Closed NengLu closed 4 years ago
Hi NengLu Is there any better way to control this? The one you mention is pretty good. That's the trick I use to fix the temperature in the air layers.
... how to input the radiogenicHeatProd of the crust in UWG? Check Tutorial_1_ThermoMechanical_Model for an example.
An exponential decrease in RHP can be achieved via a function, or a stack of layer of decreasing radiogenic heat production.
Cheers Patrice
Hi NengLu Is there any better way to control this? The one you mention is pretty good. That's the trick I use to fix the temperature in the air layers.
... how to input the radiogenicHeatProd of the crust in UWG? Check Tutorial_1_ThermoMechanical_Model for an example.
An exponential decrease in RHP can be achieved via a function, or a stack of layer of decreasing radiogenic heat production.
Cheers Patrice
Hi Patrice, Thank you, I am going to check the tutorial again.
Hello,
Is it necessary to define surface heat flow for maintaining the thermal structure in the crust? Take "Tutorial_1_ThermoMechanical_Model " for example, the near-surface temperature is too high after initial, T = 103 u.degC at 0 km. That can be imporved by fixing the surface nodes to surface temperature:
T = 32.3 u.degC at 0 km:
Is there any better way to control this?
And how to input the radiogenicHeatProd of the crust in UWG? For example, the radiogenic heat production of the crust is 1e-9 w/kg, heat production decay length is 10km, the density of the upper and lower crust is 2700 and 2800 kg/m^3, the thickness of them are both 20km.
The radiogenicHeatProd of UC and LC are 2.7 and 2.8 microwatt/m^3 ? Or taking the average value by considering the decay as 1.53 and 0.22 microwatt/m^3 in UWG? (2.7(np.exp(-20/10)+1)/2=1.53, 2.8(np.exp(-40/10)+np.exp(-20/10))/2 =0.22)