Frozen Ground

April Courtney

Fall 2011

ES 331 Ice Age Environments

Dr. J.S. Aber, Instructor


Agassiz Glacier, Montana

Table of Contents
Introduction Frost Heave Types of Ice
Patterned Ground Conclusion Short Video
References


Introduction

Frozen ground occurs when the water contained within the pore spaces of soil, pebbles, and rocks are all frozen. Depending on types of organic material present, mineral content of soil, and the location, freezing will occur perennially at surface temperatures of 0 C (32 F). A futher understanding of soils leads to a description...."as extremely complex integrative systems that function as a boundry layer at the surface of the ice-and-water free portions of the continent", Pavich 2004. Processes at work to create or maintain frozen ground situations are multiple and varied. Difference in soil types allows frost action to occur more rapidly, due to allowable moisture content of the soil - not precipitation.

There are four identified occurances of ice within frozen ground features: pore ice, needle ice, ice wedges and segregated ice. These ice forms are the vehicles of frozen ground landforms such as pingos, palsas, rock glaciers, hummocks, thufur and thermokarst lakes. For the purpose of this report, two additional frozen landform processes - frost heave and patterned ground will be discussed. Slope effects on hillsides and mountains are paramount in frozen ground situations. Lastly, climate affects frozen ground. Understanding the changing climate by observation and interpretation of frozen ground may lead to important hydrogeologic implications in relation to future ground water availability. Relating frozen ground soil orders to climates on a regional or local scale can provide the additional information needed for interpreting ground temperature records, as a climate change indicator.


Types of Ice

Pore Ice


Image courtesy of
Stevens Water Monitoring Systems, Inc

Soil moisture occurs when pore spaces within soil particles hold water.
The frozen water is otherwise known as pore ice.

Needle Ice


Photo courtesy J. Brew, of the National Snow and Ice Data Center
University of Colorado, Boulder.

Found on the ground, needle ice is composed of thin ice crystals. The crystals grow upwards from as little as a few centimeters underground (NSIDC 2011). To form needle ice, or ribbon ice, is the presence of flowing ground water that contacts freezing air is required. Typically it is formed over night when air temperatures drop and on generously sloping ground where there is water movement. Sizes of ice needles can range from one centimeter to 40 centimeters in length, under ideal conditions. As the needles grow, the surface becomes more available to wind and water erosion.


Ice Wedge


(Pidwirny and Jones 1999)

Freeze and thawing of periglacial, arctic ground over many hundreds of years forms ice wedging processes that result in drastic landscape changes. Permafrost soils are located just below the active layer of top soil. The process begins with cold winter temperatures causing the active layer of soil to shrink above the permafrost, thus causing cracks to form. During the warmer days of spring, water seeps into the cracks, is chilled by the frozen permafrost layer and expands to form wedges of ice in the soil. When summer temperatures arrive, the topmost layers of the ice wedges melt. The cycle continues with the continuing change of seasons, with each winter the cracks form in the already compromised soil; enlarging the ice wedges every year. As shown in the diagram above, eventually this ice wedges become large enough to form dramatic landscapes. A complete animation of the process can be viewed at the Arctic National Wildlife Refuge webpage.


Segregated Ice


Image courtesy of USACE Permafrost Tunnel Research Facility.

Segregated ice forms each winter in the active layer of soil and builds ontop of permafrost. These bodies of pure ice are seen as lenses, veins, or wedges. These ice bodies are formed from the mutual attraction of liquid water and vapor to the lower cold vapor pressure in the freezing plane of the soil. Soil permeability and porosity provide optimal storage and diffusion of the water throughout the soil body. As shown in the diagram above, the ice bodies build upon each other and during the cyclic seasons, soil becomes displaced by upward movement, frost heave - or is assimiliated into the lower permafrost.

Return to the beginning.


Frost Heave

Diagram courtesy of North Dakota Geological Survey
(Click for NDGS PDF on Frost Heave)

Frost heave is a physical weathering process, a form of frost action, occuring from freeze and thaw events. When ice is formed within soil, it can generate extreme force on its surroundings and cause frost heaving. The "heave" refers to upward movement of the ground surface in response to freeze / thaw processes. Frost heaving of the soil was once believed as a result only from the expansion of water on freezing surfaces. The concept of frost heave includes growing ice crystals underground drawing water from the surrounding soil that develops into ice lenses (Penner 1962). The diagram provided above, shows the concept in relation to an asphalt ground structure (road) and the formation of ice lenses breaking apart the asphalt. The large arrow on the diagram indicates the pressure upwards of the ice lenses on the surface. The dynamics of freezing form an intricate process, however, only three things are required to produce a frost heave incident: freezing temperatures, the "right" kind of soil and an abundant water supply (Manz 2011).

Frost heave effects: change in landscapes, damaged roads and unlevel building foundations.

Unconstrained frost heave mound. Yamal Peninsula, Siberia
Copyright Permafrost International, Inc. 2000

Ribbon road - Alaska June 2011
Image courtesy of Bill and Kevs Excellent Alaskan Adventure

Effects of frost heaving can damage house foundations as shown in diagram.
Copyright 1998 - 2012, The Old House Web

Return to the beginning.


Patterned Ground

,
Photo credit: U.S. Fish and Wildlife Service

The National Snow and Ice Data Center describes patterned ground as any ground surface that exhibits a discernible ordered, more-or-less symmetrical, morphological pattern of ground and, where present, vegetation. Types of patterned ground are varied and are dependent on organic material present, mineral content of soil, location and water/wind relationships. Patterned ground conditions are a naturally occuring phenomenon that produces stunning landforms often as a direct result of frost heave processes. The types of patterned ground formations can be organized into circles, polygons, nets, steps and stripes. Field studies conducted in northern Alaska have provided a classification of arctic soils and patterns; providing typical soil classification based on pattern types (Tedrow and Drew,1958). For further information regarding arctic soils and their classification: find the article here.

Patterned ground is described into two categories: sorted and non-sorted. This is true whether the ground pattern exhibits polygons, circles, nets or stripes. Sorted landforms will show a definitive ring or margin of stones/rocks. Non-sorted landforms will lack the stone margins and will exhibit some marginal vegetation .

Circles

Sizes of sorted or non-sorted circles may appear as small as 1.5 feet to over 10 feet in diameter (USACE 2012). The circles are commonly dome shaped with small polygonal cracks throughout when active. After periods of inactivity, vegetation will begin to grow within the circles. Typically, these are found on flat terrain. If the surface is on a steep slope, elongation will occur creating stripes.

Sorted circles: Sorted landforms will show a definitive ring or margin of stones/rocks.
Photographed in Kvadehukken, Svalbard.
Photo credit: Ina Timling, Geophysical Institute
University of Alaska Fairbanks

Non-sorted circles: Non-sorted landforms will lack the stone margins and will exhibit some marginal vegetation.
Photographed in Kvadehukken, Svalbard.
Photo credit: Ina Timling, Geophysical Institute
University of Alaska Fairbanks

Polygons

Polygons can be found on display as on a micro-scale of less than seven feet diameter or on a macro-scale of 50 to 100 feet diameters (USACE 2012). Polygon patterns of frozen ground will display the sorted or non-sorted features in both the micro and macro scales. Ice wedge polygons are honeycomb formations of ice formed under the surface and extend deep below the surface. They will display with cracks at the margins or with furrows, deppressions of vegetation. Polygons can be further classified into low-centered or high-centered, referring to depressions or mounds, respectively.

Low centered polygons featuring irregular ice wedge patterns.
Sagavanirktok river delta, Alaska.
Copyright 2012 Permafrost Laboratory.

Nets

Sorted and non-sorted nets are similar to polygons and circles..
Display will have vegetation intersperssed throughout "net-like" stones...appears hummocky.
Photo credit: Ronald Daanen, Geophysical Institute
University of Alaska Fairbanks

Steps

Steps are formed from parent landform features of circles, polygons and nets on mountain hillsides in periglacial climates.
The parent landform will appear to be sorted or non-sorted.
Glacier National Park, Montana.Gable Mountain, viewed from Lee Ridge.
USGS - Carrara July 25, 1984.

Stripes

Stripes display as vertical landforms down slopes/hillsides.
Like steps, the parent features will be non-sorted circles and polygons or sorted circles, polygons, and nets.
Dracoisen, Ny Friesland - Svalbard
Photo credit: Glaciers Online, M. Hambrey

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Conclusion

Processes at work to create frozen ground and subsequent land formations are varied yet simplistic in understanding. The actual mechanics of frozen ground movements however are complex. Contributions of available water to site specific soil types will produce dramaitcally different results as the mineralogical content of the soil varies. Take into account precipitation events that would provide additional thermal heat, the processes at work are phenomenal. The unlimited number of variables in frozen ground patterns are diverse and therefore an unpredictalce science, however, general conclusions can be made based on soil types. Identification of general soil types in an area displaying specfic ground pattern landforms therefore can be made. Understanding the processes of frozen ground formations can also lead to monitoring climate change effects by observing changes in the land features. Determining a base research site, or sites, for such observations are critical in determining climate change effects on mountain regions.


Short Video


Video produced and edited by April Courtney Dec 2011


References

  • Bellingham, BK. Method for Irrigation Scheduling Based on Soil Moisture Data Acquisition. Stevens Water Monitoring Systems PDF Download Link

  • Bennett, MR. and Glasser NF. 2009. Glacial Geology: Ice Sheets and Landforms. 2nd Edition. Wiley-Blackwell.

  • Bill and Kev's Excellent Alaska Adventure. Blog Entry June 10, 2011. Blog Entry Link

  • Hambrey, M. and Alean, J. 2004. Glaciers, 2nd Edition: New York, NY. Cambridge University Press. p191-199

  • Journal of Geocryology. 2010. Photo Gallery. Link

  • Manz, L. 2011Frost Heave GeoNews Newsletter . North Dakota Geological Survey (NDGS). Vol.38 No.24. pp18- July 2011. PDF Download Link

  • National Snow and Ice Data Center (NSIDC). All About Frozen Ground. University of Colorado, Boulder December 10, 2008 Link

  • Old House Web. Masonry Foundations and piers Accessed on 21 Jan 2012. Link

  • Pavich, M. and Chadwick, O. 2004 Soils and the Quaternanary climate system. Devolopments in Quaternary Science. Vol. 1. pp 311-330. Elsevier, The Netherlands.

  • Permafrost Labratory. University of Alaska, Fairbanks. Photo pages. Link

  • Penner, E. 1962 Ground Freezing and Frost Heaving Canadian Building Digest CBD-26. NRC-IRC Publications. Link

  • Pidwirny, M. and Jones, S.1999. Fundamentals of Physical Geography 2nd Edition. Ebook. Link

  • Portland State University. 2009. Glaciers of the American West- Lewis Range, MT. Link

  • Tedrow. J and Drew, J. 1958.Arctic soil classification and patterned ground. Art.15-2-109. Arctic Institute of North America. PDF Download Link

  • US Army Corps of Engineers (USACE). Permafrost: Cryostructures. Cold Regions Research and Engineering Laboratory. Link

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    Copyright 2012: April Courtney, Emporia State University, Earth Science Undergraduate Program