ABSTRACT
This work suggests that iron played a critical and dual role in determining the amount of oxalate (C2O42–) and phosphate (PO43–) that formed and persisted in the low-pressure saturated steam from the thermal breakdown of phosphonate which somehow entered the water/steam cycle. The first is a catalytic role in a thermal oxidative and/or hydrolytic breakdown of the phosphonate, which is shown clearly by the strong and steep linear relationships with C2O42– and PO43– as dependent variables from bivariate analyses involving subsets of the full data at the early stages of the incident when the iron concentration was low (≤ 47 µg ⋅ L–1). The phosphonate concentration for this scenario was presumably high as it resulted in a large yield of the two breakdown products. Second, iron may have also played the role of a counter-ion in precipitating sparingly soluble iron(II,III)-C2O42– and iron(II,III)-PO43– salts and/or as a catalyst in the conversion of soluble C2O42– into lower molecular or gaseous products like CO2, which was observable in the more gradual linear relationships with C2O42– and PO43– from the bivariate analyses, which involved most of the data throughout the incident period where the iron concentration covered a wide range ≈ 5 to 5 835 µg ⋅ L–1. The temperature and pressure dependence of C2O42– and PO43– formation and transformation in the low-pressure saturated steam due to phosphonates shows shifting correlations (positive/negative) at a threshold temperature of 160 °C and threshold pressure of 504 kPa, and coincides with the drum inlet temperature threshold of 137 °C. However, there is evidence that C2O42– and PO43– could be formed and persist in the low-pressure saturated steam beyond the threshold temperature (160 °C) without deposition and/or decomposition when in lower concentrations (projected as ≤ 62 µg ⋅ L–1 and ≤ 134 µg ⋅ L–1, respectively, based on a previously proposed C2O42–/PO43– molar ratio of ≈ 0.5 for their formation from the phosphonate).
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