2004
DOI: 10.1023/b:narr.0000032648.15016.49
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A Review and Evaluation of Specific Heat Capacities of Rocks, Minerals, and Subsurface Fluids. Part 2: Fluids and Porous Rocks

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Cited by 79 publications
(40 citation statements)
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“…The RHP in the crust, in particular from the upper part of the crystalline crust, contributes significantly to the heat flow into sedimentary basins and thus to the heat-flow density as observed near the Earth´s surface. Heat-flow density (HFD, q in mW m −2 ) is given by the Fourier's first law (Fourier 1822): Brigaud & Vasseur (1989); c Fertl & Frost (1980); d Schön (1996); e Schön (1983); f Horai (1971); gČ ermák & Rybach (1982); h Lemmon et al (2005); i Crain (2013); j Gröber (1955); k Waples & Waples (2004); l Mel'nikova et al (1975); m Dortman (1976); n Drury et al (1984), o Drury (1987); p Goto & Matsubayashi (2009); q Skauge et al (1983); r Calculated from SHC, RHO and TC following eq. 1.…”
Section: Thermal Parametersmentioning
confidence: 99%
See 1 more Smart Citation
“…The RHP in the crust, in particular from the upper part of the crystalline crust, contributes significantly to the heat flow into sedimentary basins and thus to the heat-flow density as observed near the Earth´s surface. Heat-flow density (HFD, q in mW m −2 ) is given by the Fourier's first law (Fourier 1822): Brigaud & Vasseur (1989); c Fertl & Frost (1980); d Schön (1996); e Schön (1983); f Horai (1971); gČ ermák & Rybach (1982); h Lemmon et al (2005); i Crain (2013); j Gröber (1955); k Waples & Waples (2004); l Mel'nikova et al (1975); m Dortman (1976); n Drury et al (1984), o Drury (1987); p Goto & Matsubayashi (2009); q Skauge et al (1983); r Calculated from SHC, RHO and TC following eq. 1.…”
Section: Thermal Parametersmentioning
confidence: 99%
“…carbon percentage in coals: van Krevelen 1961; volatile-matter content and temperature of coal : Richardson 1993; cf. review by Waples & Waples 2004). Beyond these possibilities, TD or SHC basically are calculated from (1) the volume fraction of the rock components by applying some mixing model, (2) the relation between TC, TD, SHC and density and (3) empirical relationships between TC, TD and/or SHC (e.g.…”
Section: Introductionmentioning
confidence: 99%
“…The temperature of the heated airflow is usually higher than that of the surface atmosphere by over 10°C, especially in the winter (although the difference may be lower in summer). Many studies have shown that the heat flux from geothermal sources to the airflow in a mine is approximately constant over the year, and therefore, so is the temperature of the airflow [1][2][3][4]. On the other hand, there are seasonal and diurnal variations in the temperature of the surface atmosphere.…”
Section: Introductionmentioning
confidence: 99%
“…It is also temperature dependent. A detailed study of specific heat capacities and their temperature dependence, on more than 150 various minerals, was done by Waples & Waples (2004). They defined heat capacity with approximation to be uniform in all directions or isotropic.…”
Section: Specific Heat Capacity Of Mineralsmentioning
confidence: 99%
“…This effect has to be included when heating rates are calculated; otherwise it can produce values which can be very different when compared with experimental results. A good equation was developed by Waples & Waples (2004) …”
Section: Specific Heat Capacity Of Mineralsmentioning
confidence: 99%