Knowledge Resource Center for Ecological Environment in Arid Area
DOI | 10.1029/2009JF001645 |
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
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ISSN | 0148-0227 |
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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