Results 251 to 260 of about 5,532,500 (299)
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Physical Geography, 1987
The temporal and spatial patterns of soil temperatures in Nigeria are examined. Because of the effect of latitudinal position on air temperatures, soil temperatures generally increase with increasing distance from the coast. There is however an exception to this general pattern on the Jos plateau, where, because of the significant effect of elevation ...
Oluwole Ameyan, O. Alabi
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The temporal and spatial patterns of soil temperatures in Nigeria are examined. Because of the effect of latitudinal position on air temperatures, soil temperatures generally increase with increasing distance from the coast. There is however an exception to this general pattern on the Jos plateau, where, because of the significant effect of elevation ...
Oluwole Ameyan, O. Alabi
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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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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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A soil temperature demonstration
Journal of Agronomic Education, 1980ABSTRACTAn exhibit was constructed to demonstrate the effects of soil moisture on the heat capacity and thermal conductivity of two different soils. Four soil columns were fitted with thermistors at depths of 0 to 1, 5, and 10 cm below the soil surface. Half the columns were saturated with water and the other half were left air‐dry.
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Nature, 1961
INFORMATION on soil temperatures in Iceland is scant except for interrupted and now discontinued observations made by the Meteorological Bureau of Iceland at two and earlier three different locations in the country1. These observations had mostly been restricted to the 1- and 2-m. depths.
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INFORMATION on soil temperatures in Iceland is scant except for interrupted and now discontinued observations made by the Meteorological Bureau of Iceland at two and earlier three different locations in the country1. These observations had mostly been restricted to the 1- and 2-m. depths.
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