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                                       Details van artikel 5 van 8 gevonden artikelen
 
 
  Ordinary Co-kriging versus Kriging with External Drift Correction: Applications to the Evaluation of the Potentiometric Level of a Free Aquifer
 
 
Titel: Ordinary Co-kriging versus Kriging with External Drift Correction: Applications to the Evaluation of the Potentiometric Level of a Free Aquifer
Auteur: Marcelo Monteiro da Rocha
Jorge Kazuo Yamamoto
Helano Regis da Nóbrega Fonteles
Verschenen in: Geologia USP. série científica
Paginering: Jaargang 9 (2009) nr. 1 pagina's 73-84
Jaar: 2009
Inhoud: Equipotential maps are obtained from monitoring wells distributed over the study area. These maps can be built using severalinterpolation methods, nevertheless the available potentiometric information is not suffi cient to ensure good estimation forunsampled locations. In these cases one can use more complex interpolators such as normal cokriging and external drift kriging,with and without correction of the smoothing effect. These methods consider not only the variable to be estimated but alsoanother correlated variable. Thus, we can use information coming from a secondary source to estimate the main variable. Forinstance, elevation is well correlated with potentiometric data and it is very easy to acquire over the study area. In this papercokriging, kriging with external drift, and kriging with external drift after correcting the smoothing effect have been used forthe preparation of the potentiometric map of a free aquifer in the NE part of Fortaleza City, Ceará State. Among the three testedmethods cokriging gave the worst results because of the instability of the system of cokriging equations. Kriging with an external drift seems to be appropriate since it is simpler to implement than cokriging, and it depends on correlation of the secondary information with the variable to be estimated. Furthermore, kriging with external drift after correcting the smoothing effect did not improve the results because available information is not uniformly distributed over the study area. Actually, errors coming from portions with few data are scattered out over other better sampled portions resulting in poorer estimates.
Uitgever: Instituto de Geociências da USP (provided by DOAJ)
Bronbestand: Elektronische Wetenschappelijke Tijdschriften
 
 

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