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Table 3 Typical properties of some sedimentary rocks and their dependence with temperature

From: Two-dimensional THM modelling of the large scale natural hydrothermal circulation at Soultz-sous-Forêts

Property

Unit

Range of values

Comments

ϕ 0

%

3 to 35

Mean value of approximately 15

ρ dry

kg.m-3

1,900 to 2,600

Mean value of approximately 2,300

b

1

0.65 to 0.80

Lavoux limestone

  

0.8 to 1.0

sandstone

c dry σ

J.kg-1.K-1

Approximately 800

Increase of approximately 15%

   

if T [20; 250]°C

K int

m2

10-16 to 10-9

High variability

λ dry

W.m-1.K-1

0.5 to 6

Mean value of approximately 2;

   

decrease of approximately 25%

   

if T [20;250]°C

α 0

10-5 K-1

1.3 to 1.5

Approximately constant if T [50; 200]°C

E

GPa

10 to 92

Limestones (mean value of approximately 50)

  

2 to 39

Sandstones (mean value of approximately 15)

  

8 to 22

Schists (mean value of approximately 14)

ν

1

0.12 to 0.33

Limestones (mean value of approximately 0.25)

  

0.06 to 0.46

Sandstones (mean value of approximately 0.24)

  

0.03 to 0.18

Schists (mean value approximately 0.08)

Θ

µW.m-3

0.3 to 1.8

 
  1. From [Guimaraes et al. (2013]); [Kappelmeyer and Haenel (1974]); [Kirk and Williamson (2012]); [May-Crespo et al. (2012]); [Pasquale et al. (2011a]); [Touloukian et al. (1981]).