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A new approach for chemical oxygen demand (COD) measurement at high salinity and low organic matter samples

dc.contributor.authorKayaalp, Necati
dc.contributor.authorErsahin, Mustafa Evren
dc.contributor.authorOzgun, Hale
dc.contributor.authorKoyuncu, Ismail
dc.contributor.authorKinaci, Cumali
dc.contributor.ituauthorErşahin, Mustafa Evren
dc.contributor.ituauthorÖzgün, Erşahin Hale
dc.contributor.ituauthorKoyuncu, İsmail
dc.date.accessioned2026-01-24T14:34:06Z
dc.date.issued2010-05-23
dc.description.abstractChemical oxygen demand (COD) is used as a discharge standard parameter in wastewater treatment plant design, environmental modelling and many other applications. Chloride interference is an important problem of COD measurement for wastewaters containing low organic matter and high chloride concentrations. In case of chloride concentrations up to 2,000 mg/L, mercury sulphate addition at a ratio of 10:1 (HgSO(4):Cl(-)) can adequately mask the interference. When chloride concentration exceeds 2,000 mg/L, this ratio becomes ineffective to hinder the interference. At this point, it is proposed to use a greater and constant ratio of mercury sulphate addition. However, this application sometimes results in extra mercury sulphate addition which is not necessary. Even in some cases, greater addition of mercury sulphate alone is not a solution to erroneous measurement results. The purpose of the study is to determine optimum HgSO(4):Cl(-) ratios according to the chloride concentrations of the samples and to show the importance of the strength of the digestion solution for the correct determination of the COD parameter.CODs of the synthetic samples containing varying COD and chloride concentrations were measured by closed reflux colorimetric method using three digestion solutions having different strengths.It is indicated in this study that a constant ratio of mercury sulphate can only prevent chloride interference up to a specific chloride concentration.Achieving high precision results in case of low organic matter and high chloride concentration can only be possible by both decreasing the concentration of oxidant and adding mercury sulphate.
dc.description.urihttps://doi.org/10.1007/s11356-010-0341-z
dc.description.urihttps://pubmed.ncbi.nlm.nih.gov/20496007
dc.description.urihttps://dx.doi.org/10.1007/s11356-010-0341-z
dc.description.urihttps://aperta.ulakbim.gov.tr/record/25391
dc.identifier.doi10.1007/s11356-010-0341-z
dc.identifier.eissn1614-7499
dc.identifier.endpage1552
dc.identifier.issn0944-1344
dc.identifier.openairedoi_dedup___::0577442b500c8bc0a806b61a553553b2
dc.identifier.orcid0000-0002-6136-5025
dc.identifier.orcid0000-0003-1607-0524
dc.identifier.orcid0000-0001-8784-8351
dc.identifier.orcid0000-0001-8354-1889
dc.identifier.startpage1547
dc.identifier.urihttps://hdl.handle.net/11527/33419
dc.identifier.volume17
dc.language.isoeng
dc.publisherSpringer Science and Business Media LLC
dc.relation.ispartofEnvironmental Science and Pollution Research
dc.rightsOPEN
dc.sdg.typeGoal 6: Clean Water and Sanitation
dc.sdg.typeGoal 11: Sustainable Cities and Communities
dc.subjectSalinity
dc.subjectMercury Compounds
dc.subjectSulfates
dc.subjectOxygen
dc.subjectChlorides
dc.subjectParticulate Matter
dc.subjectWater Pollutants, Chemical
dc.subjectEnvironmental Monitoring
dc.titleA new approach for chemical oxygen demand (COD) measurement at high salinity and low organic matter samples
dc.typeArticle
dspace.entity.typePublication
person.identifier.orcid0000-0003-1607-0524
person.identifier.orcid0000-0001-8784-8351
person.identifier.orcid0000-0001-8354-1889

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