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Spectrum Analysis on Geological Profile: A Case Study of Luzong Area in Anhui China

机译:地质配置文件的频谱分析 - 以安徽陆宗地区为例

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In order to further research the geological composition by spectral reflectance characteristics in Luzong area, this study was performed. Using ASD spectraradiometer (FieldSpec-FR), the spectra from multiple profiles were collected, the distance of 100cm from the testing surface was used. The spectral curves were smoothed with the moving average method, and the continuum removal was conducted to highlight features of optical absorbance. Each spectral curve gave the main characteristic composition of the profile, and the spectral curves from different profiles were compared and analyzed, some typical differences could be obtained obviously. All the profiles in the study area saw some similar spectral behavior: there were obsorbing valleys at 900 1450 1900 2200nm, but the number of obsorbing valleys and the bandlength of them were a little different. That is to say, the main structure and component can be obtained by testing spectrum without the help of other professional testing equipment. Using spectral analyst tool of ENVI 5.0 to give a comprehensive score, several minerals obtained high score, some of them clearly inconsistent with the actual were excluded, then the main minerals of the profiles were finalized, and which were consistent with those given by geological materials. For some profiles, the main composition and the relative proportion were also calculated out by the method of linear spectral decomposition, these results gave detailed components of the selected profiles, which had higher value and reliability than the former. Thus the differences between these profiles were also found. Another aim of this paper was to study the method to inversion material compositions and try to provide some usefull references for spectrum analysis. Furthermore, through detailed analysis on the results, it was also found that the measuring distance of 100cm from testing surface was still effective in field spectrum survey, the main structure and component could be obtained by these testing spectra. In order to grasp the nature of things quickly, a larger distance is feasible and necessary, macroscopic geological structure was provided quickly and accurately, which was not affected by local and microscopic interference. Unfortunately, there were some detail information lost, and the testing effect of 10cm from the testing surface will also be analyzed deeply in future.
机译:为了进一步研究由庐枞区域的光谱反射特性的地质组成,进行本研究。使用ASD spectraradiometer(的FieldSpec-FR),从多个简档的光谱收集,使用从测试表面百厘米的距离。的光谱曲线,用移动平均方法平滑化,并进行连续去除突出光学吸收的特征。每个光谱曲线得到轮廓的主要特征的组合物,并从不同的简档的光谱曲线进行了比较和分析,一些典型的差别可以明显获得。在研究区域内的所有配置文件看到一些相似的光谱行为:有900 1450 1900 2200nm obsorbing山谷,但山谷obsorbing的数量和它们的bandlength都有些不同。也就是说,主体结构和组件可以通过没有其他专业检测设备的帮助下测试频谱获得。使用ENVI 5.0的频谱分析工具,以提供一个综合评分,一些矿物质获得高分,其中一些显然不符合实际被排除在外,那么型材的主要矿物已最后确定,这是由地质材料中给出的一致。对于某些配置文件,在主成分和相对比例也通过线性频谱分解的方法计算出来,这些结果,得到的所选择的配置文件的详细的部件,其具有比前者更高的价值和可靠性。因此,也发现这些配置文件之间的差异。本文的另一个目的是研究的方法进行反转材料组合物,并尝试以提供用于频谱分析的一些有用的引用。此外,通过对结果的详细分析,结果还发现,从测试表面百厘米的测量距离仍然有效场谱测量,主要结构和部件可以通过这些测试的光谱来获得。为了迅速把握事物的性质,一个较大的距离是可行的,必要的,宏观的地质结构迅速而准确地提供,这是不受本地和显微干涉。不幸的是,有失去了一些细节信息,和10cm处的从测试表面的测试效果也将在未来的深入分析。

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