From the Proceedings of the 1975 Meetings of the Arizona Section - American Water Resources Assn. and the Hydrology Section - Arizona Academy of Science - April 11-12, 1975, Tempe, Arizona / Gas which effervesces from groundwater from Flagstaff's municipal wells is derived from dissolved atmospheric air. Groundwater from the Coconino aquifer at the flagstaff municipal wells is classified as calcium magnesium bicarbonate sulfate water and is similar to groundwater pumped from the Coconino aquifer by other wells in the flagstaff area. The source of the gas which effervesces from groundwater pumped by the municipal wells is believed to be air which is trapped in the Coconino aquifer during recharge.
Identifer | oai:union.ndltd.org:arizona.edu/oai:arizona.openrepository.com:10150/300514 |
Date | 12 April 1975 |
Creators | Germ, John C., Montgomery, Errol L. |
Contributors | Northern Arizona University, Flagstaff |
Publisher | Arizona-Nevada Academy of Science |
Source Sets | University of Arizona |
Language | en_US |
Detected Language | English |
Type | text, Proceedings |
Rights | Copyright ©, where appropriate, is held by the author. |
Page generated in 0.002 seconds