Tang Xiao-hong, Luo You-jin, Ren Zhen-jiang, Lü Jia-ke, Wei Chao-fu
College of Urban and Rural Construction, Dujiangyan Campus, Sichuan Agricultural University, Dujiangyan 611830, Sichuan, China.
Ying Yong Sheng Tai Xue Bao. 2011 Apr;22(4):985-91.
A 16-year field experiment was conducted in a ridge culture paddy field in the hilly region of Sichuan Basin, aimed to investigate the distribution characteristics of stable carbon isotope natural abundance (delta 13C) in soil humus fractions. The soil organic carbon (SOC) content in the paddy field under different cultivation modes ranked in the order of wide ridge culture > ridge culture > paddy and upland rotation. In soil humus substances (HS), humin (HU) was the main composition, occupying 21% - 30% of the total SOC. In the extracted soil carbon, humic acid (HA) dominated, occupying 17% - 21% of SOC and 38% - 65% of HS. The delta 13C value of SOC ranged from -27.9 per thousand to -25.6 per thousand, and the difference of the delta 13C value between 0-5 cm and 20-40 cm soil layers was about 1.9 per thousand. The delta 13C value of HA under different cultivation modes was 1 per thousand - 2 per thousand lower than that of SOC, and more approached to the delta 13C value of rapeseed and rice residues. As for fulvic acid (FA), its delta 13C value was about 2 per thousand and 4 per thousand higher than that of SOC and HA, respectively. The delta 13C value of HU in plough layer (0-20 cm) and plow layer (20-40 cm) ranged from -23.7 per thousand - -24.9 per thousand and -22.6 per thousand - -24.2 per thousand, respectively, reflecting the admixture of young and old HS. The delta 13C value in various organic carbon fractions was HU>FA>SOC>rapeseed and rice residues>HA. Long-term rice planting benefited the increase of SOC content, and cultivation mode played an important role in affecting the distribution patterns of soil humus delta 13C in plough layer and plow layer.
在四川盆地丘陵区的垄作稻田开展了为期16年的田间试验,旨在研究土壤腐殖质组分中稳定碳同位素自然丰度(δ13C)的分布特征。不同种植模式下稻田土壤有机碳(SOC)含量排序为宽垄作>垄作>水旱轮作。在土壤腐殖物质(HS)中,胡敏素(HU)为主要组成部分,占总SOC的21% - 30%。在提取的土壤碳中,腐殖酸(HA)占主导,占SOC的17% - 21%,占HS的38% - 65%。SOC的δ13C值范围为-27.9‰至-25.6‰,0 - 5 cm和20 - 40 cm土层间δ13C值差异约为1.9‰。不同种植模式下HA的δ13C值比SOC低1‰ - 2‰,且更接近油菜和水稻残茬的δ13C值。至于富里酸(FA),其δ13C值分别比SOC和HA高约2‰和4‰。耕层(0 - 20 cm)和犁底层(20 - 40 cm)中HU的δ13C值分别为-23.7‰至-24.9‰和-22.6‰至-24.2‰,反映了新老HS的混合。各有机碳组分的δ13C值为HU>FA>SOC>油菜和水稻残茬>HA。长期种植水稻有利于SOC含量增加,种植模式对耕层和犁底层土壤腐殖质δ13C的分布格局有重要影响。