Titlebook: Sustainable Spaces in Arid and Semiarid Zones of Mexico; Liliana Lizárraga-Mendiola,Carlos Alfredo Bigurra- Book 2024 The Editor(s) (if ap

Ordeal

om and/or their top surface by layers of very low permeability (clay layers), see figure 3.1. All these layers are more or less horizontal, so that it is reasonable to assume that in the permeable layers (denoted as aquifers) the flow is predominantly horizontal. The less permeable clay layers (some

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