Using scattered hyperspectral imagery data to map the soil properties of a region

European Journal of Soil Science - Tập 63 Số 1 - Trang 110-119 - 2012
Philippe Lagacherie1, Jean‐Stéphane Bailly2,1,3, Pascal Monestiez4, Cécile Gomez1
1UMR LISAH - Laboratoire d'étude des Interactions Sol - Agrosystème - Hydrosystème (Bâtiment 24 2 place Pierre Viala 34060 Montpellier cedex 1 France - France)
2AgroParisTech (22 place de l'Agronomie CS 20040 91123 Palaiseau cedex - France)
3UMR TETIS - Territoires, Environnement, Télédétection et Information Spatiale (Maison de la télédétection - 500 rue Jean-François Breton - 34093 Montpellier Cedex 5 - France)
4BioSP - Biostatistique et Processus Spatiaux (Site Agroparc Domaine St Paul 84914 Avignon cedex 9 - France)

Tóm tắt

Airborne hyperspectral imagery has been recently proved to be a successful technique for predicting soil properties of the bare soil surfaces that are usually scattered in the landscape. This new soil covariate could much improve the digital soil mapping (DSM) of soil properties over larger areas. To illustrate this, we experimented with digital soil mapping in a 24.6‐km2area located in the vineyard plain of Languedoc. As input data, we used 200 points with clay content measurements and 192 bare soil fields representing 3.5% of the total area in which the clay contents of the soil surface were successfully mapped at 5‐m resolution by hyperspectral remote sensing. The clay contents were estimated from CR2206, a spectrometric indicator that quantifies specific absorption features of clay at 2206 nm. We demonstrated by cross‐validation that the co‐kriging procedure based on our co‐regionalization model provided accurate error estimates at the clay measurement sites. Then, we applied a block co‐kriging model to map the mean clay content at increasing resolutions (50 , 100, 250 and 500 m). The results showed the following: (i) using hyperspectral data significantly increased the accuracy of the mean clay content estimations; (ii) a block co‐kriging procedure with reliable estimates of error variance can be used to estimate mean clay contents over larger areas and at coarser resolutions with acceptable and predictable errors and (iii) various maps can be produced that represent different compromises between prediction accuracy and spatial resolution.

Từ khóa


Tài liệu tham khảo

10.1007/978-90-481-8859-8_2

10.1016/j.jag.2010.06.009

Beisl U.2001.Correction of bidirectional effects in imaging spectrometer data. PhD thesis Remote Sensing Series 37 RSL University of Zurich Zurich.

10.1016/S0065-2113(07)00008-9

10.1111/j.1365-2389.2011.01364.x

10.1016/S0034-4257(02)00060-3

10.1029/JB089iB07p06329

Cressie N.A.C., 1991, Statistics for Spatial Data

10.1016/j.ecoinf.2007.06.002

10.1016/j.geoderma.2008.09.016

Goovaerts P., 1997, Geostatistics for Natural Resources Evaluation, 10.1093/oso/9780195115383.001.0001

10.1016/S0016-7061(01)00067-2

10.1016/j.geoderma.2009.06.003

ISSS ISRIC FAO1998.World Reference Base for Soil Resources.World Soil Resources Report 84 FAO Rome.

Jenny H., 1941, Factors of Soil Formation, a System of Quantitative Pedology.

Jolivet C., 2006, Le réseau de mesures de la qualité des sols de France (RMQS), Etat d’avancement et premiers résultats., Etude et Gestion des Sols, 13, 149

10.1007/978-1-4020-8592-5_1

10.1016/j.rse.2007.06.014

10.1111/j.1365-2389.1994.tb00512.x

Matheron G., 1971, The Theory of Regionalised Variables and its Applications.

10.1016/S0016-7061(03)00223-4

10.1016/0016-7061(95)00007-B

10.1016/j.geoderma.2011.04.019

10.1016/0098-3004(96)00016-7

Richter R.&Schläpfer D.A.2000.A unified approach to parametric geocoding and atmospheric/topographic correction for wide FOV airborne imagery. Part 2: atmospheric correction.InProceedings 2nd International EARSeL Workshop on Imaging Spectroscopy Enschede 11–13 July 2000.

10.1126/science.1175084

10.1016/j.geomorph.2010.11.008

10.1016/j.geoderma.2006.03.050

10.2307/2532147

10.1016/j.geoderma.2009.11.032

10.1016/j.geoderma.2005.03.007

10.1007/978-90-481-8859-8

10.1007/978-3-662-03098-1