thermal properties of sedementary rocks

Jun 30th, 2015
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mean values and ranges- Table 8. geves an overview of range and mean values for thermal conductivity of sedementary rocks. It is useful to dstinguish for further discussions between- Dense, i.e, pore and crack free sedimentary rocks and Porous sedimentary rocks. Resulting from the difference of thermal properties between minerals and pore filing materials.

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8.3.3 thermal properties of sedementary rocks8.3.3.1 mean values and rangesTable 8. geves an overview of range and mean values for thermal conductivity of sedementary rocks.It is useful to dstinguish for further discussions betweenDense, i.e, pore and crack free sedimentary rocks andPorous sedimentary rocksResulting from the difference of thermal properties between minerals and pore filing materials.Table 8.7 thermal properties of sedimentary rocks,References : b- blackwell and steele 1989; C-Cermak and Rybach, 1982; D- Dortman 1976; J- Jessop, 1990 ( data after Roy et al, 1981);K- Kobranova, 1989; S- Schuch, 1980;Rock type Wm-1K-1n range meanCF in kJ kg-1K-1n range meana in m2 s-1range meanRefAnhydriteGypsumSalt77 1.006.05 4.003 4.895.73 5.43 4.905.75 4.905.80 2.505.80 0.601.6770 1.4015 1.67per 0.810.94 0.98 0.580.61 0.901.10CJDBEK8.3.3.2 non porous sedimentary rocksDense sedimentary rocks show the same main influesces and properties which control the thermal properties of magmatic rocksMineral content and thermal properties of mineralsInterna structure of the rockTypical members of this group are non porous anhydrite, carbonater and the different typesof salt. Table 8.8 contain some examples of the thermal conductivity o

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