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OxSR: Soil Iron Oxides via Diffuse Reflectance
Calculate the ratio of iron oxides, hematite and goethite, in soil using the diffuse reflectance technique. The Kubelka-Munk theory, second derivative analysis, and spectral region amplitudes related to hematite and goethite content are used for quantification (Torrent, J., & Barron, V. (2008) <doi:10.2136/sssabookser5.5.c13>). Additionally, the package calculates soil color in the visible spectrum using Munsell and RGB color spaces, based on color theory (Viscarra et al. (2006) <doi:10.1016/j.geoderma.2005.07.017>).
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Package details |
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| Author | Gustavo Frosi [aut, cre] (<https://orcid.org/0000-0002-0324-636X>), Vidal Barrón [aut] (<https://orcid.org/0000-0003-1484-1655>), Alberto Inda [aut] (<https://orcid.org/0000-0001-5252-0313>), Kayn Bastiani [aut] (<https://orcid.org/0000-0003-2692-1695>) |
| Maintainer | Gustavo Frosi <gustavofrosi@hotmail.com> |
| License | AGPL (>= 3) |
| Version | 1.0.1 |
| URL | https://github.com/FGu5tav0/OxSR/ https://fgu5tav0.github.io/OxSR/ |
| Package repository | View on CRAN |
| Installation |
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