ISSN:
1572-8927
Keywords:
Fe(II)
;
oxidation
;
H2O2
;
ionic strength
;
NaCl
;
NaClO4
Source:
Springer Online Journal Archives 1860-2000
Topics:
Chemistry and Pharmacology
Notes:
Abstract The oxidation of Fe(II) with H2O2 has been measured in NaCl and NaClO4 solutions as a function of pH, temperature T (K) and ionic strength (M, mol-L−1). The rate constants, k (M−1-sec−1), d[Fe(II)]/DT=-k[Fe(II)][2O2] at pH=6.5 have been fitted to equations of the form log k = log k0+ AI 1/2+BI+CI 1/2/T Where log k0=15.53-3425/T in water; A=−2.3, −1.35; B=0.334, 0.180; and C=391, 235, respectively, for NaCl (σ=0.09) and NaClO4 (σ =0.08). Measurements made in NaCl solutions with added anions yield rates in the order B(OH) 4 − 〉HCO 3 − 〉ClO 4 − 〉Cl−〉NO 3 − 〉SO 4 2− and are attributed to the relative strength of the interactions of Fe2+ or FeOH+ with these anions. The FeB(OH) 4 + species is more reactive while the FeCO 3 0 , FeCl+, FeNO 3 + and FeSO 4 0 species are less reactive than the FeOH+ ion pair. The general trend is similar to our earlier studies of the oxidation of Fe(II) with O2 except for B(OH) 4 − . The effect of pH on the logk was found to be a quadratic function of the concentration of H+ or OH− from pH=4 to 8. These results have been attributed to the different rate constants for Fe2+ (k0) and FeOH+ (k1) which are related to the measured k by, k=k0αFe + k1αFeOH, where αi is the molar fraction of species i. The rates increase due to the greater reactivity of FeOH+ compared to Fe2+. k0 is independent of composition and ionic strength but k1 is a function of ionic strength and composition due to the interactions of FeOH+ with various anions.
Type of Medium:
Electronic Resource
URL:
http://dx.doi.org/10.1007/BF00649098
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