Skip to main content
. 2012 Oct 10;7(10):e45153. doi: 10.1371/journal.pone.0045153

Table 1. Soil physical properties in the experimental field.

Depth (cm) Particle size distribution (%) Bulk density g cm−3 SLLLa SDULb SSKSc cm d−1 SSATd Organic C (%) pH
Clay Silt Sand
0–15 18 50 31 1.15 0.09 0.28 1.42 0.30 1.8 6.5
15–30 24 49 26 1.25 0.09 0.28 1.43 0.30 1.5 6.6
30–45 23 52 24 1.35 0.09 0.28 2.76 0.32 1.3 7.0
Swift Current 45–60 25 33 41 1.4.0 0.10 0.27 4.32 0.34 0.9 7.7
60–90 32 28 40 1.45 0.10 0.27 5.61 0.34 0.5 7.8
90–120 33 26 41 1.55 0.10 0.25 3.04 0.34 0.3 8.1
120–150 33 28 40 1.65 0.10 0.25 3.04 0.34 0.1 8.5
0–15 60 29 11 1.30 0.11 0.37 7.40 0.59 2.9 7.0
15–45 60 28 12 1.40 0.11 0.37 7.68 0.57 1.0 7.3
Saskatoon 45–80 60 28 12 1.50 0.11 0.36 5.08 0.53 0.3 7.5
80–100 60 37 3 1.50 0.11 0.36 1.38 0.53 0.3 8.0
0–19 50 40 10 1.20 0.20 0.45 0.34 0.55 4.5 6.8
Melfort 19–58 49 44 7 1.30 0.20 0.46 0.29 0.51 1.3 7.0
58–100 52 45 3 1.30 0.20 0.46 0.25 0.51 0.5 8.0
a

Lower limit of plant extractable soil water (cm3 cm−3).

b

Drained upper limit (cm3 cm−3).

c

Saturated hydraulic conductivity cm d−1.

d

Saturated upper limit (cm3 cm−3).