“…To accomplish these objectives, pyrene removal experiments were performed at various temperatures in the presence of redox active or redox inactive minerals, and with or without water present. Pyrene was selected as the probe compound for this study because it is representative of the broad class of non-substituted PAHs, should not transform on its own at the temperatures used in this study, 26 has been shown to undergo both degradation and transformation to higher molecular weight compounds in the presence of soil, 5 and is an environmentally relevant pollutant. Some of the most common minerals in soil are silicates (e.g., quartz), feldspars, micas, carbonates, clay, and metal oxides.…”