@article{fdi:010042774,
  title = {{C}an chromite weathering be a source of {C}r in soils ?},
  author = {{G}arnier, {J}. and {Q}uantin, {C}. and {G}uimaraes, {E}. and {B}ecquer, {T}hierry},
  editor = {},
  language = {{ENG}},
  abstract = {{A}t {N}iquelandia, {C}r extracted from the soil (5,000-9,300 mg.kg(-1)) is likely the result of the {C}r-bearing {F}e-oxides compared to the {C}r-spinels, showing that low {C}r-containing minerals present in the dunite (enstatite, olivine and clay minerals) have been completely dissolved. {T}he chromites, accumulated inside soil profiles, have undergone chemical weathering, leading to a {C}r enrichment during soil genesis. {T}races of dissolution inside the soil chromites suggest that,they can be slowly weathered. {I}n this case chromites could represent a diffuse source of available {C}r({III}) within the soil profiles.},
  keywords = {},
  booktitle = {},
  journal = {{M}ineralogical {M}agazine},
  volume = {72},
  numero = {1},
  pages = {49--53},
  ISSN = {0026-461{X}},
  year = {2008},
  DOI = {10.1180/minmag.2008.072.1.49},
  URL = {https://www.documentation.ird.fr/hor/fdi:010042774},
}