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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>).

Versions across snapshots

VersionRepositoryFileSize
1.0.1 rolling linux/jammy R-4.5 OxSR_1.0.1.tar.gz 1.2 MiB
1.0.1 rolling linux/noble R-4.5 OxSR_1.0.1.tar.gz 1.2 MiB
1.0.1 rolling source/ R- OxSR_1.0.1.tar.gz 1.0 MiB
1.0.1 latest linux/jammy R-4.5 OxSR_1.0.1.tar.gz 1.2 MiB
1.0.1 latest linux/noble R-4.5 OxSR_1.0.1.tar.gz 1.2 MiB
1.0.1 latest source/ R- OxSR_1.0.1.tar.gz 1.0 MiB
1.0.1 2026-04-26 source/ R- OxSR_1.0.1.tar.gz 1.0 MiB
1.0.1 2026-04-23 source/ R- OxSR_1.0.1.tar.gz 1.0 MiB
1.0.1 2026-04-09 windows/windows R-4.5 OxSR_1.0.1.zip 1.2 MiB
1.0.1 2025-04-20 source/ R- OxSR_1.0.1.tar.gz 1.0 MiB

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