Chinese Geographical Science

, Volume 28, Issue 1, pp 61–73 | Cite as

An Estimation of Ground Ice Volumes in Permafrost Layers in Northeastern Qinghai-Tibet Plateau, China

  • Shengting Wang
  • Yu Sheng
  • Jing Li
  • Jichun Wu
  • Wei Cao
  • Shuai Ma
Article
  • 3 Downloads

Abstract

The ground ice content in permafrost serves as one of the dominant properties of permafrost for the study of global climate change, ecology, hydrology and engineering construction in cold regions. This paper initially attempts to assess the ground ice volume in permafrost layers on the Qinghai-Tibet Plateau by considering landform types, the corresponding lithological composition, and the measured water content in various regions. An approximation demonstrating the existence of many similarities in lithological composition and water content within a unified landform was established during the calculations. Considerable knowledge of the case study area, here called the Source Area of the Yellow (Huanghe) River (SAYR) in the northeastern Qinghai-Tibet Plateau, has been accumulated related to permafrost and fresh water resources during the past 40 years. Considering the permafrost distribution, extent, spatial distribution of landform types, the ground ice volume at the depths of 3.0–10.0 m below the ground surface was estimated based on the data of 101 boreholes from field observations and geological surveys in different types of landforms in the permafrost region of the SAYR. The total ground ice volume in permafrost layers at the depths of 3.0–10.0 m was approximately (51.68 ± 18.81) km3, and the ground ice volume per unit volume was (0.31 ± 0.11) m3/m3. In the horizontal direction, the ground ice content was higher in the landforms of lacustrine-marshland plains and alluvial-lacustrine plains, and the lower ground ice content was distributed in the erosional platforms and alluvial-proluvial plains. In the vertical direction, the volume of ground ice was relatively high in the top layers (especially near the permafrost table) and at the depths of 7.0–8.0 m. This calculation method will be used in the other areas when the necessary information is available, including landform type, borehole data, and measured water content.

Keywords

ground ice volume permafrost source area of the Yellow River Qinghai-Tibet Plateau 

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Notes

Acknowledgement

The digital Geomorphological Map of Western China (1: 1 000 000) was provided by the Environmental and Ecological Science Data Center for West China, National Natural Science Foundation of China (http://westdc.westgis.ac.cn).

References

  1. Bian Chunyu, Guo Pengfei, 1990. Geomorphic characteristics of periglacier in the source area of Yellow River in Qinghai-Xizang Plateau, China. Journal of Glaciology and Geocryology, 12(2): 147–153. (in Chinese)Google Scholar
  2. Bray M T, French H M, Shur Y, 2006. Further cryostratigraphic observations in the CRREL permafrost tunnel, Fox, Alaska. Permafrost and Periglacial Processes, 17(3): 233–243. doi: 10.1002/ppp.558CrossRefGoogle Scholar
  3. Brown J, Ferrians Jr O J, Heginbottom J A et al., 1997. Circum-Arctic Map of Permafrost and Ground-ice Conditions. Virginia: American Department of the Interior and American Geology Survey.Google Scholar
  4. Burn C R, 1988. The development of near-surface ground ice during the Holocene at sites near Mayo, Yukon Territory, Canada. Journal of Quaternary Science, 3(1): 31–38. doi: 10. 1002/jqs.3390030106CrossRefGoogle Scholar
  5. Cao Wenbing, Wan Li, Zhou Xun et al., 2003. A study of the geological environmental of suprapermafrost water in the headwater area of the Yellow River. Hydrogeology & Engineering Geology, 30(6): 6–10. (in Chinese)Google Scholar
  6. Cheng G D, 1983. The mechanism of repeated-segregation for the formation of thick layered ground ice. Cold Regions Science and Technology, 8(1): 57–66. doi: 10.1016/0165-232X(83)90017-4CrossRefGoogle Scholar
  7. Cheng Guodong, Jin Huijun, 2013. Groundwater in the permafrost regions on the Qinghai-Tibet Plateau and it changes. Hydrogeology & Engineering Geology, 40(1): 1–11. (in Chinese)Google Scholar
  8. Cheng Jia, Zhao Xiangqing, Yang Xiaoming, 2011. Research of frost-heaving ratio of typical soil samples from permafrost regions of Golmud-Lhasa railway. Journal of Glaciology and Geocryology, 33(4): 863–866. (in Chinese)Google Scholar
  9. Cheng Weiming, Zhou Chenghu, Li Bingyuan et al., 2011. Structure and contents of layered classification system of digital geomorphology for China. Journal of Geographical Sciences, 21(5): 771–790. doi: 10.1007/s11442-011-0879-9CrossRefGoogle Scholar
  10. Cheng Weiming, Zhou Chenghu, 2014. Methodology on hierarchical classification of multi-scale digital geomorphology. Progress in Geography, 33(1): 23–33. doi: 10.11820/dlkxjz. 2014.01.003Google Scholar
  11. French H, Shur Y, 2010. The principles of cryostratigraphy. Earth-Science Reviews, 101(3-4): 190–206. doi: 10.1016/j.earscirev.2010.04.002CrossRefGoogle Scholar
  12. Garagula L S, 1992. Forecasting Evaluation Method of Frozen Soil Conditions Changed by Human Activity. Tong Boliang trans. Lanzhou: Gansu Science and Technology Press. (in Chinese)Google Scholar
  13. Gilbert G L, Kanevskiy M, Murton J B, 2016. Recent advances (2008–2015) in the study of ground ice and cryostratigraphy. Permafrost and Periglacial Processes, 27(4): 377–389. doi: 10.1002/ppp.1912CrossRefGoogle Scholar
  14. Huang Xiling, Xi Yanjing, Wang Tiehong et al., 2011. Code for Design of Building Foundation (GB 50007–2011). Beijing: China Architecture & Building Press. (in Chinese)Google Scholar
  15. Jin Huijun, Zhao Lin, Wang Shaoling et al., 2006. Evolution of permafrost and environmental changes of cold regions in eastern and interior Qinghai-Tibetan Plateau since the Holocene. Quaternary Sciences, 26(2): 198–210. (in Chinese)Google Scholar
  16. Jin Huijun, Wang Shaoling, Lü Lanzhi et al., 2010. Features and degradation of frozen ground in the sources area of the Yellow River, China. Journal of Glaciology and Geocryology, 32(1): 10–17. (in Chinese)Google Scholar
  17. Kanevskiy M, Shur Y, Fortier D et al., 2011. Cryostratigraphy of late Pleistocene syngenetic permafrost (yedoma) in northern Alaska, Itkillik River exposure. Quaternary Research, 75(3): 584–596. doi: 10.1016/j.yqres.2010.12.003CrossRefGoogle Scholar
  18. Kanevskiy M, Shur Y, Krzewinski T et al., 2013a. Structure and properties of ice-rich permafrost near Anchorage, Alaska. Cold Regions Science and Technology, 93: 1–11. doi: 10.1016/j. coldregions.2013.05.001CrossRefGoogle Scholar
  19. Kanevskiy M, Shur Y, Jorgenson M T et al., 2013b. Ground ice in the upper permafrost of the Beaufort Sea coast of Alaska. Cold Regions Science and Technology, 85: 56–70. doi: 10.1016/j.coldregions.2012.08.002CrossRefGoogle Scholar
  20. Kokelj S V, Burn C R, 2003. Ground ice and soluble cations in near-surface permafrost, Inuvik, Northwest Territories, Canada. Permafrost and Periglacial Processes, 14(3): 275–289. doi: 10.1002/ppp.458CrossRefGoogle Scholar
  21. Kokelj S V, Burn C R, 2005. Near-surface ground ice in sediments of the Mackenzie Delta, Northwest Territories, Canada. Permafrost and Periglacial Processes, 16(3): 291–303. doi: 10.1002/ppp.537CrossRefGoogle Scholar
  22. Li J, Sheng Y, Wu J C et al., 2016a. Landform-related permafrost characteristics in the source area of the Yellow River, eastern Qinghai-Tibet Plateau. Geomorphology, 269: 104–111. doi: 10.1016/j.geomorph.2016.06.024CrossRefGoogle Scholar
  23. Li Jing, Sheng Yu, Wu Jichun et al., 2016b. Mapping frozen soil distribution and modeling permafrost stability in the Source Area of the Yellow River. Scientia Geographica Sinica, 36(4): 588–596. (in Chinese)Google Scholar
  24. Li Wanshou, Feng ling, Sun Shengli et al., 2001. Influence of Zaling and Eling Lake on the annual discharge of the Huanghe River Source Area. Acta Geographica Sinica, 56(1): 75–82. (in Chinese)Google Scholar
  25. Lin Xueyu, Liao Zisheng, Qian Yunping et al., 2009. Baseflow separation for groundwater study in the Yellow River Basin, China. Journal of Jilin University (Earth Science Edition), 39(6): 959–967. (in Chinese)Google Scholar
  26. Luo Dongliang, Jin Huijun, Lin Lin et al., 2012. New progress on permafrost temperature and thickness in the source area of the Huanghe River. Scientia Geographica Sinica, 32(7): 898–904. (in Chinese)Google Scholar
  27. Luo Dongliang, Jin Huijun, Lin Lin et al., 2013. Distributive features and controlling factors of permafrost and the active layer thickness in the Bayan Har Mountains along the Qinghai-Kangding Highway on Northeastern Qinghai-Tibet Plateau. Scientia Geographica Sinica, 33(5): 635–640. (in Chinese)Google Scholar
  28. Luo Dongliang, Jin Huijun, Lü Lanzhi et al., 2014. Spatiotemporal characteristics of freezing and thawing of the active layer in the source areas of the Yellow River (SAYR). Chinese Science Bulletin, 59(24): 3034–3045. doi: 10.1007/s11434-014-0189-6CrossRefGoogle Scholar
  29. Mackay J R, 1983. Downward water movement into frozen ground, western Arctic coast, Canada. Canadian Journal of Earth Sciences, 20(1): 120–134. doi: 10.1139/e83-012CrossRefGoogle Scholar
  30. Mackay J R, Burn C R, 2002. The first 20 years (1978–1979 to 1998–1999) of active-layer development, Illisarvik experimental drained lake site, western Arctic coast, Canada. Canadian Journal of Earth Sciences, 39(11): 1657–1674. doi: 10. 1139/e02-068CrossRefGoogle Scholar
  31. Morse P D, Burn C R, Kokelj S V, 2009. Near-surface ground-ice distribution, Kendall Island Bird Sanctuary, western Arctic coast, Canada. Permafrost and Periglacial Processes, 20(2): 155–171. doi: 10.1002/ppp.650CrossRefGoogle Scholar
  32. O’Neill H B, Burn C R, 2012. Physical and temporal factors controlling the development of near-surface ground ice at Illisarvik, western Arctic coast, Canada. Canadian Journal of Earth Sciences, 49(9): 1096–1110. doi: 10.1139/e2012-043CrossRefGoogle Scholar
  33. Penck W, 1964. Landforms Analysis. Jiang Meiqiu, trans. Beijing: Department of Geology and Geography, Peking University.Google Scholar
  34. Shur Y, Zhestkova T, 2003. Cryogenic structure of a glacio-lacustrine deposit. Proceedings of the Eighth International Conference on Permafrost. Zurich, Switzerland, 2: 1051–1056.Google Scholar
  35. Shur Y, French H M, Bray M T et al., 2004. Syngenetic permafrost growth: cryostratigraphic observations from the CRREL Tunnel near Fairbanks, Alaska. Permafrost and Periglacial Processes, 15(4): 339–347. doi: 10.1002/ppp.486CrossRefGoogle Scholar
  36. Shur Y, Hinkel K M, Nelson F E, 2005. The transient layer: implications for geocryology and climate-change science. Permafrost and Periglacial Processes, 16(1): 5–17. doi: 10.1002/ ppp.518CrossRefGoogle Scholar
  37. Vieira G, López-Martínez J, Serrano E et al., 2008. Geomorphological observations of permafrost and ground-ice degradation on Deception and Livingston Islands, Maritime Antarctica. In: Proceedings of the 9th International Conference on Permafrost. Fairbanks, Alaska, 29: 1839–1844. doi: 10.5167/uzh-3320Google Scholar
  38. Wang Genxu, Shen Yongping, Cheng Guodong, 2000. Ecoenvironmental changes and causal analysis in the Source Regions of the Yellow River. Journal of Glaciology and Geocryology, 22(3): 200–205. (in Chinese)Google Scholar
  39. Wang G X, Cheng G D, 2000. Eco-environmental changes and causative analysis in the source regions of the Yangtze and Yellow Rivers, China. Environmentalist, 20(3): 221–232. doi: 10.1023/A:1006703831018CrossRefGoogle Scholar
  40. Wang H D, 1987. The water resources of lakes in China. Chinese Journal of Oceanology and Limnology, 5(3): 263–280. doi: 10. 1007/BF02843990CrossRefGoogle Scholar
  41. Wang H J, Yang Z S, Saito Y et al., 2006. Interannual and seasonal variation of the Huanghe (Yellow River) water discharge over the past 50 years: connections to impacts from ENSO events and dams. Global and Planetary Change, 50(3-4): 212–225. doi: 10.1016/j.gloplacha.2006.01.005CrossRefGoogle Scholar
  42. Wang Jiacheng, Wang Shaoling, Qiu Guoqing, 1979. Permafrost along the Qinghai-Xizang highway. Acta Geographica Sinica, 34(1): 18–32. (in Chinese)Google Scholar
  43. Wang Shaoling, 1989. Formation and evolution of permafrost on the Qinghai-Xizang Plateau since the late Pleistocene. Journal of Glaciology and Geocryology, 11(1): 69–75. (in Chinese)Google Scholar
  44. Wu Jichun, Sheng Yu, Wu Qingbai et al., 2009. Discussion on the possibility of taking ground ice in permafrost regions as water sources under climate warming. Journal of Glaciology and Geocryology, 31(2): 350–356. (in Chinese)Google Scholar
  45. Xu Xiaozu, Wang Jiacheng, Zhang Lixin, 2010. Physics of Frozen Ground. Beijing: Science Press, 39–85. (in Chinese)Google Scholar
  46. Yang Jianping, Ding Yongjian, Chen Rensheng, 2007. Climatic causes of ecological and environmental variations in the source regions of the Yangtze and Yellow Rivers of China. Environmental Geology, 53(1): 113–121. doi: 10.1007/s00254-006-0623-4CrossRefGoogle Scholar
  47. Yasuhara H, Elsworth D, Polak A, 2004. Evolution of permeability in a natural fracture: significant role of pressure solution. Journal of Geophysical Research, 109(B3): B03204. doi: 10. 1029/2003JB002663Google Scholar
  48. Yasuhara H, Elsworth D, Polak A et al., 2006. Spontaneous switching between permeability enhancement and degradation in fractures in carbonate: lumped parameter representation of mechanically-and chemically-mediated dissolution. Transport in Porous Media, 65(3): 385–409. doi: 10.1007/s11242-006-6386-2CrossRefGoogle Scholar
  49. Zhang Senqi, Wang Yonggui, Zhao Yongzhen et al., 2004. Permafrost degradation and its environmental sequent in the Source Regions of the Yellow River. Journal of Glaciology and Geocryology, 26(1): 1–6. (in Chinese)Google Scholar
  50. Zhang T, Barry R G, Knowles K et al., 1999. Statistics and characteristics of permafrost and ground-ice distribution in the Northern Hemisphere. Polar Geography, 23(2): 132–154. doi: 10.1080/10889379909377670CrossRefGoogle Scholar
  51. Zhang Xiumin, Sheng Yu, Li Jing et al., 2012. Changes of alpine ecosystem along the ground temperature of permafrost in the source region of Datong River in the Northeastern Qinghai-Tibet Plateau. Journal of Food, Agriculture & Environment, 10(1): 970–976.Google Scholar
  52. Zhao Lin, Ding Yongjian, Liu Guangyue et al., 2010. Estimates of the reserves of ground ice in permafrost regions on the Tibetan Plateau. Journal of Glaciology and Geocryology, 32(1): 1–9. (in Chinese)Google Scholar
  53. Zhou Chenghu, Cheng Weiming, Qian Jinkai et al., 2009. Research on the classification system of digital land geomorphology of 1:1000000 in China. Journal of Geo-Information Science, 11(6): 707–724. (in Chinese)CrossRefGoogle Scholar
  54. Zhou Chenghu, Cheng Weiming, 2007. Geomorphological Map of Western China (1:1000000). Beijing: Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences. (in Chinese)Google Scholar
  55. Zhou Youwu, Guo Dongxin, 1982. Principal characteristics of permafrost in China. Journal of Glaciology and Geocryology, 4(1): 1–19, 95–96. (in Chinese)Google Scholar

Copyright information

© Science Press, Northeast Institute of Geography and Agricultural Ecology, CAS and Springer-Verlag GmbH Germany, part of Springer Nature 2018

Authors and Affiliations

  • Shengting Wang
    • 1
    • 2
  • Yu Sheng
    • 1
  • Jing Li
    • 1
  • Jichun Wu
    • 1
  • Wei Cao
    • 1
  • Shuai Ma
    • 1
    • 2
  1. 1.State Key Laboratory of Frozen Soil Engineering, Northwest Institute of Eco-Environmental and ResourcesChinese Academy of SciencesLanzhouChina
  2. 2.University of Chinese Academy of SciencesBeijingChina

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