DILUTION OF NON-REACTIVE TRACERS IN VARIABLY SATURATED SANDY STRUCTURES

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dc.contributor.author Ursino N.
dc.contributor.author Gimmi T.
dc.contributor.author Fluhler H.
dc.date.accessioned 2021-03-10T04:28:36Z
dc.date.available 2021-03-10T04:28:36Z
dc.date.issued 2001
dc.identifier https://www.elibrary.ru/item.asp?id=762780
dc.identifier.citation Advances in Water Resources, 2001, 24, 8, 877-885
dc.identifier.issn 0309-1708
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/26547
dc.description.abstract Based on a dye tracer experiment in a sand tank we addressed the problem of local dispersion of conservative tracers in the unsaturated zone. The sand bedding was designed to have a defined spatial heterogeneity with a strong anisotropy. We estimated the parameters that characterize the local dispersion and dilution from concentration maps of a high spatial and temporal resolution obtained by image analysis. The plume spreading and mixing behavior was quantified on the basis of the coefficient of variation of the concentration and of the dilution index. The heterogeneous structure modified the flow pattern depending on water saturation. The shape of the tracer plumes revealed the structural signature of the sand bedding at low saturation only. In this case pronounced preferential flow was observed. At higher flow rates the structure remained hidden by a spatially almost homogeneous behavior of the plumes. In this context, we mainly discuss the mechanism of re-distributing a finite mass of inert solutes over a large volume, due to macro- and micro-heterogeneities of the structure.
dc.title DILUTION OF NON-REACTIVE TRACERS IN VARIABLY SATURATED SANDY STRUCTURES
dc.type Статья


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