Suelos con fragipán de origen volcánico en clima semicálido y subhúmedo-el csaaso del noreste del estado de Morelos, México

Abstract

The fragipan consists of very compact horizons with high-bulk density and some brittleness. Its supposed origin could be igneous or sedimentary. In Mexico, it is known as tepetate, a Náhuatl word that means different compact or cemented materials… in order to continue, download the full paper in PDF.