Please use this identifier to cite or link to this item: http://cmuir.cmu.ac.th/jspui/handle/6653943832/58157
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dc.contributor.authorDong Xiaen_US
dc.contributor.authorKatsumi Okadaen_US
dc.contributor.authorKunio Watanabeen_US
dc.contributor.authorYukiko Miuraen_US
dc.contributor.authorRameshprabu Ramarajen_US
dc.contributor.authorNiwooti Wangchaien_US
dc.contributor.authorKanda Wangchaien_US
dc.contributor.authorTomoaki Itayamaen_US
dc.date.accessioned2018-09-05T04:20:29Z-
dc.date.available2018-09-05T04:20:29Z-
dc.date.issued2018-01-01en_US
dc.identifier.issn13652109en_US
dc.identifier.issn1355557Xen_US
dc.identifier.other2-s2.0-85029076047en_US
dc.identifier.other10.1111/are.13477en_US
dc.identifier.urihttps://www.scopus.com/inward/record.uri?partnerID=HzOxMe3b&scp=85029076047&origin=inwarden_US
dc.identifier.urihttp://cmuir.cmu.ac.th/jspui/handle/6653943832/58157-
dc.description.abstract© 2017 John Wiley & Sons Ltd This study was focused on the effect of magnesium hydroxide (Mg(OH)2) for improving the sediment of aquaculture field and eutrophic closed estuaries. Sediment samples were collected from Omura Bay, Nagasaki, Japan. The change in pH, acid volatile sulphides (AVS) and dissolved organic carbon (DOC) in interstitial water of the sediment samples were measured before and after 20-day incubation under the condition of overlapping seawater at 25°C with 0.3–0.4 mg/L of dissolved oxygen (DO). Hydrogen sulphide (H2S) and the dsrA gene copy number of Grp3 sulphate-reducing bacteria (SRB) in the sediment samples were also measured at 7-day incubation under the same condition. The pH of Mg(OH)2treatment group was significantly increased from 7.43 to 8.25; it was higher compared to the control group which pH was maintained around 7.6. Meanwhile, the AVS content of Mg(OH)2treatment group was significantly reduced and the value was lower than the control group after the 20-day incubation. Each concentration of interstitial water DOC in the treatment group and the control group increased after the incubation from initial value of 15.4–40.1 and 29.0 mg/L respectively. Furthermore, simultaneous decrease in H2S and the dsrA gene copy number of Grp3 SRB was observed at the end of the 7-day incubation by adding Mg(OH)2. It is concluded that the loss of activity of SRB was strongly related to the decrease in sulphide (H2S and AVS) and the increase in DOC was due to the alkalization of the sediment by adding Mg(OH)2.en_US
dc.subjectAgricultural and Biological Sciencesen_US
dc.titleRole of sulphide reduction by magnesium hydroxide on the sediment of the eutrophic closed bayen_US
dc.typeJournalen_US
article.title.sourcetitleAquaculture Researchen_US
article.volume49en_US
article.stream.affiliationsNagasaki Universityen_US
article.stream.affiliationsUbe Material Ind.en_US
article.stream.affiliationsMaejo Universityen_US
article.stream.affiliationsChiang Mai Universityen_US
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