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Effect of Long-term Cultivation on Physical Properties of a Sandy Soil in Sokoto, Northwestern Nigeria

机译:长期耕作对尼日利亚西北部索科托市沙质土壤物理性质的影响

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The experiment was carried out in peasant (local) farmers’ farms in Usmanu Danfodiyo University Sokoto to investigate the effect of long-term cultivation (involving organic fertilization) on physical properties of a sandy soil in Sokoto, Northwestern Nigeria. The experiment consisted of two treatments (cultivated and uncultivated lands) which were replicated 5 times. Measurement of Physical (texture, bulk density: Bd, total porosity: TP, and gravimetric moisture content: ?m) properties of the soil were made at 0-15 cm and 15-30 cm soil depths. Data obtained was analyzed using two-sample t-test. The results revealed that, long-term farmers cultivation practices has no significant (p> 0.05) effect on physical properties of the soil, except ?m, sand and silt contents. However, long-term continuous cultivation slightly deteriorated physical quality of the soil (at 0-15 cm soil depth), which is reflected by increased Bd, reduced TP and ?m contents of the soil. The study further revealed that, cultivation encourages redistribution of silt within measured depths. Cultivated soil had highest silt (103.40 g/kg) and lowest sand (876.60 g/kg) at the 0-15 cm soil depth compared to the uncultivated soil, while a reverse trend was observed at the 15-30 cm soil depth. From the results, it can be concluded that, the farmers’ long-term cultivation practice is still normal soil tillage that is capable of maintaining the soil’s physical properties for sustainable agricultural crop production over longer (20-25 years) period of cultivation.
机译:该实验是在Usmanu Danfodiyo大学Sokoto的农民(当地)农民农场中进行的,目的是调查长期耕作(涉及有机肥)对尼日利亚西北部Sokoto沙质土壤物理特性的影响。该实验由两次处理(耕地和未耕地)组成,重复5次。在0-15厘米和15-30厘米土壤深度下测量土壤的物理(质地,堆积密度:Bd,总孔隙度:TP和重量水分含量:?m)。使用两个样本的t检验分析获得的数据。结果表明,农民的长期耕作方式对土壤物理性质的影响不大(p> 0.05),除了?m,沙和粉沙含量。但是,长期连续耕作会使土壤的物理质量略有下降(在土壤深度为0-15厘米处),这可以通过增加Bd,降低TP和土壤中的mm含量来反映。研究进一步表明,耕种促进了淤泥在测量深度内的重新分布。与未耕种土壤相比,耕作土壤在0-15厘米土壤深度下的淤泥含量最高(103.40 g / kg),而沙土含量最低(876.60 g / kg),而在15-30 cm土层土壤上却观察到相反的趋势。从结果可以得出结论,农民的长期耕作方式仍是正常的土壤耕作,能够在更长的耕种时间(20-25年)内维持土壤的物理特性,以实现可持续的农业作物生产。

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