Permafrost

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Nefedieva Yu A ----------------87 Nelson F E ------------165 Nikolaev A N -------------117 Nikolaev V A -----------107 Nikolai M ----------179 Ning Jian-guo -------176 Niu Fu-jun -------23 Noskov A I --------42 Oelke C ---------162 Ogorodov S A ------42 Ohata T ---------------151, 207 Okunev S N -------23 Oleynik E V ------------203 Olsenholler J -------------94, 106 Ostanin O -----------179 Osterkamp T E ----------------198 Otsuki Y --------------200 Paetzold F R -------------83 Paramonov V -----53 Parmuzin S Yu -----------87 Parsons M A ------------7 Parsons M A-----------212 Pavlov A V ----------160 Peng Wan-wei ----------20 Perlshtein G Z -------------160 Pestryakova L -----------122 Peterson R A ----49 Petrakova S Yu ----------86 Petrikey A L ------51 Phillips M -----------10 Pikulev V P -------44 Ping C L -----------83 Popova V V------------202 Popp S ----------122 Potapov S U-----------------59 Prick A --------82 Pustovoit G P -----48 Qi Ji-lin -----32. 78 Qin Da-he ------------130 Qiu Ming-guo ---38 Qiu Wen-ge -------27, 64 Qu Xiang-min ------------------68 Raetzo H ---------105
Rapp A D---------------118 Regmi D --------85 Rist A --------------------10 Rivkin F M ----------21 Roman L T ------------96 Roman W ----43 Romanovskii N N ----------6 Romanovsky V E ----------140, 188 Rusanova CV -------------84 Saito K ----------180 Samsonova V V ----------203 Sano O -------56 Sawada Y ------113, 148, 171, 200 Seppot S -------------154 Sergueev D O ---------------164, 196 Seversky E V -----------12 Shamanova I------173 Shang Qing-sheng ---------177, 190 Shang Xiang-yu ----------------69 Sharkhuu N --------------151, 184, 186, 194 Shatz M M --------------182 Sheng Yu ---------65, 78, 178 Shesternev D M -----------4, 121 Shesternyov D M ------------196 Shiklomanov N I ------------165, 188 Shirokov R ----------------139 Shirota T --------113 Shmakin A B----------114, 202 Shpolyanskaya N -------------192 Shpuntov S --------------124 Shroder J ---------94, 106 Siegert C --------------120, 122 Simon W ------------56 Slagoda E ---------------115 Slater A G --------------118, 145 Sletten R S -----------131, 138 Smith A R ----36 Soboleva S V ------------59 Sone T ---------171, 200 Sørbel L ----------------171 Spektor V.B ----------107 Spektor V.V. --------------107
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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
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variations in different parts. Keyw
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disturbed landscapes, thaw subsiden
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⎛ ⎜ 1 ⎛ ⎞ ⎜ ε σ = Eε e
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Mountain permafrost study in the Ru
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Permafrost Distribution and Thickne
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Permafrost Distribution and Thickne
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studies (Natsagdorj et al. 2000), t
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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 234 and 235: Theme 1-3: Engineering: Frozen grou
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 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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