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首页> 外文期刊>Revue Roumaine de Geographie >SOIL FACIES – A GEOGRAPHIC LOCAL-REGIONAL COMPLETING OF SOIL TAXONOMIC UNITS
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SOIL FACIES – A GEOGRAPHIC LOCAL-REGIONAL COMPLETING OF SOIL TAXONOMIC UNITS

机译：土壤相–土壤分类学单元的地理局部完成

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摘要

Soil facies – a geographic local-regional completing of soil taxonomic units. Because the soil units have a double nature, genetic and geographic (“double identity”), not completely reflected by the system of soil taxonomy, it was proposed to complete the name of the soil taxa by some additional aspects, named regional and local soil facies. These soil facies refer to the soil differentiating features of regional and respectively local significance. The soil name according to the soil taxonomy will be completed with the names of regional and local soil facies, generally geographic terms; for example F?g?ra? skeletal loamy sand, Carpathian, Leptic- Entic Podzol. Of course, the system of soil facies entities, the criteria of differentiation and terminology of the delineated units needs to be discussed and to be agreed on. The European taxonomies could also be completed in this way with specific moisture and temperature regimes and other site characteristics. This particularization of the soil entities using soil facies can be carried on to the individualization of each soil area (delineation) in the framework of an information system and database correlated with the cadastral survey.
机译：土壤相-土壤分类单位在地理上局部的完整区域。由于土壤单元具有自然，遗传和地理的双重特征（“双重身份”），并未完全反映在土壤分类系统中，因此建议通过一些其他方面来完善土壤分类的名称，即区域和本地土壤。相。这些土壤相指的是区域意义和局部意义的土壤分化特征。根据土壤分类法的土壤名称将以区域和本地土壤相的名称（通常为地理术语）完成;例如F？g？ra？骨骼质壤质砂，喀尔巴阡，枯燥的Entic Podzol。当然，还需要讨论并商定土壤相实体系统，区分标准和所用单位的术语。欧洲分类法也可以用特定的湿度和温度制度以及其他现场特征来完成。利用土壤相对土壤实体的这种特殊化可以在与地籍调查相关的信息系统和数据库的框架内进行到每个土壤区域的个性化（描绘）。

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