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dc.contributor.author池淵, 周一ja
dc.contributor.author森岡, 武一ja
dc.contributor.alternativeIKEBUCHI, Shuichien
dc.contributor.alternativeMORIOKA, Takekazuen
dc.date.accessioned2009-04-09T05:55:24Z-
dc.date.available2009-04-09T05:55:24Z-
dc.date.issued1987-04-01-
dc.identifier.issn0386-412X-
dc.identifier.urihttp://hdl.handle.net/2433/72030-
dc.description.abstractThere are many studies to estimate parameters in numerical models of groundwater flow.However, before parameter estimation, numerical analysis of uncertainty propagation ofparameters is required in order to know which parameter to estimate, and how to estimateit.In this paper, an approximate solution to the distribution of dependent random variablesis applied to numerical models of groundwater. First-order second-moment method ofmultidimensional Tayor-series expansion, that is, is presented in matrix form for such analysisso as to calculate the mean and the covariance of predicted groundwater heads due to manyuncertainty parameters.This algorithm is applied to an assumed groundwater basin and its results are presentedin graphic formula, and are compared with those calculated by Monte Carlo simulation.en
dc.format.mimetypeapplication/pdf-
dc.language.isojpn-
dc.publisher京都大学防災研究所ja
dc.publisher.alternativeDisaster Prevention Research Institute, Kyoto Universityen
dc.subject.ndc452.95-
dc.subject.ndc517-
dc.title浅層地下水流動モデルの不確定要因とその時・空間伝播特性ja
dc.title.alternativeUNCERTAIN FACTORS IN NUMERICAL MODELS OF FREE GROUNDWATER FLOW AND THEIR PROPAGATION IN TIME-SPACEen
dc.typedepartmental bulletin paper-
dc.type.niitypeDepartmental Bulletin Paper-
dc.identifier.ncidAN00027784-
dc.identifier.jtitle京都大学防災研究所年報. Bja
dc.identifier.volume30-
dc.identifier.issueB-2-
dc.identifier.spage377-
dc.identifier.epage392-
dc.textversionpublisher-
dc.sortkey23-
dc.relation.urlhttp://www.dpri.kyoto-u.ac.jp/nenpo/nenpo.html-
dcterms.accessRightsopen access-
dc.identifier.pissn0386-412X-
dc.identifier.jtitle-alternativeDisaster Prevention Research Institute Annuals. Ben
出現コレクション:No.30 B-2

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