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Ground water recharge and flow characterization using multiple isotopes. Stable isotopes of delta(18)O, delta(2)H, and (13)C, radiogenic isotopes of (14)C and (3)H, and ground water chemical compositions were used to distinguish ground water, recharge areas, and possible recharge processes in an arid zone, fault-bounded alluvial aquifer. Recharge mainly occurs through exposed stream channel beds as opposed to subsurface inflow along mountain fronts. This recharge distribution pattern may also occur in other fault-bounded aquifers, with important implications for conceptualization of ground water flow systems, development of ground water models, and ground water resource management. Ground water along the mountain front near the basin margins contains low delta(18)O, (14)C (percent modern... Categories: Publication; Types: Citation, Journal Citation; Tags: Ground Water, Isotopes: analysis, altitude, environmental monitoring, environmental monitoring: methods, All tags... geography, isotopes, isotopes: chemistry, models, seasons, theoretical, water movements, water supply, water supply: analysis, Fewer tags