Process Study of Sorted Patterns on Arctic Soils

Patterned ground is ubiquitous in Arctic and alpine areas. To improve understanding of this phenomenon, we developed extensive field instrumentation that has been recording principal soil properties over the past four years. The resulting data constitute the first quantitative year-round records of...

Full description

Bibliographic Details
Main Authors: Hallet, Bernard, Waddington, Edwin
Other Authors: WASHINGTON UNIV SEATTLE QUATERNARY RESEARCH CENTER
Format: Text
Language:English
Published: 1991
Subjects:
Ice
Online Access:http://www.dtic.mil/docs/citations/ADA234089
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA234089
id ftdtic:ADA234089
record_format openpolar
spelling ftdtic:ADA234089 2023-05-15T14:51:08+02:00 Process Study of Sorted Patterns on Arctic Soils Hallet, Bernard Waddington, Edwin WASHINGTON UNIV SEATTLE QUATERNARY RESEARCH CENTER 1991-03-01 text/html http://www.dtic.mil/docs/citations/ADA234089 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA234089 en eng http://www.dtic.mil/docs/citations/ADA234089 Approved for public release; distribution is unlimited. DTIC AND NTIS Soil Mechanics Snow Ice and Permafrost Theoretical Mathematics *ARCTIC REGIONS BUOYANCY CIRCLES CIRCULATION DEFORMATION DETERMINANTS(MATHEMATICS) DYNAMICS FIELD EQUIPMENT FORCE(MECHANICS) FREEZING FROST HEAVE INSTRUMENTATION LAYERS LONG RANGE(TIME) MATHEMATICAL MODELS MOTION MOUNTAINS NUMERICAL ANALYSIS PATTERNS RECORDS SEASONAL VARIATIONS SOILS STOCHASTIC PROCESSES THAWING *FROZEN SOILS PATTERNED GROUND PERMAFROST SPITSBERGEN SOIL MODELS ARCTIC OCEAN ISLANDS SELF ORGANIZING SYSTEMS LPN-ARO-P-24376-GS Text 1991 ftdtic 2016-02-24T08:11:14Z Patterned ground is ubiquitous in Arctic and alpine areas. To improve understanding of this phenomenon, we developed extensive field instrumentation that has been recording principal soil properties over the past four years. The resulting data constitute the first quantitative year-round records of important seasonal process such as freezing, thawing, frost heaving, and settling in the active layer in a sorted circle area. The data provide unprecedented insight into the long-term dynamics of active sorted soil patterns. We have complemented our field research with analytical and numerical studies of sorted pattern formation. Deterministic and stochastic analyses of pattern development in the absence of significant soil deformation reveal strong textural instabilities; stones initially distributed at random through the soil tend to migrate quickly toward domains slightly richer in stones, which eventually leads to the distinct sorting characteristic of diverse forms of patterned ground. Our numerical model of sorted stripe formation successfully simulates stripe development, and sheds considerable light on formative process. We have also developed a novel model to assess buoyancy forces that arise in the thaw process, and may be responsible for the long-term circulatory soil motion documented in sorted circles in Spitsbergen. Text Arctic Arctic Ocean Ice permafrost Spitsbergen Defense Technical Information Center: DTIC Technical Reports database Arctic Arctic Ocean Stripe ENVELOPE(9.914,9.914,63.019,63.019)
institution Open Polar
collection Defense Technical Information Center: DTIC Technical Reports database
op_collection_id ftdtic
language English
topic Soil Mechanics
Snow
Ice and Permafrost
Theoretical Mathematics
*ARCTIC REGIONS
BUOYANCY
CIRCLES
CIRCULATION
DEFORMATION
DETERMINANTS(MATHEMATICS)
DYNAMICS
FIELD EQUIPMENT
FORCE(MECHANICS)
FREEZING
FROST HEAVE
INSTRUMENTATION
LAYERS
LONG RANGE(TIME)
MATHEMATICAL MODELS
MOTION
MOUNTAINS
NUMERICAL ANALYSIS
PATTERNS
RECORDS
SEASONAL VARIATIONS
SOILS
STOCHASTIC PROCESSES
THAWING
*FROZEN SOILS
PATTERNED GROUND
PERMAFROST
SPITSBERGEN
SOIL MODELS
ARCTIC OCEAN ISLANDS
SELF ORGANIZING SYSTEMS
LPN-ARO-P-24376-GS
spellingShingle Soil Mechanics
Snow
Ice and Permafrost
Theoretical Mathematics
*ARCTIC REGIONS
BUOYANCY
CIRCLES
CIRCULATION
DEFORMATION
DETERMINANTS(MATHEMATICS)
DYNAMICS
FIELD EQUIPMENT
FORCE(MECHANICS)
FREEZING
FROST HEAVE
INSTRUMENTATION
LAYERS
LONG RANGE(TIME)
MATHEMATICAL MODELS
MOTION
MOUNTAINS
NUMERICAL ANALYSIS
PATTERNS
RECORDS
SEASONAL VARIATIONS
SOILS
STOCHASTIC PROCESSES
THAWING
*FROZEN SOILS
PATTERNED GROUND
PERMAFROST
SPITSBERGEN
SOIL MODELS
ARCTIC OCEAN ISLANDS
SELF ORGANIZING SYSTEMS
LPN-ARO-P-24376-GS
Hallet, Bernard
Waddington, Edwin
Process Study of Sorted Patterns on Arctic Soils
topic_facet Soil Mechanics
Snow
Ice and Permafrost
Theoretical Mathematics
*ARCTIC REGIONS
BUOYANCY
CIRCLES
CIRCULATION
DEFORMATION
DETERMINANTS(MATHEMATICS)
DYNAMICS
FIELD EQUIPMENT
FORCE(MECHANICS)
FREEZING
FROST HEAVE
INSTRUMENTATION
LAYERS
LONG RANGE(TIME)
MATHEMATICAL MODELS
MOTION
MOUNTAINS
NUMERICAL ANALYSIS
PATTERNS
RECORDS
SEASONAL VARIATIONS
SOILS
STOCHASTIC PROCESSES
THAWING
*FROZEN SOILS
PATTERNED GROUND
PERMAFROST
SPITSBERGEN
SOIL MODELS
ARCTIC OCEAN ISLANDS
SELF ORGANIZING SYSTEMS
LPN-ARO-P-24376-GS
description Patterned ground is ubiquitous in Arctic and alpine areas. To improve understanding of this phenomenon, we developed extensive field instrumentation that has been recording principal soil properties over the past four years. The resulting data constitute the first quantitative year-round records of important seasonal process such as freezing, thawing, frost heaving, and settling in the active layer in a sorted circle area. The data provide unprecedented insight into the long-term dynamics of active sorted soil patterns. We have complemented our field research with analytical and numerical studies of sorted pattern formation. Deterministic and stochastic analyses of pattern development in the absence of significant soil deformation reveal strong textural instabilities; stones initially distributed at random through the soil tend to migrate quickly toward domains slightly richer in stones, which eventually leads to the distinct sorting characteristic of diverse forms of patterned ground. Our numerical model of sorted stripe formation successfully simulates stripe development, and sheds considerable light on formative process. We have also developed a novel model to assess buoyancy forces that arise in the thaw process, and may be responsible for the long-term circulatory soil motion documented in sorted circles in Spitsbergen.
author2 WASHINGTON UNIV SEATTLE QUATERNARY RESEARCH CENTER
format Text
author Hallet, Bernard
Waddington, Edwin
author_facet Hallet, Bernard
Waddington, Edwin
author_sort Hallet, Bernard
title Process Study of Sorted Patterns on Arctic Soils
title_short Process Study of Sorted Patterns on Arctic Soils
title_full Process Study of Sorted Patterns on Arctic Soils
title_fullStr Process Study of Sorted Patterns on Arctic Soils
title_full_unstemmed Process Study of Sorted Patterns on Arctic Soils
title_sort process study of sorted patterns on arctic soils
publishDate 1991
url http://www.dtic.mil/docs/citations/ADA234089
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA234089
long_lat ENVELOPE(9.914,9.914,63.019,63.019)
geographic Arctic
Arctic Ocean
Stripe
geographic_facet Arctic
Arctic Ocean
Stripe
genre Arctic
Arctic Ocean
Ice
permafrost
Spitsbergen
genre_facet Arctic
Arctic Ocean
Ice
permafrost
Spitsbergen
op_source DTIC AND NTIS
op_relation http://www.dtic.mil/docs/citations/ADA234089
op_rights Approved for public release; distribution is unlimited.
_version_ 1766322203190624256