On relaxation-spectrum estimation for decades of data: accuracy and sampling-localization considerations
On relaxation-spectrum estimation for decades of data: accuracy and sampling-localization considerations
复制标题
关于数十年数据的松弛谱估计:准确性和采样定位考虑因素
DOI:
10.1088/0266-5611/16/5/324
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发表时间:
2000
期刊:
影响因子:
2.1
通讯作者:
J. Macdonald
中科院分区:
文献类型:
--
作者:
J. Macdonald
In the inversion of data using the relaxation-spectrum model of electrical and rheological phenomena and processes, an important goal is to obtain a comprehensive and accurate approximation of the distribution of relaxation times (DRT) associated with the phenomenon or process under investigation. The estimation of such a DRT poses theoretical as well as experimental challenges. In the latter, it is often necessary to measure many decades of frequency-response data before sufficient information has been collected to allow an adequate estimate of the structure of the required spectrum to be calculated. At the theoretical level, among other things, one must solve the inverse problem of the relaxation-spectrum estimation, along with the frequent need to work with many decades of data. Some consequences of these two aspects of the problem are examined in this paper. In order to address this problem, accurate (or noisy), wide-range frequency-response data sets derived from the Kohlrausch-Williams-Watts (KWW) continuous DRT function (with a value of its β0 parameter of 0.5) are inverted numerically using a complex nonlinear least-squares method with variable τ free parameters and variable quadrature weighting, a method superior to Tikhonov regularization for data of the present type when inversion accuracy need not be sacrificed for increased resolution. The relative errors in the resulting DRT point estimates are investigated for various frequency ranges for both frequency-response data derived from the usual KWW DRT and from such a DRT which is abruptly cut off at its low τ end. Although the inversions are ill-posed, DRT errors were found to be very small over appreciable τ ranges, but the effects of cutoff of the range of the DRT and of a limited frequency range led to rapid relative-error increases at the ends of the DRT τ range, and allowed separation and quantification of the effects of these two limitations. Important resolution differences are illustrated between the results of inversions of accurate and of noisy data by the present method and by Tikhonov regularization. Finally, the temporal response was calculated very simply from frequency-response inversion DRT estimates and compared with exact stretched-exponential response function values associated with the KWW dispersion model. Extremely small relative errors were found, but they nevertheless showed the effects of the above limitations at short and long times. Transformation to the time domain of the kind illustrated here for wide-range data is far simpler, more accurate, and more convenient than Fourier transformation.