Abstract

We studied the influence of acid pretreatment on the effective distinction between elemental carbon (EC) and organic carbon (OC), and between char-EC and soot-EC. Though widely employed in the pretreatment of soils and sediments for EC quantification, the use of HCl, HF, and HNO 3 could decrease soot thermal stability as acid remains, leading to an underestimation of soot-EC by thermal methods. We compared thermal optical reflectance (TOR) measurements of EC concentrations in char reference materials and in lacustrine and marine sediments following pretreatment with various acids. The results showed that pretreatment with 2 M HCl, concentrated HNO 3, 7 M HNO 3, and 1 M HNO 3 did not result in EC oxidation. However, hot concentrated HNO 3 oxidized EC significantly, leading to lower concentrations of EC, char-EC and soot-EC. By comparing the removal of potentially interfering materials, which contain little fire-derived carbon, with different acid pretreatments, we recommend the HCl–HF–HCl and concentrated (not hot) HNO 3–HF–HCl pretreatments for the determination of EC, char-EC, and soot-EC in soils and sediments using the TOR method.

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