{"title":"埃塞俄比亚西北高地Lay Gayint地区Yikalo小流域土壤特征与分类","authors":"E. Fekadu, K. Kibret, B. Bedadi, A. Melese","doi":"10.18393/EJSS.376267","DOIUrl":null,"url":null,"abstract":"Soil resource information is vital for sound land use planning and sustainable fertility management. This study was carried out with the objective of characterizing and classifying soils of Yikalo Subwatershed at Lay Gayint district, Northwestern Ethiopia. Representative soil pedons were opened along topographic positions and described on genetic horizon basis in the field for their morphological characteristics and analyzed in the laboratory for selected physical and chemical soil properties. The soils were classified following the FAO (2014). The results revealed the presence of variations in the selected morphological properties within a pedon and along the topographic positions. Soils differed in reaction from 4.57 to 6.42. On the surface horizons of the soil pedons, available P content varied from 0.21 to 3.25 mg kg -1 , while exchangeable acidity ranged from 0.17 to 3.65 cmol c kg -1 soil. There was no consistent trend for cation exchange capacity (CEC) and PBS (percent base saturation) with soil depth and topographic positions. The soils in Yikalo Subwatershed were classified as Hyperdystric Cambisols (Humic), Haplic Alisols (Humic), Cambic Umbrisols (Colluvic) , Haplic Luvisols (Epidystric), and Pellic Vertisols ( Mesotrophic). Optimum rates of organic and inorganic amendments should be applied to reduce the level of soil acidity, and improve the fertility level of the soils for better crop production and productivity.","PeriodicalId":36945,"journal":{"name":"Eurasian Journal of Soil Science","volume":"7 1","pages":"151-166"},"PeriodicalIF":0.0000,"publicationDate":"2018-04-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"13","resultStr":"{\"title\":\"Characterization and classification of soils of Yikalo Subwatershed in Lay Gayint District, Northwestern Highlands of Ethiopia\",\"authors\":\"E. Fekadu, K. Kibret, B. Bedadi, A. Melese\",\"doi\":\"10.18393/EJSS.376267\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"Soil resource information is vital for sound land use planning and sustainable fertility management. This study was carried out with the objective of characterizing and classifying soils of Yikalo Subwatershed at Lay Gayint district, Northwestern Ethiopia. Representative soil pedons were opened along topographic positions and described on genetic horizon basis in the field for their morphological characteristics and analyzed in the laboratory for selected physical and chemical soil properties. The soils were classified following the FAO (2014). The results revealed the presence of variations in the selected morphological properties within a pedon and along the topographic positions. Soils differed in reaction from 4.57 to 6.42. On the surface horizons of the soil pedons, available P content varied from 0.21 to 3.25 mg kg -1 , while exchangeable acidity ranged from 0.17 to 3.65 cmol c kg -1 soil. There was no consistent trend for cation exchange capacity (CEC) and PBS (percent base saturation) with soil depth and topographic positions. The soils in Yikalo Subwatershed were classified as Hyperdystric Cambisols (Humic), Haplic Alisols (Humic), Cambic Umbrisols (Colluvic) , Haplic Luvisols (Epidystric), and Pellic Vertisols ( Mesotrophic). Optimum rates of organic and inorganic amendments should be applied to reduce the level of soil acidity, and improve the fertility level of the soils for better crop production and productivity.\",\"PeriodicalId\":36945,\"journal\":{\"name\":\"Eurasian Journal of Soil Science\",\"volume\":\"7 1\",\"pages\":\"151-166\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2018-04-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"13\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Eurasian Journal of Soil Science\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.18393/EJSS.376267\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q3\",\"JCRName\":\"Agricultural and Biological Sciences\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Eurasian Journal of Soil Science","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.18393/EJSS.376267","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q3","JCRName":"Agricultural and Biological Sciences","Score":null,"Total":0}
引用次数: 13
摘要
土壤资源信息对于健全的土地利用规划和可持续的肥力管理至关重要。本研究的目的是对埃塞俄比亚西北部Lay Gayint地区Yikalo小流域土壤进行特征和分类。沿着地形位置打开有代表性的土壤桩,在田间对其形态特征进行遗传水平描述,并在实验室对选定的土壤理化性质进行分析。土壤分类遵循粮农组织(2014年)。结果显示,在一个pedon内和沿着地形位置的选择形态属性的变化存在。不同土壤的反应系数在4.57 ~ 6.42之间。土壤层位有效磷含量在0.21 ~ 3.25 mg kg -1之间,交换酸度在0.17 ~ 3.65 cmol c kg -1之间。阳离子交换容量(CEC)和碱基饱和度百分比(PBS)与土壤深度和地形位置没有一致的趋势。依卡洛亚流域土壤可分为高营养性腐殖型(Cambisols)、半营养性腐殖型(Haplic Alisols)、半营养性腐殖型(cambiic umbriols)、半营养性腐殖型(Haplic Luvisols)和中营养型(Pellic Vertisols)。应适当施用有机和无机改良剂,以降低土壤酸度,提高土壤肥力水平,提高作物产量和生产力。
Characterization and classification of soils of Yikalo Subwatershed in Lay Gayint District, Northwestern Highlands of Ethiopia
Soil resource information is vital for sound land use planning and sustainable fertility management. This study was carried out with the objective of characterizing and classifying soils of Yikalo Subwatershed at Lay Gayint district, Northwestern Ethiopia. Representative soil pedons were opened along topographic positions and described on genetic horizon basis in the field for their morphological characteristics and analyzed in the laboratory for selected physical and chemical soil properties. The soils were classified following the FAO (2014). The results revealed the presence of variations in the selected morphological properties within a pedon and along the topographic positions. Soils differed in reaction from 4.57 to 6.42. On the surface horizons of the soil pedons, available P content varied from 0.21 to 3.25 mg kg -1 , while exchangeable acidity ranged from 0.17 to 3.65 cmol c kg -1 soil. There was no consistent trend for cation exchange capacity (CEC) and PBS (percent base saturation) with soil depth and topographic positions. The soils in Yikalo Subwatershed were classified as Hyperdystric Cambisols (Humic), Haplic Alisols (Humic), Cambic Umbrisols (Colluvic) , Haplic Luvisols (Epidystric), and Pellic Vertisols ( Mesotrophic). Optimum rates of organic and inorganic amendments should be applied to reduce the level of soil acidity, and improve the fertility level of the soils for better crop production and productivity.