阿尔及利亚西北地区天然土壤的理化复合体

Fatima Zohra Meftah, N. Benabadji, A. Merzouk
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摘要

本研究的目的是确定阿尔及利亚西部Remchi至Beni-Saf平原土壤理化因子对物质空间分布的影响。这项研究告诉我们土壤与物质多样性之间的关系。在生物气候学水平上,该地区具有半干旱的特征,热热作用加剧。使用已知方法进行土壤分析(Stokes粒度法,pH电测法,1/5萃取法电导率,Bernard钙法CaCO3, Anne法有机碳)。结果显示出纹理多样性;泥泞的“Remchi”,沙质的“Rachgoun 1和Rechgoun 2”,离Beni-Saf不远。低粘土含量(Remchi:剖面1:地平线1:粘土10%,剖面2:地平线1:粘土16%,剖面3:地平线1:粘土5%,Rechgoun:剖面1:地平线1:粘土3%,剖面3:地平线1:粘土2%和地平线2:粘土3%)导致结构稳定性差,导致土壤表面通过侵蚀而退化。后者通过在这些粗糙的斜坡上可见的小侵蚀爪的存在而揭示出来。
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Physico-Chemical Complex of Matorral Soils of the North Western Region of Algeria
The objective of this study is to determine the influence of soil physico-chemical factors on the spatial distribution of matorrals in the plain from Remchi to Beni-Saf located in the western region of Algeria. This study informs us of the relationships that soil can have on the diversity of matorrals. On the bioclimatic level, the region is characterized by semi-aridity accentuating the phenomena of therophysation. Soil analyzes carried out using known methods (Stokes Particle Size Method, Electrometric Method for pH, 1/5 Extract Method for Electrical Conductivity, Bernard Calcium Method for CaCO3, Anne Method for Organic Carbon). The results show a textural diversity; sandy-muddy “Remchi”, sandy “Rachgoun 1 and Rechgoun 2”, not far from Beni-Saf. The low clay content (Remchi: Profile 1: Horizon 1: Clays 10%, Profile 2: Horizon 1: Clays 16%, Profile 3: Horizon 1: Clays 5%, Rechgoun: Profile 1: Horizon 1: Clays 3%, Profile 3: Horizon 1: 2% Clays and Horizon 2: 3% Clays) leads to poor structural stability leading to degradation of the soil surface through erosion. The latter is revealed by the presence of small erosion claws visible on these rough slopes or almost.
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