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Frozen Water sentence examples within soil freezing characteristic
A property of these phenomena is the relationship between unfrozen water content and sub-freezing temperature, known as the soil freezing characteristic curve (SFC).
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The relationship between the unfrozen water content in frozen soil and negative temperature is defined as the soil freezing characteristic curve (SFCC).
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Frozen Water sentence examples within differential scanning calorimetry
The differential scanning calorimetry (DSC), NMR spin-spin relaxation time, unfrozen water and water diffusion coefficient measurements were carried out in meat cured with ultrasound treated and untreated salt solutions.
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Using differential scanning calorimetry
(DSC) on emulsified micron-sized droplets, we derived onset temperatures of
heterogeneous ( Thet ) and homogeneous ( Thom ) freezing as
well as heterogeneously frozen water volume fractions ( Fhet ).
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Frozen Water sentence examples within total water content
In addition, the soil moisture probes below the frozen layer measured an increase in unfrozen water content, whereas total water content in the frozen layer was constant.
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The average root mean squared errors of the temperature, unfrozen water content, total water content, and freezing depth of the soil were 1.
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Frozen Water sentence examples within nuclear magnetic resonance
To determine the unfrozen water content variation characteristics of coal from the low temperature freezing based on the good linear relationship between the amplitude of the nuclear magnetic resonance (NMR) signal and movable water, pulsed NMR technology was used to test water-saturated coal samples and analyze the relationship between the unfrozen water content, the temperature and pore pressure during freeze–thaw from a microscopic perspective.
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Based on nuclear magnetic resonance (NMR) technique, the variation characteristics of unfrozen water content and the occurrence law of unfrozen water in pore structure of silty clay, red clay and remolded mudstone were analyzed by thawing experiments under different temperature gradients.
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Frozen Water sentence examples within Artificially Frozen Water
The current work builds on the research and development of a novel production method Ice Formwork facilitated through single-use moulds made of artificially frozen water.
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The proper setting of these parameters is a sine qua non for creating adequate mathematical models of heat and mass processes in the artificially frozen water-saturated rock mass.
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Frozen Water sentence examples within Heterogeneously Frozen Water
Using differential scanning calorimetry
(DSC) on emulsified micron-sized droplets, we derived onset temperatures of
heterogeneous ( Thet ) and homogeneous ( Thom ) freezing as
well as heterogeneously frozen water volume fractions ( Fhet ).
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0, were investigated in emulsified droplets by means
of differential scanning calorimetry (DSC) and analyzed in terms of the onset
temperature of the heterogeneous freezing signal Thet and the
heterogeneously frozen water volume fraction Fhet.
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Frozen Water sentence examples within frozen water content
In this study, microwave irradiation tests of frozen soils with five moisture contents were conducted and changes in their temperature, unfrozen water content and strength were measured.
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To determine the unfrozen water content variation characteristics of coal from the low temperature freezing based on the good linear relationship between the amplitude of the nuclear magnetic resonance (NMR) signal and movable water, pulsed NMR technology was used to test water-saturated coal samples and analyze the relationship between the unfrozen water content, the temperature and pore pressure during freeze–thaw from a microscopic perspective.
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Frozen Water sentence examples within frozen water droplet
Measurements show that after facets form on frozen water droplets, those facets grow laterally across the crystal surface leading to an increase in volume and surface area with only a small increase in maximum dimension.
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At the end of solidification, we obtain a small protrusion shape at the top of the frozen water droplet and its height is also higher than that of the initial water droplet.
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Frozen Water sentence examples within frozen water present
The research results show that the unfrozen water presents a “concave” shape change, and as the degree of freezing deepens, the total water content continues to increase; the salt content also shows an increasing trend, with the 0 ~ 100 cm soil layer salt rate being 43.
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Monitoring changes in ground temperature and/or the amount of unfrozen water present and help manage potential risk to our planet.
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Frozen Water sentence examples within frozen water sample
During the water purification process, the value of the thermal effect of frozen water samples melting declines (from 515.
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The hydrogen isotopes in liquid and frozen water samples were analyzed by laser ablation molecular isotopic spectrometry (LAMIS), which employs the molecular emission from laser-induced plasma for isotope analysis.
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Frozen Water sentence examples within frozen water volume
Using differential scanning calorimetry
(DSC) on emulsified micron-sized droplets, we derived onset temperatures of
heterogeneous ( Thet ) and homogeneous ( Thom ) freezing as
well as heterogeneously frozen water volume fractions ( Fhet ).
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0, were investigated in emulsified droplets by means
of differential scanning calorimetry (DSC) and analyzed in terms of the onset
temperature of the heterogeneous freezing signal Thet and the
heterogeneously frozen water volume fraction Fhet.
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Manipulating the retention of unfrozen water in freezing contaminated soil to achieve prolonged bioremediation in cold climates remains unformulated.
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Microcrystals of propane hydrates formed in frozen aqueous poly(vinyl alcohol) solutions in the course of ice melting are smaller in size than the propane hydrate crystals formed in frozen water under equal conditions of hydrate formation.
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As the water content increased, the thermal conductivity could likely not remain efficient enough to refreeze all the trapped water and thus allowed unfrozen water to lubricate particle corners, which enhanced mixture mobility.
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Summary Frozen soils are a multi-component system consisting of unfrozen water, ice, gas and solid particles.
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Publications on unfrozen water in frozen soil (UWFS) retrieved from the Web of Science were analyzed with scientometric software tools including VOSviewer, CiteSpace, and HistCite Pro.
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Furthermore, the amount of frozen water on the tapered surface is related to the duration of the transmission intensity peak during the defrosting process.
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The article presents the results of experimental studies of the content of unfrozen water in the zeolite of the Honguruu deposit of the Republic of Sakha (Yakutia).
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And more studies should focus on the accuracy of the hydraulic processes, especially soil hydraulic conductivity, unfrozen water, and snow processes.
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Nonclathrated water is analogous to unfrozen water in permafrost soils and has a significant effect on the properties of hydrate-bearing reservoirs.
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On the one hand, permafrost in general, and especially rock glaciers are considered key stores of frozen water in view of the recession of glaciers, and degrading permafrost is expected to partly compensate the decreasing glacial discharge in future.
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This paper uses worth of monitoring data to examine the temperature, unfrozen water, and deformation behaviors of a new High-speed Railway (HSR) anti-frost cutting bed in a deep seasonally frozen ground region.
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Sodium iodide was confirmed to enhance the contrast between the unfrozen water and ice in sorbets.
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Driven by the temperature gradient, the unfrozen water in the active layer moves from bottom to top during the freezing stage.
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To verify the effectiveness of ice content calculation and estimate the measuring accuracy while considering the presence of unfrozen water, the ice contents recorded by frequency domain reflectometry (FDR) sensors were used to provide the theoretical calculation equation of ice content reference values.
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The experimental data also suggest that besides frozen and unfrozen water, there is broad distribution of water state and dynamics in Nafion as the temperature is lowered from above zero down to -70 °C.
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The global cryosphere, Earth's frozen water, is in precipitous decline.
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In most porous media, the interface between liquid and frozen water is not sharp and a slushy zone is present.
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<p>Cryopeg is a volume of permafrost with a significant amount of cryotic unfrozen water as a result of freezing-point depression by dissolved salt content.
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The variation of the amount of unfrozen water in a frozen soil, which is primarily influenced by subzero temperature, has great impacts on the physical and mechanical behavior of the soil.
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Rheology and differential scanning calorimetry (DSC) analysis showed that MEL-A significantly improved the rheological properties of frozen dough and reduced the content of frozen water.
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Canada has the longest coastline in the world and includes diverse
ocean environments, from the frozen waters of the Canadian Arctic
Archipelago to the confluence region of Labrador and Gulf Stream waters on
the east coast.
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It is recommended to use hydrocarbon complexes consisting of HGFS-98 and GFS-30 in the ratio of 30:70 to 80:20 to reduce the content of frozen water in ice cream of different chemical compositions.
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We provide model based insights on how decreasing temperature below the freezing point of tissue relates to the percentage of frozen water.
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The most beneficial change to the model parameterizations was incorporation of unfrozen water in frozen soils.
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The ice is not simply an impervious layer of frozen water, but does in fact provide a variety of habitats to create a productive biome which is pertinent in the biogeochemical processes in the surface waters and at the air–ocean interface.
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We did not observe unfrozen water below our surveyed bedfast ice lakes, whereas unfrozen water (indicating permafrost thaw) was measured below floating ice lakes.
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In addition, ultrasonic testing is used to determine the volume of unfrozen water in frozen soil.
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One proposed method to detect the presence of spilled or leaked oil under the surface ice of frozen waters would rely on measuring the reverberation time of an impulsive acoustic source generated beneath that surface.
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The soil in the freezing-thawing front is filled with unfrozen water and ice, and its water content is high, which directly lead to frost heave.
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The increase in viscosity and unfrozen water with the addition of strawberry powder also caused a reduction in ice crystallization, which resulted in softer and more stable desserts over time.
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The DC resistivity method is a common tool in periglacial research because it can delineate zones of large resistivities, which are often associated with frozen water.
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To this end, a novel description of the local thermodynamic equilibrium of frozen water (ice) and a mixture of water vapour and an inert gas is derived, where anisotropic surface energy densities can be considered.
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An additional mechanism is proposed herein to address 2 key questions: (1) the existence of unfrozen water (i.
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This new structure, cemented with soil particles, unfrozen water, and ice, filled in the voids of frozen soil and effectively decreased the WIRFS compression coefficient and thaw strain.
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Frozen water has a quasi-liquid layer at its surface that exists even well below the bulk melting temperature; the formation of this layer is termed premelting.
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Another explanation may be that organisms from the water were compressed by freezing down to the sediment layer, leaving primarily relic DNA of dead cells to be detected higher in the frozen water.
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The ice is not simply an impervious layer of frozen water, but does in fact provide a variety of habitats to create a productive biome which is pertinent in the biogeochemical processes in the surface waters and at the air–ocean interface.
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This paper tries to investigate the unfrozen water, matric suction of aeolian sand, which is related to its thermal and mechanical properties.
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Water motions on nanoscale timescales present in non-frozen water, remained unaffected on the addition of MCC.
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The DC resistivity method is a common tool in periglacial research because it can delineate zones of large resistivities, which are often associated with frozen water.
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Significant portions of the deployed water, however, are thought to be lost to sublimation, evaporation and wind drift while traveling through the air, and to drainage of unfrozen water on the ground.
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In order to study the mechanism of lyoprotectants to protect cells and determine an optimal lyoprotectant formula, the thermophysical properties and percentage of unfrozen water of different lyoprotectants in freezing were investigated with differential scanning calorimeter (DSC).
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Migration of unfrozen water during freezing was considered to match the actual situation in practice.
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Freezing time was 1–2 min for OCT and the glue alternative, while a third group was in frozen water for 2–3 min.
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According to 1H NMR spectroscopy, the content of mobile (non-frozen) water in the frozen water-sodium alginate systems also depended on the initial polymer concentration and freezing temperature.
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We examined the impact of an urban trail created on a frozen waterway on visitor counts and PA levels.
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Raw seaweeds contained high amount of salts and water soluble fraction on the surface, that influences significantly the amount of unfrozen water at low temperatures (up to 11.
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Maximum stresses in frozen water-saturated sand are higher than those in frozen sand of 10% humidity.
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