A laboratory model has been carried out to evaluate a measurement methodology to determine dispersivity values of several pollutants in groundwater systems. The simulated phenomenon has been hydrodynamic dispersion in a phreatic, porous nosorbing aquifer situated between two basins of infinite capacity and different piezometric heads. The value of dispersivity, obtained for a natural siliceous sand from the Ticino Valley, having diameter d=1 mm, in average, has been about 2.0 mm. This value has been evaluated by calibration of breakthrough curves of experimental data of concentration using the analytical solution of the one-dimensional advection-dispersion equation.
Un modello di laboratorio e' stato messo a punto per valutare una metodologia di misura per la determinazione dei valori della dispersivita' di alcuni inquinanti in sistemi di acque sotterranee. Il fenomeno simulato e' stato quello della dispersione idrodinamica in un acquifero freatico a matrice porosa non reagente situato tra due bacini aventi capacita' infinita e differenti livelli della superficie libera. Il valore della dispersivita', ottenuto per una sabbia silicea della valle del Ticino, con diametro d pari, in media, ad un millimetro, e' stato di circa 2.0 mm. Questo valore e' stato detrminato attraverso il "fit" delle curve sperimentali dei dati di concentrazione utilizzando la soluzione analitica dell'equazione di advezione-dispersione unidimensionale.
Evaluation of Dispersivity using a Laboratory Model
Passarella G;Masciopinto C
1994
Abstract
A laboratory model has been carried out to evaluate a measurement methodology to determine dispersivity values of several pollutants in groundwater systems. The simulated phenomenon has been hydrodynamic dispersion in a phreatic, porous nosorbing aquifer situated between two basins of infinite capacity and different piezometric heads. The value of dispersivity, obtained for a natural siliceous sand from the Ticino Valley, having diameter d=1 mm, in average, has been about 2.0 mm. This value has been evaluated by calibration of breakthrough curves of experimental data of concentration using the analytical solution of the one-dimensional advection-dispersion equation.I documenti in IRIS sono protetti da copyright e tutti i diritti sono riservati, salvo diversa indicazione.