Abstract
A new method for continuous recording of the hydrogen content of atmospheric air is described. The method is based on reduction of mercuric oxide and the determination of the resulting mercury vapor by absorption in the 2537-A line. The standard error of the calibration for 0.5 ppm H2 is 3%. The limit of detection is 0.01 ppm. Preliminary results are discussed.
Sign-in/Register to access full text options 
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
