Hydraulic characteristics of sedimentary deposits at the j-parc proton-accelerator, japan

Hydraulic characteristics of sediments were investigated at J-PARC for the purpose of site characterization in relation with the construction of Japan's largest proton-accelerator. A total of 340 samples extracted from 9 exploratory wells were examined by standard laboratory tests and complemen...

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Autores:
H. Gallardo, Adrian
Marui, Atsunao
Tipo de recurso:
Article of journal
Fecha de publicación:
2007
Institución:
Universidad Nacional de Colombia
Repositorio:
Universidad Nacional de Colombia
Idioma:
spa
OAI Identifier:
oai:repositorio.unal.edu.co:unal/34009
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https://repositorio.unal.edu.co/handle/unal/34009
http://bdigital.unal.edu.co/24089/
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Atribución-NoComercial 4.0 Internacional
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spelling Atribución-NoComercial 4.0 InternacionalDerechos reservados - Universidad Nacional de Colombiahttp://creativecommons.org/licenses/by-nc/4.0/info:eu-repo/semantics/openAccesshttp://purl.org/coar/access_right/c_abf2H. Gallardo, Adrian57e41944-8f73-4ccc-85e0-bb63f318a441300Marui, Atsunaofb3f3f17-5d4f-4a5e-af9e-2a847e1720203002019-06-27T23:09:41Z2019-06-27T23:09:41Z2007https://repositorio.unal.edu.co/handle/unal/34009http://bdigital.unal.edu.co/24089/Hydraulic characteristics of sediments were investigated at J-PARC for the purpose of site characterization in relation with the construction of Japan's largest proton-accelerator. A total of 340 samples extracted from 9 exploratory wells were examined by standard laboratory tests and complemented with statistical analyses to quantitatively determine the main terrain attributes. Two main hydro-geological units were recognized, although a number of embedded layers defined amultilevel aquifer. Grain-size distribution derived from sieve analysis and the coefficient of uniformity showed that soils are poorly sorted. On the other hand, hydraulic conductivity was measured by anumber of parameters such as a log-normal distribution. Conductivity was also predicted by empirical formulas, yielding values up to three orders of magnitude higher. Discrepancies were explained interms of soil anisotropy and intrinsic differences in the calculation methods. Based on the Shepherd's approach, a power relationship between permeability and grain size was found at 2 wells. Hydraulicconductivity was also correlated to porosity. However, this  nterdependence was not systematic and therefore, properties at many parts of the profile were considered to be randomly distributed. Finally,logs of electrical conductivity suggested that variations of soil hydraulic properties can be associated to changes in water quality. In spite of the remaining uncertainties, results yielded from the study are useful to better understand the numerical modelling of the subsurface system in the site.application/pdfspaUNIVERSIDAD NACIONAL DE COLOMBIAhttp://revistas.unal.edu.co/index.php/esrj/article/view/21203Universidad Nacional de Colombia Revistas electrónicas UN Earth Sciences Research JournalEarth Sciences Research JournalEarth Sciences Research Journal; Vol. 11, núm. 2 (2007); 139-154 Earth Sciences Research Journal; Vol. 11, núm. 2 (2007); 139-154 2339-3459 1794-6190H. Gallardo, Adrian and Marui, Atsunao (2007) Hydraulic characteristics of sedimentary deposits at the j-parc proton-accelerator, japan. Earth Sciences Research Journal; Vol. 11, núm. 2 (2007); 139-154 Earth Sciences Research Journal; Vol. 11, núm. 2 (2007); 139-154 2339-3459 1794-6190 .Hydraulic characteristics of sedimentary deposits at the j-parc proton-accelerator, japanArtículo de revistainfo:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501http://purl.org/coar/resource_type/c_2df8fbb1http://purl.org/coar/version/c_970fb48d4fbd8a85Texthttp://purl.org/redcol/resource_type/ARTORIGINAL21203-71953-1-PB.pdfapplication/pdf460759https://repositorio.unal.edu.co/bitstream/unal/34009/1/21203-71953-1-PB.pdf217d3616fb8d02e6750d1d22b5773af4MD51THUMBNAIL21203-71953-1-PB.pdf.jpg21203-71953-1-PB.pdf.jpgGenerated Thumbnailimage/jpeg7822https://repositorio.unal.edu.co/bitstream/unal/34009/2/21203-71953-1-PB.pdf.jpg1c3bb7530bd32e9cc2e8cca61fd2bbdaMD52unal/34009oai:repositorio.unal.edu.co:unal/340092023-12-24 23:05:30.988Repositorio Institucional Universidad Nacional de Colombiarepositorio_nal@unal.edu.co
dc.title.spa.fl_str_mv Hydraulic characteristics of sedimentary deposits at the j-parc proton-accelerator, japan
title Hydraulic characteristics of sedimentary deposits at the j-parc proton-accelerator, japan
spellingShingle Hydraulic characteristics of sedimentary deposits at the j-parc proton-accelerator, japan
title_short Hydraulic characteristics of sedimentary deposits at the j-parc proton-accelerator, japan
title_full Hydraulic characteristics of sedimentary deposits at the j-parc proton-accelerator, japan
title_fullStr Hydraulic characteristics of sedimentary deposits at the j-parc proton-accelerator, japan
title_full_unstemmed Hydraulic characteristics of sedimentary deposits at the j-parc proton-accelerator, japan
title_sort Hydraulic characteristics of sedimentary deposits at the j-parc proton-accelerator, japan
dc.creator.fl_str_mv H. Gallardo, Adrian
Marui, Atsunao
dc.contributor.author.spa.fl_str_mv H. Gallardo, Adrian
Marui, Atsunao
description Hydraulic characteristics of sediments were investigated at J-PARC for the purpose of site characterization in relation with the construction of Japan's largest proton-accelerator. A total of 340 samples extracted from 9 exploratory wells were examined by standard laboratory tests and complemented with statistical analyses to quantitatively determine the main terrain attributes. Two main hydro-geological units were recognized, although a number of embedded layers defined amultilevel aquifer. Grain-size distribution derived from sieve analysis and the coefficient of uniformity showed that soils are poorly sorted. On the other hand, hydraulic conductivity was measured by anumber of parameters such as a log-normal distribution. Conductivity was also predicted by empirical formulas, yielding values up to three orders of magnitude higher. Discrepancies were explained interms of soil anisotropy and intrinsic differences in the calculation methods. Based on the Shepherd's approach, a power relationship between permeability and grain size was found at 2 wells. Hydraulicconductivity was also correlated to porosity. However, this  nterdependence was not systematic and therefore, properties at many parts of the profile were considered to be randomly distributed. Finally,logs of electrical conductivity suggested that variations of soil hydraulic properties can be associated to changes in water quality. In spite of the remaining uncertainties, results yielded from the study are useful to better understand the numerical modelling of the subsurface system in the site.
publishDate 2007
dc.date.issued.spa.fl_str_mv 2007
dc.date.accessioned.spa.fl_str_mv 2019-06-27T23:09:41Z
dc.date.available.spa.fl_str_mv 2019-06-27T23:09:41Z
dc.type.spa.fl_str_mv Artículo de revista
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dc.relation.ispartof.spa.fl_str_mv Universidad Nacional de Colombia Revistas electrónicas UN Earth Sciences Research Journal
Earth Sciences Research Journal
dc.relation.ispartofseries.none.fl_str_mv Earth Sciences Research Journal; Vol. 11, núm. 2 (2007); 139-154 Earth Sciences Research Journal; Vol. 11, núm. 2 (2007); 139-154 2339-3459 1794-6190
dc.relation.references.spa.fl_str_mv H. Gallardo, Adrian and Marui, Atsunao (2007) Hydraulic characteristics of sedimentary deposits at the j-parc proton-accelerator, japan. Earth Sciences Research Journal; Vol. 11, núm. 2 (2007); 139-154 Earth Sciences Research Journal; Vol. 11, núm. 2 (2007); 139-154 2339-3459 1794-6190 .
dc.rights.spa.fl_str_mv Derechos reservados - Universidad Nacional de Colombia
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dc.rights.license.spa.fl_str_mv Atribución-NoComercial 4.0 Internacional
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rights_invalid_str_mv Atribución-NoComercial 4.0 Internacional
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dc.publisher.spa.fl_str_mv UNIVERSIDAD NACIONAL DE COLOMBIA
institution Universidad Nacional de Colombia
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