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Application of geostatistical and deterministic interpolators applied for analysis of the spatial distribution of soil ph in Sorocaba city (São Paulo state)
Author(s) -
Darllan Collins da Cunha e Silva,
Renan Angrizani de Oliveira,
Vanessa Cezar Simonetti,
Érico Tadao Teramoto,
Jomil Costa Abreu Sales
Publication year - 2021
Publication title -
scientia agrária paranaensis/revista scientia agrária paranaensis
Language(s) - English
Resource type - Journals
eISSN - 1983-1471
pISSN - 1677-4310
DOI - 10.18188/sap.v20i1.26070
Subject(s) - kriging , interpolation (computer graphics) , spatial variability , geostatistics , soil science , inverse distance weighting , variogram , environmental science , mean squared error , standard deviation , statistics , hydrology (agriculture) , multivariate interpolation , mathematics , computer science , geology , geotechnical engineering , bilinear interpolation , animation , computer graphics (images)
Soil is a natural resource that allows the maintenance of life on Earth, therefore, it is important to appreciate techniques to assist the conservation of their quality, since the inadequate management of its use causes their degradation. In this sense, the soil pH values of the city of Sorocaba (SP) were analyzed using a pHmeter and a GPS, with 112 points distributed homogeneously in the study area and another 50 random points to verify spatial variability through geostatistical interpolators of ordinary kriging and deterministic of inverse square distance (ISD). The predominant values of pH per soil class were also determined. The pH values predominated between the ranges of 6.0 and 6.5; totaling 74.98% of the study area for the ordinary kriging method and 75.93% for the ISD, observing a low variation among the methods, which result in a root mean square error values of 0.349951 for ordinary kriging and 0.349019 for the ISD. The concordance index for both methods was 0.9944 with mean standard deviation of 0.0374 for ISD and 0.0369 for ordinary kriging. For the different soil classes, pH values ranged from 5.9 to 6.3. Therefore, both the theoretical models applied in the interpolation of the pH data efficiently explain the pH variability of the Sorocaba soil.

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