Sample typea | Fe2O3 (%) | MnO (ppm) | Co (ppm) | Ni (ppm) | Cr (ppm) | MgO (%) | Method, Reference |
---|---|---|---|---|---|---|---|
Serpentine soils (30) | 14.0–52.1 | 2000–6350 | 70–406 | 1660–13,920 | 1000–12,380 | 2.5–26.4 | XRF, This study (Additional file 1: Table S3) |
Soils (6) | 10.2–16.0 b | 1450–2600 c | 152–325 | 3240–7220 | 1400–3640 | 3.8–15.6 d | ICP-ES [31] |
Soils (8) |  < 0.2–6.8 b | 11–32 e | 18–150 (339) f | 24–230 (933, 1047, 2602, 6400)f | 25–658 (896, 1014, 1670)f | 2.1–31.2 g | AAS (Mg, Mn) and ICP-ES (Co, Cr, Fe, Ni) [65] |
Fluvial sediments (NR) | 5.6–6.8 b | 560–920 c | 34–70 |  > 100 | – | – | AAS [32] |
Serpentinized peridotite rocks (19) | 7.6–13.5 | 488–2340 c | 91–198 | 1759–10,752 | 1870–3480 | 24.6–35.6 | Bulk XRF, This study |
Peridotite and ultramafic rocks (NR) | – | – | – | 1993–2380 | 1931–2471 | 34–45 | NR [1] |
Diabase and basalt rocks (23) | 8.9–15.1 | 130–250 | 23–37 | 15–106 | 30–368 | 5.0–8.1 | XRF (majors) and LA-ICP-MS (traces) [2] |