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dc.contributor.authorCartwright, Nicken_US
dc.contributor.authorNielsen, Peteren_US
dc.contributor.authorLi, Lingen_US
dc.date.accessioned2017-05-03T14:31:08Z
dc.date.available2017-05-03T14:31:08Z
dc.date.issued2004en_US
dc.identifier.issn03091708en_US
dc.identifier.doi10.1016/j.advwatres.2004.08.006en_US
dc.identifier.urihttp://hdl.handle.net/10072/16714
dc.description.abstractObservations of horizontal and vertical variations in piezometric head in a homogeneous, laboratory aquifer are presented and discussed. The observed fluctuations are induced by a simple harmonic oscillation in the clear water reservoir acting across a sloping boundary. The data qualitatively supports existing theories in that higher harmonics are generated in the active forcing zone and that a significant increase in the inland, asymptotic watertable over height (relative to that found for the vertical boundary case) is observed. The observed overheight is shown to be accurately reproduced by existing small-amplitude perturbation theory. Detailed measurements in the vicinity of the sloping boundary reveal that the signal of generated higher harmonics is strongest near the sand surface and that vertical flows are significant in this region. The aquifer is of finite-depth and is influenced by capillary effects, the experimental data therefore exposes limitations of theories which are based on the assumption of a shallow aquifer free of capillary effects. The dispersive properties of the measured pressure wave in the aquifer are comparable to those found from field observations and likewise do not agree with those predicted by the capillary free, shallow aquifer theory. Although some improvement is obtained, discrepancies between the data and theory persist even when a finite-depth aquifer and capillary effects are considered in the theoretical model. Further sand column experiments eliminate a truncated capillary fringe as a possible contributor to these discrepancies. However, the neglect of horizontal flows in the fringe may have caused the discrepancies.en_US
dc.description.peerreviewedYesen_US
dc.description.publicationstatusYesen_US
dc.languageEnglishen_US
dc.language.isoen_US
dc.publisherPergamonen_US
dc.publisher.placeUnited Kingdomen_US
dc.relation.ispartofpagefrom991en_US
dc.relation.ispartofpageto1004en_US
dc.relation.ispartofissue10en_US
dc.relation.ispartofjournalAdvances in Water Resourcesen_US
dc.relation.ispartofvolume27en_US
dc.subject.fieldofresearchcode260501en_US
dc.titleExperimental observations of watertable waves in an unconfined aquifer with a sloping boundaryen_US
dc.typeJournal articleen_US
dc.type.descriptionC1 - Peer Reviewed (HERDC)en_US
dc.type.codeC - Journal Articlesen_US
gro.date.issued2015-02-02T04:16:00Z
gro.hasfulltextNo Full Text


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