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High-resolution permeability determination and two-dimensional porewater flow in sandy sediment

dc.contributor.authorRocha, C
dc.contributor.authorForster, S
dc.contributor.authorKoning, E
dc.contributor.authorEpping, E
dc.date.accessioned2018-12-07T14:53:12Z
dc.date.available2018-12-07T14:53:12Z
dc.date.issued2005-01
dc.description.abstractA new, inexpensive method is proposed to measure permeability in natural sandy sediment with high spatial resolution. This methodology allows for a reconstruction of the vertical permeability anisotropy in natural sediments, with a depth resolution of a few millimeters. Thus, the possible intrusion depth of advective flow over the water-sediment interface of sandy sediments can be deduced. Shipboard measurements on five natural sandy sediment cores taken from North Sea sediments are used to demonstrate that both the direction and magnitude of the second-order permeability tensor can be calculated from direct measurements using this method. This presents a major improvement over previous methods particularly in the context of quantifying flow and reaction in permeable sediments.
dc.description.versioninfo:eu-repo/semantics/publishedVersion
dc.identifier.doi10.4319/lom.2005.3.10
dc.identifier.urihttp://hdl.handle.net/10400.1/11397
dc.language.isoeng
dc.peerreviewedyes
dc.publisherAmer Soc Limnology Oceanography
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/
dc.subjectContinental-shelf sediments
dc.subjectHydraulic conductivity
dc.subjectIntertidal sediments
dc.subjectSolute transport
dc.subjectOxygen
dc.subjectManure
dc.subjectWater
dc.subjectMechanisms
dc.subjectConvection
dc.subjectBoundary
dc.titleHigh-resolution permeability determination and two-dimensional porewater flow in sandy sediment
dc.typejournal article
dspace.entity.typePublication
oaire.citation.endPage23
oaire.citation.startPage10
oaire.citation.titleLimnology and Oceanography: Methods
oaire.citation.volume3
rcaap.rightsopenAccess
rcaap.typearticle

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