Estimates of the Lunar Surface Composition with Clementine Images and Lscc
نویسندگان
چکیده
Introduction: There have been several approaches to develop remote sensing technique to estimate composition of the lunar surface using multispectral observations. We present a new approach based on statistical analysis of spectral and compositional data for lunar samples by the Lunar Soil Characterization Consortium (LSCC) and using the UVVIS Clementine data with 1 km resolution. This technique allows us to estimate and map the abundance of TiO2, SiO2, and FeO, pyroxene and plagioclase content, and maturity degree (Is/FeO). Data and Their Analysis: We use data for LSCC -characterized mare soils of the Apollo-11, 12, 15, and 17 missions [1] and recent data for several Apollo-14 and -16 soils (highland regolith). Coordinated compositional and spectral measurements were carried out for samples with controlled particle size: <10 μm, 10-20 μm, and 20-45 μm. We used 42 samples for analysis. Bi-directional spectra were obtained with the RELAB spectrometer in the spectral range 300–2600 nm [2]. We have transposed the soil spectra to the Clementine spectral bands (415, 750, 900, 950, and 1000 nm). The main point of our approach is to find relationships that provide the highest correlation coefficients between different linear combinations of optical parameters, on one hand, and chemical/mineral composition and degree of maturity, on the other hand. We used the following optical parameters: albedo AR = A(750 nm), color-indexes: CBR = A(415 nm) / A(750 nm), CIR1 = A(900 nm) / A(750 nm), CIR2 = A(950 nm) / A(750 nm), CIR3 = A(1000 nm) / A(750 nm), and bend D = A(750 nm) A(1000 nm) / [A(900 nm)]. An optimal empirical expression to derive high correlation coefficients is: logP = aAR(%)+bCBR+cCIR1+hCIR2+ eCIR3+fD+g, where P is a studied parameter. The weight coefficients a, b, c, h, e, f, and g minimize the RMS deviations of the calculated values of P from the measured values. Using the current set of LSCC data these coefficients are given in the following Table: a b c h e f g TiO2 -0.040 1.873 50.662 -17.747 -13.531 13.011 -32.542 FeO -0.023 0.349 24.664 -15.632 -1.233 5.190 -11.968 SiO2 0.002 -0.214 -2.091 -0.554 1.597 -0.736 3.511 Py -0.023 0.079 16.771 -19.487 4.959 1.666 -2.782 Pl 0.016 0.861 -6.888 7.360 -1.527 -0.322 1.972 Is/FeO -0.013 -2.466 -35.496 17.736 5.303 -10.710 26.712
منابع مشابه
Completion of the Unified Lunar Control Network 2005 and Topographic
Introduction: We have completed a new general unified lunar control network and lunar topographic model based on Clementine images. This photogrammetric network solution is the largest planetary control network ever completed. It includes the determination of the 3-D positions of 272,931 points on the lunar surface and the correction of the camera angles for 43,866 Clementine images, using 546,...
متن کاملEstimation of Lunar Elemental Abundances Using Clementine UVVIS+NIR Data
Many attempts have been made to derive elemental abundances of the lunar surface from multispectral images. A method to predict Fe abundance based on Clementine UVVIS data is presented in [1]. A refined method which also addresses the TiO2 abundance is provided in [2], demonstrating that in spite of issues posed by soil maturity, grain size, mineral content, topographic shading, and glass conte...
متن کاملConstraining Lunar Surface Mineralogy with Combined Thermal- and Near- Infrared Spectral Data
Introduction: The current understanding of lunar surface mineralogy largely comes from two sources: samples (Apollo and meteorite [e.g. 1]) and remote near-infrared spectroscopic measurements (telescopic and Clementine [e.g. 2]). Samples provide detailed compositional analysis of a limited number of sites across the lunar surface and NIR measurements provide global, high-resolution coverage of ...
متن کاملNew Method of Photometric Correction for Lunar Uvvis Images
Introduction: An accurate phase function is necessary for precise photometric correction of the Clementine lunar UVVIS images. Although several researchers have proposed photometric models for Clementine UVVIS images using empirical phase functions (e.g., [1] [2] [3]), additional work is required for correction of the data at small phase angle (<20), because the phase function at small phase an...
متن کاملComposition and exposure age of the Apollo 16 Cayley and Descartes regions from Clementine data: Normalizing the optical effects of space weathering
In order to quantitatively assess the composition of the lunar surface from reflectance spectroscopy, it is necessary to be able to differentiate between the optical effects due to composition and those due to exposure to space weathering processes. Laboratory analyses of returned lunar soils are used to show that limited quantitative compositional information and the exposure age of the lunar ...
متن کامل