Permafrost

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Theme 1-3: Engineering: Frozen ground interactions and models (Location: Small Hall of North Building) Chairs: Luxin Zhang, Aldar Gorbunov Zhaohui (Joey) Yang, Tpal Dutta Effects of seasonal frozen soil on soil-foundation-structure interaction Aldar P.Gorbunov, Edward V.Seversky The features of engineering and geological researches under opening up of permafrost of the high mountains of Central Asia Yue-dong Wang, Li Hongsheng Numerical simulation of nonlinear fracture failure process in frozen soil Rorik A Peterson, Julian B Murton Laboratory and numerical modeling of rock and concrete fracture due to thermally-induced water migration Jian-bing Chen, Shuang-jie Wang, Jin-zhao Zhang, Wei Ma Study on the formation and mechanisms of high subgrade diseases of the Qinghai-Tibet Highway Theme 5-1: Mapping: Monitoring and modeling (Location: No.1 Conference-room of Zhongxiaolou Building) Chairs: Sergey Marchenko, Tingjun Zhang Xiaozhen Xiong, Chris Barnet, Eric Maddy, Xingpin Liu, Lihang Zhou, Walter Wolf, Mitch Goldberg Towards the satellite monitoring of methane emission from permafrost N. Sharkhuu, Sh. Anarmaa Monitoring of permafrost in Mongolia Tonghua Wu, Shuxun Li, Guodong Cheng, Lin Zhao, Qinxue Wang, Masataka Watanabe Application of GPR in permafrost detection and field survey design in Mongolia Nikolay I. Shiklomanov, Oleg A. Amisimov, Tingjun Zhang, Vladimir E. Romanovsky Multiscale, hierarchical approach to validation of spatial permafrost models Fuqun Zhou, Aining Zhang, Robert Li Surface-coupled 3-D permafrost model for impact assessment on building foundations in Northern Canada due to permafrost degradation Theme 2-1: Slope processes, rock glaciers, and planetary (Location: Multifunctional-hall of VIP Building) Chairs: W A Mitchell, Stuart Harris V.N. Zaitsev Features of hydrothermal conditions and cryogenic structure of kurums in the Udokan Range W A Mitchell Rock glaciers and mountain permafrost in Zanskar, NW Indian Himalaya 9
10 Reynald DELALOYE, Christophe LAMBIEL, Jonathan DORTHE, Sébastien MORARD Mapping and monitoring strategies for detecting air circulation processes in blocky terrain Stuart A. Harris, Guodong Cheng, Cui Zhijiu Active lag block streams in the Chinese Tian Shan 16:00–16:20 Coffee Break 16:20–18:00 Oral session Theme 1-4: Engineering: Construction methods and results (Location: Small Hall of North Building) Chairs: Bo Liang, Zhaohui Yang Vladimir Petroveth Vlasov Effect of seismic events on the stability of buildings on permafrost: a case study Bo Liang, Yuan-ping Cao, Jian-jun Ge , Cheng Wang Test and analysis about the development of depth of seasonal-thawing of L-type retaining wall Xue-fu Zhang The elementary study on the chain-styled mechanism and the new-typed method to the chain breakage of the water leakage hazard in Kunlun mountain tunnel Zhi-qiang Ji, Xue-yan Xu, Lin-lin Yu Study on the influence of artificial frozen soil layer to the temperature field and displacement field of the frozen wall Theme 5-2: Mapping: Land surface processes (Location: No.1 Conference-room of Zhongxiaolou Building) Chairs: Xiaozhen Xiong Tingjun Zhang Modeled Changes in Active-Layer Depth over the Tibetan Plateau Oliver W. Frauenfeld, Tingjun Zhang The role of land surface processes and permafrost on temperature variability in the Tibetan Plateau Rui Jin, Xin Li, Tao Che Decision tree to classify the surface frozen/thaw using SSM/I brightness temperature Dmitry A. Streletskiy, Nikolay I. Shiklomanov, Anna E. Klene, and Frederick E. Nelson Air and ground surface temperature monitoring in Arctic Foothills of Alaska Galina Mazhitova, Dmitry Kaverin* Local-level processes associated with progressive permafrost thaw as exemplified by data from a CALM grid Y. Ma, Y. Wang, W. Ma, Z.Su, M.Menenti, Z. Hu, J. Wang, H.Ishikawa, T.Koike Progress on the Study of Land Surface Processes over the Tibetan Plateau Area Theme 2-2: Frost hazards: <strong>Permafrost</strong> chemistry (Location: Multifunctional-hall of VIP Building)
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SEE AUTHOR INDEX AND REVISED PROGRA
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G.М. Dolgih, Dolgih D.G., Okunev S
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Rev I. Gavriliev The thermal conduc
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Xiao-zu Xu,Bin-xiang Sun,Qi Liu,Shu
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Lopez CML, Katamura F, Argunov R, F
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Grebenets V., Kraev G. Nagornov D.
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V.A. Istratov, A. Kuchmin, A.D. Fro
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Mamoru Ishikawa Mountain permafrost
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ORGANIZING COMMITTEE Co-Chairs Acad
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CO-SPONSORS Chinese Academy of Scie
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curve of the accumulated displaceme
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zone of Tien Shan. Key words: Compl
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negotiations currently under way am
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distribution according to the seaso
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number of freeze-thaw cycles. With
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The Technique of Geoinformation Mod
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Monitoring Study on the Boundary Th
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The Calculation and Control Methods
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observations are presented. Key wor
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frost heave is one typical case of
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whose total water content and poros
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effectively and restrain subgrade d
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Peninsula, Pur and Tar interfluve,
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1-D Numerical Analysis to Predict a
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of the two simulation-analysis meth
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frozen soil. While compared with th
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The maximum vertical deformations a
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dangerous pollutants, including hea
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fact of the rising of artificial pe
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The Thermal Conductivity of Segrega
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discussed in view of geotechnical a
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Numerical modeLling of thawing rail
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experiment for obtaining those para
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lake and in purpose to protect surr
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The Concept of an Engineering-geocr
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Effect of seismic events on the sta
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Electrical Conductivity of Rocks in
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mechanics parameters both in frozen
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influence its temperature change pr
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Experimental and numerical simulati
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signifies that the diffusion action
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Experimental Study on the Influence
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does not spread the energy in the f
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and seismic response of infrastruct
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Cooling effect of crushed rock reve
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The analysis of the data concerning
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the extended duration of freezing p
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Distribution of Rock Glaciers in th
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Methods of Theoretical and Experime
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properties, and is able to move bot
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especially water flooding, could be
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mechanisms during the compression a
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inundations and catastrophic breako
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of quantity of neglected interactio
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Past and present salinization in na
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Temperature Regime of Atmosphere an
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disturbance: conflicting, critical
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Application of ERS InSAR for detect
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critical to melt-water irrigation i
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Features of hydrothermal conditions
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associated with the southwest summe
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Significance of Microtopography and
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Reconstruction of paleocryogenic st
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Dendroclimatic investigations of fo
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anthropogenic disturbance. Despite
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and +38°C in summer. Continuous pe
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asis for palaeolimnological reconst
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eneath a path (34 cm.) In the end o
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can lead to a global ecological cat
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Assessment of Frozen Soils Environm
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No Thawing of the Cold Permafrost H
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Cryospheric changes in the West Sib
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Response of Ice-rich Permafrost to
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About Role of Thermokarst in Global
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presence may be debated since there
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territories have natural and anthro
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will contribute to the resolution o
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Impact of Frozen Ground Change on S
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Antarctica. Key words: Cape Hallett
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The sensitivity of Tibetan Plateau
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infrapermafrost waters that are dis
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Keywords: cryosphere, anthropogenic
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Key words: Alaska, oil exploration,
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Possible Change of Runoff in the Up
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Theme 5. Monitoring, mapping and mo
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Mathematical model for quantitative
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heat transfer model with phase chan
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e.s.l.). In 2005 this mine was equi
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Surface- coupled 3-D Permafrost Mod
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• the territories where the perma
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associated soil surface temperature
Page 184 and 185: variations in different parts. Keyw
Page 186 and 187: disturbed landscapes, thaw subsiden
Page 188 and 189: ⎛ ⎜ 1 ⎛ ⎞ ⎜ ε σ = Eε e
Page 190 and 191: Mountain permafrost study in the Ru
Page 192 and 193: Permafrost Distribution and Thickne
Page 194 and 195: Permafrost Distribution and Thickne
Page 196 and 197: studies (Natsagdorj et al. 2000), t
Page 198 and 199: on the basis of determining tempera
Page 200 and 201: models were run using standardized
Page 202 and 203: organized into segments and contact
Page 204 and 205: depends on the microclimate of spec
Page 206 and 207: soundings, borehole temperature mea
Page 208 and 209: In high mountain regions, as well a
Page 210 and 211: ottom at a rate of 4 cm/year and ac
Page 212 and 213: Birch trees (Betula ermanii) are do
Page 214 and 215: Monitoring of the snow cover in the
Page 216 and 217: deterministic model combined with p
Page 218 and 219: We have the map of seasonally froze
Page 220 and 221: approximately with the -5°C mean a
Page 222 and 223: Theme 6. Others Developing an Onlin
Page 224 and 225: The FGDC identifies, archives, docu
Page 226 and 227: Final Revised Program (August 28, 2
Page 228 and 229: Professor Dr. Lin Zhao, CAREERI, CA
Page 230 and 231: Monday, Aug 7, 2006 Location: Ningw
Page 232 and 233: Bending properties monitored in ful
Page 236 and 237: Chairs: Bernhard Diekman, Ron Slett
Page 238 and 239: Theme 5-3: Mapping: Permafrost and
Page 240 and 241: Experimental research on thermal co
Page 242 and 243: A Preliminary Permafrost and Ground
Page 244 and 245: Bulley H----------94 Caffee M W ---
Page 246 and 247: Guo Jian-wen -------177 Guo Jian-We
Page 248 and 249: Kudryavtsev S -------53 Kulish E M
Page 250 and 251: Nefedieva Yu A ----------------87 N
Page 252 and 253: Stauch G -------89 Streletskaya I.
Page 254: Zhang Jian-min --------25 Zhang Jin
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Permafrost

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