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Abstract
In the present paper we study the relationship among redox potential and sorne of the factors that they condition it, in eight soíl profils from Cabo de Gata región (Almeria-Spain), all them al'e developed on limestone or other richo in calcium carbonate, rocks. The climate is warmsubdesertic. We found the Eh value is related with the amounts of organic matter and manganese and the pH value. The Eh value is not related with the iron content.
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