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Long-term fertilization and manuring effects on physically-separated soil organic matter pools under a wheat-wheat-maize cropping system in an arid region of China

机译:干旱地区小麦-小麦-玉米种植体系下长期分离土壤有机质库的施肥和肥效

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摘要

With increasing food demand worldwide, agriculture in semiarid and arid regions becomes increasingly important, though knowledge about organic matter (OM) conserving management systems is scarce. This study aimed at examining organic C (OC) and nitrogen (N) concentrations in various soil OM pools affected by 26-years application of chemical fertilizer and farmyard manure at an arid site of Gansu Province, China. Macro OM (>0.05 mm) was extracted by wet sieving and then separated into light macro OM (<1.8 g cm super(-3)) and heavy macro OM (>1.8 g cm super(-3)) sub-fractions; bulk soil was differentiated into free particulate OM (FPOM, <1.6 g cm super(-3)), occluded particulate OM (OPOM, 1.6-1.8 g cm super(-3)) and mineral-associated OM (>1.8 g cm super(-3)). OC and N concentrations of heavy macro OM and FPOM were slightly affected by long-term N fertilization alone and its combination with P and K, but their magnitudes of change had not significantly contributed to total soil OC and N concentrations. Farmyard manure increased light macro OC and N by 58 and 70%, heavy macro OC and N by 86 and 117%, free particulate OC and N by 29 and 55%, occluded particulate OC and N by 29 and 55%, and mineral-associated OC and N by 44 and 48%, respectively, compared to nil-manure. Mineral fertilization improved soil OM quality by decreasing C/N ratio in the light macro OM and FPOM fractions where farmyard manure was absent. Organic manure led to a decline of the C/N ratio in all physically-separated OM fractions possibly due to the increased input of processed organic materials. We found about two thirds of macro OM was actually located within 2-0.05 mm organo-mineral associations or/and aggregates. In conclusion, this study stresses the vital importance to apply organic manure to the wheat-corn production system characterized by straw removal and conventional tillage in the region.
机译:随着全球粮食需求的增长,尽管缺乏有关有机物(OM)保存管理系统的知识,半干旱和干旱地区的农业也变得越来越重要。这项研究的目的是研究在甘肃省干旱地区,受化肥和农家粪肥施用长达26年的各种土壤OM池中有机碳(OC)和氮(N)的浓度。通过湿法筛分提取大颗粒OM(> 0.05 mm),然后分离为轻大颗粒OM(<1.8 g cm super(-3))和重大颗粒OM(> 1.8 g cm super(-3))子级分;散装土壤分为游离颗粒OM(FPOM,<1.6 g cm super(-3)),封闭颗粒OM(OPOM,1.6-1.8 g cm super(-3))和与矿物相关的OM(> 1.8 g cm super(-3)) (-3))。单独施用长期氮肥及其与磷和钾的组合,对重肥大OM和FPOM的OC和N浓度影响较小,但其变化幅度并未显着影响土壤总OC和N浓度。农家肥使轻型宏大OC和N分别增加了58%和70%,重重宏大OC和N分别增加了86%和117%,游离微粒OC和N分别增加了29%和55%,闭塞的微粒OC和N分别增加了29%和55%以及矿物质与零肥相比,相关的OC和N分别减少了44%和48%。矿物肥料通过降低缺少农家肥的轻质有机肥和轻质有机肥中的碳氮比来改善土壤有机质。有机肥料导致所有物理上分离的OM馏分的C / N比降低,这可能是由于增加了加工有机材料的投入所致。我们发现大约三分之二的宏观OM实际上位于2-0.05毫米的有机-矿物组合或/和聚集体内。总之,这项研究强调了在该地区以秸秆除草和常规耕作为特征的小麦-玉米生产系统中应用有机肥料至关重要。

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