Table 1 Example minimum and maximum values for the thermal characteristics of a magma chamber used to calculate thermal contraction
From: What causes subsidence following the 2011 eruption at Nabro (Eritrea)?
Param. | Units | Max value | Reference | Min value | Reference |
|---|---|---|---|---|---|
C p | J Kg −1 K −1 | 1100 | Martin et al. (1987) | 1047 | Armienti et al. (1984) |
f | 0.9 | Tallarico et al. (2003) | 0.6 | Armienti et al. (1984) | |
k | W m −1 K −1 | 3 | Chapman (1986) | 2.3 | Armienti et al. (1984) |
Q l | J Kg −1 | 800000 | Armienti et al. (1984) | 334944 | Tallarico et al. (2003) |
T s | K | 1130 | Donovan et al. (2018) | 1030 | Donovan et al. (2018) |
Δ T | K | 350 | Armienti et al. (1984) | 150 | Huppert and Sparks (1981) |
ρ s | kg m −3 | 3300 | Scandone and Giacomelli (1998) | 3084 | Scandone and Giacomelli (1998) |
ρ l | kg m −3 | 2750 | Sparks and Huppert (1984) | 2570 | Armienti et al. (1984) |