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Quantitative analysis of the water of crystallization of gypsum by near-infrared spectroscopy in Yungang Grottoes

机译:云冈石窟近红外光谱法定量分析石膏结晶水

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摘要

Near infrared spectroscopy is considered to be an effective analytical tool which is used in various fields, however, it is rarely used in the analysis of the water of crystallization of rocks from stone relics. In the present study, a calibration model was developed for the non-destructive estimation of the water of crystallization content of dihydrate gypsum in rocks using Fourier transform near infrared spectroscopy. A total of 51 samples were prepared in the laboratory to simulate the actual samples from Yungang Grottoes, their Fourier transform near infrared spectra were correlated to the water of crystallization content by means of partial least square regression, and then the calibration model was developed. 5 actual samples from Yungang Grottoes were analyzed by X-ray diffraction and X-ray fluorescence. The optimal model was achieved with a correlation coefficient of 0.9899 and a root mean square error of cross validation of 0.2190, and the correlation coefficient and the root mean square error of the prediction of the validation set were 0.9834 and 0.4558, respectively.
机译:近红外光谱法被认为是一种有效的分析工具,已在各个领域中使用,但是,它很少用于分析来自石器遗址的岩石的结晶水。在本研究中,使用傅立叶变换近红外光谱法开发了一种用于无损估算岩石中二水合石膏结晶水的校准模型。为了模拟云冈石窟的实际样品,实验室共准备了51个样品,通过偏最小二乘回归将它们的傅里叶变换近红外光谱与结晶水含量关联起来,建立了校正模型。通过X射线衍射和X射线荧光分析了5个云冈石窟的实际样品。最佳模型的相关系数为0.9899,交叉验证的均方根误差为0.2190,验证集预测的相关系数和均方根误差分别为0.9834和0.4558。

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