Title of article :
Mercury concentrations in water from an unconfined aquifer
system, New Jersey coastal plain
Author/Authors :
Julia L. Barringera، نويسنده , , *، نويسنده , , Zoltan Szaboa، نويسنده , , Leon J. Kauffmana، نويسنده , , Thomas H. Barringera، نويسنده , ,
Paul E. Stackelberga، نويسنده , , Tamara Ivahnenkob، نويسنده , , Shilpa Rajagopalana، نويسنده , , 1، نويسنده , , David P. Krabbenhoftc، نويسنده ,
Issue Information :
هفته نامه با شماره پیاپی سال 2005
Abstract :
Concentrations of total mercury (Hg) from 2 Ag/L (the USEPA maximum contaminant level) to 72 Ag/L in water from about
600 domestic wells in residential parts of eight counties in southern New Jersey have been reported by State and county
agencies. The wells draw water from the areally extensive (7770 km2) unconfined Kirkwood–Cohansey aquifer system, in
which background concentrations of Hg are about 0.01 Ag/L or less. Hg is present in most aquifer materials at concentrations
b50 Ag/kg, but is at 100–150 Ag/kg in undisturbed surficial soils. No point sources of contamination to the affected areas have
been conclusively identified.
To determine whether high levels of Hg in ground water are related to a particular land use and (or) water chemistry, water
samples from 105 wells that tap the aquifer system were collected by the United States Geological Survey. These included
randomly selected domestic wells, domestic and observation wells in selected land uses, and sets of clustered observation
wells—including two sets that are downgradient from residential areas with Hg-contaminated ground water. Hg concentrations
in filtered samples (Hgf) were at or near background levels in water from most wells, but ranged from 0.1 to 3.8 Ag/L in water
from nearly 20% of wells. Hgf concentrations from 0.0001 to 0.1 Ag/L correlated significantly and positively with
concentrations of other constituents associated with anthropogenic inputs (Ca, Cl, Na, and NO3) and with dissolved organic
carbon. Hgf concentrations N0.1 Ag/L did not correlate significantly with concentrations of the inorganic constituents. Hgf
concentrations near or exceeding 2 Ag/L were found only in water from wells in areas with residential land use, but
concentrations were at background levels in most water samples from undeveloped land. The spatial distribution of Hg-contaminated ground water appears to be locally and regionally heterogeneous; no extensive plumes of Hg contamination have
yet been identified.
Keywords :
Nitrate (NO3) , ground water , Chloride (Cl) , Mercury (Hg) , land use
Journal title :
Science of the Total Environment
Journal title :
Science of the Total Environment