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Pore morphology reveals interaction of biological and physical processes for structure formation in soils of the semiarid Argentinean Pampa
In order to obtain baseline values for the evaluation of soil degradation, the biological and physical quality of petrocalcic Paleustolls, of the calcrete plains of the Semiarid Region Pampa of Argentina, soils under agricultural (Ag) and native vegetation (NV) were selected, with the same clay cont
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