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GEOL0012_25-26 **********GEOL0012 Moodle Test (unassessed) 2025/26**********

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Question text1. The one-dimensional heat flow equation is: [math: ρCP∂T∂t=κ∂2T∂z2+A] where ρ, Cp, and κ are the density, specific heat and thermal conductivity, and A represents heat sinks and sources. The boundary conditions in a given system are: (i) T=320 K at z=0 (ii) T=1200 K at z=40 km and we also have [math: κ=3Wm−1K−1]. Assuming no internal heat sources, calculate a) The thermal gradient of the equilibrium geotherm in [math: K/km] to two significant figures.Thermal gradient = Answer 1 Question 3[input] [math: K/km] [6] b) The temperature at a depth of 100km as predicted by this geotherm model. Give answer in K to two significant figures. T(z=100 km) = Answer 2 Question 3[input] K [4]

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The problem gives the one-dimensional heat flow with no internal sources and asks for the thermal gradient of the equilibrium geotherm and the temperature at 100 km depth. Since there are no internal heat sources (A = 0) and we’re likely dealing with a steady state (no explicit time dependence in the equilibrium geotherm), the......Login to view full explanation

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