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Mendes, R.M. and Lorandi, R. (2008) Analysis of Spatial Variability of SPT Penetration Resistance in Collapsible Soils Considering Water Table Depth. Engineering Geology, 101, 218-225.
http://dx.doi.org/10.1016/j.enggeo.2008.06.001

has been cited by the following article:

  • TITLE: Mapping of the Water Table Levels of Unconfined Aquifers Using Two Interpolation Methods

    AUTHORS: Oswaldo Augusto Filho, Wanessa Soares, Clemente Iriguay Fernandéz

    KEYWORDS: Water Table, Deterministic and Geostatistical Interpolation Methods, SPT Boreholes, Geological-Geotechnical Database

    JOURNAL NAME: Journal of Geographic Information System, Vol.8 No.4, August 3, 2016

    ABSTRACT: The spatial prediction of the water table can be used for many applications related to civil works (foundations, excavations) and other urban and environmental management activities. Deterministic and geostatistical interpolation methods were used to predict the spatial distribution of water table levels (unconfined aquifers) of important geological formations of the Joao Pessoa City (capital of Paraiba State, Brazil) with dense urban occupation and high demand for new civil works. The deterministic (topo to raster) and geostatistical (ordinary kriging) interpolation methods were evaluated using a Geographic Information System (GIS)-based investigation. The water table levels were obtained from 276 boring logs of Standard Penetration Test (SPT) in situ investigation distributed over the geological formations studied (an area of 59.8 km2, covering 40 districts of the Joao Pessoa City). The Nspt values and textural characterization data are stored for levels of 1 m depth. Some boreholes located in the area investigated were not included in the interpolation processes in order to be compared with estimated values (validation of the results). Maps of the water table depths were also produced to further analyze the quality of the water table surfaces interpolated by both methods. The phreatic surface interpolations provided satisfactory results for both methods (RMSE = 1.8 m). The topo to raster method showed a slight general tendency to be less affected by local values in relation to the kriging method and also has the advantage of integrating the drainage flow system, which is a relevant aspect for spatial models of the water table levels of unconfined aquifers. The ordinary kriging (geostatistical method) provides a prediction surface and some measure of the certainty or accuracy of the predictions.