CLASSIFICATION AND TAXONOMY OF SOILS AND SOILSCAPES

N. Florea
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Abstract

Pedology, as any field of geography, deals with both elementary territorial entities and aggregates (juxtapositions) of elementary entities that form unitary (genetically and functionally) territorial units known in last time as soilscapes. The classification of the elementary (territorial) soil entities can be achieved by different criteria. The most important systematization from scientific point of view is the natural classification, based on the essential characteristics of soils, reflection of soil genesis and evolution, named now soil taxonomy The soil taxonomy is therefore a generalization and systematization of soils based on main soil properties that reflect in the same time also the vertical organization of the threedimensional soils bodies. Depending on some differences of the manner of approach, several soil taxonomies where realized, national and international. Besides soil taxonomy, one utilize in practice soil systematization for different purposes; these ones represents technical or pragmatic classification that have for an object, known as land classification because also the terrain conditions are taken into consideration (soil - terrain). Unlike the elementary soil entities, the soilscapes have been not enough studied as natural segments of soil cover or systematized on the base of their spatial organization expressed by their pedogeographical assemblage, although the soils regions and soil zones represent aggregates of soilscapes at high levels. Elementary or low level soilscapes, as functional and natural territorial entities, can be generalized and systematized; a special taxonomy for soil landscapes can be developed. The soilscapes, being an ensemble of soils and land forms, may not be studied, systematized and characterized without the approach of the previous and present pedogenetic and reliefogenetic processed, in the correlation. Also the soilscapes can be classified according to pragmatic criteria (technical classification) in different purposes (agriculture, forestry, land improvement, erosion control). The studies of the soilscapes with their spatial organization and the soilscape classifications represent a new field of the pedogeography that must be developed.
土壤和土壤景观的分类和分类学
土壤学和地理学的任何领域一样,既研究基本的领土实体,也研究基本实体的集合(并置),这些基本实体形成统一的(遗传上和功能上的)领土单位,在上次被称为土壤景观。基本(领土)土壤实体的分类可以通过不同的标准来实现。从科学的角度来看,最重要的系统分类是基于土壤本质特征的自然分类,反映了土壤的发生和演变,现在称为土壤分类学。因此,土壤分类学是基于主要土壤性质的土壤的概括和系统分类,同时也反映了三维土壤体的垂直组织。根据研究方法的不同,有几种不同的土壤分类,包括国内的和国际的。除了土壤分类学之外,人们在实践中还利用土壤系统化来实现不同的目的;这些分类代表了对一个对象的技术或实用分类,称为土地分类,因为也考虑了地形条件(土壤-地形)。与基本土壤实体不同,土壤景观作为土壤覆盖的自然片段或以土壤地理组合表示的空间组织为基础进行系统化的研究还不够,尽管土壤区域和土壤带在高层次上代表了土壤景观的集合。初级或低级土壤景观作为功能性和自然的地域实体,可以被概括和系统化;可以发展一种专门的土壤景观分类学。土壤景观是土壤和地貌的集合体,如果没有对过去和现在的成土作用和地貌作用进行对比处理,就不可能对其进行研究、系统化和特征化。此外,还可以根据不同用途(农业、林业、土地改良、侵蚀控制)的实用标准(技术分类)对土壤景观进行分类。土壤景观的空间组织及其分类研究是土壤地理学亟待发展的一个新领域。
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