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Estuarine Subaqueous Soil Temperature
Soil Science Society of America Journal, 2011Most biological and chemical processes related to soil function and formation are temperature dependent. To begin understanding soil temperature in estuarine subaqueous soils, this parameter was investigated in two shallow coastal lagoons in southern New England.
Salisbury, Alexander, Stolt, Mark H.
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Soil atmosphere and soil temperature
1987Plant roots, soil microorganisms and fauna are consumers of oxygen and producers of carbon dioxide. This gives rise under ordinary conditions to the well known carbon dioxide concentration gradient from about 50 000 ppm (5%) in soil pores to a little over 300 ppm in the general atmosphere.
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Soil Temperature and Heat Transport in Soils
2018Soil temperature varies over a wide range, depending on annual and diurnal cycles of incoming solar energy and on the soil surface properties. Plants can grow when soil root zone temperatures are in the relatively narrow range 0–40 °C. Soil-water hydraulic conductivity and soil-water retention curves are functions of temperature because of the ...
Viliam Novák, Hana Hlaváčiková
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Eos, Transactions American Geophysical Union, 1949
This paper develops a method for computing temperatures at a point in a soil from surface temperatures. The method is adaptable to the irregular fluctuations in temperature ordinarily found in nature as well as to ideal cases. The temperature at a point in the soil is expressed as a weighted function of antecedent temperatures at the surface.
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This paper develops a method for computing temperatures at a point in a soil from surface temperatures. The method is adaptable to the irregular fluctuations in temperature ordinarily found in nature as well as to ideal cases. The temperature at a point in the soil is expressed as a weighted function of antecedent temperatures at the surface.
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Effects of photovoltaic panels on soil temperature and moisture in desert areas
Environmental science and pollution research international, 2021Shengjuan Yue +4 more
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Soil Temperature Profiles of Two Alaskan Soils
Soil Science Society of America Journal, 1987Abstract Soil temperatures of a thawed phase of a Pergelic Cryaquept were measured with copper‐constantin thermocouples at 20, 50, 100, 150, 210, 240, and 300 cm under a fallow plot for 5 yr in Fairbanks, AK. Soil temperatures of a Typic Cryorthent were measured the same way at 5, 10, 20, 50, 100, 150, and 300 cm under both grass and ...
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ANALYTICAL SOIL–TEMPERATURE MODEL
Soil Science Society of America Journal, 2004The exponential‐sinusoidal one‐dimensional analytical model reasonably describes soil temperature profile. Surface temperature may be represented by the sum of two sinusoids, one related to annual and the other to daily temperature variations, each one having constant amplitude.
Elimoel A. Elias +3 more
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Modeling Soil Temperature Variations
Journal of Agricultural Research and Development, 2009This paper reports on modeling soil temperature variations. Transient heat flow principles were used in the study, with the assumptions that the heat flow was one-dimensional, the soil was homogenous and that the thermal diffusivity was constant. Average conditions are also assumed.
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Improved soil temperature modeling
Environmental Earth Sciences, 2010Soil temperature affects a number of physical, chemical, and biological processes, yet it is often difficult and costly to measure on a wide scale. Practical and accurate models are required to forecast spatial and temporal soil temperature variations.
Shaogang Lei +3 more
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The Journal of Agricultural Science, 1928
1. The soil temperatures in Egypt at a number of depths have been recorded by means of continuous recording thermometers. In general, the records show that the amplitude of the temperature wave at the surface of the soil is considerably greater than the air temperature wave.
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1. The soil temperatures in Egypt at a number of depths have been recorded by means of continuous recording thermometers. In general, the records show that the amplitude of the temperature wave at the surface of the soil is considerably greater than the air temperature wave.
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