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Heat resistance of fungi from soil
International Journal of Food Microbiology, 1993The survival of fungi from soil samples has been investigated after exposure to temperatures of 60, 70, 80 and 90 degrees C in Sabouraud agar. The least resistant fungi surviving 60 degrees C for 60 min were the Aspergillus (A.) niger group, Chaetomium spp, Penicillium spp, and Scytalidium lignicola. None of these survived 70 degrees C for 10 min.
Z, Jesenská, E, Piecková, D, Bernát
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Applied Thermal Engineering, 2014
Abstract Due to the imbalance of heating and cooling demand, the soil temperature decreases after several years' operation for soil source heat pump system, and consequently the coefficient of performance (COP) decreases. Soil heat charging with solar energy was proposed for solar-soil source heat pump compound system.
Hongbing Chen +5 more
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Abstract Due to the imbalance of heating and cooling demand, the soil temperature decreases after several years' operation for soil source heat pump system, and consequently the coefficient of performance (COP) decreases. Soil heat charging with solar energy was proposed for solar-soil source heat pump compound system.
Hongbing Chen +5 more
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INFLUENCE OF THE HEAT STATE OF THE SOIL ON EFFICIENCY OF HEAT PUMP UNIT WITH SOIL HEAT EXCHANGER
2019-
Kostikov, Andrii Olehovych +1 more
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1979
Energy conversions on the soil surface and the temperature conditions that result from them in the ground-proximate air only become entirely clear when one knows more concerning the heat movement in soil and in the air. In order to understand heat movement in the soil, one first needs to know something concerning the physical properties of soils. Every
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Energy conversions on the soil surface and the temperature conditions that result from them in the ground-proximate air only become entirely clear when one knows more concerning the heat movement in soil and in the air. In order to understand heat movement in the soil, one first needs to know something concerning the physical properties of soils. Every
openaire +1 more source
Fixation of Radionuclides in Soil and Minerals by Heating
Environmental Science & Technology, 2001Heating of fine sand-sized common mineral powders (quartz, feldspar, or calcite) or a soil (from the Department of Energy's Hanford site) up to 1000 degrees C, in contact with sorbed radioisotopes (85Sr, 57Co, 134Cs, or U), markedly increased each isotope's immobilization.
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Soil pH and Soluble Organic Matter Shifts Exerted by Heating Affect Microbial Response
International Journal of Environmental Research and Public Health, 2022Nicasio T Jiménez-Morillo +2 more
exaly