Volcanic crop soil physicochemical characterization in semi-arid and temperate climates: two Mexican case studies
2024
O A Luévano-Rivas | G Chavez-Esquivel | D Ángeles-Beltrán | J A Tavizón-Pozos
In this work, two crop soils were characterized: Querétaro (Bajío) and the State of Mexico (Edomex). Both states are part of the Sierra Madre Occidental, where temperate and subhumid climates are experienced. The surface soils are predominantly Leptosols in the Bajio and Andosols-Feozems in the Edomex. The dynamic mobility of water and fertilizers is associated with humic substances, mineralogical phases, metal dispersion, pore type, pore volume, and thermal behavior ^4 . Both agricultural soils exhibited high porosity and surfaces with co-dispersion of Al ^3+ /Si ^4+ and Ti ^4+ /Fe ^2+,3+ ions and mixed mineralogical phases such as montmorillonite, anorthite, quartz, magnetite, goethite, hematite, and kaolinite. On the one hand, the C/N values for the Bajio-crop and Edomex-crop soils showed values of 15 and 11, respectively. On the other hand, the Bajio-crop and Edomex-crop soils showed C/O values of 0.38 and 0.42, respectively, indicating the accumulation of organic carbon and the presence of various humic substances. Finally, the Bajio-crop soil presented a higher surface area, pore diameter, and pore volume than the Edomex-crop soil, which is associated with high adsorption and nutrient retention. On the contrary, the Edomex-crop soil presented greater thermal resistance than the Bajio-crop soil, which is associated with a better capacity for heat dissipation during irrigation processes or fertilizer application.
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