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Both Neutron Moisture Meter and Time Domain Reflectometry techniques were used to investigate the total soil water content (TSWC) and liquid soil water content (LSWC), respectively, and further based on to calculate soil ice content (SIC) and ice ratio (IR).
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In the present study, the required variable of layer thickness increase was calculated using the soil temperature from the climate models, and the ground ice content was obtained from the map of permafrost and ground ice conditions.
However, isolated masses of relic permafrost exist at temperatures close to 0 °C protected from rapid thawing by a thick layer of peat and soils with high ice content.
The model is then applied to frozen sandy soil with a range of ice contents and various temperature conditions; quantitative results agree well with practically measured stress strain data.
Numerical modeling was used for simulating the long-term thermal stability of the foundations soils and impacts of the TE effect, ice contents, mean annual ground temperature (MAGT), embedding depths of tower footings, and climate warming on ground thermal regime.
Measuring ice contents (θi) in partially frozen soils is important for both engineering and environmental applications.
The boreholes provided cryostratigraphic information on soil texture, cryostructures, ground ice, and gravimetric moisture content of frozen soils.
It is a composite of bedrock, soils, ice-covered lakes, ephemeral streams, and alpine glaciers.
Another challenge is the soil's content.
Soil moisture content.
Soil temperature and soil water content affected soil respiration differently.
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