Measurement of Helium in Fossil Water

摘要

Helium generated deep within the Earth/Es mantle eventually reaches the earth's crust and surface carried in solution from aquifer-gathered fossil water, the concentration level providing a key indicator of the rate of helium generation and transport. Hiden Analytical manufacture the HPR-40 mass spectrometer series specifically for analysis of gaseous species in aqueous solution, using membrane separation interfaces to inhibit water vapour transfer and maximise the transmission of the gaseous species of interest. Hiden now develop a new membrane interface specifically optimised for detection of trace levels of helium in aqueous solution, with detection capability down to 10 picomoles of helium per litre of water.