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, pp. 137 – 158 . Scharli , U. , L. Rybach 2001 : Determination of the specific heat capacity on rock fragments . — Geothermics , 30 , pp. 93 – 110

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pores. H 0 = [ ( 1 − P ) × ρ m × c m + P × ρ w × c w ] × ( T t − T 0 ) × A × Δ z , where ρ m and ρ w denote the density of the rock matrix and the water (kg/m 3 ); c m and c w , specific heat capacity of the matrix and the water (Jkg −1 K −1 ); P

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