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interactions at depth to the regional aquifer systems. Faults are
              important conduits for fluid transport and mixing and impart
              a tectonic influence on water quality. The result is a multi-  TRAVEL GRANTS
              porosity system resulting from variable ages and mixing of   TO NEGSA 2019
              meteoric recharge, karst system transport, matrix sandstone
              transport, fault connectivity, and endogenic inputs.   Undergraduate and graduate students who work full-
              Quantitative forecasting of the effects of climate change on
              water quality depends on understanding these deep inputs   time or care for dependents while earning a degree are
              (diminishing surface flows affecting recharge rates), as well   eligible for generous travel funding to attend the GSA
              as aquifer recharge flowpaths and quantities. Results from   Northeastern Section Meeting, 17–19 March 2019, in
              Grand Canyon and other spring-supported stream systems   Portland, Maine, USA. Students from all GSA Sections
              in the western U.S. indicate the need for development of   are welcome to apply before Friday, 22 Feb.
              hydrologic baselines that recognize these complexities.    Questions: Tahlia Bear, tbear@geosociety.org
              This can be accomplished through use of both natural and
              artificial tracers to unravel mixing and environmental   Application link: http://bit.ly/2F4mq15
              sensors to monitor real-time changes. These investments
              are needed to inform water management decisions that
              address societal and ecosystem needs.




























































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