Isotope Geochemistry
An electron multiplier is a type of detector used in mass spectrometry that amplifies the signal produced by incoming charged particles, typically ions. It works by using a series of dynodes to generate multiple secondary electrons for each primary electron that strikes them, resulting in a significant increase in detectable current. This amplification is crucial for detecting low-abundance ions, making it an essential component in instruments like thermal ionization mass spectrometry (TIMS).
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