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. 2011 Dec 1;6(5):1032–1045. doi: 10.1038/ismej.2011.168

Table 1. Basic properties of soils used in this study.

  HZ YH QJ QY TY
Location N 30°10′ N 30°25′ N 25°24′ N 26°45′ N 28°25′
  E 120°05′ E 119°44′ E 103°48 E 111°52′ E 111°26′
pH (H2O)a 4.20 4.21 4.36 4.43 4.47
pH (KCl)b 3.29 3.34 3.66 3.87 3.89
Total N (g kg−1) 5.02 2.07 2.46 1.27 1.79
Total C (g kg−1) 54.9 22.7 22.0 12.7 17.9
SOC (g kg−1) 31.9 12.1 12.8 7.60 9.54
NH4+-N (mg kg−1) 39.2 9.45 22.1 11.5 12.9
NO3-N (mg kg−1) 31.3 13.2 203 2.77 2.87
CEC (cmol kg−1) 24.1 18.0 10.7 22.1 19.0
H2O % 28.8 29.5 24.0 22.7 27.4
           
Particle size (%)
 Sand 43.4 14.1 14.2 8.2 11.5
 Silt 41.2 45.0 32.7 63.9 68.3
 Clay 15.4 40.9 53.1 28.9 20.2

Abbreviations: CEC, cation exchange capacity; HZ, Hangzhou; SOC, soil organic carbon; TY, Taoyuan; QJ, Qujing; QY, Qiyang; YH, Yuhang.

a

pH (H2O) was determined with a soil to water ratio of 1:2.5.

b

pH (KCl) was determined with a soil to 1  KCl ratio of 1:2.5.