Direct Observations of Nonintegral Hydrous Ferric Oxide Solubility Products: Kso*=[Fe3+][H+]-2.86
Digital Object Identifier (DOI)
Previous studies have indicated that hydrous ferric oxide precipitates, formed and aged at low temperatures, exhibit solubility products of the form K∗S0 = [Fe3+][H+]−m, where m < 3 ([ ] free ion concentration). Although previous observations have either been obtained over a very narrow pH range or have involved phase separations and solution chemical modeling, the present work involves direct potentiometric observations of log [Fe3+] and log [H+] over a wide range of Fe3+ concentrations and pH. Our observations obtained at 25°C in 0.7 molar NaClO4 provide substantial evidence for log [Fe3+] vs. pH relationships with slopes (m) smaller than three but larger than those obtained in previous works (m = 2.70 and m = 2.35). Over a four unit range in pH and a nearly 12 order of magnitude range in [Fe3+] the observed relationship between pH and log [Fe3+] in this work is log [Fe3+] = 4.28 ± 0.05 − (2.86 ± 0.009) pH. This solubility behavior has substantial implications for the behavior of FeIII in natural waters.
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Citation / Publisher Attribution
Geochimica et Cosmochimica Acta, v. 64, issue 11, p. 1873-1877
Scholar Commons Citation
Byrne, Robert H. and Luo, Yu-Ran, "Direct Observations of Nonintegral Hydrous Ferric Oxide Solubility Products: Kso*=[Fe3+][H+]-2.86" (2000). Marine Science Faculty Publications. 1726.