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首页> 外文期刊>Revista Caatinga >PEDOGENESIS AND SOIL CLASSIFICATION OF AN EXPERIMENTAL FARM IN MOSSORó, STATE OF RIO GRANDE DO NORTE, BRAZIL
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PEDOGENESIS AND SOIL CLASSIFICATION OF AN EXPERIMENTAL FARM IN MOSSORó, STATE OF RIO GRANDE DO NORTE, BRAZIL

机译:巴西里奥格兰德多诺特州莫索罗的一个实验农场的成岩作用和土壤分类

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The Rafael Fernandes experimental farm is located in the Alagoinha district, northwest of Mossoró, State of Rio Grande do Norte, Brazil, over two pedogenic formations of different edaphic characteristics, thus needing a more detailed description of its soil types, since this area hosts several experimental fields for researches on agriculture. The objective of this work was to characterize the morphological, physical, chemical and mineralogical features of the most representative soils of this farm, in order to understand its pedogenesis and define its classifications. The whole area was surveyed in order to assess its more representative pedogenic formations. Three soil profiles were classified and described, from which samples were collected in all horizons for physical, chemical and mineralogical analysis. The parent materials and the relief were the determining factors for pedogenic processes of desilication, podzolization and laterization, generating the three main soil types of the area, which were classified up to the 4 th categorical level and described as: Typic Rhodustults (P1), Rhodic Haplustox (P2) and Typic Plinthustalfs (P3).
机译:拉斐尔·费尔南德斯(Rafael Fernandes)实验农场位于巴西北里约格兰德州莫索罗市西北的Alagoinha地区,位于两个具有不同前卫特征的成岩层上,因此需要对其土壤类型进行更详细的描述,因为该地区拥有多个农业研究的实验领域。这项工作的目的是表征该农场最具代表性的土壤的形态,物理,化学和矿物学特征,以便了解其成土作用并确定其分类。为了评估其更具代表性的成岩作用,对整个地区进行了调查。对三种土壤剖面进行了分类和描述,从各个层面收集了样本进行物理,化学和矿物学分析。母体材料和地势是造成硅化作用,松土化和后土化的成因过程的决定因素,产生了该地区的三种主要土壤类型,分类为第4类,并描述为:典型的Rhodustults(P1), Rhodic Haplustox(P2)和Typic Plinthustalfs(P3)。

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