badain Jaran Desert. Chinese Science Bulletin, 49(1): 22–27. (in Chinese)
Ma J Z, Edmunds W M, 2006. Groundwater and lake evolution in the Badain Jaran Desert ecosystem, Inner Mongolia. Hydrogeology Journal, 14: 1231–1243.
Ma J Z, Edmunds W M, Chen F, 2003. Groundwater geochemistry evolution and unsaturated zone archives of climatic change in arid NW China. XVI INQUA Congress; Shaping the Earth: A Quaternary perspective, 177–178.
Ma J Z, Edmunds W M, He J H et al., 2009. A 2000 year geochemical record of palaeoclimate and hydrology derived from dune sand moisture. Palaeogeography, Palaeoclimatology, Palaeoecology, 276: 38–46.
Ma J Z, Qian J, 2000. The groundwater evolution and its influence on the fragile ecology in the south edge of Tarim Basin. Journal of Desert Research, 20: 145–149.
Ma J Z, Wang S X, Edmunds W M, 2005. The characteristics of groundwater resources and their changes under the impacts of human activity in the arid northwest China: A case study of the Shiyang River Basin. Journal of Arid Environment, 61: 277–295.
Ma L, 2002. Geological Atlas of China. Beijing: Geological Press. (in Chinese)
Ma N N, Yang X P, 2008. Environmental isotopes and water chemistery in the Badain Jaran Desert and in its southeastern adjacent areas, Inner Mongolia and their hydrological implications. Quaternary Sciences, 28(4): 702–712. (in Chinese)
Mao S F, Liu K N, 2000. Application of Ion Chromatography and Method. Beijing: Chemical Industry Press, 64–128. (in Chinese)
National Technology Agency of China (NTAC), 1996. Methods for Examination of Drinking Natural Mineral Water. Beijing: Norms in China Press, 2–147. (in Chinese)
Ren M, 1980. The Outline of Physical Geography of China. Rev. ed. Beijing: The Commercial Press, 412. (in Chinese)
Shao T J, Zhao J B, Li E J et al., 2010. Grain size composition of typical mega-dune in Badain Jaran Desert. Scientia Geographica Sinica, 30(5): 790–796. (in Chinese)
Wang G, Cheng G, 1999. Water resource development and its influence on the environment in arid areas of China: The case of the Hei River basin. Journal of Arid Environments, 43: 121–131.
Wang Q Y, 2004. The exploitation of groundwater in the plain of Hexi Corridor in Gansu Province. Gansu Hydropower Technology, 40(3): 202–204. (in Chinese)
Wang T, 1990. Formation and evolution of Badain Jirin Sandy Desert, China. Journal of Desert Research, 10: 29–40. (in Chinese)
Yan M C, Wang G Q, Li B S et al., 2001. Formation and growth of high megadunes in Badain Jaran Desert. Acta Geographica Sinica, 56(1): 83–91. (in Chinese)
Yang X P, 2002. Water chemistry of the lakes in the Badain Jaran Desert and their Holocene evolutions. Quaternary Sciences, 22(2): 97–10. (in Chinese)
Yang X P, 2006. Chemistry and late Quaternary evolution of ground and surface waters in the area of Yabulai Mountains, western Inner Mongolia, China. Catena, 66: 135–144.
Yang X P, 2000. Landscape evolution and precipitation changes in the Badain Jaran Desert during the last 30,000 years. Chinese Science Bulletin, 45: 1042–1047. (in Chinese)
Yang X P, Liu T S, Xiao H L, 2003. EEvolution of megadunes and lakes in the Badain Jaran Desert, Inner Mongolia, China during the last 31000 yrs. Quaternary International, 104: 99–112.
Yang X P, Louis A Scuderi, 2010. Hydrological and climatic changes in deserts of China since the late Pleistocene. Quaternary Research, 73: 1–9.
Yang X P, Ma N N, Dong J F et al., 2010. Recharge to the inter-dune lakes and Holocene climatic changes in the Badain Jaran Desert, western China. Quaternary Research, 73: 10–19.
Yang X P, Williams M A, 2003. The ion chemistry of lakes and late Holocene desiccation in the Badain Jaran Desert, Inner Mongolia, China. Catena, 51: 45–60.
Yu S, Li B, Cai W et al., 1962. Expedition into Gobi of western Inner Mongolia and the Badain Jaran Desert. Research on Sand Stabilization 3, 96–107. (in Chinese)
Zhao C F, Li S B, Feng Z D et al., 2009. Dynamics of groundwater level in the water table fluctuant belt at the lower reaches of Heihe River. Journal of Desert Research, 29(2): 365–370. (in Chinese)
Zhao J B, Shao T J, Lv X H et al., 2010. The study on CO2 concentration and the diurnal variation laws of the highest mega dune in the Badain Jaran Desert. Geographical Research, 29(11): 1994–2005. (in Chinese)
Zhu Z, Wu Z, Liu S et al., 1980. An Outline of Chinese Deserts. Beijing: Science Press. (in Chinese)
Zhu Z D, Jürgen Hövermann, Diter Jakel, 1998. Aeolian Landform Map of Badain Jaran Desert. Xi’an: Xi’an Map Press.
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Foundation: Yangtze River Scholar Bonus Schemes of China, No.801813; National Natural Science Foundation of China, No.40672108
Author: Shao Tianjie (1982–), Ph.D Candidate, specialized in regional environment in arid regions.
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Shao, T., Zhao, J., Zhou, Q. et al. Recharge sources and chemical composition types of groundwater and lake in the Badain Jaran Desert, northwestern China. J. Geogr. Sci. 22, 479–496 (2012). https://doi.org/10.1007/s11442-012-0941-2
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DOI: https://doi.org/10.1007/s11442-012-0941-2