Dinssa Berhanu, Elias Eyasu
Department of Plant Sciences, College of Agriculture, Ambo University, P.O Box. 19, Ambo, Ethiopia.
Centre of Environmental Sciences, College of Natural and Computational Sciences, Addis Ababa University, Ethiopia.
Heliyon. 2021 Oct 28;7(11):e08279. doi: 10.1016/j.heliyon.2021.e08279. eCollection 2021 Nov.
The study was carried out at Bako Tibe District, West Shewa zone, Oromiya Region of Ethiopia, to characterize and classify agriculturally important acidic soils. Four soil types were considered and six representative pedons were opened and a total of 27 disturbed and 20 core ring soil samples were collected from identified horizons of each pedon and analyzed. The field and laboratory data revealed the soils were clay and sandy clay in texture, slightly acidic to strongly acidic in reaction (pH 5.2-6.63). The organic carbon content of the soil ranges between moderate 21.4 g kg to high 30 g kg for surface soil while very low (4 g kg) to high (26 g kg) for sub-surface soils. Both the surface and subsurface soils were very low (1.7-2.2 g kg) in total N and deficient (5.99-7.85 mg kg) in available P content. The cation exchange capacity (CEC) was high for all surface and sub-surface percent base saturation was low (25 cmol kg) for Alisols and medium for Nitisols, Luvisols, and Cambisols (51 and 50 cmolkg). The soils were sufficient in available Fe, Mn, and Zn but deficient in B and Cu. Pedon-1 was Dystric, Rhodic Nitisols (Humic); pedon-2, Dystric Nitisols (Humic); pedon-3, Umbric Nitisols; pedon-4, Rhodic Alisols (Hyperdystric); pedon-5, Rhodic Luvisols (Hypereutric); pedon-6, Leptic Cambisols (Humic). Soil characterization is helpful to use the land according to its capability and limitations. pedons 2 and 4 were categorized under LCC IIs. pedons 1, 3, and 5 were grouped within LCC IIIes while Pedon 6 was grouped under LCC IVes. All the soil profiles studied can be used for crop production with appropriate management practices. Different agronomic and physical soil and water conservation measures such as cover crops, counter farming, graded bands, and lime application are some of the corrective measures for the limitations.
该研究在埃塞俄比亚奥罗米亚地区西谢瓦州的巴科蒂贝区开展,旨在对具有农业重要性的酸性土壤进行特征描述和分类。研究考虑了四种土壤类型,挖掘了六个代表性的土系,并从每个土系的已确定土层中总共采集了27个扰动土样和20个原状土芯样进行分析。田间和实验室数据显示,这些土壤质地为黏土和砂质黏土,反应呈微酸性至强酸性(pH值5.2 - 6.63)。表层土壤的有机碳含量中等,为21.4克/千克至较高的30克/千克,而亚表层土壤的有机碳含量则很低(4克/千克)至较高(26克/千克)。表层和亚表层土壤的全氮含量都很低(1.7 - 2.2克/千克),有效磷含量不足(5.99 - 7.85毫克/千克)。所有表层和亚表层土壤的阳离子交换量(CEC)都很高,酸铝土的碱饱和度低(25厘摩尔/千克),而变性土、淋溶土和始成土的碱饱和度中等(51和50厘摩尔/千克)。土壤中的有效铁、锰和锌含量充足,但硼和铜含量不足。土系1为强酸性、暗红色变性土(腐殖质);土系2为强酸性变性土(腐殖质);土系3为暗沃变性土;土系4为暗红色酸铝土(超酸性);土系5为暗红色淋溶土(富营养);土系6为薄层始成土(腐殖质)。土壤特征描述有助于根据土地的能力和限制来利用土地。土系2和4被归类为土地能力分类(LCC)二级。土系1、3和5被归为LCC三级,而土系6被归为LCC四级。所有研究的土壤剖面通过适当的管理措施都可用于作物生产。不同的农艺和物理水土保持措施,如覆盖作物、等高耕作、分级条带和施用石灰等,是针对这些限制的一些纠正措施。