Permafrost

More documents

Recommendations

Info

A Preliminary <strong>Permafrost</strong> and Ground Ice Map of Antarctica 17
Author Index (08-28-06) Abramenko O N -----------101 Akagawa S ---53, 54 Aksenov V I -----------11 Alekseev V R -----------------4 Alekseeva O I ----------------4 Aleshire L ---------99 Allard M --------------125 Amisimov O A ------------188 Anarmaa Sh ------------184, 186. 194 Andreev A A -----------122 Antonov-Drouginin V P ---------------156 Argunov R. ----------99 Armstrong R ----------170 Atsuoka N -------------159 Bai Guo-quan ------27 Bakalin V A ------------200 Balagansky A P ------------58 Baldunova K ------34 Balks M R ------------------146 Ballagh L ---------213 Barnet C ----------204 Barry R G --------------7 Basisty V A----------------62, 153 Basylev V --------------120 Battogtokh D -------------56, 151, 163, 206 Bayasan R M ---------48 Belova N G -----42 Bezkorovainaya I N --------91 Bie Xiao-yong -------27, 33 Bin Hui ------55 Bing Hui ------43 Bishop M --------94, 106 Bochkov M. -----------124 Bockheim J G-----------175 Boelhouwers J---------175 Bogatyrev L G ------------95 Bosikov N -----------116 Brewer M C --------------131 Brouchkov A -----------161 Brown J ------------------------1 Bulley H ---------106
Page 2 and 3:
SEE AUTHOR INDEX AND REVISED PROGRA
Page 4 and 5:
G.М. Dolgih, Dolgih D.G., Okunev S
Page 6 and 7:
Rev I. Gavriliev The thermal conduc
Page 8 and 9:
Xiao-zu Xu,Bin-xiang Sun,Qi Liu,Shu
Page 10 and 11:
Lopez CML, Katamura F, Argunov R, F
Page 12 and 13:
Grebenets V., Kraev G. Nagornov D.
Page 14 and 15:
V.A. Istratov, A. Kuchmin, A.D. Fro
Page 16 and 17:
Mamoru Ishikawa Mountain permafrost
Page 18 and 19:
ORGANIZING COMMITTEE Co-Chairs Acad
Page 20 and 21:
CO-SPONSORS Chinese Academy of Scie
Page 22 and 23:
curve of the accumulated displaceme
Page 24 and 25:
zone of Tien Shan. Key words: Compl
Page 26 and 27:
negotiations currently under way am
Page 28 and 29:
distribution according to the seaso
Page 30 and 31:
number of freeze-thaw cycles. With
Page 32 and 33:
The Technique of Geoinformation Mod
Page 34 and 35:
Monitoring Study on the Boundary Th
Page 36 and 37:
The Calculation and Control Methods
Page 38 and 39:
observations are presented. Key wor
Page 40 and 41:
frost heave is one typical case of
Page 42 and 43:
whose total water content and poros
Page 44 and 45:
effectively and restrain subgrade d
Page 46 and 47:
Peninsula, Pur and Tar interfluve,
Page 48 and 49:
1-D Numerical Analysis to Predict a
Page 50 and 51:
of the two simulation-analysis meth
Page 52 and 53:
frozen soil. While compared with th
Page 54 and 55:
The maximum vertical deformations a
Page 56 and 57:
dangerous pollutants, including hea
Page 58 and 59:
fact of the rising of artificial pe
Page 60 and 61:
The Thermal Conductivity of Segrega
Page 62 and 63:
discussed in view of geotechnical a
Page 64 and 65:
Numerical modeLling of thawing rail
Page 66 and 67:
experiment for obtaining those para
Page 68 and 69:
lake and in purpose to protect surr
Page 70 and 71:
The Concept of an Engineering-geocr
Page 72 and 73:
Effect of seismic events on the sta
Page 74 and 75:
Electrical Conductivity of Rocks in
Page 76 and 77:
mechanics parameters both in frozen
Page 78 and 79:
influence its temperature change pr
Page 80 and 81:
Experimental and numerical simulati
Page 82 and 83:
signifies that the diffusion action
Page 84 and 85:
Experimental Study on the Influence
Page 86 and 87:
does not spread the energy in the f
Page 88 and 89:
and seismic response of infrastruct
Page 90 and 91:
Cooling effect of crushed rock reve
Page 92 and 93:
The analysis of the data concerning
Page 94 and 95:
the extended duration of freezing p
Page 96 and 97:
Distribution of Rock Glaciers in th
Page 98 and 99:
Methods of Theoretical and Experime
Page 100 and 101:
properties, and is able to move bot
Page 102 and 103:
especially water flooding, could be
Page 104 and 105:
mechanisms during the compression a
Page 106 and 107:
inundations and catastrophic breako
Page 108 and 109:
of quantity of neglected interactio
Page 110 and 111:
Past and present salinization in na
Page 112 and 113:
Temperature Regime of Atmosphere an
Page 114 and 115:
disturbance: conflicting, critical
Page 116 and 117:
Application of ERS InSAR for detect
Page 118 and 119:
critical to melt-water irrigation i
Page 120 and 121:
Features of hydrothermal conditions
Page 122 and 123:
associated with the southwest summe
Page 124 and 125:
Significance of Microtopography and
Page 126 and 127:
Reconstruction of paleocryogenic st
Page 128 and 129:
Dendroclimatic investigations of fo
Page 130 and 131:
anthropogenic disturbance. Despite
Page 132 and 133:
and +38°C in summer. Continuous pe
Page 134 and 135:
asis for palaeolimnological reconst
Page 136 and 137:
eneath a path (34 cm.) In the end o
Page 138 and 139:
can lead to a global ecological cat
Page 140 and 141:
Assessment of Frozen Soils Environm
Page 142 and 143:
No Thawing of the Cold Permafrost H
Page 144 and 145:
Cryospheric changes in the West Sib
Page 146 and 147:
Response of Ice-rich Permafrost to
Page 148 and 149:
About Role of Thermokarst in Global
Page 150 and 151:
presence may be debated since there
Page 152 and 153:
territories have natural and anthro
Page 154 and 155:
will contribute to the resolution o
Page 156 and 157:
Impact of Frozen Ground Change on S
Page 158 and 159:
Antarctica. Key words: Cape Hallett
Page 160 and 161:
The sensitivity of Tibetan Plateau
Page 162 and 163:
infrapermafrost waters that are dis
Page 164 and 165:
Keywords: cryosphere, anthropogenic
Page 166 and 167:
Key words: Alaska, oil exploration,
Page 168 and 169:
Possible Change of Runoff in the Up
Page 170 and 171:
Theme 5. Monitoring, mapping and mo
Page 172 and 173:
Mathematical model for quantitative
Page 174 and 175:
heat transfer model with phase chan
Page 176 and 177:
e.s.l.). In 2005 this mine was equi
Page 178 and 179:
Surface- coupled 3-D Permafrost Mod
Page 180 and 181:
• the territories where the perma
Page 182 and 183:
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 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 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
show all

Permafrost

Create successful ePaper yourself

Delete template?

Save as template?