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Influence of conservation tillage on soil physicochemical properties in a tropical rainfed agricultural system of northeast India

机译:保护性耕作对印度东北部热带雨养农业系统中土壤理化特性的影响

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In agricultural systems, especially where the soils are highly erodible, there is always a need for a better synchronization of nutrient release and nutrient demand by the growing crops. Management practices, such as conservation tillage could serve as a viable alternative to the mounting crisis and could enhance SOM besides other physicochemical properties. A field study was conducted in the rainfed agricultural system of northeast India with variedly tilled implements (indigenous spade, Country Plough, Bose Plough and Mouldboard Plough) from 2006 to 2007 to study the effect of these implements on the soils' physiochemical properties during different growth phases of Oryza sativa in a rainfed valley agricultural system. A marked change in the bulk density values was observed up to 15-20cm depth only in the Mouldboard Plough tilled plots. Over all, bulk density showed a significant positive correlation only with total N (r =0.263, n =30, p <0.01). In all the study sites, a significant variation (p <0.01) of soil moisture content with respect to time duration, tillage type and soil depth was observed. In Sites I and II, pH showed significant variation (p <0.01) with time duration (F =6.6, 3.0, d.f.=5) and tillage type (F =73.0, 48.5, d.f.=4), respectively. Amongst all the study sites, Site II had comparatively higher value for soil organic matter followed by Sites III and I. Total N too showed variation with duration, tillage type and soil depth with ANOVA for the factors showing significant variation between and amongst them across the sites. Available P of the soil too varied remarkably along the crop's growing duration, its depth and upon the tillage method followed. Thus, our results suggest that conservation tillage, especially no-tillage, could serve as an effective tool with respect to increasing soil C and N sequestration in the subtropical agroecosystem of northeast India.
机译:在农业系统中,特别是在土壤高度易腐蚀的地方,始终需要使生长中的作物更好地同步释放养分。保护性耕作之类的管理实践可以替代日益严峻的危机,并且除了其他理化特性外,还可以提高SOM。 2006年至2007年,在印度东北部的雨养农业系统中进行了田间调查,研究使用了不同耕作的农具(土铲,乡村犁,Bose犁和Mouldboard Plough),研究了这些农具对不同生长过程中土壤理化性质的影响。雨养谷农业系统中水稻的两个阶段。仅在Mouldboard Plow耕作地块中,直到15-20cm的深度才观察到堆密度值的显着变化。总体而言,堆密度仅与总氮呈显着正相关(r = 0.263,n = 30,p <0.01)。在所有研究地点,观察到的土壤水分含量随时间,耕作类型和土壤深度的变化显着(p <0.01)。在站点I和站点II中,pH随持续时间(F = 6.6,3.0,d.f. = 5)和耕作类型(F = 73.0,48.5,d.f. = 4)表现出显着变化(p <0.01)。在所有研究地点中,地点II具有较高的土壤有机质价值,其次是地点III和I。总氮也显示了随时间,耕作类型和土壤深度的变化,而方差分析表明要素之间的显着变化。网站。土壤的有效磷含量随作物的生长历程,深度和耕作方法的不同而显着变化。因此,我们的结果表明,保护性耕作(尤其是免耕)可以作为增加印度东北亚热带农业生态系统中土壤碳和氮固存的有效工具。

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