Skip to main content

Table 2 Spectral indices of DOM extracted from 59 soils of four soil types under two land-uses (natural land and cropped land) across China

From: Compositional and chemical characteristics of dissolved organic matter in various types of cropped and natural Chinese soils

Items

n

SUVA254

HIX

BIX

FI

All soils

59

1.49 ± 0.68

0.77 ± 0.10

0.79 ± 0.14

1.73 ± 0.15

Chernozem soils

16

2.03 ± 0.48a

0.92 ± 0.02a

0.60 ± 0.05b

1.60 ± 0.06b

 Natural

7

1.99 ± 0.32

0.91 ± 0.01

0.59 ± 0.05

1.63 ± 0.04

 Cropped

9

2.05 ± 0.60

0.92 ± 0.03

0.61 ± 0.04

1.57 ± 0.07

Cinnamon soils

14

1.52 ± 0.64ab

0.86 ± 0.03a

0.66 ± 0.06b

1.69 ± 0.06b

 Natural

5

1.24 ± 0.14

0.85 ± 0.03

0.70 ± 0.07

1.68 ± 0.06

 Cropped

9

1.67 ± 0.76

0.87 ± 0.03

0.64 ± 0.03

1.71 ± 0.04

Paddy soils

18

1.10 ± 0.54b

0.79 ± 0.05b

0.77 ± 0.11a

1.81 ± 0.14a

Red soils

11

1.29 ± 0.72b

0.75 ± 0.14b

0.88 ± 0.19a

1.88 ± 0.16a

 Natural

4

1.59 ± 0.74

0.70 ± 0.08

0.77 ± 0.08

1.91 ± 0.15

 Cropped

7

1.12 ± 0.71

0.78 ± 0.16

0.84 ± 0.16

1.83 ± 0.17

  1. The value was given by mean ± standard error. Different letters represent significant differences in DOM spectral indices between soil types
  2. n number of samples, HIX humification index, FI fluorescence index, BIX biological index