乌拉圭土壤水文类群的分类

A. Duran
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引用次数: 0

摘要

根据美国土壤保持局(SCS)开发的程序,对乌拉圭侦察土壤地图的测绘单元的优势土壤进行了初步的水文类群(GH)分类。由于还没有关于降水和径流之间关系的资料,分类主要是根据土壤形态:层序、它们的质地和结构、土壤基质颜色、斑驳和铁锰结块的存在作为氧合现象的指示。基于剖面形态的土壤渗透性和排水量的估计和对水文制度的了解支持了GH的分类。结果表明:A组土壤数量极少,主要为砂质土或极砾质土;B组(24条剖面)主要包括中等至良好排水的亚营养Brunosols (Udolls)。C组(68个剖面)包括亚中性和中性Brunosols (Udolls)和Argisols (Udolls和Udalfs),大多排水良好或稍差,底土质地良好。D组(63个剖面)包括所有的垂直土壤、平流层土壤(Albolls和aqualls)、Gleysols(主要是Aquolls和Udolls)和solonetzic土(Aqualfs)、大多数石质土壤(Lithic Orthents和Udolls)和少数Brunosols (Udolls);排水范围从有些过度到较差。所获得的分类与某些土壤的入渗速率和水力导电性测量的现有信息相当一致。与美国已知土壤进行比较,发现美国和乌拉圭在为土壤分配正确的生长激素时所使用的分类标准之间没有明显的矛盾。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Classification in hydrologic groups of soil of Uruguay
Dominant soils of the mapping units of the Reconnaissance Soil Map of Uruguay were tentatively classified in hydrologic groups (GH) following the procedure developed by the U.S. Soil Conservation Service (SCS). Since information on the relationship between precipitation and runoff is not available yet, the classification is mostly based on soil morphology: horizons sequence, their texture and structure, soil matrix color, mottling and presence of Fe-Mn concretions as indications of redoximorphic phenomena. Estimates of soil permeability and drainage on the basis of profile morphology and the knowledge of the hydric regime support the classification in GH. The results show that only very few soils are included in Group A, mainly Arenosols (Psamments) or very gravelly soils. Group B (24 profiles) includes mainly moderately well to well drained Subeutric Brunosols (Udolls). Group C (68 profiles) includes Subeutric and Eutric Brunosols (Udolls) and Argisols (Udolls and Udalfs), mostly moderately well to somewhat poorly drained, with a fine textured subsoil. Group D (63 profiles) includes all Vertisols, Planosols (Albolls and Aqualfs), Gleysols (mostly Aquolls and Udolls) and solonetzic soils (Aqualfs), most Litosols (Lithic Orthents and Udolls) and a few Brunosols (Udolls); drainage range from somewhat excessive to poor. the classification achieved is razonably consistent with available information on infiltration rate and hydraulic conductivity measurements for some soils. The comparison with known soils of USA, classified in GH with a more scientific basis, has not shown any evident contradiction between the classification criteria used both in US and Uruguay to assign each soil to the correct GH.
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