期刊
ENVIRONMENTAL FORENSICS
卷 15, 期 1, 页码 66-77出版社
TAYLOR & FRANCIS LTD
DOI: 10.1080/15275922.2013.873097
关键词
Medicine Lake; groundwater; Fall River; magmatic; isotopes
资金
- US Department of Energy by Lawrence Livermore National Laboratory [DE-AC52-07NA27344]
Isotopic measurements of the 34m(3)/s discharge from the Fall River Springs of northern California indicate recharge from 50km upgradient in high elevation regions of Medicine Lake Volcano. Age determinations suggest less than 20-year travel time. Data demonstrate Klamath Basin further north cannot be a recharge source. Mass balance calculations support that annual precipitation on the volcano supplies observed spring discharge, requiring 50%-75% recharge rates. Radiocarbon and delta C-13 of dissolved inorganic carbon indicate 30%-40% is derived from magmatic CO2. Measured excess He-3 is also consistent with the presence of magmatic gas derived from the Quaternary Age Medicine Lake Volcano.
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