Experimental evidence for the formation of doubly charged oxide and hydroxide ions in inductively coupled plasma mass spectrometry

Abstract

The formation of doubly charged polyatomic ions in inductively coupled plasma mass spectrometers was investigated using commercially available instruments. The species observed were ThO²⁺ and ThOH²⁺, which were found in similar amounts with the different instruments used in this study, when operated under routine analytical conditions. The signal ratios for ThO²⁺ were between 1.8 × 10^–4 and 4.2 × 10^–4 relative to the singly charged elemental ion and between 1.4 × 10^–2 and 2.2 × 10^–2 relative to the doubly charged elemental ion. The formation of ThOH²⁺ was between 1.1 × 10^–4 and 2.8 × 10^–4 relative to the singly charged elemental ion and between 0.72 × 10^–2 and 1.3 × 10^–2 relative to the doubly charged elemental ion. A mechanism is proposed for the formation of the doubly charged oxide and hydroxide ions that is based on the condensation of the doubly charged elemental ion with water or oxygen molecules in the interface region of the mass spectrometer.