Isotope hydrology of southern Nevada groundwater: Stable isotopes and radiocarbon

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Isotope hydrology of southern Nevada groundwater: Stable isotopes and radiocarbon

A new !O map of southern Nevada groundwater shows a systematic decrease in !O of !5‰ from 36" to 39"N latitude. The variation is consistent with higher-latitude recharge following continuous flow paths along north-south trending graben valleys and systematically increasing in !O due to mixing with lower-latitude, higher-!O recharge. The data do not suggest that large masses of groundwater with ...

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ژورنال

عنوان ژورنال: Water Resources Research

سال: 1999

ISSN: 0043-1397

DOI: 10.1029/1998wr900040