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Identification of the Dominant Factors in Groundwater Recharge Process, Using Multivariate Statistical Approaches in a Semi-Arid Region

dc.contributor.authorUc Castillo, José Luis
dc.contributor.authorRamos Leal, José Alfredo
dc.contributor.authorMartínez Cruz, Diego Armando
dc.contributor.authorCervantes Martínez, Adrián
dc.contributor.authorMarín Celestino, Ana Elizabeth
dc.date.accessioned2022-03-10T19:33:52Z
dc.date.available2022-03-10T19:33:52Z
dc.date.issued2021
dc.identifier.citationCastillo, J.L.U.; Ramos Leal, J.A.; Martínez Cruz, D.A.; Cervantes Martínez, A.; Marín Celestino, A.E. Identification of the Dominant Factors in Groundwater Recharge Process, Using Multivariate Statistical Approaches in a Semi-Arid Region. Sustainability 2021, 13, 11543. https://doi.org/10.3390/su132011543
dc.identifier.urihttp://hdl.handle.net/11627/5791
dc.description.abstract"Identifying contributing factors of potential recharge zones is essential for sustainable groundwater resources management in arid regions. In this study, a data matrix with 66 observations of climatic, hydrogeological, morphological, and land use variables was analyzed. The dominant factors in groundwater recharge process and potential recharge zones were evaluated using K-means clustering, principal component analysis (PCA), and geostatistical analysis. The study highlights the importance of multivariate methods coupled with geospatial analysis to identify the main factors contributing to recharge processes and delineate potential groundwater recharge areas. Potential recharge zones were defined into cluster 1 and cluster 3; these were classified as low potential for recharge. Cluster 2 was classified with high potential for groundwater recharge. Cluster 1 is located on a flat land surface with nearby faults and it is mostly composed of ignimbrites and volcanic rocks of low hydraulic conductivity (K). Cluster 2 is located on a flat lowland agricultural area, and it is mainly composed of alluvium that contributes to a higher hydraulic conductivity. Cluster 3 is located on steep slopes with nearby faults and is formed of rhyolite and ignimbrite with interbedded layers of volcanic rocks of low hydraulic conductivity. PCA disclosed that groundwater recharge processes are controlled by geology, K, temperature, precipitation, potential evapotranspiration (PET), humidity, and land use. Infiltration processes are restricted by low hydraulic conductivity, as well as ignimbrites and volcanic rocks of low porosity. This study demonstrates that given the climatic and geological conditions found in the Sierra de San Miguelito Volcanic Complex (SSMVC), this region is not working optimally as a water recharge zone towards the deep aquifer of the San Luis Potosí Valley (SLPV). This methodology will be useful for water resource managers to develop strategies to identify and define priority recharge areas with greater certainty."
dc.publisherMDPI
dc.rightsAttribution-NonCommercial-NoDerivatives 4.0 Internacional
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/4.0/
dc.subjectGroundwater recharge
dc.subjectInfiltration
dc.subjectK-means clustering
dc.subjectPCA
dc.subjectSierra de San Miguelito
dc.subjectVolcanic Complex
dc.subject.classificationCIENCIAS TECNOLÓGICAS
dc.titleIdentification of the Dominant Factors in Groundwater Recharge Process, Using Multivariate Statistical Approaches in a Semi-Arid Region
dc.typearticle
dc.identifier.doihttps://doi.org/10.3390/su132011543
dc.rights.accessAcceso Abierto


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Attribution-NonCommercial-NoDerivatives 4.0 Internacional
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