THE ROLE OF PEDOLOGICAL INFORMATION IN AGRICULTURAL LAND SUITABILITY ASSESSING

D. Dicu, D. Țărău, I. Borza
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引用次数: 2

Abstract

Soil characteristics can exert an influence on the development of root systems, mineral nutrition, providing the required heat treatment and conduct aerohidric main physiological processes, and plants (phytocoenosis, in turn, act both directly and indirectly on the state of soil fertility). In the soil conditions can be defined certain characteristics that may be conducive to land productivity and other properties derived from the first. Attributes such as size and composition of soil, humus content are crucial features, while cationic exchange capacity is determined by the first two and by the mineralogical nature of clay. Similarly, available water capacity can be considered as determined by soil texture and structure. Our research concerns an area of 141,249 ha. (72721ha. in Timis county and 68,528 ha in Arad county), belonging to areas located in Vinga Plain and its connection to the low plains or Lipova hills. The research of ecopedological conditions, data ordering and processing was done according to the Methodology of pedological studies elaboration; (vol I, II, III), developed by ICPA Bucharest in 1987 and the Romanian System of Soil Taxonomy (SRTS-2003). In assessing of land pretability for culture systems are considered soil factors who determine the degree of suitability, soil texture and soil moisture excess. Pretability estimation can be based on the information contained in existing soil studies in the area but also in the field research conducted on soils representative of a particular physical and geographical space.
土壤学信息在农用地适宜性评价中的作用
土壤特性可以对根系的发育、矿物质营养、提供所需的热处理和进行气湿主要生理过程以及植物(植物群落又直接或间接地影响土壤肥力状态)产生影响。在土壤条件下可以确定某些特征,这些特征可能有利于土地生产力和其他属性的产生。土壤的大小和组成、腐殖质含量等属性是至关重要的特征,而阳离子交换能力是由前两者和粘土的矿物学性质决定的。同样,有效水量也可以认为是由土壤的质地和结构决定的。我们研究的面积为141249公顷。(72721公顷。在蒂米斯县和在阿拉德县68 528公顷),属于位于温加平原及其与低平原或利波瓦丘陵相连的地区。根据土壤学研究方法论的阐述,对生态条件、数据整理和处理进行了研究;(第一,二,三卷),由ICPA布加勒斯特于1987年和罗马尼亚土壤分类系统(SRTS-2003)开发。在评估土地耕作系统的适宜性时,考虑了决定适宜程度、土壤质地和土壤水分过剩的土壤因素。可预估性既可以根据该地区现有土壤研究所载的资料,也可以根据对具有特定物理和地理空间代表性的土壤进行的实地研究。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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