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Fig. 5. Comparison of water contents determined from core samples (Washington Group International, 2003) and conductivity data determined by borehole induction geophysics in drill hole R-8. Samples for gravimetric water measurement and conductivity data were collected in the same season (fall). Points on the water abundance curve indicate locations of core samples analyzed. Blue circles highlight water abundance data that deviate most from locally increasing or decreasing trends in conductivity data.
