National Water-Quality Assessment (NAWQA) Program
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By Bernard T. Nolan, Arthur L. Baehr, and Leon J. Kauffman
[Vadose Zone Journal, vol.2, issue 4, November 2003, p. 677-691]Abstract
Point estimates of groundwater recharge at 48 sediment-coring
locations vary substantially (-18.5-1840 cm yr-1) in a 930-km2 area
of southern New Jersey. Darcian estimates of steady, long-term
recharge made at depth in the unsaturated zone were estimated using
pedotransfer functions of soil texture and interpolated (mapped)
with nonparametric methods to assess aquifer vulnerability in the
area. The probability of exceeding the median recharge (29.1 cm yr-1)
is low in the southwestern and northeastern portions of the study
area and high in the eastern and southeastern portions. Estimated
recharge is inversely related to measured percentage clay and
positively related to the percentage of well-drained soils near
wells. Spatial patterns of recharge estimates, exceedance
probabilities, and clay content indicate that sediment texture
controls recharge in the study area. Relations with land elevation and
a topographic wetness index were statistically insignificant. Nitrate
concentration and atrazine
(6-chloro-N2-ethyl-N4-isopropyl-1,3,5-triazine-2,4-diamine) percentage
detection in samples of shallow groundwater (typically <10 m) are
higher for low recharge sites (<=29.1 cm yr-1) than for high recharge
sites (>29.1 cm yr-1) in agricultural and urban areas. Differences
between high and low recharge sites in these areas are highly
significant for NO3 concentration, but not for atrazine
concentration.
Table of Contents
Materials and methods
Description of Study Area
Point Recharge Estimates
Mapping and Spatial Analysis Techniques
Water Quality Relations
Results and discussion
Uncertainty of Recharge Estimates
Application of Geostatistical Techniques
Potential Causes of Recharge Variability
Relation of Recharge to Shallow Groundwater Quality
Verification of Recharge Map
Conclusions
Acknowledgments
References