Molecular dynamics investigation of ferrous-ferric electron transfer in a hydrolyzing aqueous solution: Calculation of the pH dependence of the diabatic transfer barrier and the potential of mean force

被引:34
作者
Rustad, JR [1 ]
Rosso, KM [1 ]
Felmy, AR [1 ]
机构
[1] Pacific NW Natl Lab, Richland, WA 99352 USA
关键词
D O I
10.1063/1.1687318
中图分类号
O64 [物理化学(理论化学)、化学物理学];
学科分类号
070304 ; 081704 ;
摘要
We present a molecular model for ferrous-ferric electron transfer in an aqueous solution that accounts for electronic polarizability and exhibits spontaneous cation hydrolysis. An extended Lagrangian technique is introduced for carrying out calculations of electron-transfer barriers in polarizable systems. The model predicts that the diabatic barrier to electron transfer increases with increasing pH, due to stabilization of the Fe3+ by fluctuations in the number of hydroxide ions in its first coordination sphere, in much the same way as the barrier would increase with increasing dielectric constant in the Marcus theory. We have also calculated the effect of pH on the potential of mean force between two hydrolyzing ions in aqueous solution. As expected, increasing pH reduces the potential of mean force between the ferrous and ferric ions in the model system. The magnitudes of the predicted increase in diabatic transfer barrier and the predicted decrease in the potential of mean force nearly cancel each other at the canonical transfer distance of 0.55 nm. Even though hydrolysis is allowed in our calculations, the distribution of reorganization energies has only one maximum and is Gaussian to an excellent approximation, giving a harmonic free energy surface in the reorganization energy F(DeltaE) with a single minimum. There is thus a surprising amount of overlap in electron-transfer reorganization energies for Fe2+-Fe(H2O)(6)(3+), Fe2+-Fe(OH)(H2O)(5)(2+), and Fe2+-Fe(OH)(2)(H2O)(+) couples, indicating that fluctuations in hydrolysis state can be viewed on a continuum with other solvent contributions to the reorganization energy. There appears to be little justification for thinking of the transfer rate as arising from the contributions of different hydrolysis states. Electronic structure calculations indicate that Fe(H2O)(6)(2+)-Fe(OH)(n)(H2O)(6-n)((3-n)+) complexes interacting through H3O2- bridges do not have large electronic couplings. (C) 2004 American Institute of Physics.
引用
收藏
页码:7607 / 7615
页数:9
相关论文
共 31 条
[21]   Molecular simulation of the magnetite-water interface [J].
Rustad, JR ;
Felmy, AR ;
Bylaska, EJ .
GEOCHIMICA ET COSMOCHIMICA ACTA, 2003, 67 (05) :1001-1016
[22]   Molecular models of surface relaxation, hydroxylation, and surface charging at oxide-water interfaces [J].
Rustad, JR .
MOLECULAR MODELING THEORY: APPLICATIONS IN THE GEOSCIENCES, 2001, 42 :169-197
[23]   MOLECULAR-DYNAMICS SIMULATION OF IRON(III) AND ITS HYDROLYSIS PRODUCTS IN AQUEOUS-SOLUTION [J].
RUSTAD, JR ;
HAY, BP ;
HALLEY, JW .
JOURNAL OF CHEMICAL PHYSICS, 1995, 102 (01) :427-431
[24]   MOLECULAR-DYNAMICS STUDIES OF COMPLEXING IN BINARY MOLTEN-SALTS WITH POLARIZABLE ANIONS - MAX4 [J].
SABOUNGI, ML ;
RAHMAN, A ;
HALLEY, JW ;
BLANDER, M .
JOURNAL OF CHEMICAL PHYSICS, 1988, 88 (09) :5818-5823
[25]   Reduction of hexavalent chromium by ferrous iron [J].
Sedlak, DL ;
Chan, PG .
GEOCHIMICA ET COSMOCHIMICA ACTA, 1997, 61 (11) :2185-2192
[26]   THE EXCHANGE REACTION BETWEEN THE 2 OXIDATION STATES OF IRON IN ACID SOLUTION [J].
SILVERMAN, J ;
DODSON, RW .
JOURNAL OF PHYSICAL CHEMISTRY, 1952, 56 (07) :846-852
[27]   A NEW DETERMINATION OF THE STRUCTURE OF WATER AT 25-DEGREES-C [J].
SOPER, AK ;
PHILLIPS, MG .
CHEMICAL PHYSICS, 1986, 107 (01) :47-60
[28]   POLARIZATION MODEL FOR WATER AND ITS IONIC DISSOCIATION PRODUCTS [J].
STILLINGER, FH ;
DAVID, CW .
JOURNAL OF CHEMICAL PHYSICS, 1978, 69 (04) :1473-1484
[29]   THE THEORY OF THE FE2+-FE3+ ELECTRON EXCHANGE IN WATER [J].
TEMBE, BL ;
FRIEDMAN, HL ;
NEWTON, MD .
JOURNAL OF CHEMICAL PHYSICS, 1982, 76 (03) :1490-1507
[30]   REDOX PROCESSES CATALYZED BY HYDROUS OXIDE SURFACES [J].
WEHRLI, B ;
SULZBERGER, B ;
STUMM, W .
CHEMICAL GEOLOGY, 1989, 78 (3-4) :167-179