Vermeire, Marie-Liesse; Cornu, Sophie; Fekiacova, Zuzana; Detienne, Marie; Delvaux, Bruno; Cornélis, Jean-Thomas (2017): (Table 1) Major soil characteristics from a Sitka spruce (Picea sitchensis) forest near Cox Bay, on the west coast of Vancouver Island, British Columbia [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.881645, In supplement to: Vermeire, M-L et al. (2016): Rare earth elements dynamics along pedogenesis in a chronosequence of podzolic soils. Chemical Geology, 446, 163-174, https://doi.org/10.1016/j.chemgeo.2016.06.008
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Coverage:
Latitude: 49.600000 * Longitude: -125.520000
Minimum DEPTH, soil: 0.0350 m * Maximum DEPTH, soil: 1.5300 m
Event(s):
Parameter(s):
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
335 data points
Data
1 Profile ID | 2 Age [ka BP] | 3 Soil hori | 4 Depth top [m] | 5 Depth bot [m] | 6 Depth soil [m] | 7 Classification | 8 pH | 9 CEC [cmol/kg] | 10 Ca2+ [mmol/kg] | 11 K+ [mmol/kg] | 12 Mg2+ [mmol/kg] | 13 Na+ [mmol/kg] | 14 BS [%] | 15 Sand [%] | 16 Silt [%] | 17 Clay min [%] | 18 TOC [mg/kg] |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
P.M. (parental material) | 0.000 | C | 7.7 | 1.55 | 190 | 230 | 330 | 730 | 95.57 | 99.9 | 0.1 | 0.0 | 320 | ||||
P1 | 0.120 | BC1 | 0.000 | 0.350 | 0.1750 | Dystric Cambisol | 5.9 | 3.72 | 250 | 100 | 350 | 180 | 23.76 | 99.2 | 0.6 | 0.3 | 9120 |
P1 | 0.120 | BC2 | 0.350 | 0.600 | 0.4750 | Dystric Cambisol | 5.9 | 3.32 | 230 | 60 | 330 | 180 | 24.21 | 7790 | |||
P2 | 0.175 | BW | 0.030 | 0.440 | 0.2350 | Dystric Cambisol | 5.8 | 4.34 | 230 | 70 | 350 | 250 | 20.66 | 99.0 | 0.6 | 0.4 | 3330 |
P2 | 0.175 | BC | 0.440 | 0.750 | 0.5950 | Dystric Cambisol | 5.9 | 2.38 | 120 | 80 | 180 | 220 | 25.30 | 99.6 | 0.2 | 0.1 | 2550 |
P3 | 0.270 | E | 0.000 | 0.070 | 0.0350 | Albic Podzol | 4.6 | 6.04 | 480 | 50 | 560 | 110 | 19.94 | 90.8 | 6.1 | 3.1 | 12630 |
P3 | 0.270 | Bh | 0.070 | 0.230 | 0.1500 | Albic Podzol | 5.1 | 5.94 | 590 | 40 | 410 | 130 | 19.76 | 97.2 | 1.7 | 1.1 | 16170 |
P3 | 0.270 | BW | 0.230 | 0.570 | 0.4000 | Albic Podzol | 5.3 | 5.57 | 520 | 40 | 400 | 110 | 19.14 | 97.4 | 1.8 | 0.9 | 8180 |
P3 | 0.270 | BC | <0.570 | Albic Podzol | 5.4 | 5.71 | 390 | 100 | 220 | 110 | 14.53 | 98.2 | 1.1 | 0.7 | 6870 | ||
P4 | 0.330 | E | 0.000 | 0.100 | 0.0500 | Placic Podzol | 4.9 | 5.66 | 70 | 20 | 50 | 40 | 3.22 | 82.3 | 14.4 | 3.3 | 8480 |
P4 | 0.330 | Bh | 0.100 | 0.170 | 0.1350 | Placic Podzol | 5.5 | 15.72 | 220 | 40 | 100 | 60 | 2.67 | 88.0 | 8.7 | 3.2 | 16180 |
P4 | 0.330 | Bhs | 0.170 | 0.175 | 0.1725 | Placic Podzol | 15.18 | 130 | 40 | 70 | 60 | 1.96 | 90.0 | 6.8 | 3.2 | 22990 | |
P4 | 0.330 | Bs | 0.175 | 0.230 | 0.2025 | Placic Podzol | 5.3 | 5.88 | 40 | 30 | 10 | 30 | 1.80 | 94.9 | 4.2 | 0.9 | 4530 |
P4 | 0.330 | Bw | 0.230 | 0.630 | 0.4300 | Placic Podzol | 5.4 | 4.31 | 30 | 30 | 10 | 40 | 2.58 | 96.1 | 2.4 | 1.5 | 2670 |
P4 | 0.330 | BC1 | 0.630 | 1.130 | 0.8800 | Placic Podzol | 5.3 | 3.15 | 20 | 60 | 0 | 20 | 3.21 | 1260 | |||
P4 | 0.330 | BC2 | 1.130 | 1.930 | 1.5300 | Placic Podzol | 5.3 | 2.72 | 20 | 10 | 0 | 20 | 2.33 | 1480 | |||
P4 | 0.330 | BC3 | <1.930 | Placic Podzol | 5.2 | 2.71 | 20 | 40 | 0 | 20 | 3.14 | 98.2 | 1.8 | 0.0 | 1030 | ||
P5 | 0.530 | E | 0.000 | 0.080 | 0.0400 | Placic Podzol | 4.5 | 5.31 | 220 | 40 | 150 | 60 | 8.63 | 31900 | |||
P5 | 0.530 | Bh | 0.080 | 0.095 | 0.0875 | Placic Podzol | 4.5 | 15.32 | 330 | 30 | 160 | 60 | 3.78 | 31180 | |||
P5 | 0.530 | Bhs | 0.095 | 0.100 | 0.0975 | Placic Podzol | 4.5 | 23.35 | 240 | 80 | 130 | 70 | 2.23 | 40480 | |||
P5 | 0.530 | Bs | 0.100 | 0.150 | 0.1250 | Placic Podzol | 4.8 | 9.85 | 40 | 40 | 30 | 40 | 1.60 | 11600 | |||
P5 | 0.530 | Bw | 0.150 | 0.400 | 0.2750 | Placic Podzol | 5.0 | 3.53 | 20 | 10 | 0 | 30 | 2.02 | 1170 | |||
P5 | 0.530 | BC | 0.400 | 0.600 | 0.5000 | Placic Podzol | 5.1 | 2.45 | 30 | 20 | 0 | 10 | 2.56 | 640 |