Arid
DOI10.1029/2009JF001645
Mapping iron oxides and the color of Australian soil using visible-near-infrared reflectance spectra
Rossel, R. A. Viscarra1; Bui, E. N.1; de Caritat, P.2; McKenzie, N. J.1
通讯作者Rossel, R. A. Viscarra
来源期刊JOURNAL OF GEOPHYSICAL RESEARCH-EARTH SURFACE
ISSN0148-0227
出版年2010
卷号115
英文摘要

Iron (Fe) oxide mineralogy in most Australian soils is poorly characterized, even though Fe oxides play an important role in soil function. Fe oxides reflect the conditions of pH, redox potential, moisture, and temperature in the soil environment. The strong pigmenting effect of Fe oxides gives most soils their color, which is largely a reflection of the soil’s Fe mineralogy. Visible-near-infrared (vis-NIR) spectroscopy can be used to identify and measure the abundance of certain Fe oxides in soil, and the visible range can be used to derive tristimuli soil color information. The aims of this paper are (1) to measure the abundance of hematite and goethite in Australian soils from their vis-NIR spectra, (2) to compare these results to measurements of soil color, and (3) to describe the spatial variability of hematite, goethite, and soil color and map their distribution across Australia. We measured the spectra of 4606 surface soil samples from across Australia using a vis-NIR spectrometer with a wavelength range of 350-2500 nm. We determined the Fe oxide abundance for each sample using the diagnostic absorption features of hematite (near 880 nm) and goethite (near 920 nm) and derived a normalized iron oxide difference index (NIODI) to better discriminate between them. The NIODI was generalized across Australia with its spatial uncertainty using sequential indicator simulation, which resulted in a map of the probability of the occurrence of hematite and goethite. We also derived soil RGB color from the spectra and mapped its distribution and uncertainty across the country using sequential Gaussian simulations. The simulated RGB color values were made into a composite true color image and were also converted to Munsell hue, value, and chroma. These color maps were compared to the map of the NIODI, and both were used to interpret our results. The work presented here was validated by randomly splitting the data into training and test data sets, as well as by comparing our results to existing studies on the distribution of Fe oxides in Australian soils.


类型Article
语种英语
国家Australia
收录类别SCI-E
WOS记录号WOS:000285464300001
WOS关键词DUNE SANDS ; WESTERN-AUSTRALIA ; NORTH QUEENSLAND ; MAGHEMITE ; LATERITE ; SPECTROSCOPY ; REGOLITH ; DESERT ; REGION ; COBAR
WOS类目Geosciences, Multidisciplinary
WOS研究方向Geology
来源机构Commonwealth Scientific and Industrial Research Organisation
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/165256
作者单位1.CSIRO Land & Water, Canberra, ACT 2601, Australia;
2.Geosci Australia, Canberra, ACT 2601, Australia
推荐引用方式
GB/T 7714
Rossel, R. A. Viscarra,Bui, E. N.,de Caritat, P.,et al. Mapping iron oxides and the color of Australian soil using visible-near-infrared reflectance spectra[J]. Commonwealth Scientific and Industrial Research Organisation,2010,115.
APA Rossel, R. A. Viscarra,Bui, E. N.,de Caritat, P.,&McKenzie, N. J..(2010).Mapping iron oxides and the color of Australian soil using visible-near-infrared reflectance spectra.JOURNAL OF GEOPHYSICAL RESEARCH-EARTH SURFACE,115.
MLA Rossel, R. A. Viscarra,et al."Mapping iron oxides and the color of Australian soil using visible-near-infrared reflectance spectra".JOURNAL OF GEOPHYSICAL RESEARCH-EARTH SURFACE 115(2010).
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