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Soil classification and phosphorus relationships as influenced by soil iron and manganese in soils of the Mbo Plain in Cameroon.

机译:喀麦隆姆博平原土壤铁和锰对土壤分类和磷素关系的影响。

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摘要

Decreasing yield of crops grown in soils of the Mbo Plain has been attributed to deficiencies of soil P. The objectives of this study were to classify these soils using the United States Soil Taxonomy System and to determine P, Fe, and Mn status at four sublocations (Nzock5, Mbomi4, Mbomi2 and Mbomi10) of the Mbo Plain. Two pedons were described at each sublocation. Phosphate rates (0, 25, 50, and 75 mg P kg;Properties of the Mbo Plain soils were similar in all sublocations. The texture alternated between clay and clay loam. Base saturation was low and ranged from 4 to 52%. Soils are acidic with a water pH range of 3.8 to 5.0. Aluminum saturation percentage varied from 16 to 92%. Clay mineralogy was kaolinitic and ECEC ranged from 2.3 to 11.4 cmol kg;The main P fractions were Al- and Fe-bound P. Sorption isotherms indicated 50 to 439 mg P kg;Iron and Mn in plant tissue were present in apparent toxic concentrations (
机译:Mbo平原土壤中生长的农作物产量下降归因于土壤P的缺乏。本研究的目的是使用美国土壤分类系统对这些土壤进行分类,并确定四个子区域的P,Fe和Mn状况。 Mbo平原的(Nzock5,Mbomi4,Mbomi2和Mbomi10)。每个子位置描述了两个脚钉。磷酸盐速率(0、25、50和75 mg P kg;在所有分区中,Mbo平原土壤的性质都相似。质地在粘土和壤土之间交替变化。基层饱和度较低,范围为4%至52%。酸性,水的pH范围为3.8至5.0;铝的饱和度百分比为16至92%;粘土矿物学为高岭土,ECEC范围为2.3至11.4 cmol kg;主要的P组分为与Al和Fe结合的P。表示50至439 mg P kg;植物组织中的铁和Mn以明显的毒性浓度存在(

著录项

  • 作者

    Takow, Julius Agbor.;

  • 作者单位

    Texas A&M University.;

  • 授予单位 Texas A&M University.;
  • 学科 Agriculture Agronomy.
  • 学位 Ph.D.
  • 年度 1991
  • 页码 326 p.
  • 总页数 326
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

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