<HashMap><database>biostudies-literature</database><scores/><additional><submitter>Rout SP</submitter><funding>Engineering and Physical Sciences Research Council</funding><pagination>4455</pagination><full_dataset_link>https://www.ebi.ac.uk/biostudies/studies/S-EPMC5849744</full_dataset_link><repository>biostudies-literature</repository><omics_type>Unknown</omics_type><volume>8(1)</volume><pubmed_abstract>&lt;sup>14&lt;/sup>C is an important consideration within safety assessments for proposed geological disposal facilities for radioactive wastes, since it is capable of re-entering the biosphere through the generation of &lt;sup>14&lt;/sup>C bearing gases. The irradiation of graphite moderators in the UK gas-cooled nuclear power stations has led to the generation of a significant volume of &lt;sup>14&lt;/sup>C-containing intermediate level wastes. Some of this &lt;sup>14&lt;/sup>C is present as a carbonaceous deposit on channel wall surfaces. Within this study, the potential of biofilm growth upon irradiated and &lt;sup>13&lt;/sup>C doped graphite at alkaline pH was investigated. Complex biofilms were established on both active and simulant samples. High throughput sequencing showed the biofilms to be dominated by Alcal</pubmed_abstract><journal>Scientific reports</journal><pubmed_title>The Impact of Alkaliphilic Biofilm Formation on the Release and Retention of Carbon Isotopes from Nuclear Reactor Graphite.</pubmed_title><pmcid>PMC5849744</pmcid><funding_grant_id>EP/P006930/1</funding_grant_id><funding_grant_id>EP/I036354/1</funding_grant_id><pubmed_authors>Heard P</pubmed_authors><pubmed_authors>Boxall SA</pubmed_authors><pubmed_authors>Bond G</pubmed_authors><pubmed_authors>Shah P</pubmed_authors><pubmed_authors>Walker S</pubmed_authors><pubmed_authors>Charles C</pubmed_authors><pubmed_authors>Rout SP</pubmed_authors><pubmed_authors>Bills P</pubmed_authors><pubmed_authors>Humphreys PN</pubmed_authors><pubmed_authors>Scott T</pubmed_authors><pubmed_authors>Eccles H</pubmed_authors><pubmed_authors>Williams SJ</pubmed_authors><pubmed_authors>Payne L</pubmed_authors><pubmed_authors>Jackson BR</pubmed_authors><pubmed_authors>Laws AP</pubmed_authors></additional><is_claimable>false</is_claimable><name>The Impact of Alkaliphilic Biofilm Formation on the Release and Retention of Carbon Isotopes from Nuclear Reactor Graphite.</name><description>&lt;sup>14&lt;/sup>C is an important consideration within safety assessments for proposed geological disposal facilities for radioactive wastes, since it is capable of re-entering the biosphere through the generation of &lt;sup>14&lt;/sup>C bearing gases. The irradiation of graphite moderators in the UK gas-cooled nuclear power stations has led to the generation of a significant volume of &lt;sup>14&lt;/sup>C-containing intermediate level wastes. Some of this &lt;sup>14&lt;/sup>C is present as a carbonaceous deposit on channel wall surfaces. Within this study, the potential of biofilm growth upon irradiated and &lt;sup>13&lt;/sup>C doped graphite at alkaline pH was investigated. Complex biofilms were established on both active and simulant samples. High throughput sequencing showed the biofilms to be dominated by Alcal</description><dates><release>2018-01-01T00:00:00Z</release><publication>2018 Mar</publication><modification>2026-05-02T06:47:39.224Z</modification><creation>2019-03-26T23:22:55Z</creation></dates><accession>S-EPMC5849744</accession><cross_references><pubmed>29535412</pubmed><doi>10.1038/s41598-018-22833-5</doi></cross_references></HashMap>