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>).
| Version: | 1.0.1 | 
| Depends: | R (≥ 4.1.0) | 
| Imports: | colorSpec, dplyr, ggplot2, grDevices, janitor, munsellinterpol, rlang, stats | 
| Suggests: | spelling, testthat (≥ 3.0.0) | 
| Published: | 2025-03-18 | 
| DOI: | 10.32614/CRAN.package.OxSR | 
| Author: | Gustavo Frosi  [aut, cre],
  Vidal Barrón  [aut],
  Alberto Inda  [aut],
  Kayn Bastiani  [aut] | 
| Maintainer: | Gustavo Frosi  <gustavofrosi at hotmail.com> | 
| BugReports: | https://github.com/FGu5tav0/OxSR/issues | 
| License: | AGPL (≥ 3) | 
| URL: | https://github.com/FGu5tav0/OxSR/,
https://fgu5tav0.github.io/OxSR/ | 
| NeedsCompilation: | no | 
| Language: | en-US | 
| Materials: | README, NEWS | 
| CRAN checks: | OxSR results | 
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