Ptaquiloside (PTA) is a well-known toxin produced by the bracken fern (Pteridium aquilinum (L.) Kuhn). It is proposed that PTA from bracken stands can leach through soil and sediments into drinking-water reservoirs, thus representing a concern for human health. To predict the persistence of the toxin, a full understanding of the PTA degradation in aqueous environments is important. The kinetics of PTA hydrolysis was examined at 22 degrees C in aqueous buffered solutions (pH 2.88-8.93). The reaction was found to follow first-order kinetics with respect to PTA at all pH and temperature conditions. At pH lower than 4.43 (+/- 0.32), the reaction is acid-mediated, whereas the reaction is base-mediated at pH higher than 6.39 (+/- 0.28). The rate constants for the acid-catalyzed, base-catalyzed, and neutral hydrolysis are 25.70 (+/- 0.96), 4.83 (+/- 0.03) X 10(4), and 9.49 (+/- 6.02) x 10(-4) h(-1), respectively. The PTA hydrolysis at pH 4.46 is strongly dependent on temperature, with an activation energy of 74.4 (+/- 2.6) kJ mol(-1). Stoichiometric calculations, reaction kinetics, and ultraviolet-visible spectrophotometry strongly indicates the formation of an intermediary compound at pH 5.07 and 6.07 via a mechanism comprising two first-order consecutive reactions. Ptaquiloside has the lowest rate of hydrolysis at slightly acidic pH and low temperatures. Therefore, because PTA is not sorbed in soil, slightly acidic sandy soils in cold climates are most prone to PTA leaching to deeper soil layers and aquifers.

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The reductive dechlorination of carbon tetrachloride (CT) by Fe(II)-Fe(III) hydroxide (green rust) intercalated with dodecanoate, Fe(II)(4)Fe(III)(2)(OH)(12)(C(12)H(23)O(2))(2) · yH(2)O (designated GR(C12)), at pH ~ 8 and at room temperature was investigated. CT at concentration levels similar to those found in heavily contaminated groundwater close to polluted industrial sites (14-988 μM) was reduced mainly to the fully dechlorinated products carbon monoxide (CO, yields >54%) and formic acid (HCOOH, yields >6%). Minor formation of chloroform (CF), the only chlorinated degradation product, was also detected (yields <6.3%). Reactions carried out with excess GR followed pseudo first-order kinetics with respect to CT with rate constants ranging from 6.5 × 10(-2) to 0.47 h(-1). These rate constants are comparable to those measured for CT dechlorinations mediated by zerovalent iron. Reduction of the highest concentration of CT (1.4 mM) proceeds until 56% of the Fe(II) sites of GR(C12) was consumed. This reaction ceased after 10 h due to surface passivation of GR(C12).

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Mixed FeIIFeIII hydroxides, commonly referred to as ‘green rusts’ (GRs), are important reactive phases in both man-made and natural geochemical systems. Determinations of the standard Gibbs energy of formation of GRs are needed to understand and predict the occurrence and possible reactions of GRs in these systems. Slow acid titration of crystalline green rust sulfate (GRSO4\$\end{document}) with the formation of magnetite was used as a novel method to determine the standard Gibbs energy of formation of GRSO4\$\end{document}, ΔfGo(GRSO4)\$\end{document}. Aqueous suspensions of GRSO4\$\end{document}, with pH slightly >8, were titrated slowly with 1 M H2SO4 until pH = 3 under strict anoxic conditions. Powder X-ray diffraction and Mössbauer analysis revealed that magnetite was the only solid phase formed during the initial part of the titration, where the equilibrium pH was maintained above 7.0. The ratio of Fe2+ release to consumption of protons confirmed the stoichiometry of dissolution of GRSO4\$\end{document} and the formation of magnetite at equilibrium conditions. The estimate of the absolute value of ΔfGo(GRSO4)\$\end{document} was −3819.43±6.44 kJ mol−1 + y × [ΔfGo(H2O(1))], where y is the number of interlayer water molecules per formula unit. The logarithm of the solubility product, log Ksp, was estimated to be −139.2±4.8 and is invariable with y. Using the new value for ΔfGo(GRSO4)\$\end{document}, the reduction potentials of several GRSO4\$\end{document}-Fe oxide couples were evaluated, with the GRSO4\$\end{document}-magnetite half cell showing the smallest redox potential at pH 7 and free ion activities of 10−3.