有机肥和化肥施用对地方油菜和叶茎蔬菜生长、产量及土壤生化特性的影响

Takamitsu Kai, M. Tamaki
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引用次数: 4

摘要

在日本,Norabona通常在使用化肥和合成化学农药的管理系统下种植。然而,这些肥料和农药的持续使用破坏了土壤环境,减少了土壤微生物的数量。有机肥和化肥施用对土壤生物化学及紫花蓟马生长和产量的影响研究较少。本研究在2019年9月至2020年5月的norabona生长季,研究了有机肥和化肥施用对这些因子的影响。在栽培前期(3月),有机肥处理的叶长、茎高和茎宽显著高于化肥处理。然而,在随后的几个月里,这些生长参数和其他任何参数在处理之间没有显著差异。收获后有机肥处理土壤全氮、全磷含量显著高于栽培前和化肥处理后。此外,有机肥处理的土壤TC和体积含水量显著高于化肥处理。有机肥处理土壤中较高的TC、TN和C/N似乎增加了细菌生物量,通过N、P循环活性促进养分循环,形成土壤微生物活性丰富的土壤环境。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Effect of Organic and Chemical Fertilizer Application on Growth, Yield, and Soil Biochemical Properties of Landrace Brassica napus L. Leaf-and-Stem Vegetable and Landrace (Norabona)
Norabona is generally cultivated in Japan under management systems that use chemical fertilizers and synthetic chemical pesticides. However, the continuous use of these fertilizers and pesticides damages the soil environment and reduces the number of soil microorganisms. There has been little research investigating the effect of organic and chemical fertilizer applications on soil biochemistry and the growth and yield of norabona. In this study, we investigated the effect of organic and chemical fertilizer application on these factors during the norabona growing season from September 2019 to May 2020. Leaf length, shoot height, and shoot width were significantly higher under organic fertilizer management in the early stage of cultivation (in March) than under chemical fertilizer management. However, there was no significant difference between treatments for these growth parameters in later months, nor for any other parameters. Soil TN, and TP contents were significantly higher in the organic fertilizer treatment after harvest than prior to cultivation or after the chemical fertilizer treatment. In addition, soil TC, and volumetric water content were significantly higher in the organic fertilizer treatment than in chemical fertilizer treatment. The higher TC, TN, and C/N ratio in organic fertilizer treated soil appeared to increase the bacterial biomass, leading to enhanced nutrient circulation via N and P circulation activity, producing a rich soil environment with active soil microorganisms.
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