Three methods are applied to identify the transmissivity field in 2D heterogeneous aquifers strarting from the knowledge of transmissivity and head observations in few locations. The methods are: co-kriging, modified Marquardt, and the Differential system. The results are compared with attention to the differences in transmissivity and head fields and to the arrival time and dispersion of the breakthrough curves.
Applicazione comparativa di tre metodi di risoluzione del problema inverso in un acquifero eterogeneo bidimensionale / Butera, I.; Grella, E.; Maione, U.; Tanda, Maria Giovanna. - I:(1998), pp. 477-487. (Intervento presentato al convegno XXVI Convegno di Idraulica e Costruzioni Idrauliche tenutosi a Catania (Italia) nel 9-12 settembre 1998).
Applicazione comparativa di tre metodi di risoluzione del problema inverso in un acquifero eterogeneo bidimensionale
TANDA, Maria Giovanna
1998-01-01
Abstract
Three methods are applied to identify the transmissivity field in 2D heterogeneous aquifers strarting from the knowledge of transmissivity and head observations in few locations. The methods are: co-kriging, modified Marquardt, and the Differential system. The results are compared with attention to the differences in transmissivity and head fields and to the arrival time and dispersion of the breakthrough curves.I documenti in IRIS sono protetti da copyright e tutti i diritti sono riservati, salvo diversa indicazione.
