Research Article

Lead and Chromium Immobilization Process Subjected to Different Freeze-Thaw Treatments in Soils of the Northeastern Qinghai-Tibet Plateau

Table 4

Pseudo-first-order and Weber–Morris parameters of Cr in soils under different freeze-thaw conditions.

Site areaFTCsCr (pseudo-first-order kinetics)Cr (Weber–Morris)
kCk

S-1F0 + W0%11.77 ± 0.350.06 ± 0.230.02
F15 + W60%17.21 ± 1.1012.19 ± 3.920.5912.34692 ± 0.870422.87 ± 0.570.86
F15 + W100%12.75 ± 0.4412.71 ± 2.270.7910.08 ± 0.781.41 ± 0.520.64

S-2F0 + W0%25.64 ± 0.5120.82 ± 3.080.7623.58 ± 1.300.97 ± 0.860.24
F15 + W60%24.39 ± 3.45−5.21 ± 2.280.56
F15 + W100%18.26 ± 1.81−3.35 ± 1.190.66

S-3F0 + W0%37.63 ± 1.8415.42 ± 4.330.6732.54 ± 4.102.32 ± 2.710.15
F15 + W60%50.45 ± 3.937.16 ± 2.410.7721730.47 ± 7.1610.28 ± 4.730.54
F15 + W100%55.03 ± 2.9812.31 ± 3.350.6705640.54 ± 3.148.33 ± 2.070.80

S-4F0 + W0%24.80 ± 3.2610.75 ± 6.740.33883
F15 + W60%28.20 ± 1.5259.07 ± 220.480.00127.34 ± 2.230.68 ± 1.470.05
F15 + W100%27.50 ± 1.5535.73 ± 32.360.01720.78 ± 1.4726.30 ± 2.230.06

S-5F0 + W0%25.21 ± 1.603.36 ± 0.820.9100412.08 ± 3.985.72 ± 2.630.54
F15 + W60%32.00 ± 1.9611.48 ± 3.450.6606123.50 ± 2.864.69 ± 1.890.60
F15 + W100%36.29 ± 1.9118.04 ± 6.110.4222629.72 ± 1.654.10 ± 1.090.77

S-6F0 + W0%35.72 ± 2.9211.36 ± 4.520.4821424.06 ± 1.187.06 ± 0.780.95311
F15 + W60%40.61 ± 1.5622.07 ± 6.640.3531737.35 ± 2.461.68 ± 1.620.21163
F15 + W100%37.18 ± 1.1715.77 ± 2.890.7770830.81 ± 2.163.52 ± 1.420.60374

Note. “—” means that these data could not be fitted using the pseudo-first-order and Weber–Morris models. F0 and F15 refer to the number of freeze-thaw cycles (0 and 15 cycles), and W0%, W60%, and W100% refer to water ratio of field capacity (0%, 60%, and 100% water ratio).