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. 2016 Oct 26;6:36105. doi: 10.1038/srep36105

Table 2. Soil organic carbon (SOC), inorganic carbon (SIC) stocks and the SIC:SOC ratio in typical croplands of North China.

Region The annual precipitation (mm) Soil types pH SOC stock (kg C m−2)
SIC stock (kg C m−2)
The SIC/SOC ratio
Reference
0–30 cm 30–100 cm 0–30 cm 30–100 cm 0–30 cm 0–100 cm
Yanqi (n = 9) 80 Brown Desert Soil 8.2 4.53 ± 0.52 4.38 ± 1.69 11.07 ± 1.45 31.3 ± 7.42 2.44 4.72 Wang et al.15
Urumqi (n = 5)* 299 Gray Desert Soil 8.1 4.25 ± 1.49 4.90 ± 0.65 2.03 ± 0.31 3.38 ± 0.77 0.48 0.59 Wang et al.8
Lanzhou (n = 33) 300 Loess Soil 8.9 2.46 ± 0.74 3.64 ± 1.44 6.24 ± 0.99 14.54 ± 2.39 2.54 3.41 Zhang et al.22
Yangling (n = 5)* 585 Manural Loess Soil 8.6 4.16 ± 0.93 5.18 ± 0.26 3.94 ± 0.27 5.06 ± 0.19 0.95 0.96 Wang et al.8
Zhengzhou (n = 5)* 641 Fluvo-aquic Soil 8.3 3.29 ± 0.59 3.31 ± 0.28 2.95 ± 0.08 5.19 ± 0.39 0.9 1.27 Wang et al.8
Zibo-Binzhou (n = 31) 600 Fluvo-aquic Soil 8.2 2.70 ± 0.64 3.03 ± 0.64 4.06 ± 0.81 12.83 ± 2.80 1.50 2.95 This study

*Each site collected in 2002 and 2009 with three replicates.