흄산의 침적에 미치는 금속이온의 영향
In the presence of metal ions(Co(Ⅱ), Ni(Ⅱ), Sr(Ⅱ), Cu(Ⅱ), Fe(Ⅲ), U(Ⅵ)), the sedimentation of humic acid was increased at constant pH with increasing metal concentration and the strength was increased in the following order: Sr < Ni < Co < Cu < Fe < U. At constant metal concentration,...
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Veröffentlicht in: | Journal of the Korean Chemical Society 1996, Vol.40 (1), p.50-58 |
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creator | 박영재(Yeong-Jae Park) 박경균(Kyoung-Kyun Park) 전관식(Kwan-Sik Chun) |
description | In the presence of metal ions(Co(Ⅱ), Ni(Ⅱ), Sr(Ⅱ), Cu(Ⅱ), Fe(Ⅲ), U(Ⅵ)), the sedimentation of humic acid was increased at constant pH with increasing metal concentration and the strength was increased in the following order: Sr < Ni < Co < Cu < Fe < U. At constant metal concentration, Cu(Ⅱ), Ni(Ⅱ), and Co(Ⅱ) ions caused an increase in sedimentation of humic acid as the solution pH increased, whereas Fe(Ⅲ) and U(Ⅵ) ions caused a decrease. Sr(Ⅱ) ions did not affect the sedimentation even with the variation of pH. The analysis of FT-IR spectra for the sediments prepared from the reaction between humic acid and metal ions showed that metal ions were bound to humic acid to form complexes, suggesting that the metal complexation plays an important role in the sedimentation of humic acid. 일정한 pH에서 Co(II), Ni(II), Sr(II), Cu(II), Fe(III) 및 U(VI) 등의 금속이온농도가 증가할 수록 흄산의 침적율이 증가하였으며, Sr |
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At constant metal concentration, Cu(Ⅱ), Ni(Ⅱ), and Co(Ⅱ) ions caused an increase in sedimentation of humic acid as the solution pH increased, whereas Fe(Ⅲ) and U(Ⅵ) ions caused a decrease. Sr(Ⅱ) ions did not affect the sedimentation even with the variation of pH. The analysis of FT-IR spectra for the sediments prepared from the reaction between humic acid and metal ions showed that metal ions were bound to humic acid to form complexes, suggesting that the metal complexation plays an important role in the sedimentation of humic acid. 일정한 pH에서 Co(II), Ni(II), Sr(II), Cu(II), Fe(III) 및 U(VI) 등의 금속이온농도가 증가할 수록 흄산의 침적율이 증가하였으며, Sr<Ni<Co<Cu<Fe<U 순으로 증가하였다. 또한, 일정한 금속이온농도에서 pH를 변화시키면서 흄산의 침적율을 측정한 결과, Cu(II), Ni(II) 및 Co(II) 이온의 경우에는 pH가 증가할 수록 흄산의 침적율이 증가한 반면에, Fe(III) 와 U(VI) 이온의 경우에는 오히려 감소하였으며, Sr(II) 이온은 pH가 변하더라도 흄산침적율이 거의 일정하였다. 침적된 흄산의 적외선분광스펙트럼으로부터 금속이온과 흄산간의 착물형성을 확인하였으며, 이러한 착물형성이 흄산의 침적이 일어나기 위한 주요한 메카니즘임을 알수 있었다.]]></description><identifier>ISSN: 1017-2548</identifier><identifier>EISSN: 2234-8530</identifier><language>kor</language><publisher>대한화학회</publisher><ispartof>Journal of the Korean Chemical Society, 1996, Vol.40 (1), p.50-58</ispartof><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>230,314,776,780,881,4010</link.rule.ids></links><search><creatorcontrib>박영재(Yeong-Jae Park)</creatorcontrib><creatorcontrib>박경균(Kyoung-Kyun Park)</creatorcontrib><creatorcontrib>전관식(Kwan-Sik Chun)</creatorcontrib><title>흄산의 침적에 미치는 금속이온의 영향</title><title>Journal of the Korean Chemical Society</title><addtitle>Journal of the Korean Chemical Society</addtitle><description><![CDATA[In the presence of metal ions(Co(Ⅱ), Ni(Ⅱ), Sr(Ⅱ), Cu(Ⅱ), Fe(Ⅲ), U(Ⅵ)), the sedimentation of humic acid was increased at constant pH with increasing metal concentration and the strength was increased in the following order: Sr < Ni < Co < Cu < Fe < U. At constant metal concentration, Cu(Ⅱ), Ni(Ⅱ), and Co(Ⅱ) ions caused an increase in sedimentation of humic acid as the solution pH increased, whereas Fe(Ⅲ) and U(Ⅵ) ions caused a decrease. Sr(Ⅱ) ions did not affect the sedimentation even with the variation of pH. The analysis of FT-IR spectra for the sediments prepared from the reaction between humic acid and metal ions showed that metal ions were bound to humic acid to form complexes, suggesting that the metal complexation plays an important role in the sedimentation of humic acid. 일정한 pH에서 Co(II), Ni(II), Sr(II), Cu(II), Fe(III) 및 U(VI) 등의 금속이온농도가 증가할 수록 흄산의 침적율이 증가하였으며, Sr<Ni<Co<Cu<Fe<U 순으로 증가하였다. 또한, 일정한 금속이온농도에서 pH를 변화시키면서 흄산의 침적율을 측정한 결과, Cu(II), Ni(II) 및 Co(II) 이온의 경우에는 pH가 증가할 수록 흄산의 침적율이 증가한 반면에, Fe(III) 와 U(VI) 이온의 경우에는 오히려 감소하였으며, Sr(II) 이온은 pH가 변하더라도 흄산침적율이 거의 일정하였다. 침적된 흄산의 적외선분광스펙트럼으로부터 금속이온과 흄산간의 착물형성을 확인하였으며, 이러한 착물형성이 흄산의 침적이 일어나기 위한 주요한 메카니즘임을 알수 있었다.]]></description><issn>1017-2548</issn><issn>2234-8530</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>1996</creationdate><recordtype>article</recordtype><sourceid>JDI</sourceid><recordid>eNpFjT9Lw0AYhw9RMNR-hyyOgXvv3veSG0utf4tZuodLcoHQWqTRwbEiIoLgIJol4CJ008Gh_Ur2-h0sKjj9nuHh-W0wTwiJQUSSbzIPOISBIIy2WbuqypSTlGHItfQYrpobd_3hmtp3i5l7nbqXR3_5PneLenn_5H_N79ztg2s-XT37cerp6vlth20VZlTZ9t-22GC_N-geBv344Kjb6QfDSOhAgbRZTjyXRlkSBCYD4gIJtcrSQiBamZFJVWqUUGRR5doUlGmwhsCCbLHd3-ywrC7KZJxXo-S4cxKD1us2KiRQoYj-vfHlpDyzeWmS8zWYyVVyGu_1AAjX71p-A3W_XJ0</recordid><startdate>1996</startdate><enddate>1996</enddate><creator>박영재(Yeong-Jae Park)</creator><creator>박경균(Kyoung-Kyun Park)</creator><creator>전관식(Kwan-Sik Chun)</creator><general>대한화학회</general><scope>DBRKI</scope><scope>TDB</scope><scope>JDI</scope></search><sort><creationdate>1996</creationdate><title>흄산의 침적에 미치는 금속이온의 영향</title><author>박영재(Yeong-Jae Park) ; 박경균(Kyoung-Kyun Park) ; 전관식(Kwan-Sik Chun)</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-k829-613ecd50d3a6e5251ac150245496cbf244e3c5ab6ba6265e46d9af5c91ea51e13</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>kor</language><creationdate>1996</creationdate><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>박영재(Yeong-Jae Park)</creatorcontrib><creatorcontrib>박경균(Kyoung-Kyun Park)</creatorcontrib><creatorcontrib>전관식(Kwan-Sik Chun)</creatorcontrib><collection>DBPIA - 디비피아</collection><collection>DBPIA</collection><collection>KoreaScience</collection><jtitle>Journal of the Korean Chemical Society</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>박영재(Yeong-Jae Park)</au><au>박경균(Kyoung-Kyun Park)</au><au>전관식(Kwan-Sik Chun)</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>흄산의 침적에 미치는 금속이온의 영향</atitle><jtitle>Journal of the Korean Chemical Society</jtitle><addtitle>Journal of the Korean Chemical Society</addtitle><date>1996</date><risdate>1996</risdate><volume>40</volume><issue>1</issue><spage>50</spage><epage>58</epage><pages>50-58</pages><issn>1017-2548</issn><eissn>2234-8530</eissn><abstract><![CDATA[In the presence of metal ions(Co(Ⅱ), Ni(Ⅱ), Sr(Ⅱ), Cu(Ⅱ), Fe(Ⅲ), U(Ⅵ)), the sedimentation of humic acid was increased at constant pH with increasing metal concentration and the strength was increased in the following order: Sr < Ni < Co < Cu < Fe < U. At constant metal concentration, Cu(Ⅱ), Ni(Ⅱ), and Co(Ⅱ) ions caused an increase in sedimentation of humic acid as the solution pH increased, whereas Fe(Ⅲ) and U(Ⅵ) ions caused a decrease. Sr(Ⅱ) ions did not affect the sedimentation even with the variation of pH. The analysis of FT-IR spectra for the sediments prepared from the reaction between humic acid and metal ions showed that metal ions were bound to humic acid to form complexes, suggesting that the metal complexation plays an important role in the sedimentation of humic acid. 일정한 pH에서 Co(II), Ni(II), Sr(II), Cu(II), Fe(III) 및 U(VI) 등의 금속이온농도가 증가할 수록 흄산의 침적율이 증가하였으며, Sr<Ni<Co<Cu<Fe<U 순으로 증가하였다. 또한, 일정한 금속이온농도에서 pH를 변화시키면서 흄산의 침적율을 측정한 결과, Cu(II), Ni(II) 및 Co(II) 이온의 경우에는 pH가 증가할 수록 흄산의 침적율이 증가한 반면에, Fe(III) 와 U(VI) 이온의 경우에는 오히려 감소하였으며, Sr(II) 이온은 pH가 변하더라도 흄산침적율이 거의 일정하였다. 침적된 흄산의 적외선분광스펙트럼으로부터 금속이온과 흄산간의 착물형성을 확인하였으며, 이러한 착물형성이 흄산의 침적이 일어나기 위한 주요한 메카니즘임을 알수 있었다.]]></abstract><pub>대한화학회</pub><tpages>9</tpages><oa>free_for_read</oa></addata></record> |
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title | 흄산의 침적에 미치는 금속이온의 영향 |
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