Abstract
Los Pedroches pasture settles on granitic-magmatic rocks evolving to young sandy soils, poor in nutrients and clays including Lithosols, Haplic and Cambic Arenosols and Cambisols. Exclusively in older and erosion-protected surfaces Chromic Luvisols (FAO, 1989) have been preserved.
Highlights
ҐРУНТИ ПАСОВИЩ У РАЙОНІ ВАЛЬЄ-ДЕ-ЛОС-ПЕДРОЧЕС (КОРДОБА, ІСПАНІЯ)
From the Calatraveño gate the region of Los Pedroches can be characterized using different names which refer to this important natural area: From a structural point of view as a lithological and granite batholith, geomorphologically the Pedroche peneplain is a highly peneplained relief, hydrographically it constitutes a convexe water divide, the vegetation is the pasture of the Pedroches, and physiographically is known as the place name of Los Pedroches «valley», without a forming river, but so named in contrast to the characteristically relief of the Sierra Morena in the south
Regolith, lehm, or alteration mantle is the result of differentiation and formation time of the most recent horizontal layers with different physicochemical characteristics which clearly differ from the rock or starting material through the impact of the biosphere
Summary
ҐРУНТИ ПАСОВИЩ У РАЙОНІ ВАЛЬЄ-ДЕ-ЛОС-ПЕДРОЧЕС (КОРДОБА, ІСПАНІЯ) Що знаходяться під пасовищами в районі Вальє-де-лос-Педрочес (Кордова, Іспанія), в першу чергу було проведено дослідження з визначення родючості ґрунту в районі Пособланко, Вільянуева-де-Кордова, Конкіста і Торрекампо, виконане в 1979 р.
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