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: |
1.0.0 |
Depends: |
R (≥ 4.1.0) |
Imports: |
colorSpec, dplyr, ggplot2, grDevices, janitor, munsellinterpol, rlang, stats |
Suggests: |
spelling, testthat (≥ 3.0.0) |
Published: |
2025-03-11 |
DOI: |
10.32614/CRAN.package.OxSR |
Author: |
Frosi Gustavo
[aut, cre],
BarrĂ³n Vidal
[ctb],
Inda, Alberto
[ctb],
Bastiani, Kayn
[ctb] |
Maintainer: |
Frosi Gustavo <gustavofrosi at hotmail.com> |
BugReports: |
https://github.com/FGu5tav0/OxSR/issues |
License: |
AGPL (≥ 3) |
URL: |
https://github.com/FGu5tav0/OxSR |
NeedsCompilation: |
no |
Language: |
en-US |
Materials: |
README NEWS |
CRAN checks: |
OxSR results |
Documentation:
Downloads:
Linking:
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