Health & Environmental Research Online (HERO)


Print Feedback Export to File
7666339 
Journal Article 
Moisture Effect on Soil Humus Characteristics in a Laboratory Incubation Experiment 
Li, C; Gao, S; Zhang, J; Zhao, L; Wang, L; , 
2016 
1 
Soil and Water Research
ISSN: 1801-5395 
CZECH ACADEMY AGRICULTURAL SCIENCES 
PRAGUE 
37-43 
WOS:000370912200005 
A 180-day laboratory incubation experiment (30 degrees C) was conducted to investigate the quantitative and qualitative characteristics of humic fractions in a Mollisol at different moisture conditions. The soil moisture contents were 30, 60, and 250% field water-holding capacity (WHC), which represented the low, middle, and high moisture levels, respectively. The results showed that the carbon contents of the total soil and corresponding humic fractions generally decreased with increasing soil moisture. A significant difference was observed between the 250% WHC and the two other moisture levels. By contrast, the carbon content of the water soluble fraction significantly increased with increasing soil moisture levels. The solid-state C-13 nuclear magnetic resonance (NMR) spectra showed that the alkyl C/O-alkyl C, aliphatic C/aromatic C, and hydrophobic C/hydrophilic C ratios were in the order of 250% WHC > 30% WHC approximate to 60% WHC, 30% WHC approximate to 60% WHC > 250% WHC and 250% WHC > 60% WHC approximate to 30% WHC for humic acid, and 250% WHC > 30% WHC approximate to 60% WHC, 60% WHC approximate to 250 % WHC > 30% WHC and 30% WHC approximate to 250% WHC > 60% WHC for humin, respectively. These results indicated that a high moisture level was unfavourable for the carbon accumulation of the total soil and humic fractions, whereas it was favourable for the accumulation of water soluble carbon. Although soil moisture levels had a distinct effect on the chemical composition of humic acid and humin, the decomposition degree of the two humic substances components, as indicated by the alkyl C/O-alkyl C ratio, were both higher at a high moisture level than at a low moisture level. Therefore, the lower soil organic carbon content at a high moisture level than at a low moisture level can be ascribed to the higher water soluble carbon content and larger decomposition degree of humic acid and humin in the former. Our results are important for understanding the behaviour and mechanisms of humic substances at specific soil moisture conditions.