The Effect of Moisture Content on the Thermal Conductivity of Moss and Organic Soil Horizons From Black Spruce Ecosystems in Interior Alaska

No abstract is available for this paper.

• Publication year

  2009

• Venue

  Soil Science

• Publication date

  2009-12-01

• Fields of study

  Chemistry, Environmental Science

• Identifiers
  DOI 10.1097/SS.0b013e3181c4a7f8
• External record

  Open on Semantic Scholar

• Source metadata

  Semantic Scholar

• No claims are published for this paper.

• No concepts are published for this paper.

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  2007influential reference
• In situ measurements of the thermal properties of a northern peatland: Implications for peatland temperature models

  2007cited by this paper
• Understory Vegetation Dynamics of North American Boreal Forests

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  2002influential reference
• The representation of arctic soils in the land surface model: The importance of mosses

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• Thermal Conductivity and Water Retention of a Black Spruce Forest Floor

  1997influential reference
• Comparison of Single and Dual Probes for Measuring Soil Thermal Properties with Transient Heating

  1994cited by this paper
• A biophysical surface energy budget analysis of soil temperature in the boreal forests of interior Alaska

  1991influential reference
• Environmental Factors and Ecological Processes in Boreal Forests

  1989cited by this paper
• Methods of soil analysis. Part 1. Physical and mineralogical methods.

  1988cited by this paper
• Changing Climate: Geothermal Evidence from Permafrost in the Alaskan Arctic

  1986cited by this paper
• Taiga Ecosystems in Interior Alaska

  1983cited by this paper
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  1983cited by this paper
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  1982cited by this paper
• Geotechnical engineering for cold regions

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  1973cited by this paper
• Thermal Properties of Soils

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