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Buchumschlag
Gespeichert in:
Bibliographische Detailangaben
Beteiligte Personen: Harris, Stuart A. 1931- (VerfasserIn), Brouchkov, Anatoli 1957- (VerfasserIn), Cheng, Guodong 1943- (VerfasserIn)
Format: Buch
Sprache:Englisch
Veröffentlicht: Boca Raton, Fla CRC Press, Taylor & Francis Group [2018]
Schlagwörter:
Frozen ground
Dauerfrostboden
Frostboden
Periglazial
Links:http://bvbr.bib-bvb.de:8991/F?func=service&doc_library=BVB01&local_base=BVB01&doc_number=029858943&sequence=000001&line_number=0001&func_code=DB_RECORDS&service_type=MEDIA
http://bvbr.bib-bvb.de:8991/F?func=service&doc_library=BVB01&local_base=BVB01&doc_number=029858943&sequence=000002&line_number=0002&func_code=DB_RECORDS&service_type=MEDIA
Umfang:xliii, 765 Seiten Illustrationen, Diagramme, Karten (farbig)
ISBN:9781138054165
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Datensatz im Suchindex

_version_ 1819270907631239168
adam_text Table of contents Preface xv About the authors xvii Acknowledgements xix Dedication xxi List of figures xxiii List of tables xxxix List of symbols xli Part I Introduction and characteristics of permafrost I I Definition and description 3 1.1 Introduction 3 1.2 Additional terms originating in Russia 7 1.3 History of permafrost research 8 1.4 Measurement of ground temperature 9 1.5 Conduction, convection and advection 9 1.6 Thermal regimes in regions based on heat conduction 10 1.7 Continentality index 15 1.8 Moisture movement in the active layer during freezing and thawing 16 1.9 Moisture conditions in permafrost ground 18 1.10 Results of freezing moisture 20 1.11 Strength of ice 22 1.12 Cryosols, gelisols, and leptosols 22 1.13 Fragipans 22 1.14 Salinity in permafrost regions 24 1.15 Organic matter 28 1.16 Micro-organisms in permafrost 3 0 1.16.1 Antarctic permafrost 31 1.16.2 High-latitude permafrost 31 1.16.3 High altitude permafrost in China 32 1.16.4 Phenotypic traits 32 1.16.5 Relation to climate change on the Tibetan plateau 34 1.17 Gas and gas hydrates 35 vi Table of contents 1.18 Thermokarst areas 3 7 1.19 Offshore permafrost 3 8 2 Cryogenic processes where temperatures dip below 0°C 43 2.1 Introduction 43 2.2 The nature of ice and water 43 2.3 Effects of oil pollution on freezing 50 2.4 Freezing and thawing of the active layer in permafrost in equilibrium with a stable climate 51 2.5 Relation of clay mineralogy to the average position of the permafrost table 53 2.6 Ground temperature envelopes in profiles affected by changes in mean annual ground surface temperature (MASGT) 54 2.7 Needle ice 58 2.8 Frost heaving 59 2.9 Densification and thaw settlement 60 2.10 Cryostratigraphy, cryostructures, cryotextures and cryofacies 60 2.11 Ground cracking 61 2.12 Dilation cracking 63 2.13 Frost susceptibility 64 2.14 Cryoturbation, gravity processes and injection structures 65 2.14.1 Cryoturbation 65 2.14.2 Upward injection of sediments from below 69 2.14.3 Load-casting 69 2.15 Upheaving of objects 71 2.16 Upturning of objects 72 2.17 Sorting 73 2.18 Weathering and frost comminution 74 2.19 Karst in areas with permafrost 78 2.20 Seawater density and salinity 80 3 Factors affecting permafrost distribution 85 3.1 Introduction 85 3.2 Climatic factors 85 3.2.1 Heat balance on the surface of the Earth and its effect on the climate 85 3.2.2 Relationship between air and ground temperatures 91 3.2.3 Thermal offset 93 3.2.4 Relation to air masses 96 3.2.5 Precipitation 99 3.2.6 Latitude and longitude 103 3.2.7 Topography and altitude 105 3.2.8 Cold air drainage 107 3.2.9 Buffering of temperatures against change in mountain ranges 108 3.3 Terrain factors 109 3.3.1 Vegetation 109 Table of contents vii 3.3.2 Hydrology 111 3.3.3 Lakes and water bodies 115 3.3.4 Nature of the soil and rock 117 3.3.5 Fire 118 3.3.6 Glaciers 119 3.3.7 The effects of Man 122 4 Permafrost distribution 123 4.1 Introduction 123 4.2 Zonation of permafrost 126 4.3 Permafrost mapping 127 4.4 Examples of mapping units used 129 4.5 Modeling permafrost distribution 130 4.6 Advances in geophysical methods 131 4.7 Causes of variability reducing the reliability of small-scale maps 131 4.8 Maps of permafrost-related properties based on field observations 135 4.8.1 Permafrost thickness 135 4.8.2 Maps of ice content 135 4.8.3 Water resources locked up in perennially frozen ground 136 4.8.4 Total carbon content 139 4.9 Use of remote sensing and airborne platforms in monitoring environmental conditions and disturbances 140 4.10 Sensitivity to climate change: Hazard zonation 140 4.11 Classification of permafrost stability based on mean annual ground temperature 142 Partii Permafrost iandforms 145 II. 1 Introduction 145 5 Frost cracking, ice-wedges, sand, loess and rock tessellons 149 5.1 Introduction 149 5.2 Primary and secondary wedges 153 5.2.1 Primary wedges 153 5.2.1.1 Ice-wedges 153 5.2.1.2 Sand tessellons 167 5.2.1.3 Loess tessellons 170 5.2.1.4 Rock tessellons 170 5.2.2 Secondary wedges 170 5.2.2.1 Ice-wedge casts 171 5.2.2.2 Soil wedges 173 6 Massive ground ice in lowlands 179 6.1 Introduction 179 6.2 Distribution of massive icy beds in surface sediments 181 6.3 Sources of the sediments 182 6.4 Deglaciation of the Laurentide ice sheet 183 6.5 Methods used to determine the origin of the massive icy beds 186 viii Table of contents 6.6 Massive icy beds interpreted as being formed by cryosuction 186 6.7 Massive icy beds that may represent stagnant glacial ice 187 6.8 Other origins of massive icy beds 189 6.9 Ice complexes including yedoma deposits 189 6.10 Conditions for growth of thick ice-wedges 190 6.11 The mechanical condition of the growth of ice-wedges and its connection to the properties of the surrounding sediments 192 6.12 Buoyancy of ice-wedges 193 6.13 Summary of the ideas explaining yedoma evolution 195 6.14 Aufeis 195 6.15 Perennial ice caves 198 6.16 Types of ice found in perennial ice caves 200 6.17 Processes involved in the formation of perennial ice caves 202 6.18 Cycles of perennial cave evolution 204 6.18.1 Perennial ice caves in deep hollows 204 6.18.2 Sloping caves with two entrances 205 6.18.3 Perennial ice caves with only one main entrance but air entering through cracks and joints in the bedrock walls 206 6.18.4 Perennial ice caves with only one main entrance and no other sources of cooling 206 6.19 Ice caves in subtropical climates 207 6.20 Massive blocks of ice in bedrock or soil 210 7 Permafrost mounds 213 7.1 Introduction 213 7.2 Mounds over 2.5 m diameter 214 7.2.1 Mounds formed predominantly of injection ice 215 7.2.1.1 Pingo mounds 215 7.2.1.2 Hydrostatic or closed system pingos 216 7.2.1.3 Hydraulic or open system pingos 218 7.2.1.4 Pingo plateaus 222 7.2.1.5 Seasonal frost mounds 225 7.2.1.6 Icing blisters 226 7.2.1.7 Perennial mounds of uncertain origin 228 7.2.1.8 Similar mounds that can be confused with injection phenomena 228 7.2.2 Mounds formed dominantly by cryosuction 229 7.2.2.1 Paisas 230 7.2.2.1.1 Paisas in maritime climates 231 7.2.2.1.2 Paisas in cold, continental climates 234 7.2.2.1.3 Lithalsas 239 7.2.2.1.4 Palsa/Lithalsa look-alikes 243 7.2.3 Mounds formed by the accumulation of ice in the thawing fringe: Peat plateaus 244 7.3 Cryogenic mounds less than 2.5 m in diameter 249 7.3.1 Oscillating hummocks 252 Table of contents be 7.3.2 Thufurs 256 7.3.3 Silt-cycling hummocks 260 7.3.4 Niveo-aeolian hummocks 261 7.3.5 Similar-looking mounds of uncertain origin 263 7.3.6 String bogs 264 7.3.7 Pounus 265 8 Mass wasting of fine-grained materials in cold climates 267 8.1 Introduction 267 8.2 Classification of mass wasting 267 8.3 Slow flows 269 8.3.1 Cryogenic creep 269 8.3.1.1 Needle ice creep 270 8.3.1.2 Frost heave and frost creep 272 8.3.1.3 Gelifluction 274 8.3.1.4 Other creep-type contributions to downslope movement of soil 276 8.3.2 Landforms produced by cryogenic slow flows in humid areas 279 8.3.3 Landforms developed by cryogenic flows in more arid regions 284 8.4 Cryogenic fast flows 287 8.4.1 Cryogenic debris flows 287 8.4.2 Cryogenic slides and slumps 296 8.4.3 Cryogenic composite slope failures 297 8.4.3.1 Active-layer detachment slides 298 8.4.3.2 Retrogressive thaw failures 300 8.4.3.3 Snow avalanches and slushflows 304 8.4.3.3.1 Snow avalanches 306 8.4.3.3.2 Slush avalanches 310 8.5 Relative effect in moving debris downslope in the mountains 313 9 Landforms consisting of blocky materials in cold climates 315 9.1 Introduction 315 9.2 Source of the blocks 315 9.3 Influence of rock type 317 9.4 Weathering products 318 9.5 Biogenic weathering 319 9.6 Fate of the soluble salts produced by chemical and biogenic weathering 320 9.7 Rate of cliff retreat 321 9.8 Landforms resulting from the accumulation of predominantly blocky materials in cryogenic climates 322 9.8.1 Cryogenic block fields 322 9.8.1.1 Measurement of rates of release of blocks on slopes 326 x Table of contents 9.8.2 Cryogenic block slopes and fans 326 9.8.3 Classification of cryogenic talus slopes 329 9.8.3.1 Coarse blocky talus slopes 331 9.8.4 Protection of infrastructure from falling rock 332 9.9 Talus containing significant amounts of finer material 333 9.9.1 Rock glaciers 334 9.9.1.1 Sedimentary composition and structure of active rock glaciers 337 9.9.1.2 Origin of the ice in active rock glaciers 338 9.9.1.3 Relationship to vegetation 339 9.9.2 Movement of active rock glaciers 340 9.9.2.1 Horizontal movement 340 9.9.2.2 Movement of the front 341 9.9.3 Distribution of active rock glaciers 345 9.9.4 Inactive and fossil rock glaciers 347 9.9.5 Streams flowing from under rock glaciers 348 9.10 Cryogenic block streams 349 9.10.1 Characteristics 351 9.10.2 Classification 354 9.10.2.1 Siberian active dynamic block streams ֊֊֊ kurums 355 9.10.2.2 The Tibetan type of active dynamic block streams 357 9.10.2.3 Active cryogenic lag block streams 359 9.10.2.4 Inactive, relict block streams 359 9.11 Surface appearance of bločky landforms 365 Cryogenic patterned ground 367 10.1 Introduction 367 10.2 Forms of cryogenic patterned ground 368 10.3 Factors affecting the development of cryogenic patterned ground 369 10.4 Macroforms of cryogenic patterned ground 373 10.4.1 Cryogenic nonsorted circles 374 10.4.1.1 Cryogenic mudboils 375 10.4.1.1.1 Arctic mudboils 376 10.4.1.1.2 Subarctic mudboils 379 10.4.1.2 Xeric nonsorted circles 381 10.4.1.3 Nonsorted circles in maritime climates 384 10.4.1.4 Frost boils 385 10.4.1.5 Plug circles 386 10.5 Cryogenic sorted patterned ground 387 10.5.1 Cryogenic sorted circles 388 10.5.2 Cryogenic sorted polygons, and nets 391 10.5.2.1 Sorted stripes 391 10.5.2.2 Stone pits 392 Table of contents xi 10.6 Identification of active versus inactive forms of macro-sorted patterns 393 10.7 Microforms of cryogenic patterned ground 394 II Thermokarst and thermal erosion 397 11.1 Introduction 397 11.2 Causes of thermokarst 400 11.3 Cavity development in permafrost 402 11.4 Effect of thermokarst on soil 403 11.5 Thermokarst landforms 405 11.5.1 Thermokarst pits 406 11.5.2 Thermokarst mounds 407 11.5.3 Pingo, paisa and lithalsa scars 409 11.5.4 Beaded streams 411 11.5.5 Thermokarst lakes 412 11.5.6 Oriented lakes 415 11.5.7 Alases 417 11.5.8 Cycle of alas formation 418 11.6 Thermokarst and thermal erosion along river banks 424 11.6.1 Ice jams 425 11.7 Thermal erosion and thermokarst processes along sea coasts 429 11.7.1 Effects of seasonal sea ice 430 11.7.2 Effects of geology 433 11.7.3 Topographic effects 433 11.7.4 Sea conditions 434 11.7.5 Deposition of sediments 435 11.8 Processes involved in the erosion of ice-rich arctic coastal sediments 435 11.9 Importance of coastal erosion of sediments containing permafrost 439 Part III Use of permafrost areas 441 III.1 Introduction 441 12 The mechanics of frozen soils 445 12.1 Introduction 445 12.2 Strains and stresses in the freezing and thawing of soils resulting in frost heaving 445 12.3 Rheological processes 456 12.4 Frost susceptibility 460 13 Foundations in permafrost regions: building stability 465 13.1 Introduction 465 13.2 The effect of construction on permafrost stability 468 13.3 Choice of method of construction 470 13.4 Building materials 471 xii Table of contents 13.5 Timing of construction 472 13.6 Types of foundations 473 13.6.1 Pads 473 13.6.2 Slabs and rafts 474 13.6.3 Sills 475 13.6.4 Spread footings 476 13.6.5 Piles 477 13.6.6 Thermosiphons 482 13.6.7 Artificial refrigeration 489 13.6.8 Ventilation ducts 490 13.6.9 Angle of slope of the embankment sides 492 13.6.10 Snow removal 492 13.6.11 The diode effect: use of rocks 493 13.6.12 Shading 496 13.6.13 Insulation 497 13.6.14 Use of geotextiles and waterproof plastics 498 Roads, railways and airfields 501 14.1 Introduction 501 14.2 The problems 501 14.3 Types of roads 502 14.4 Experimental embankments 504 14.5 Winter roads 505 14.6 Environmental effects of winter roads 507 14.7 Embankment heights 508 14.8 Unpaved embankments 509 14.9 Main problems with embankment stability 518 14.10 Concrete versus ballast railway tracks 524 14.11 Paving of road and airfield runways 527 14.12 Use of white paint 529 14.13 Bridges 530 14.14 Icings 532 14.15 Cut slopes 538 14.16 Airfield construction 538 Oil and gas industry 543 15.1 Introduction 543 15.2 Oil and gas exploration 543 15.3 Drilling rigs 546 15.4 Production and keeper wells 547 15.5 Sump problems 549 15.6 Pipelines 550 15.6.1 Buried mode 551 15.6.2 Pipelines on piles 559 15.6,2,1 Design parameters 563 Table of contents xiii 15.6.2.2 Construction methods 564 15.6.2.3 Failures in the buried section 564 15.7 Monitoring 566 15.8 Compressor stations 566 15.9 Pipeline crossings 569 15.10 Effects of heat advection from producing wells 571 15.11 Gas hydrates in permafrost ice 571 16 Mining in permafrost areas 577 16.1 Introduction 577 16.2 Placer mining 577 16.3 Open cast/pit mining 580 16.3.1 Exploration 582 16.3.2 Extraction of the ore 582 16.4 Underground mining 587 16.4.1 Transport of the ore around the mine 589 16.4.2 Support facilities 590 16.5 Waste materials and tailings ponds 590 16.5.1 Toxic wastes 592 17 Provision of utilities 597 17.1 Introduction 597 17.2 Water supply 598 17.2.1 Sources of water 598 17.2.2 Dams to impound water on permafrost 600 17.2.3 Municipal water storage 602 17.2.4 Water treatment 602 17.2.5 Water requirements 603 17.2.6 Transportation methods for water and waste water 604 17.3 Waste disposal 607 17.3.1 Wastewater treatment and disposal 607 17.3.1.1 Undiluted wastes 608 17.3.1.2 Moderately diluted wastes 608 17.3.1.3 Conventional strength wastewater 609 17.3.1.4 Very dilute waste water 609 17.3.2 Solid waste disposal 610 17.4 Electric transmission lines 610 17.4.1 Foundation problems for transmission lines built on permafrost 611 17.4.2 Transmission tower foundation types 614 18 Agriculture and forestry 617 18.1 Introduction 617 18.2 Zonation of natural vegetation across Siberia 621 18.3 Zonation of natural vegetation in North America 623 xiv Table of contents 18.4 Southern and Eastern Kazakhstan, Mongolia and the Qinghai-Tibet Plateau 625 18.5 The Eichfeld zones 626 18.5.1 Eichfeld zone I 627 18.5.2 Eichfeld zone II 627 18.5.3 Eichfeld zone III 629 18.5.3.1 The northern Taiga 629 18.6 Asian steppe grasslands and deserts 630 18.7 The development of modern agriculture in permafrost areas 632 18.8 Forestry 633 18.9 Potential effects of climate changes 634 References 637 Subject index 755 This book provides a general survey of Geocryology, which is the study of frozen ground called permafrost, Frozen ground is the product of cold climates as well as a variety of environmental factors. Its major characteristic is the accumulation of large quantities of ice which may exceed 90% by volume. Soil water changing to ice results in ground heaving, white thawing of this ice produces ground subsidence often accompanied by soil flowage. Permafrost is very susceptible to changes in weather and climate as well as to changes in the microenvironment. Cold weather produces contraction of the ground, resulting in cracking of the soil as well as breakup of concrete, rock, etc. Thus permafrost regions have unique landforms and processes not found in warmer lands. The book is divided into three parts. Part t provides an introduction to the characteristics of permafrost. Four chapters deal with its definition and characteristics, the unique processes operating there, the factors affecting it, and its general distribution. Part 2 consists of seven chapters describing the characteristic landforms unique to these areas and the processes involved in their formation. Part 3 discusses the special problems encountered by engineers in construction projects including settlements, roads and railways, the oil and gas industry, mining, and the agricultural and forest industries. The three authors represent three countries and three language groups, and together have over 120 years of experience of working in permafrost areas throughout the world. The book contains over 300 illustrations and photographs, and includes an extensive bibliography in order to introduce the interested reader to the large current literature.
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Brouchkov, Anatoli 1957-
Cheng, Guodong 1943-
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id DE-604.BV044458187
illustrated Illustrated
indexdate 2024-12-20T18:03:40Z
institution BVB
isbn 9781138054165
language English
lccn 2017024668
oai_aleph_id oai:aleph.bib-bvb.de:BVB01-029858943
oclc_num 1011609245
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physical xliii, 765 Seiten Illustrationen, Diagramme, Karten (farbig)
publishDate 2018
publishDateSearch 2018
publishDateSort 2018
publisher CRC Press, Taylor & Francis Group
record_format marc
spellingShingle Harris, Stuart A. 1931-
Brouchkov, Anatoli 1957-
Cheng, Guodong 1943-
Geocryology characteristics and use of frozen ground and permafrost landforms
Frozen ground
Dauerfrostboden (DE-588)4129794-5 gnd
Frostboden (DE-588)4155496-6 gnd
Periglazial (DE-588)4173765-9 gnd
subject_GND (DE-588)4129794-5
(DE-588)4155496-6
(DE-588)4173765-9
title Geocryology characteristics and use of frozen ground and permafrost landforms
title_auth Geocryology characteristics and use of frozen ground and permafrost landforms
title_exact_search Geocryology characteristics and use of frozen ground and permafrost landforms
title_full Geocryology characteristics and use of frozen ground and permafrost landforms Stuart A. Harris (Department of Geography, University of Calgary, Calgary Alberta, Canada), Anatoli Brouchkov (Geocryology Department, Faculty of Geology, Moscow State University, Moscow, Russia), Cheng Guodong (Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou, China)
title_fullStr Geocryology characteristics and use of frozen ground and permafrost landforms Stuart A. Harris (Department of Geography, University of Calgary, Calgary Alberta, Canada), Anatoli Brouchkov (Geocryology Department, Faculty of Geology, Moscow State University, Moscow, Russia), Cheng Guodong (Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou, China)
title_full_unstemmed Geocryology characteristics and use of frozen ground and permafrost landforms Stuart A. Harris (Department of Geography, University of Calgary, Calgary Alberta, Canada), Anatoli Brouchkov (Geocryology Department, Faculty of Geology, Moscow State University, Moscow, Russia), Cheng Guodong (Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou, China)
title_short Geocryology
title_sort geocryology characteristics and use of frozen ground and permafrost landforms
title_sub characteristics and use of frozen ground and permafrost landforms
topic Frozen ground
Dauerfrostboden (DE-588)4129794-5 gnd
Frostboden (DE-588)4155496-6 gnd
Periglazial (DE-588)4173765-9 gnd
topic_facet Frozen ground
Dauerfrostboden
Frostboden
Periglazial
url http://bvbr.bib-bvb.de:8991/F?func=service&doc_library=BVB01&local_base=BVB01&doc_number=029858943&sequence=000001&line_number=0001&func_code=DB_RECORDS&service_type=MEDIA
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work_keys_str_mv AT harrisstuarta geocryologycharacteristicsanduseoffrozengroundandpermafrostlandforms
AT brouchkovanatoli geocryologycharacteristicsanduseoffrozengroundandpermafrostlandforms
AT chengguodong geocryologycharacteristicsanduseoffrozengroundandpermafrostlandforms
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