Hyperspectral core logging for fire reconstruction studies

Springer Science and Business Media LLC - Tập 59 - Trang 297-308 - 2017
Antonin Van Exem1, Maxime Debret1,2, Yoann Copard1, Boris Vannière3, Pierre Sabatier4, Stephane Marcotte5, Benoit Laignel1, Jean-Louis Reyss4, Marc Desmet6
1UNIROUEN, UNICAEN, CNRS, M2C, Normandie Univ., Rouen, France
2UMR CNRS 6143 - Morphodynamique Continentale et Côtière, Bâtiment Blondel - UFR Sciences et Techniques, Université de Rouen, Mont-Saint-Aignan Cedex, France
3Chrono-Environnement UMR 6249, MSHE USR 3124, CNRS, Univ. Bourgogne Franche-Comté, Besançon, France
4Environnement, Dynamique et Territoires de Montagne (EDYTEM), CNRS, University Savoie Mont Blanc, Le Bourget du Lac, France
5INSA Rouen, UNIROUEN, CNRS, COBRA (UMR 6014), Normandy University, Saint-Étienne-du-Rouvray, France
6GeHCO, University of Tours, Tours, France

Tóm tắt

Lacustrine sediments contain a wide range of proxies that enable paleoenvironmental reconstructions. For instance, charcoal can be used to document past fire regime changes. In order to analyse high-temporal- and spatial-resolution records, however, it is necessary to develop fast, low-cost and high-stratigraphic-resolution methods. We developed a new paleo-fire proxy by studying a lacustrine core from the Esterel Massif, SE France, an area affected by two recent fire events, in AD 1987 and 2003. For this purpose, we searched for charcoal deposited and preserved in the lake sediments by combining a number of complementary methods, including: classic macrocharcoal tallying, scanning spectrophotometry, scanning hyperspectral imaging and high pressure liquid chromatography analyses. Macrocharcoal quantification is efficient, but time-consuming, and only provides intermediate-resolution data (cm scale). Spectrophotometry, used classically to quantify colour, is very fast, provides high-resolution data (4 mm) and is non-destructive (core preservation). Hyperspectral data have the same advantages as spectrophotometry, but offer higher spatial resolution (64-µm pixel size) and higher spectral resolution (6 nm) for core logging applications. The main result of this research is based on hyperspectral analysis at very high stratigraphic resolution using the I-band index. This index usually measures reflectance values at [660, 670 nm] corresponding to the trough in red reflectance produced by Chlorophyll a and its diagenetic products. This [660, 670 nm] reflectance trough, however, is also affected by the presence of altered organic matter and decreases with altered organic matter such as charcoal particles. Charcoal effect on the reflectance of Chlorophyll a and its diagenetic products is identified on first derivative spectra by a characteristic pattern around 675 nm, which is also in agreement with the Chlorophyll a concentrations measured by high-pressure liquid chromatography and charcoal particles. The I-band index is hence suitable for detecting burned organic matter, by quantifying the dilution of the chlorophyll signal by the charcoal signal. Thus, this adaptation of the I-band index can be applied in fire reconstruction studies.

Tài liệu tham khảo

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