In the analyses of the kinetics of diffusion-controlled phase transformation the availability of analyticalsolutions for dissolution is limited compared to those for growth. The difficulty seems to arise from the fact thatone has to deal with a non-zero initial radius in the dissolution of precipitates. To alleviate this difficulty severalapproximate analyses, i.e. invariant-field, invariant-size (stationary-interface, SI) and linearized gradient (LG)approximations etc., were devised and the accuracy of

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