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Long-term effects of wheat production management practices on some carbon fractions of a semiarid Plinthustalfs

机译:小麦生产管理实践对Memiarid Plinthusthusthustalfs的一些碳分数的长期影响

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This study evaluated wheat production effects on carbon (C) fractions and soil organic C (SOC) molecular composition of a semiarid Plinthustalf in a trial established near Bethlehem. Treatments applied for 20 consecutive years included two straw management (unburned and burned), three tillage (no-tillage, ploughing and stubble mulch) and two weed control (chemical and mechanical) methods. Samples collected from 0-50mm depth of specific treatment combinations were analyzed for SOC, soil inorganic C (SIC), permanganate oxidizable C (POXC), cold (CWEC) and hot (HWEC) water extractable C, extractable humic substances (CEX), humic acids, fulvic acids (CFA) and SOC functional groups. Humification (HI) and polymerization (PI) indices and alkyl C/O-alkyl C ratios were calculated. No-tillage combinations demonstrated potential to reverse losses of soil C fractions in the 0-50mm layer. Increased POXC, CWEC, CEX and CFA revealed the labile nature of accumulated SOC in no-tillage, suggesting that SOC therein could be rapidly lost if no-tilled soils were again cultivated. Although the HI and PI were not always significant, their decrease in the no-tillage combinations suggest minimal decomposition, which is a benefit in Plinthustalfs with low storage capacity. Positive correlations between SIC and SOC fractions implied that an increase in SOC fractions protected SIC, resulting in its accumulation in no-tillage combinations. Functional groups seemed to mimic fractionated SOC fractions because O-alkyl C decreased with concomitant increase in alkyl, aromatic and carbonyl C. These responses highlighted that no-tillage combinations could be ideal to restore SOC quality in drought-prone agro-ecosystems dominated by sandy soils.
机译:该研究评估了在伯内仑附近建立的试验中的半干旱普斯塔尔F的碳(C)分数和土壤有机C(SoC)分子组合物的小麦生产作用。连续20年适用的治疗包括两个秸秆管理(未燃烧和烧伤),三个耕作(无耕作,耕种和腐烂的覆盖物)和两种杂草控制(化学和机械)方法。分析了从0-50mm的特异性处理组合中收集的样品,用于SoC,土壤无机C(SiC),高锰酸盐可氧化C(POXC),冷(CWEC)和热(HWEC)水可溶性C,可提取的腐殖质(CEX),腐殖酸,富含酸(CFA)和SoC官能团。计算湿度(HI)和聚合(PI)索引和烷基C / O-烷基C比率。无耕作组合证明了0-50mm层中土壤C馏分逆转损失的潜力。增加痘,CWEC,CEX和CFA揭示了累积SoC的无耕作的不稳定性,这表明如果再次耕种土壤耕种土壤,那么其中的SOC可能会迅速丢失。虽然HI和PI并不总是显着的,但它们在无耕作组合中的减少表明,最小的分解,这在储存能力低的PLINTHUSTALF中是一种益处。 SIC和SOC级分之间的正相关性暗示了SOC级分的增加保护SIC,导致其在无耕作组合中的积累。官能团似乎是模拟分级的SOC级分,因为O-烷基C随着烷基,芳族和羰基C的伴随增加而增加。这些反应突出显示,无耕作组合可能是恢复由桑迪主导的干旱易受农业生态系统中的SOC质量的理想选择土壤。

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