We use cookies to ensure that we give you the best experience on our website. By continuing to browse this repository, you give consent for essential cookies to be used. You can read more about our Privacy and Cookie Policy.

Durham e-Theses
You are in:

Mineralogical mapping using airborne imaging spectrometry data

Mackin, Stephen (1989) Mineralogical mapping using airborne imaging spectrometry data. Doctoral thesis, Durham University.



With the development of airborne, high spectral resolution imaging spectrometers, we now have a tool, that allows us to examine surface materials with enough spectral detail to identify them. Identification is based on the analysis of position and shape of absorption features in the material spectra in the visible and infrared (0.4µm to 2.5µm). These absorption features are caused by the interaction of Electro-Magnetic Radiation (EMR) with the atoms and molecules of the surface material. Airborne data were collected to evaluate these new high spectral resolution systems. The data quality was assessed prior to processing and analysis and several problems were noted for each data set (striping, geometric distortion, etc.). These problems required some preparation of the data. After data preparation, data processing methods were evaluated, concentrating primarily on the log residuals and hull quotients methods. The processing steps convert the data to a form suitable for analysis. The data was analysed using the Spectral Analysis Manager (SPAM) package, developed by JPL. Two Imaging spectrometers were evaluated. The AIS - 1 instrument was flown over an area in Queensland, Australia. Ground data and laboratory work confirmed the presence of anomalous areas detected by the instrument. The data quality was poor and only basic classification of the data was possible. Anomalies were classed as "GREEN VEGETATION", "DRY VEGETATION", "CLAY" or "CARBONATE" based on the position of the major absorptions observed. The second instrument, the GER - II was flown over an area of Nevada, USA. Ground data and laboratory work confirmed the presence of the anomalies detected by the instrument. The data quality was somewhat better. Identification of sericite, dolomite and illite was possible. However, most of the area could still only be classed in the broad groupings listed above. To conclude, the effectiveness of identification is limited to a large degree by the poor data quality. If the data quality can be improved, techniques can be applied to automatically locate and identify material spectra, from the airborne data alone.

Item Type:Thesis (Doctoral)
Award:Doctor of Philosophy
Thesis Date:1989
Copyright:Copyright of this thesis is held by the author
Deposited On:18 Dec 2012 12:15

Social bookmarking: del.icio.usConnoteaBibSonomyCiteULikeFacebookTwitter