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基于可见/近红外高光谱成像的中国云冈石窟砂岩粉状风化剖面研究进展

[Advance in the study of the powdered weathering profile of sandstone on China Yungang Grottoes based on VIS/NIR hyperspectral imaging].

作者信息

Zhou Xiao, Gao Feng, Zhang Ai-wu, Zhou Ke-chao

机构信息

Chinese Academy of Culture Heritage, Beijing 100029, China.

出版信息

Guang Pu Xue Yu Guang Pu Fen Xi. 2012 Mar;32(3):790-4.

Abstract

Yungang Grottoes were built in the mid-5th century A. D., and named as a UNESCO World Heritage site in 2001. Most of the grottoes were built on the feldspathic quartz sandstones. They were seriously damaged due to the environmental impact. The main form of the weathering is the powdered weathering. The weathering conditions are generally characterized by electrical sounding, penetration resistance, molecular spectroscopy, etc. However, although these methods can give good results about the weathering conditions for a specified sample or site, they are not suitable for providing a global profile of the weathering conditions. The present paper provides a method for effectively and roundly assessing the overall powdered weathering conditions of the Yungang Grottoes based on hyperspectral imaging. Powdered weathering could change the structure and granularity of the sandstone, and thus change the spectral reflectance of the sandstone surface. Based on the hyperspectral data collected from 400 nm to 1 000 nm and normalized by log residuals method, the powdered weathering conditions of the sandstones were classified into strong weathering and weak weathering. The weathering profile was also mapped in the Envi platform. The mapping images were verified using the measured hyperspectal data of the columns in front of the 9th and 10th grottoes as the examples. The mapping images were substantially fitted to the real observations, showing that hyperspectral imaging can be used to estimate the overall powdered weathering of the sandstones.

摘要

云冈石窟建于公元5世纪中叶,2001年被联合国教科文组织列为世界遗产。大部分石窟建于长石石英砂岩上。由于环境影响,它们遭到了严重破坏。风化的主要形式是粉末状风化。风化状况通常用电测深、贯入阻力、分子光谱等方法来表征。然而,尽管这些方法能对特定样本或地点的风化状况给出良好结果,但它们并不适合提供风化状况的全局概况。本文基于高光谱成像提供了一种有效且全面评估云冈石窟整体粉末状风化状况的方法。粉末状风化会改变砂岩的结构和粒度,进而改变砂岩表面的光谱反射率。基于从400纳米到1000纳米收集的高光谱数据并采用对数残差法进行归一化处理后,将砂岩的粉末状风化状况分为强风化和弱风化。风化剖面图也在Envi平台上绘制出来。以第9窟和第10窟前立柱的实测高光谱数据为例对绘制图像进行了验证。绘制图像与实际观测结果基本吻合,表明高光谱成像可用于估算砂岩的整体粉末状风化情况。

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