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Homogeneous porous silica for positronium production in AEgIS
Positronium (Ps) formation measurements in homogeneous porous silica (Xerogel of 85 mg cm−3 and swollen MCM-41 of 390 mg cm−3) were performed at different temperatures (8K–293K) by means of a variable energy positron beam equipped with a Ge detector. The results indicate that Xerogel and swollen MCM...
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Published in: | Journal of physics. Conference series 2011-01, Vol.262 (1), p.012020-4 |
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container_title | Journal of physics. Conference series |
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creator | Ferragut, R Dupasquier, A Calloni, A Consolati, G Quasso, F Petkov, M P Jones, S M Galarneau, A Di Renzo, F |
description | Positronium (Ps) formation measurements in homogeneous porous silica (Xerogel of 85 mg cm−3 and swollen MCM-41 of 390 mg cm−3) were performed at different temperatures (8K–293K) by means of a variable energy positron beam equipped with a Ge detector. The results indicate that Xerogel and swollen MCM-41 samples have a high Ps production, which is independent on the temperature. An estimation of the ortho-Ps mean diffusion length was obtained by measuring samples capped with an Al film (~110 nm). An efficient formation of cooled Ps atoms is a requisite for efficient production of antihydrogen, with the aim of a direct measurement of the Earth gravitational acceleration of antimatter, a primary scientific goal of AEgIS (Antimatter Experiment: gravity, Interferometry, Spectroscopy, CERN). Porous materials with open pores at the surface are necessary to produce a high yield of Ps atoms as well as to cool Ps through collisions with the inner walls of the pores before emerging in the free space outside the target. The results indicate that Xerogel and swollen MCM-41 are good candidates for an efficient formation of cold Ps atoms within the framework of the AEgIS project. |
doi_str_mv | 10.1088/1742-6596/262/1/012020 |
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The results indicate that Xerogel and swollen MCM-41 samples have a high Ps production, which is independent on the temperature. An estimation of the ortho-Ps mean diffusion length was obtained by measuring samples capped with an Al film (~110 nm). An efficient formation of cooled Ps atoms is a requisite for efficient production of antihydrogen, with the aim of a direct measurement of the Earth gravitational acceleration of antimatter, a primary scientific goal of AEgIS (Antimatter Experiment: gravity, Interferometry, Spectroscopy, CERN). Porous materials with open pores at the surface are necessary to produce a high yield of Ps atoms as well as to cool Ps through collisions with the inner walls of the pores before emerging in the free space outside the target. 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Porous materials with open pores at the surface are necessary to produce a high yield of Ps atoms as well as to cool Ps through collisions with the inner walls of the pores before emerging in the free space outside the target. The results indicate that Xerogel and swollen MCM-41 are good candidates for an efficient formation of cold Ps atoms within the framework of the AEgIS project.</description><subject>Acceleration</subject><subject>Antihydrogen</subject><subject>Antimatter</subject><subject>Atomic beam spectroscopy</subject><subject>Diffusion length</subject><subject>Formations</subject><subject>Physics</subject><subject>Porosity</subject><subject>Porous materials</subject><subject>Positron beams</subject><subject>Positronium</subject><subject>Silicon dioxide</subject><subject>Synchrotrons</subject><subject>Xerogels</subject><issn>1742-6596</issn><issn>1742-6588</issn><issn>1742-6596</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2011</creationdate><recordtype>article</recordtype><sourceid>PIMPY</sourceid><recordid>eNqNkEFLwzAYhoMoOKd_QQpevNTmS9KkPXgYY-pg4EE9hzZNR0bb1KQ9-O9NrYjIDubyheR5P14ehK4B3wHOsgQEIzFPc54QThJIMBBM8Ala_Hyc_rqfowvvDxjTcMQC3T_Z1u51p-3oo966aXjTGFVEtXXhxZvB2c6MbdQ7W41qMLaLTBetNvvtyyU6q4vG66vvuURvD5vX9VO8e37crle7WDHGhrhIBctTWmccFMkBV1rruqzKMoO0Yhogg4pARgXBCijXrCpwWqqc6ZwKrRRdott5b-jwPmo_yNZ4pZum-CougQuRYyw4DujNH_RgR9eFdpKkIieEUAaB4jOlnPXe6Vr2zrSF-5CA5WRVTsLkJEwGqxLkbDUEYQ4a2_8_Ex_JHGVlX9X0E-FrhVI</recordid><startdate>20110101</startdate><enddate>20110101</enddate><creator>Ferragut, R</creator><creator>Dupasquier, A</creator><creator>Calloni, A</creator><creator>Consolati, G</creator><creator>Quasso, F</creator><creator>Petkov, M P</creator><creator>Jones, S M</creator><creator>Galarneau, A</creator><creator>Di Renzo, F</creator><general>IOP Publishing</general><scope>AAYXX</scope><scope>CITATION</scope><scope>8FD</scope><scope>8FE</scope><scope>8FG</scope><scope>ABUWG</scope><scope>AFKRA</scope><scope>ARAPS</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BGLVJ</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>H8D</scope><scope>HCIFZ</scope><scope>L7M</scope><scope>P5Z</scope><scope>P62</scope><scope>PIMPY</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PRINS</scope><scope>7U5</scope><scope>8BQ</scope><scope>JG9</scope></search><sort><creationdate>20110101</creationdate><title>Homogeneous porous silica for positronium production in AEgIS</title><author>Ferragut, R ; Dupasquier, A ; Calloni, A ; Consolati, G ; Quasso, F ; Petkov, M P ; Jones, S M ; Galarneau, A ; Di Renzo, F</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c444t-a574953f861c2910deeefbdbb815d4e1181d2183720c136e4da05bc94e937ecc3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2011</creationdate><topic>Acceleration</topic><topic>Antihydrogen</topic><topic>Antimatter</topic><topic>Atomic beam spectroscopy</topic><topic>Diffusion length</topic><topic>Formations</topic><topic>Physics</topic><topic>Porosity</topic><topic>Porous materials</topic><topic>Positron beams</topic><topic>Positronium</topic><topic>Silicon dioxide</topic><topic>Synchrotrons</topic><topic>Xerogels</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Ferragut, R</creatorcontrib><creatorcontrib>Dupasquier, A</creatorcontrib><creatorcontrib>Calloni, A</creatorcontrib><creatorcontrib>Consolati, G</creatorcontrib><creatorcontrib>Quasso, F</creatorcontrib><creatorcontrib>Petkov, M P</creatorcontrib><creatorcontrib>Jones, S M</creatorcontrib><creatorcontrib>Galarneau, A</creatorcontrib><creatorcontrib>Di Renzo, F</creatorcontrib><collection>CrossRef</collection><collection>Technology Research Database</collection><collection>ProQuest SciTech Collection</collection><collection>ProQuest Technology Collection</collection><collection>ProQuest Central (Alumni)</collection><collection>ProQuest Central</collection><collection>Advanced Technologies & Aerospace Collection</collection><collection>ProQuest Central Essentials</collection><collection>ProQuest Databases</collection><collection>Technology Collection</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central</collection><collection>Aerospace Database</collection><collection>SciTech Premium Collection</collection><collection>Advanced Technologies Database with Aerospace</collection><collection>Advanced Technologies & Aerospace Database</collection><collection>ProQuest Advanced Technologies & Aerospace Collection</collection><collection>Publicly Available Content Database (Proquest) (PQ_SDU_P3)</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>ProQuest Central China</collection><collection>Solid State and Superconductivity Abstracts</collection><collection>METADEX</collection><collection>Materials Research Database</collection><jtitle>Journal of physics. Conference series</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Ferragut, R</au><au>Dupasquier, A</au><au>Calloni, A</au><au>Consolati, G</au><au>Quasso, F</au><au>Petkov, M P</au><au>Jones, S M</au><au>Galarneau, A</au><au>Di Renzo, F</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Homogeneous porous silica for positronium production in AEgIS</atitle><jtitle>Journal of physics. Conference series</jtitle><date>2011-01-01</date><risdate>2011</risdate><volume>262</volume><issue>1</issue><spage>012020</spage><epage>4</epage><pages>012020-4</pages><issn>1742-6596</issn><issn>1742-6588</issn><eissn>1742-6596</eissn><abstract>Positronium (Ps) formation measurements in homogeneous porous silica (Xerogel of 85 mg cm−3 and swollen MCM-41 of 390 mg cm−3) were performed at different temperatures (8K–293K) by means of a variable energy positron beam equipped with a Ge detector. The results indicate that Xerogel and swollen MCM-41 samples have a high Ps production, which is independent on the temperature. An estimation of the ortho-Ps mean diffusion length was obtained by measuring samples capped with an Al film (~110 nm). An efficient formation of cooled Ps atoms is a requisite for efficient production of antihydrogen, with the aim of a direct measurement of the Earth gravitational acceleration of antimatter, a primary scientific goal of AEgIS (Antimatter Experiment: gravity, Interferometry, Spectroscopy, CERN). Porous materials with open pores at the surface are necessary to produce a high yield of Ps atoms as well as to cool Ps through collisions with the inner walls of the pores before emerging in the free space outside the target. The results indicate that Xerogel and swollen MCM-41 are good candidates for an efficient formation of cold Ps atoms within the framework of the AEgIS project.</abstract><cop>Bristol</cop><pub>IOP Publishing</pub><doi>10.1088/1742-6596/262/1/012020</doi><tpages>4</tpages><oa>free_for_read</oa></addata></record> |
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subjects | Acceleration Antihydrogen Antimatter Atomic beam spectroscopy Diffusion length Formations Physics Porosity Porous materials Positron beams Positronium Silicon dioxide Synchrotrons Xerogels |
title | Homogeneous porous silica for positronium production in AEgIS |
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