Soil taxonomy and distribution characteristics of the permafrost region in the Qinghai-Tibet Plateau, China

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• 作者：Hong-bing Fang ; Lin Zhao ; Xiao-dong Wu ; Yu-guo Zhao&#8230
• 关键词：Qinghai ; Tibet Plateau ; Permafrost region ; Soil taxonomy ; Soil distribution
• 刊名：Journal of Mountain Science
• 出版年：2015
• 出版时间：November 2015
• 年：2015
• 卷：12
• 期：6
• 页码：1448-1459
• 全文大小：587 KB
• 参考文献：Bad铆a D, Mart铆 C, Aznar JM, et al. (2013) Influence of slope and parent rock on soil genesis and classification in semiarid mountainous environments. Geoderma 193: 13鈥?1. DOI: 10.1016/j.geoderma.2012.10.020CrossRef
  Baumann F, He JS, Schmidt K, et al. (2009) Pedogenesis, permafrost, and soil moisture as controlling factors for soil nitrogen and carbon contents across the Tibetan Plateau. Global Change Biology 15: 3001鈥?017. DOI: 10.1111/j.1365-2486.2009.01953.xCrossRef
  Bockheim JG (1997) Properties and classification of cold desert soils from Antarctica. Soil Science Society of America Journal 61: 224鈥?31. DOI: 10.2136/sssaj1997.03615995006100010031xCrossRef
  Cheng GD, Wu TH (2007) Responses of permafrost to climate change and their environmental significance, Qinghai-Tibet Plateau. Journal of Geophysical Research 112: 1鈥?0. DOI: 10.1029/2006JF000631CrossRef
  Cheng ZG, Liu XD (2008) A preliminary study of future permafrost distribution on the Qinghai-Tibet Plateau under global warming conditions. Areal Research and Development 27: 80鈥?5. DOI: 10.3969/j.issn.1003-2363.2008.06.020
  Chinese Soil Taxonomy Research Group, Institute of Soil science, Chinese Academy of Sciences, Cooperative Research Group on Chinese Soil Taxonomy (2001) Keys to Chinese Soil Taxonomy (3rd Ed.). Chinese Science and Technological University Press, Hefei, China. pp 21鈥?91. (In Chinese)
  Dahlgren RA, Boettinger JL, Huntington GL, et al. (1997) Soil development along an elevational transect in the western Sierra Nevada, California. Geoderma 78: 207鈥?36. DOI: 10.1016/S0016-7061(97)00034-7CrossRef
  Day JH, Rice HM (1964) The characteristics of some permafrost soils in the Mackenzie Valley, N.W.T. Arctic 17: 222鈥?36. DOI: 10.14430/arctic3506CrossRef
  Duan ZH, Zhang Y, Zhang W, et al. (2012) Application research of four cold regions land surface and hydrological model to Qinghai-tibet Plateau frozen soil region. Journal of Water Resources and Water Engineering 23: 43鈥?0.
  Eash NS, Sandor JA (1995) Soil chronosequence and geomorphology in a semi-arid valley in the Andes of southern Peru. Geoderma 65: 59鈥?9. DOI: 10.1016/0016-7061(94) 00025-6CrossRef
  Gong ZT (1999) Chinese Soil Taxonomy: Theories, Methods and Practices. Science Press, Beijing, China. p 29. (In Chinese)
  Gong ZT, Zhang GL, Chen ZC, et al. (2007) Pedogenesis and soil taxonomy. Science Press, Beijing, China. pp 29鈥?4. (In Chinese)
  H枚fle C, Ping CL (1996) Properties and soil development of late-Pleistocene paleosols from Seward Peninsula, northwest Alaska. Geoderma 71: 219鈥?43. DOI: 10.1016/0016-7061(96)00007-9CrossRef
  H枚fle C, Ping CL, Kimble JM (1998) Properties of permafrost soils on the northern Seward Peninsula, northwest Alaska. Soil Science Society of America Journal 62: 1629鈥?639. DOI: 10.2136/sssaj1998.03615995006200060021xCrossRef
  Huang CY (2000) Pedology. China Agriculture Press, Beijing, China. pp 3鈥?42. (In Chinese)
  Krasnoshchekov YN (2008) Soil cover of mountain forests in the East Khubsugul region of Mongolia. Eurasian Soil Science 41: 694鈥?03. DOI: 10.1134/S106422930807003XCrossRef
  Krasnoshchekov YN (2010) Soils and the soil cover of mountainous tundra and forest landscapes in the Central Khangai of Mongolia. Eurasian Soil Science 43: 117鈥?26. DOI: 10.1134/S1064229310020018CrossRef
  Li N, Wang GX, Gao YH, et al. (2009) On soil organic carbon of alpine ecosystem in Qinghai-Tibet Plateau. Soils 41: 512鈥?19. DOI: 10.3321/j.issn:0253-9829.2009.04.002
  Li SD, Cheng GD (1996) Map of Frozen Ground on Qinghai-Xizang Plateau. Gansu Culture Press, Lanzhou, China.
  National Soil Survey Center, Natural Resources Conservation Service, U.S. Department of Agriculture (2002) Field Book for Describing and Sampling Soils.
  Niu YF (1999) The study of environment in the Qinghai-Xizang Plateau. Progress in Geography 18: 163鈥?71.
  Ping CL, Gary J, Michaelson MT, et al. (2008) High stocks of soil organic carbon in the North American Arctic region. Nature Geoscience 1: 615鈥?19, DOI: 10.1038 /ngeo284CrossRef
  Ran YH, Li X, Cheng GD, et al. (2012) Distribution of permafrost in China: An overview of existing permafrost maps. Permafrost and Periglacial Processes 23: 322鈥?33. DOI: 10.1002/ppp.1756CrossRef
  Singh S, Parkash B, Rao MS, et al. (2006) Geomorphology, pedology and sedimentology of the Deoha/Ganga-Ghaghara Interfluve, Upper Gangetic Plains (Himalayan Foreland Basin) -Extensional tectonic implications. Catena 67: 183鈥?03. DOI: 10.1016/j.catena.2006.03.013CrossRef
  Sommer M (2006) Influence of soil pattern on matter transport in and from terrestrial biogeosystems-A new concept for landscape pedology. Geoderma 133: 107鈥?23. DOI: 10.1016/j. geoderma.2006.03.040CrossRef
  Tarnocai C, Canadell J, Schuur E, et al. (2009) Soil organic carbon pools in the northern circumpolar permafrost region. Global Biogeochemical Cycles 23: 1鈥?1. DOI: 10.1029/2008GB003327CrossRef
  Wang GX, Li YS, Wang YB, et al. (2008) Effects of permafrost thawing on vegetation and soil carbon pool losses on the Qinghai-Tibet Plateau, China. Geoderma 143: 143鈥?52. DOI: 10.1016/j.geoderma.2007.10.023CrossRef
  Wang GX, Qian J, Cheng GD, et al. (2002) Soil organic carbon pool of grassland soils on the Qinghai-Tibetan Plateau and its global implication. Science of the Total Environment 291: 207鈥?17. DOI: 10.1016 0048-9697(01)01100-7CrossRef
  Wang GX, Wang YB, Li YS, et al. (2007) Influences of alpine ecosystem responses to climatic change on soil properties on the Qinghai-Tibet Plateau, China. Catena 70: 506鈥?14. DOI: 10.1016/j.catena.2007.01.001CrossRef
  Wang JF, Wu QB (2011) Influences of the vegetation degradation on the shallow cryic soil environment in the wet meadow areas on the Qinghai-Tibetan Plateau. Journal of Lanzhou University (Natural Sciences) 47: 39鈥?5.
  Wei SG, Dai YJ, Duan QY, et al. (2014) A global soil dataset for Earth System Modeling. Journal of Advances in Modeling Earth Systems 6: 249鈥?63. DOI: 10.1002/2013MS000293CrossRef
  Wei SG, Dai YJ, Liu BY, et al. (2012) A soil particle-size distribution dataset for regional land and climate modelling in China. Geoderma 171(SI): 85鈥?1. DOI: 10.1016/j.geoderma. 2011.01.013
  Wei SG, Dai YJ, Liu BY, et al. (2013) A China data set of soil properties for land surface modeling. Journal of Advances in Modeling Earth Systems 5: 212鈥?24. DOI: 10.1002/jame. 20026CrossRef
  Wei YL, Zhou ZH, Liu GC (2012) Physico-chemical properties and enzyme activities of the arable soils in Lhasa, Tibet, China. Journal of Mountain Science 9: 558鈥?69. DOI: 10.1007/s11629-012-2165-4CrossRef
  Wu XD, Zhao L, Chen MJ, et al. (2012) Soil organic carbon and its relationship to vegetation communities and soil properties in permafrost areas of the central western Qinghai -Tibet Plateau, China. Permafrost and Periglacial Processes 23: 162鈥?69. DOI: 10.1002/ppp.1740CrossRef
  Yang JP, Ding YJ, Chen RS (2005) NDVI reflection of alpine vegetation changes in the source regions of the Yangtze and Yellow Rivers. Acta Geographica Sinica 60: 467鈥?78. DOI: 10.3321/j.issn:0375-5444.2005.03.013
  Yang MX, Wang SL, Yao TD, et al. (2004) Desertification and its relationship with permafrost degradation in Qinghai-Xizang (Tibet) Plateau. Cold Regions Science and Technology 39: 47鈥?3. DOI:10.1016/j.coldregions.2004.01.002CrossRef
  Zhang XM, Sheng Y, Zhao L, et al. (2012) Permafrost distribution using sub-region classification and multivariate data in the Wenquan area over the Qinghai-Tibet Plateau. Scientia Geographica Sinica 32: 1513鈥?520.CrossRef
  Zhao L, Ping CL, Yang DQ, et al. (2004) Changes of climate and seasonally frozen ground over the past 30 years in Qinghai-Xizang (Tibetan) Plateau, China. Global and Planetary Change 43: 19鈥?1. DOI: 10.1016/j.gloplacha.2004.02.003CrossRef
  Zhao YG, Zhang GL (2011) Chinese Soil Map. Science Press, Beijing, China.
  Zhou YW, Guo DX, Qiu GQ, et al. (2000) Geocryology in China. Science Press, Beijing, China. p 44.
  
• 作者单位：Hong-bing Fang (1) (2) (3)
  Lin Zhao (1)
  Xiao-dong Wu (1)
  Yu-guo Zhao (4)
  Yong-hua Zhao (1)
  Guo-jie Hu (1)
  
  1. Cryosphere Research Station on the Qinghai-Tibetan Plateau, State Key Laboratory of Cryospheric Sciences, Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou, 730000, China
  2. Graduate University of Chinese Academy of Sciences, Beijing, 100049, China
  3. School of Environmental and Municipal Engineering, Lanzhou Jiaotong University, Lanzhou, 730070, China
  4. State Key Laboratory of Soil and Sustainable Agriculture, Institute of Soil Science, Chinese Academy of Sciences, Nanjing, 210008, China
  
• 刊物主题：Earth Sciences, general; Geography (general); Environment, general; Ecology;
• 出版者：Springer Berlin Heidelberg
• ISSN：1993-0321

文摘

Understanding the soil taxonomy and distribution characteristics of the permafrost region in the Qinghai-Tibet Plateau (QTP) is very important. On the basis of extensive field surveys and experimental analysis, this study carries out soil taxonomic classification of the permafrost region in the QTP. According to Chinese Soil Taxonomy, the soil of the permafrost region in the QTP can be divided into 6 Orders (Histosols, Aridosols, Gleyosols, Isohumosols, Cambosols, Primosols), 11 Suborders, 19 Groups and 24 Subgroups. Cambosols are the dominant soil type in the permafrost region, followed by Aridosols. From the east to the west of the permafrost region in the QTP, the soil type gradually changes from Cambosols to Aridosols, showing a meridional zonality. The eastern region is dominated by Cambosols, with no obvious latitudinal zonality. From the south to the northwest of the western region, the dominance of Aridosols and Cambosols gradually transited to Aridosols, presenting a latitudinal zonality. The soil in the western region shows a poor vertical zonality, while the distribution of suborders of Cambosols in the eastern region shows a more obvious vertical zonality. The result indicates that precipitation and vegetation are the main factors that influence the zonal distribution of soil. The permafrost in the east has some effect on the vertical soil zonality, but the effect is weakened in the west. Keywords Qinghai-Tibet Plateau Permafrost region Soil taxonomy Soil distribution