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首页> 外文期刊>Communications in Soil Science and Plant Analysis >Stabilization of Functional Soil Organic Matter Fractions in Response to Long-Term Fertilization in Tropical Rice-Rice Cropping System
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Stabilization of Functional Soil Organic Matter Fractions in Response to Long-Term Fertilization in Tropical Rice-Rice Cropping System

机译:热带稻米种植体系中长期施肥函数土壤有机质级分的稳定性

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Soil organic matter (SOM) and its fractions play an important role in many soil chemical, physical, and biological properties. We studied functional groups of SOM fraction using a physical and chemical fractionation scheme in long-term application of a fertilization in a rice-rice system, which started in 2005 (sandy loam). Replicated soil samples of experimental plots of four different manure and fertilizer treatments and one unfertilized control were evaluated. The unprotected coarse particulate organic matter (POM) (cPOM), pure physical protected POM (iPOM), and the biochemically silt-sized fractions (NH-dSilt) contributed the major carbon storage fractions constituting 32.16-40.37%, 13.78-23.32%, and 14.44-28.66% of the total soil organic carbon (SOC) content, respectively. Combined application of organic manure like farmyard manure along with fertilizer improved the SOC content in all unprotected, physically protected, and chemically protected, silt and clay-associated physico-biochemically, clay-associated physicochemically protected and silt-associated biochemically protected fractions compared to control. Besides, the SOC increase expressed as SOC content per unit of total SOC for iPOM, cPOM, silt associated physicochemically and physico-biochemically protected fractions (H-mu Silt and NH-mu Silt) were the highest and as large as 70%, 60%, 45%, 38%, respectively. Our study indicates that long-term addition of manure with fertilizer for a long period of soil submergence under rice cultivation promoted the formation of more stabilized pools of C through physical and chemical protection mechanism.
机译:土壤有机物(SOM)及其级分在许多土壤化学,物理和生物学性质中起重要作用。我们使用物理和化学分馏方案研究了SOM级分的官能团,这些分馏方案在2005年(桑迪壤土)开始的水稻系统中的施肥中的长期应用。评估了四种不同肥料和肥料治疗的实验曲线和一个未受精对照的典型的实验图的土壤样本。未受保护的粗颗粒有机物(POM)(CPOM),纯物理受保护的POM(IPOM)和生物化学淤泥型分数(NH-DSILT)导致构成32.16-40.37%,13.78-23.32%的主要碳储存级分。占土壤总有机碳(SoC)含量的14.44-28.66%。有机肥料如农场粪便以及肥料的综合施用改善了所有未受保护,物理保护和化学保护,淤泥和粘土相关的物理生物化学,粘土相关的物理化学保护和淤泥相关的生物化保护的级分与对照相比。此外,表达为每单位SOC的SOC内容为IPOM,CPOM,淤泥相关的物理化学和物理化学和物理化学保护分数(H-MU SINT和NH-MU SILT)的SOC内容,最高,大约70%,60% %,45%,38%。我们的研究表明,在水稻栽培中长期加入肥料的肥料,促进了通过物理和化学保护机制形成更稳定的C池。

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