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Heat capacity and specific heat


, : Heat capacity and specific heat. Methods of soil analysis Part 1 Physical and mineralogical methods: 941-944

A method for the determination of the heat capacity of soil using a calorimeter is described.

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Related references

Kluitenberg G.J., 2002: Soil heat; heat capacity and specific heat. Soil Science Society of America Book Series 5: 1201-1208

Miess Michael, 1971: Specific heat and the spatial and periodic distribution of heat capacity of soils at three differently adapted locations. Investigations made in profiles of brown podzolic soil, high moor and low moor.

Blake, A.S.; Petley, G.W.; Deakin, C.D., 2000: Effects of changes in packed cell volume on the specific heat capacity of blood: implications for studies measuring heat exchange in extracorporeal circuits. Extracorporeal circuits such as cardiopulmonary bypass (CPB) and renal dialysis machines cause active and/or passive loss of body heat. Attempts to quantify this heat loss are generally based on the Fick principle which requires knowledge of the s...

Hatta Tamao, 1987: Changes of specific heat capacity and heat capacity during weathering. An approach is presented which must be followed in the study of a deep-weathering profile. The present research pursues the evaluation of changes in specific heat capacity and heat capacity during weathering. For the first step to obtain the value...

Hatta T., 1986: Changes in thermal properties of rock during weathering; 1, Evaluation of specific heat capacity and volumetric heat capacity during rock weathering. Kobutsugaku Zasshi = Journal of the Mineralogical Society of Japan 17: 47-54

Makhatadze, G.I.; Privalov, P.L., 1990: Heat capacity of proteins. I. Partial molar heat capacity of individual amino acid residues in aqueous solution: hydration effect. The partial molar heat capacities of various peptides and various organic compounds that model the amino acid side-chains or their parts in aqueous solution have been determined by precise scanning microcalorimetry in the temperature range from 5...

Sochava, I.V.; Smirnova, O.I., 1993: Heat capacity of hydrated and dehydrated globular proteins: Denaturation increment of heat capacity. The experimental results obtained indicate that the dominating contribution to the denaturation increment of heat capacity is connected with thermal motion in a protein globule, which is in contrast to commonly accepted ideas. Absolute values of h...

Sochava, I.V.; Smirnova, O.I., 1993: Heat capacity of hydrated and dehydrated globular proteins. The denaturing increment of heat capacity. Absolute values of heat capacity for some hydrated globular proteins (11S globulin, ovalbumin, ribonuclease A, and lysozyme) have been studied by differential scanning calorimetry. It has been found that for proteins with bound water, as in the ca...

Fei Yingwei, 1986: Heat capacity of minerals relevant to the Earth's mantle; a new equation for the heat capacity of solids. Papers and Proceedings of the General Meeting - International Mineralogical Association Pages 97

Bouhifd M.A.; Richet P., 1994: Heat capacity, configurational heat capacity and viscosity of titanosilicate melts. Abstracts of the : eral Meeting of the International Mineralogical Association. 16; Pages 54. 1994.