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Publications— Scientific Investigations Reports |
National Water Quality Assessment Program
U.S. Geological Survey Scientific Investigations Report 2006-5104
By Bruce D. Lindsey, William F. Falls, Matthew J. Ferrari, Tammy M. Zimmerman, Douglas A. Harned, Eric M. Sadorf, and Melinda J. Chapman
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Results of ground-water sampling from 255 wells and 19 springs in 11 studies done by the U.S. Geological Survey
National Water-Quality Assessment (NAWQA) Program within the Piedmont Aquifer System (PAS) were analyzed to determine
the factors affecting occurrence and distribution of selected contaminants. The contaminants, which were selected on
the basis of potential human-health effects, included nitrate, pesticides, volatile organic compounds (VOCs), and radon.
The PAS was subdivided on the basis of the general rock type of the aquifers into three areas for the study—crystalline,
carbonate, and siliciclastic. The 11 studies were designed to areally represent an individual aquifer rock type and
overall are representative of the PAS in their distribution; 7 studies are in the crystalline-rock aquifers, 3 studies
are in the siliciclastic-rock aquifers, and 1 study is in the carbonate-rock aquifers. Four of the studies were focused
on land use, 1 in an agricultural area and 3 in urban areas. The remaining studies had wells representing a range of
land-use types.
Analysis of results of nitrate sampling indicated that in 8 of the 10 areas where nitrate concentrations were measured,
median concentrations of nitrate were below 3 mg/L (milligrams per liter); 2 of the 10 areas had statistically
significant higher median concentrations when compared to the other 8 areas. The agricultural land-use study in the
carbonate-rock aquifer in the Lower Susquehanna River Basin had the highest median nitrate concentration (11 mg/L),
and 60 percent of the wells sampled exceeded the U.S. Environmental Protection Agency (USEPA) Maximum Contaminant
Level (MCL) of 10 mg/L. The major aquifer study in the crystalline-rock aquifer of the Lower Susquehanna River Basin
Study Unit had the second-highest median nitrate concentration. Nitrate concentrations were positively correlated to
the percentage of agricultural land use around the well, the total input of nitrogen from all sources, dissolved oxygen
concentration, lithology, depth to water, and soil-matrix characteristics. A linear regression model was used to determine
that increases in the percentage of agricultural land use, the input of nitrogen from all sources, and dissolved oxygen
were the most significant variables affecting increased concentration of nitrate. A logistic regression model
was used to determine that those same factors were the most significant variables affecting whether or not the nitrate
concentration would exceed 4 mg/L.
Of the analysis of samples from 253 wells and 19 springs for 47 pesticides, no sample had a pesticide concentration that
exceeded any USEPA MCL. The most frequently detected pesticide was desethyl atrazine, a degradation product of atrazine;
the detection frequency was 47 percent. Other frequently detected pesticides included atrazine, metolachlor, simazine,
alachlor, prometon, and dieldrin. Detection frequency was affected by the analytical reporting limits; the frequency of
detection was somewhat lower when all pesticides were censored to the highest common detection limit. Source factors
such as agricultural land use (for agricultural herbicides), urban land use (for insecticides), and the application rate
were found to have positive statistical correlations with pesticide concentration. Transport factors such as depth to
water and percentage of well-drained soils, sand, or silt typically were positively correlated with higher pesticide
concentrations.
Sampling for VOCs was conducted in 187 wells and 19 springs that were sampled for 59 VOCs. There were 137 detections
of VOCs above the common censoring limit of 0.2 micrograms per liter. The most frequently detected VOCs were chloroform, a trihalomethane,
and methyl-tert butyl ether (MTBE), a fuel oxygenate. Seventy-nine wells had at least one VOC detected. The detections
were related to land use and well depth. Kendall’s tau correlations indicated a significant positive correlation between
chloroform concentration and urban land use, leaking underground storage tanks, population density, and well depth.
MTBE concentrations also were positively correlated to urban land use, leaking underground storage tanks, population
density, and well depth.
Radon was sampled at 205 sites. The subdivisions used for analysis of other contaminants were not adequate for analysis
of radon because radon varies on the basis of variations in mineralogy that are not reflected by the general lithologic
categories used for the rest of the studies. Concentrations of radon were highest in areas where the crystalline-rock
aquifers had felsic mineralogy, and the lowest concentrations of radon were in areas where the crystalline-rocks aquifer
had mafic mineralogy. Water from wells in siliciclastic-rock aquifers had concentrations of radon lower than that in the
felsic crystalline-rock aquifers. More than 90 percent of the wells sampled for radon exceeded the proposed MCL of
300 pCi/L (picoCuries per liter); however, only 13 percent of those wells had concentrations in water that exceeded the
alternative maximum contaminant level (AMCL), a higher level that can be used by municipalities addressing other sources
of radon exposure.
Overall, concentrations of constituents were related to land-use factors for nitrate, pesticides, VOCs, and to aquifer
lithology for radon. None of the 47 pesticides or 59 VOCs analyzed exceeded the MCLs where those constituents were sampled.
Concentrations exceeded the MCL for nitrate in 11 percent of the wells sampled. Nearly 91 percent of the wells sampled
exceeded the proposed MCL for radon. Additional sampling in selected areas would improve overall understanding of the PAS
and increase the possibility of creating predictive models of ground-water quality in this area.
Abstract
Introduction
Purpose and Scope
Description of the Study Area
Physiography and Geology
Land Use, Population, and Water Use
Climate
Description of Piedmont Aquifers and NAWQA Ground-Water Study Areas
Crystalline-Rock Aquifers
Hydrology
Water Quality
NAWQA Studies in Crystalline-Rock Aquifers
Carbonate-Rock Aquifers
Hydrology
Water Quality
NAWQA Studies in Carbonate-Rock Aquifers
Siliciclastic-Rock Aquifers
Hydrology
Water Quality
NAWQA Studies in Siliciclastic-Rock Aquifers
Description of NAWQA Well Networks
Physical Characteristics of Wells and Surrounding Areas
Chemical Characteristics of Natural Ground Water
Statistical Methods Used to Analyze Water-Quality Data
Categorical Statistics
Continuous Explanatory Variable Statistics
Discrete Response Statistics
Occurrence and Distribution of Selected Contaminants in the Piedmont Aquifers
Nitrate in Ground Water
Nitrogen Sources
Distribution of Nitrate Concentrations
Factors Affecting Nitrate Concentrations
Pesticides in Ground Water
Pesticide Sources
Distribution of Pesticide Concentrations
Factors Affecting Pesticide Concentrations
Volatile Organic Compounds in Ground Water
VOC Sources
Distribution of Detections of VOCs
Factors Affecting VOC Detections
Radon in Ground Water
Radon Sources
Distribution of Radon Concentrations
Factors Affecting Radon Concentrations
Limitations of Water-Quality Data and Recommendations for Future Study
Summary and Conclusions
References Cited
This report is available online in Portable Document Format (PDF). If you do not have the Adobe Acrobat PDF Reader, it is available for free download from Adobe Systems Incorporated.
View the full report in PDF 5.1 MB
For more information about USGS National Water-Quality Assessment activities in the Piedmont Aquifer System contact: A full listing of NAWQA activities is available at :
Bruce D. Lindsey, Piedmont Aquifer Lead Scientist
USGS Pennsylvania Water Science Center
215 Limekiln Road
New Cumberland, Pennsylvania 17070
Telephone: (717) 730-6964
Fax: (717) 730-6997
http://water.usgs.gov/nawqa/.