A time domain unconditionally stable explicit method is presented which may be used to model processes governed by the diffusion equation such as transient heat flow. Unlike the explicit finite difference routine, the method models the diffusion process within the time step (MPWT). Being explicit, t
Different methods for estimating thermal diffusivity of a heat process
โ Scribed by B. Leden; M.H. Hamza; M.A. Sheirah
- Publisher
- Elsevier Science
- Year
- 1976
- Tongue
- English
- Weight
- 1000 KB
- Volume
- 12
- Category
- Article
- ISSN
- 0005-1098
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โฆ Synopsis
Compared to the widespread and highly accurate a~ngstr~m's 1861 method for determining the thermal ditusivity of a long copper rod the maximum likelihood method provides greater accuracy but more computational time and storage.
Summary---The purpose of this study is to compare three different methods for determining the thermal diffusivity of a one dimensional heat diffusion process. A modified ]U~ttr6m's method, an on-line least squares method and a maximum h]telihood method have been applied to data obtained from experiments on a long copper rod. The accuracy, the amount of computation, the storage capacity and in general the advantages and the limitations of the different methods are discussed.
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A method is devised for measuring soil thermal diffusivity in situ. It is based on direct experimental simulation of the finite difference approximation to the one-dimensional heat conduction equation. The method does not require the soil to be homogeneous except between the three thermometers that