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Spatial Variability of Groundwater Recharge and its Effect on Shallow Groundwater Quality in Southern New Jersey

Bernard T. Nolan*,a, Arthur L. Baehrb and Leon J. Kauffmanb

a U.S. Geological Survey, 413 National Center, Reston, VA 20192
b U.S. Geological Survey, West Trenton, NJ



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Fig. 1. Glassboro, NJ study area and outcrop of the Kirkwood-Cohansey aquifer.

 


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Fig. 2. Soil coring locations, recharge estimates, and percentage clay in the Glassboro, NJ study area. Percentage clay is from the USDA Soil Survey Geographic database.

 


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Fig. 3. (a) Omnidirectional, experimental variograms of binary recharge indicators for all cut-offs and (b) anisotropic, spherical variogram models corresponding to the 60th percentile cut-off (36.5 cm yr-1).

 


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Fig. 4. Predicted probability of exceeding median recharge (29.1 cm yr-1) in the Glassboro, NJ study area. Conditional cumulative distribution functions (CCDFs) in Fig. 5 were developed for the two locations shown.

 


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Fig. 5. Conditional cumulative distribution functions (CCDFs) corresponding to low and high recharge locations in the Glassboro, NJ study area. The recharge locations corresponding to the CCDFs are shown in Fig. 4.

 


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Fig. 6. Relation between NO3 concentration and estimated recharge in the Glassboro, NJ study area (middle 50% of recharge estimates is shown).

 


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Fig. 7. Distributions of (a, b) NO3 and (c, d) atrazine concentrations in relation to land-use and recharge categories (excludes undeveloped lands). ANOVA p values are based on ranked concentrations.

 


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Fig. 8. Geographic information system overlay of land use and areas with high recharge probability (likely >29.1 cm yr-1) in the Glassboro, NJ study area.

 


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Fig. 9. Distribution of urban wells with and without (validation) recharge estimates in relation to indicator kriging standard deviations associated with kriged map of median recharge indicators.

 





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