Page tree

You are viewing an old version of this page. View the current version.

Compare with Current View Page History

« Previous Version 33 Next »


Motivation


The

This is a  (see Fig. 1).




Fig. 1. Sample Temperature Profile for Semispace Linear Conduction model.



Heat flow equation for Semispace Linear Conduction:

(1) \frac{\partial T}{\partial t} = a^2 \Delta T = a^2\frac{\partial^2 T}{\partial z^2}

Initial Conditions

(2) T(t=0, z) = T_G(z)

Boundary conditions

(3) T(t, z=0) = T_f = {\rm const}, \quad T(t, z \rightarrow \infty) = T_G(z)

The exact solution is given by following formula:

(4) T(t,z) = T_f + (T_G(z) - T_f) \cdot \frac{2}{\sqrt{\pi}} \int_0^{z/\sqrt{4at}} e^{-\xi^2} d\xi

A fair approximation at late times ( \zeta \sim 0) is given by expanding the integral:

(5) T(t,z) = T_f + (T_G(z) - T_f) \cdot \Bigg[ 1- \frac{\exp(-\zeta^2)}{\sqrt{\pi} \zeta} \bigg( 1- \frac{1}{2 \zeta} + \frac{3}{4 \zeta^3} \bigg) \Bigg]

where

(6) \zeta = \frac{z}{4 a t}

The final solution for temperature  above the flowing unit is represented by RHK pipe flow solution where TG is replaced with Tb from  (5).


For the intervals between two injection units the one needs to account for the SLC contribution from upper flowing unit and from lower flowing unit which can be done using the superposition.


First, let's rewrite  (5) in terms of temperature gain:

(7) dT(t, z) = T(t,z) - T_G(z)= - (T_G(z) - T_f) \cdot \frac{\exp(-\zeta^2)}{\sqrt{\pi} \zeta} \bigg( 1- \frac{1}{2 \zeta} + \frac{3}{4 \zeta^3} \bigg)


Now one can write down the temperature disturbance from the overlying flowing unit A1:

(8) dT_{b,over}(t, z) = T_{b,up}(t,z) - T_G(z)= - (T_G(z) - T_{f, A1}) \cdot \frac{\exp(-\zeta^2)}{\sqrt{\pi} \zeta} \bigg( 1- \frac{1}{2 \zeta} + \frac{3}{4 \zeta^3} \bigg)
and from the underlying flowing unit A2:
(9) dT_{b,under}(t, z) = T_{b,up}(t,z) - T_G(z)= - (T_G(z) - T_{f, A2}) \cdot \frac{\exp(-\zeta^2)}{\sqrt{\pi} \zeta} \bigg( 1- \frac{1}{2 \zeta} + \frac{3}{4 \zeta^3} \bigg)


The background temperature disturbance between the flowing units will be:

(10) T_b(t, z) = T_G(z) + dT_{b,over}(t, z) + dT_{b,under}(t, z)


Replacing the static value of  T_G(z) in RHK model with dynamic value of   T_b(t, z) one arrives to the final wellbore temperature model with account of heat exchange with surrounding rocks and cooling effects from flowing units (Semispace Linear Conduction).


See also


Physics / Fluid Dynamics / Linear Fluid Flow 


References


  • No labels