Retrieval of multidimensional heat transfer coefficient distributions using an inverse BEM-based regularized algorithm: numerical and experimental results

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Abstract

The surface distribution of heat transfer coefficients (h) is often determined point by point using surface temperature measurements of the tested object, initially at a uniform temperature and impulsively imposed with a convective boundary condition, and the solution to the transient heat conduction equation for a semi-infinite medium. There are many practical cases where this approach fails to adequately model the temperature field and, consequently, leads to erroneous h values. In this paper, we present an inverse BEM-based approach for the retrieval of spatially varying h distributions from surface temperature measurements. In this method, a convolution BEM marching scheme is used to solve the conduction problem. At each time level, a regularized functional is minimized to estimate the current heat flux and simultaneously smooth out uncertainties in calculated h values due to experimental uncertainties in measured temperatures. Newton's cooling law is then invoked to compute h. Results are presented from a numerical simulation and from an experiment. It is also shown that the method can be readily applied to steady-state.

Section snippets

Introduction and problem definition

Non-intrusive experimental techniques to determine convective heat transfer coefficients (h) currently in use both in industry and academia essentially rely on certain theoretical models and temperature driven physical phenomenon to accurately determine surface temperature histories. For instance, techniques which rely on characteristic color changes of liquid crystal films at a given temperature [1], [2] and the more recent laser induced fluorescence-based method [3], both rely on the

Time-dependent boundary element method for diffusion

The boundary element method (BEM) is a numerical implementation of boundary integral methods for solution of field problems and is described in detail in classic texts [19]. The BEM is now a well established numerical method which can be efficiently used to solve heat conduction problems in linear and nonlinear media [20], non-homogeneous isotropic media [21], [22], and non-homogenous anisotropic media [23], [24], using boundary-only discretization. As discussed previously, a distinct feature

Inverse problem definition and functional regularization

Film coefficient modeling is actually a direct problem due to the fact that time history temperature measurements are used as imposed first kind boundary conditions at the convective boundaries. However, small measurement noise at such boundaries reflect into large deviations of computed heat fluxes and consequently erroneous values of h. A remedy for this sensitivity problem is to reformulate h retrieval as an inverse problem and to regularize the functional. To this end, the following

Numerical implementation

Following standard BEM [19] the domain boundary, Γ, is discretized using N constant elements modeling the geometry as piecewise linear and the temperature and its flux as constant. Influence coefficients HijFp and GijFp are integrated analytically in time and via quadratures in space, and, in 2-D,HijFp=Γjρc2πr2{exp(ρcr24k(tFtp1))exp(ρcr24k(tFtp))}[(xxi)nx+(yyi)ny]dΓwhere nx and ny are the x- and y-components of the outward-drawn normal, while analytical integration of coefficients GijFp

Numerical example in a backward-facing step under convection

A numerical example is now presented to validate the inverse BEM formulation. The backward-facing step geometry is shown in Fig. 3 along with imposed boundary conditions. Fig. 4(a) presents the backward-facing step discretization consisting of 60 equally spaced constant boundary elements. Thermophysical properties of pure aluminum are used: k=2.37 W/cm K, ρ=0.002702 kg/cm3, and c=903 J/kg. The initial temperature of the field is Ti=30 °C and the convective ambient temperature is Ta=800 °C. The

Experiment

A schematic of the test set up is displayed in Fig. 9. A blower supplies ambient air to the flow conditioning section. Upon exiting the blower, inlet air is heated from room temperature to 60 °C via a heat exchanger. Water is supplied to the heat exchanger through an externally heated water supply and pump system that is controlled to maintain constant flow temperature based on a flow temperature measurement prior to the test section. The flow then passes through a flow conditioning section and

Conclusion

In this paper, we develop a BEM-based inverse algorithm to retrieve multi-dimensional h distributions from transient surface temperature measurements. A regularization procedure serves to provide a ‘best fit’ through noisy input data. Results presented for studies over a square, a backward facing step, and a rib-like structure demonstrate accuracy and robustness of the method. Results from an experiment using TLC are also presented.

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