USGS · 70161894
Spectrochemical computer analysis - argon-oxygen d-c arc method for silicate rocks
Abstract
Use of an argon-oxygen atmosphere eliminates the interference of cyanogen bands with many sensitive analytical lines. The jet-controlled atmosphere also improves the stability of the arc. These procedural changes, coupled with computerized analysis of the spectra, result in increased detectability, precision, and speed as compared to the former visual semiquantitative technique.
Explore related subjects
Keep this discovery
Explore connections, maps & timelines
A. F. Dorrzapf. 1973. Spectrochemical computer analysis - argon-oxygen d-c arc method for silicate rocks. https://pubs.usgs.gov/publication/70161894
Cite the original work for its findings. Save a collection to share your selection of sources.