Water Exchange Rates and Molecular Mechanism around Aqueous Halide Ions Harsha V. R. Annapureddy and Liem X. Dang* AUTHOR ADDRESS: Physical Sciences Division, Pacific Northwest National Laboratory, Richland, WA 93352. *[email protected] (509) 375-2557 Activation volumes were evaluated using rate constants computed with different theories at various pressures. GH theory rate Pressure, M Pa Chloride Bromide Iodide k TST , ps !1 ! GH constant RF method ! RF k GH = ! GH k TST 0 1.07 0.043 100 1.20 0.027 200 1.32 0.018 0 1.22 0.034 100 1.33 0.025 200 1.46 0.020 0 1.52 0.035 100 1.64 0.028 200 1.78 0.020 k RF = ! GH k TST 0.10 0.046 0.04 0.033 0.02 0.024 0.09 0.042 0.05 0.033 0.04 0.030 0.09 0.053 0.05 0.047 0.04 0.036 rate constant 0.108 0.052 0.032 0.104 0.070 0.066 0.142 0.074 0.078 As discussed in the manuscript, we computed the activation volumes using the following equation: Using the rate constants computed at different pressures, we plot linear function. The slope obtained from this fitting gives vs. and fit it to a . The plots obtained for TST are provided below. All of the plots exhibit a positive slope, which gives a negative activation volume ( ). !"#$%&'($)%*#*+)!,+("-) /013) !" !! ! !! /01/) -).)/0//15854) ) /052) <,=("&;+) /053) /01/) /01/) -).)/0//12324) ) /052) >"(?&;+) /051) /051) /05/) /0/7) /0/7) /0/3) /0/6) /0/6) /0//) /0/) 1/0/) 6/0/) 2/0/) 7/0/) /0//) /0//) 5//0/) 1/0//) 6/0//) 2/0//) 7/0//) 5//0//) /0//) /0//) -).)/0//59634) ) :(;&;+) 1/0//) 6/0//) 2/0//) 7/0//) 5//0//) P RT Next, we use the same procedure with rate constants obtained from the RF method. Fits to the rate constants obtained from the RF method are provided below. These plots have negative slopes (with some statistical error), which give a positive activation volume ( ). !"#$%&"'()*+',"-./0' !" !! ! !! 4544' 4544' 345;4' ;4544' :4544' <4544' 84544' 644544' ;4544' :4544' <4544' 84544' 644544' 34564' 1'2'345467879+' ' 345:4' 345<4' 1'2'34544<76;+' ' 345;4' 345=4' 34584' 36544' 4544' 4544' P RT 345:4' !"#$%&'() 365;4' 34574' 365:4' 345<4' 4544' 4544' ;4544' :4544' <4544' 84544' 644544' 34564' 345;4' 345=4' 345:4' *%$+&'()) 34574' 1'2'34544>;86+' ' ,$'&'() 345<4' 34594' 34584' Fits obtained using GH theory rate constants are provided below. Similar to the trend observed for the RF method, all the plots yield negative slopes (with some statistical error), which give a positive activation volume ( ). !"#$%&'()%*+,-%#"(+ P RT /0//+ /0//+ 8/0//+ 3/0//+ 6/0//+ 1/0//+ 9//0//+ &/09/+ !! ! !! &/02/+ !" &/08/+ &/07/+ /0//+ /0//+ 8/0//+ 3/0//+ 6/0//+ 1/0//+ 9//0//+ (+.+&/0//12345+ + &/09/+ !"#$%&'() &/08/+ &/03/+ &/06/+ &/09/+ (+.+&/0//384:5+ + *%$+&'() &/02/+ &/08/+ (+.+&/0//37:25+ + ,$'&'()) &/02/+ &/03/+ &/04/+ &/01/+ /0//+ /0//+ 8/0//+ 3/0//+ 6/0//+ 1/0//+ 9//0//+ &/03/+ &/07/+ We followed the same process as reported in the literature by Kerisit and Rosso1 and Rustad and Stack2 who also determined the activation volumes using rate constants from TST, the RF method, and GH theory. From our current studies, we observed that the trend in the variation of rate constants with pressure for GH theory and the RF method is opposite to the trend noticed in TST for all the halide ions. In the case of solvent exchange around aqueous lithium studied previously by our group and also by Rustad and Stack,2 the TST rate constants and transmission coefficients both increase as pressure increases. In their studies, Kerisit and Rosso1 observed that the TST rates and transmission coefficients decrease as pressure increases. Contrary to the two previous observations described above, we observed in this current study that, for halides, TST rates and transmission coefficients have the opposite trend when pressure increases. Because the computed transmission coefficients are very small and they also decrease significantly as pressure increases, the effect on transmission coefficients overshadows the effect of pressure on the activation barrier, thereby resulting in a decrease of rate constants (from GH theory and RF method) as pressure increases. As a result, we noted an opposite sign in activation volumes. We also would like to point out that the rate constants and mechanism of exchange are sensitive to several factors, such as choice of reaction coordinates, potential models, etc. Refrences 1. Kerisit S and KM Rosso. Transition path sampling of water exchange rates and mechanisms around aqueous ions. Journal of Chemical Physics 2009, 131(11):114512. 2. Rustad JR and AG Stack. Molecular dynamics calculation of the activation volume for water exchange on Li. Journal of the American Chemical Society 2006, 128 (46): 14778-14779.
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