Predictive mapping of soil electrical conductivity as a Proxy of soil salinity in south-east of Algeria

dc.contributor.authorAbdennour, Mohamed Amine
dc.contributor.authorDouaoui, Abdelkader
dc.contributor.authorPiccini, Chiara
dc.contributor.authorPulido, Manuel
dc.contributor.authorBennacer, Amel
dc.contributor.authorBradaï, Abdelhamid
dc.contributor.authorBarrena, Jesús
dc.contributor.authorYahiaoui, Ibrahim
dc.date.accessioned2021-02-17T11:58:34Z
dc.date.available2021-02-17T11:58:34Z
dc.date.issued2020
dc.description.abstractIn semi-arid and arid areas soil salinity has adverse effects both on the environment and agricultural production. The region of Biskra (South-East of Algeria) underwent a strong agricultural transformation from traditional oasis agriculture to an almost exclusive production of dates involving market gardening throughout the year. The main goal was to predict the spatial variation of EC using geostatistics and a Geographic Information System (GIS), comparing also the performance of two classical geostatistical interpolators - Ordinary Kriging (OK), using only point data, and Cokriging (CK), introducing also auxiliary variables to improve prediction accuracy (SI gypsum and SO42−, obtained from the analysis of the chemical and geochemical processes of soil salinization). For this study, a total of 42 soil samples were randomly collected from topsoil (0–15 ​cm) in the irrigated perimeter of El Ghrous, a representative rural community located in the west of Biskra. Aiming to better understand the processes that most influence the evolution of soil salinity in this area, some chemical parameters were determined, among which the electrical conductivity (EC). Moreover, some terrain parameters were derived from a digital elevation model as auxiliary information, and Normalized Difference Vegetation Index (NDVI) was calculated from satellite imagery. The prediction efficiency of the methods was evaluated by calculating the mean error (ME) and the root mean square error (RMSE). The resulting maps showed that soils in the study area are affected by salinization. Cross-validation results showed a better performance in estimating EC of CK, after the introduction of the covariates, than OK, with an RMSE value of 0.92 vs. 1.53. This suggests a greater efficiency of CK in EC prediction in this area, confirming that the introduction of some auxiliary data correlated to the target variable significantly improves the interpolation. A third kriging technique, Indicator Kriging (IK) was applied to generate a map of the probability of exceeding a given thresholden_US
dc.identifier.otherhttps://doi.org/10.1016/j.indic.2020.100087
dc.identifier.urihttps://www.sciencedirect.com/science/article/pii/S2665972720300714
dc.identifier.urihttps://dspace.univ-boumerdes.dz/handle/123456789/6438
dc.language.isoenen_US
dc.publisherElsevieren_US
dc.relation.ispartofseriesEnvironmental and Sustainability Indicators/ Vol.8 (2020);pp. 1-14
dc.subjectOrdinary krigingen_US
dc.subjectCokrigingen_US
dc.subjectIndicator krigingen_US
dc.subjectSpatial variabilityen_US
dc.subjectSaturation indexen_US
dc.subjectBiskraen_US
dc.titlePredictive mapping of soil electrical conductivity as a Proxy of soil salinity in south-east of Algeriaen_US
dc.typeArticleen_US

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