Temperature Dependence of Excited State Proton Transfer in Ice
We have studied the excited-state proton-transfer rate of four photoacids in ice as a function of temperature. For all four photoacids, we have found a non Arrhenius behavior of the proton-transfer rate constant, k PT. d(ln k PT)/d(1/T) decreases as the temperature decreases. The average slope of ln...
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Veröffentlicht in: | The journal of physical chemistry. A, Molecules, spectroscopy, kinetics, environment, & general theory Molecules, spectroscopy, kinetics, environment, & general theory, 2007-06, Vol.111 (23), p.4998-5007 |
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creator | Leiderman, Pavel Uritski, Anna Huppert, Dan |
description | We have studied the excited-state proton-transfer rate of four photoacids in ice as a function of temperature. For all four photoacids, we have found a non Arrhenius behavior of the proton-transfer rate constant, k PT. d(ln k PT)/d(1/T) decreases as the temperature decreases. The average slope of ln(k PT)versus 1/T depends on the photoacid strength (pK*). The stronger the photoacid is, the smaller the slope. For the strongest photoacid 2-naphthol-6,8-disulfonate (2N68DS) the largest slope is 35 kJ/mol at about 270 K, and the smallest measured slope is about 8 kJ/mol at about 215 K. We propose that the temperature dependence of k PT in ice at the temperature range 270 > T > 200 K can be explained as arising from contributions of two proton-transfer mechanisms over the barrier and tunneling under the barrier. At very low temperatures T < 200 K, the slope of ln(k PT) versus 1/T increases again. At about 170 K, the proton-transfer rate is much slower than the radiative rate, and the deprotonated form of the photoacid cannot be detected in the steady-state emission spectrum. At lower temperatures, T < 200 K, the rate further decreases because of a limitation on the reaction caused by the restrictions on the H2O hydrogen reorientations. |
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For all four photoacids, we have found a non Arrhenius behavior of the proton-transfer rate constant, k PT. d(ln k PT)/d(1/T) decreases as the temperature decreases. The average slope of ln(k PT)versus 1/T depends on the photoacid strength (pK*). The stronger the photoacid is, the smaller the slope. For the strongest photoacid 2-naphthol-6,8-disulfonate (2N68DS) the largest slope is 35 kJ/mol at about 270 K, and the smallest measured slope is about 8 kJ/mol at about 215 K. We propose that the temperature dependence of k PT in ice at the temperature range 270 > T > 200 K can be explained as arising from contributions of two proton-transfer mechanisms over the barrier and tunneling under the barrier. At very low temperatures T < 200 K, the slope of ln(k PT) versus 1/T increases again. At about 170 K, the proton-transfer rate is much slower than the radiative rate, and the deprotonated form of the photoacid cannot be detected in the steady-state emission spectrum. At lower temperatures, T < 200 K, the rate further decreases because of a limitation on the reaction caused by the restrictions on the H2O hydrogen reorientations.</description><identifier>ISSN: 1089-5639</identifier><identifier>EISSN: 1520-5215</identifier><identifier>DOI: 10.1021/jp070424g</identifier><identifier>PMID: 17518449</identifier><language>eng</language><publisher>United States: American Chemical Society</publisher><ispartof>The journal of physical chemistry. 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A, Molecules, spectroscopy, kinetics, environment, & general theory</title><addtitle>J. Phys. Chem. A</addtitle><description>We have studied the excited-state proton-transfer rate of four photoacids in ice as a function of temperature. For all four photoacids, we have found a non Arrhenius behavior of the proton-transfer rate constant, k PT. d(ln k PT)/d(1/T) decreases as the temperature decreases. The average slope of ln(k PT)versus 1/T depends on the photoacid strength (pK*). The stronger the photoacid is, the smaller the slope. For the strongest photoacid 2-naphthol-6,8-disulfonate (2N68DS) the largest slope is 35 kJ/mol at about 270 K, and the smallest measured slope is about 8 kJ/mol at about 215 K. We propose that the temperature dependence of k PT in ice at the temperature range 270 > T > 200 K can be explained as arising from contributions of two proton-transfer mechanisms over the barrier and tunneling under the barrier. At very low temperatures T < 200 K, the slope of ln(k PT) versus 1/T increases again. At about 170 K, the proton-transfer rate is much slower than the radiative rate, and the deprotonated form of the photoacid cannot be detected in the steady-state emission spectrum. At lower temperatures, T < 200 K, the rate further decreases because of a limitation on the reaction caused by the restrictions on the H2O hydrogen reorientations.</description><issn>1089-5639</issn><issn>1520-5215</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2007</creationdate><recordtype>article</recordtype><recordid>eNpt0E1Lw0AQBuBFFFurB_-A5KLgIbqb_cjmIkhbbaVgodHrstmdSGqbxN0E6r83klIvnmZgHt6BF6FLgu8Ijsj9usYxZhH7OEJDwiMc8ojw427HMgm5oMkAnXm_xhgTGrFTNCAxJ5KxZIgeUtjW4HTTOggmUENpoTQQVHkw3ZmiARusGt1AsHRVU5VB6nTpc3BBUQZzA-foJNcbDxf7OUJvT9N0PAsXr8_z8eMi1JSTJqSCUhBWxpLgPDMxYVgzg7mkLDGJzrUVRBsJkksdRcbmnEbSZhkj1FCTWTpCN31u7aqvFnyjtoU3sNnoEqrWqxgLTITEHbztoXGV9w5yVbtiq923Ilj9lqUOZXX2ah_aZluwf3LfTgfCHhS-gd3hrt2nEjGNuUqXKzV5WUr6PhFq1vnr3mvj1bpqXdl18s_jH1DBfpU</recordid><startdate>20070614</startdate><enddate>20070614</enddate><creator>Leiderman, Pavel</creator><creator>Uritski, Anna</creator><creator>Huppert, Dan</creator><general>American Chemical Society</general><scope>BSCLL</scope><scope>NPM</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7X8</scope></search><sort><creationdate>20070614</creationdate><title>Temperature Dependence of Excited State Proton Transfer in Ice</title><author>Leiderman, Pavel ; Uritski, Anna ; Huppert, Dan</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a351t-3633e6d87810fbc7140a4c058349c9afad61ac8e858a22cdf5328dbb413c3cbd3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2007</creationdate><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Leiderman, Pavel</creatorcontrib><creatorcontrib>Uritski, Anna</creatorcontrib><creatorcontrib>Huppert, Dan</creatorcontrib><collection>Istex</collection><collection>PubMed</collection><collection>CrossRef</collection><collection>MEDLINE - Academic</collection><jtitle>The journal of physical chemistry. A, Molecules, spectroscopy, kinetics, environment, & general theory</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Leiderman, Pavel</au><au>Uritski, Anna</au><au>Huppert, Dan</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Temperature Dependence of Excited State Proton Transfer in Ice</atitle><jtitle>The journal of physical chemistry. A, Molecules, spectroscopy, kinetics, environment, & general theory</jtitle><addtitle>J. Phys. Chem. A</addtitle><date>2007-06-14</date><risdate>2007</risdate><volume>111</volume><issue>23</issue><spage>4998</spage><epage>5007</epage><pages>4998-5007</pages><issn>1089-5639</issn><eissn>1520-5215</eissn><abstract>We have studied the excited-state proton-transfer rate of four photoacids in ice as a function of temperature. For all four photoacids, we have found a non Arrhenius behavior of the proton-transfer rate constant, k PT. d(ln k PT)/d(1/T) decreases as the temperature decreases. The average slope of ln(k PT)versus 1/T depends on the photoacid strength (pK*). The stronger the photoacid is, the smaller the slope. For the strongest photoacid 2-naphthol-6,8-disulfonate (2N68DS) the largest slope is 35 kJ/mol at about 270 K, and the smallest measured slope is about 8 kJ/mol at about 215 K. We propose that the temperature dependence of k PT in ice at the temperature range 270 > T > 200 K can be explained as arising from contributions of two proton-transfer mechanisms over the barrier and tunneling under the barrier. At very low temperatures T < 200 K, the slope of ln(k PT) versus 1/T increases again. At about 170 K, the proton-transfer rate is much slower than the radiative rate, and the deprotonated form of the photoacid cannot be detected in the steady-state emission spectrum. At lower temperatures, T < 200 K, the rate further decreases because of a limitation on the reaction caused by the restrictions on the H2O hydrogen reorientations.</abstract><cop>United States</cop><pub>American Chemical Society</pub><pmid>17518449</pmid><doi>10.1021/jp070424g</doi><tpages>10</tpages></addata></record> |
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title | Temperature Dependence of Excited State Proton Transfer in Ice |
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