<HashMap><database>NODE</database><scores/><additional><omics_type>Genomics</omics_type><submitter>高 壮</submitter><technology_type>WGS</technology_type><experiment_platform>Illumina NovaSeq 6000</experiment_platform><full_dataset_link>https://www.biosino.org/node/experiment/detail/OEX00027756</full_dataset_link><experiment_library_layout>Paired</experiment_library_layout><experiment_library_selection>RANDOM</experiment_library_selection><experiment_mate_pair>Y</experiment_mate_pair><sample_count>1</sample_count><taxonomy>['uncultured bacteria Geo ensemble']</taxonomy><repository>NODE</repository></additional><is_claimable>false</is_claimable><name>OEX_高_2404202217</name><description>The reactor can use both organic matter in the water and hydrogen reduced by the cathode as an electron supply for sulfate reduction. A 40h hydraulic retention time (HRT) yielded a 33.6% higher sulfate reduction rate in R4 than in R1. Sufficiently prolonged HRT has a negative effect on sulfate reduction. When the COD/SO42- influent ratio decreased from 1.7 to 1.3, sulfate removal rate decreased from 70.47% to 32.82%. Optimal conditions for reactor operation were an HRT of 60 h, COD/sulfate ratio of 1.7, and current of 50 mA. These conditions achieved a sulfate removal rate of 70.47% and a COD removal rate of 85.58%. The reactor had higher abundance of Proteobacteria, Bacteroidetes, Euryarchaeota, and Chloroflexi phyla.</description><dates><publication>2024-06-19</publication><submission>2024-04-20</submission></dates><accession>OEX00027756</accession><cross_references><NODE>OEP00005225</NODE></cross_references></HashMap>