Reservoirs are a prominent feature of the hydrology of river systems in the midwestern United States (Midwest), where they are used to impound and store water for public water supply, flood control, irrigation, recreation, hydropower, and wildlife habitat. There is no recent count of the number of reservoirs in the United States, but a 1982 inventory of artificial barriers that are more than 25 feet high or that impound more than 50 acre-feet of water, listed approximately 66,000 structures (U.S. Army Corps of Engineers, 1982). Reservoirs may also store undesirable substances such as agricultural chemicals (herbicides, insecticides, other pesticides, and nutrients) and sediment. Most sediment entering a reservoir is trapped behind the dam. However, soluble chemicals including some herbicides remain in the dissolved phase in water and are stored in the reservoir until they are discharged or are removed by biotic or abiotic processes.
Agricultural activities in the Midwest have resulted in the contamination of surface water with agricultural chemicals. Numerous recent investigations (Goolsby and Battaglin, 1995; Schottler et al., 1994; Baker and Richards, 1990) indicate that significant quantities of some herbicides are flushed from cropland to streams each spring and summer during rainfall events following application. Peak concentration of several herbicides can exceed 10 ug/L during these events (Coupe et al., 1995; Scribner et al., 1994).
Only a few studies have investigated the herbicide content of reservoirs or the way in which physical, hydrologic, and land use characteristics of reservoir drainage basins interact to affect herbicide concentrations in reservoir outflow. Preliminary results from this study (Scribner et al., 1996; Goolsby et al., 1993) and results from other investigations (Kalkhoff, 1993; Leung et al., 1982; Miller and Kennedy, 1995; Stamer et al., 1995) indicated that reservoirs and rivers regulated by reservoir outflows are likely to have lower peak herbicide concentrations but a longer period of elevated herbicide concentration than unregulated rivers. The implication is that water in or released from reservoirs is likely to have a higher time-weighted annual mean herbicide concentration than water in unregulated rivers. Time-weighted annual mean concentrations are used to determine compliance with U.S. EPA maximum contaminant levels (MCLs) and lifetime health advisory levels (HALs) for herbicides in drinking water supplies (U.S. Environmental Protection Agency, 1989; 1995).
The objective of this research is to develop models for the annual mean concentration of selected herbicides in midwestern reservoirs. To accomplish this objective, water quality data are analyzed both statistically and graphically. A geographic information system (GIS) is used to manage and quantify characteristics on land use, agricultural chemical use, climatic conditions, topographic character, and soil type within the reservoir drainage basins. Multiple linear and logistic regression equations are developed to estimate annual mean herbicide concentrations in reservoir outflow as a function of these land use, hydrologic, and physical characteristics.
The study area consists of 76 reservoirs and reservoir drainage basins in parts of 11 midwestern States (figure 1). The two primary considerations in reservoir selection were (1) reservoir outflow was accessible for sampling, and (2) information on the volume and discharge of the reservoir was obtainable. Drainage basin boundaries for the 76 reservoirs were extracted primarily from hydrologic unit boundaries (Steeves and Nebert, 1994). Drainage basin areas range from 44 to 64,560 square kilometers (km2), and the mean basin area is 6,140 km2.
The study area encompasses a large region with considerable variability in land use, soil type, and climatic conditions. Harvested cropland represents more than 50 percent of the land area in about 25 percent of the basins and less than 5 percent of the land area in less than 5 percent of the basins. Soils in the eastern part of the study area tend to be finer textured and poorly drained, while soils in the western part tend to be coarser grained and well drained (U.S. Department of Agriculture, 1993).
Sample Collection and Analysis
Reservoir outflow was sampled eight times (approximately bimonthly) from April 1992 through
September 1993 (table 1).
Samples were collected using non-contaminating and non-adsorbing pre-cleaned containers
from near the centroid of flow or other outflow point that provided a representative sample of
reservoir discharge. Prior to shipping to the lab for analysis, samples were filtered through 0.7
micron glass fiber filters and chilled (Scribner et al., 1996). The samples collected in this study
are measures of water passing through or leaving the studied reservoirs and do not account for the
variability of herbicide concentration within reservoirs.
All samples were analyzed for 11 herbicides (alachlor, ametryn, atrazine, cyanazine, metolachlor, metribuzin, prometon, prometryn, propazine, simazine, and terbutryn), 2 atrazine metabolites (desethylatrazine, desisopropylatrazine), and 3 cyanazine metabolites (deethylcyanazine, cyanazine amide, and deethylcyanazine amide) by gas chromatography/mass spectrometry (GC/MS). A metabolite of alachlor, alachlor ethane sulfonic acid (ESA), was analyzed by enzyme-linked immunosorbent assay after solid phase extraction (Scribner et al., 1996).
A GIS was used to manage and display the large quantity of spatial data in this investig
ation. County-level estimates of agricultural chemical use, agricultural land use, crop acre
age, and livestock were constructed by processing tabular data into GIS coverages (Battaglin
and Goolsby, 1995). Other natural and anthropogenic variables defined within drainage basins
from digital and non-digital data sources include basin area; population density (U.S.
Department of Commerce, 1990); the soils variables hydrologic group, porosity, water-holding
capacity, and permeability from STATSGO (U.S. Department of Agriculture, 1993); runoff (Rea
and Cederstrand, 1994); and several hydrological parameters calculated for the TOPMODEL
(Wolock, 1993) watershed model using digital elevation model and STATSGO data (Wolock, D.M.,
USGS, written commun., 1995). Area-weighted transfer and area-weighted sum algorithms,
programmed in the GIS, were used to estimate the masses of agricultural chemical applied,
acreages of crops, or numbers of people or livestock within drainage basins. In many cases,
variable estimates were normalized by dividing by basin area. Explanatory variables that
appear in models presented in this paper are listed in table 2.
Multiple linear regression (MLR) and logistic regression (LGR) models were used to
investigate relations between explanatory variables and the estimated annual mean
concentrations of atrazine, cyanazine, and the total of 11 herbicides. Both MLR and
LGR models provided satisfactory results and are presented in this paper.
MLR is a statistical technique that uses one or more explanatory variables to
explain as much of the variation observed in the response variable as possible
(Helsel and Hirsch, 1992). Once calibrated, MLR models can be used to estimate
the response variable from knowledge of the explanatory variable values. MLR
models with as many as six explanatory variables were tested. The best models
generally had four or fewer explanatory variables. Models with more explanatory
variables often had problems with autocorrelation among the explanatory variables,
as indicated by variance inflation factor (VIF) values of greater than 10 (Helsel
and Hirsch, 1992).
LGR is a statistical technique that uses one or more explanatory variables to predict
the probability of a categorical response (Helsel and Hirsch, 1992). The response variable
in LGR is the log of the odds ratio (logit). The logit transforms a variable (p) constrained
between zero and one into a continuous variable that is linear with respect to the vector
of the explanatory variables (equation 1):
Y = log [p/(1-p)] = b0 {b00} + b1X1 +... bkXk (1)
where: Y is the response variable; [p/(1-p)] is the odds ratio; b0 is the first
intercept and b00 is the second intercept, X is the vector of k explanatory variables,
b1 is the slope coefficient for the first explanatory variable X1; and bk
is the slope coefficient for the kth explanatory variable Xk. LGR models presented here
are comprised of two parallel linear equations. Models were compared based on fit statistics and
on their ability to correctly estimate categories of annual mean herbicide concentration. The
modeled category was selected as the one with the largest probability. Model accuracy is
defined as the number of correct classifications (modeled concentration category matches
observed category) divided by the number of attempted classifications.
Atrazine, its two metabolites, and alachlor ESA, were the most frequently detected herbicide
compounds, all being detected in more than 60 percent of the samples. Cyanazine and
metolachlor were also detected in about 50 percent of the samples. The highest herbicide
concentration was for atrazine (12.4 ug/L) and the highest herbicide metabolite
concentration was for ESA (19.7 ug/L).
A temporal pattern of herbicide concentration occurred in outflow from many of
the 76 reservoirs. Like in streams and rivers (Goolsby and Battaglin, 1995) the
highest herbicide concentrations occurred after the planting season in late spring
and summer (sampling rounds 2 and 7). Herbicide metabolite concentrations occasionally
peak later, in sampling rounds 3 and 8. The temporal patterns of alachlor, atrazine,
cyanazine, metolachlor, desethylatrazine, and ESA concentrations in the outflow from
all reservoirs are shown in
Estimates of the time-weighted annual mean herbicide concentration in reservoir
outflow were calculated from the sample data. Annual mean herbicide concentration
estimates are time-weighted not flow-weighted because time-weighted estimates are
more representative of annual mean exposure via drinking water and are more relevant
to water suppliers, who need to comply with federal regulations. For this report the
eight sampling rounds were divided into two sets for the purposes of computing annual
mean concentrations. The first set consists of samples collected in 1992 (rounds 1-4)
and the second set consists of samples collected primarily in 1993 (rounds 5-8). Annual
mean concentrations were estimated as the mean of the sample values. The resulting
sampling frequency (quarterly) is probably inadequate to accurately estimate annual
mean herbicide concentrations in reservoir outflow at some sites (Battaglin and Hay, 1996).
Estimates of annual mean herbicide concentration are used to condition MLR and LGR models
which can then be used to forecast expected annual mean herbicide concentrations from
knowledge about the required explanatory variables.
MLR was used to model the observed annual mean concentrations of atrazine, cyanazine,
and the total of 11 herbicides in outflow from 76 midwestern reservoirs. Two of t
he best models for atrazine, cyanazine, and total herbicide concentrations an
d the coefficients of determination (R2) and variation (CV) for the m
odels are listed in table 3.
LGR was tested to determine if an improvement could be made over MLR models.
LGR requires a discrete response variable; therefore, annual mean agricultural
chemical concentration values were divided into three categories with roughly
equal numbers of observations. The concentration categories and accuracy of two
of the best models for atrazine, cyanazine, and total herbicide are listed in
table 4.
As with the MLR models, a chemical use, chemical expense, or cropland variable is
significant in every model, having a direct relation to annual mean herbicide
concentrations. CNCT is significant in several models, always having a direct
relation to annual mean herbicide concentration. HYGP and PSTP area each significant
in two models, both always having a direct relation herbicide concentration.
PERM and TOPM are each significant in two models, both always having an inverse
relation to herbicide concentrations. Annual mean temperature (TEMP) and SLTK are
each significant in three models, both always having a direct relation to annual
mean herbicide concentration.
Both MLR and LGR models helped to identify land use, chemical use, soil, and
climatic variables in upstream drainage basins that affect annual mean herbicide
concentrations in reservoir outflows. Results demonstrate a strong association
between annual mean herbicide concentrations in reservoir outflow and the use
of those herbicides within associated drainage basins. In many cases, models
that use cropland acreage or agricultural chemical expenditure estimates work
nearly as well as models using the harder to come by herbicide use estimates.
The authors thank James Fallon, Michael Meyer and John Flager for critical reviews of the
manuscript; Gail Thelin and Naomo Nakagaki for providing raw Census of Agricultural data;
and Laurie Boyer for html document preparation.
Baker, D. B. and R. P. Richards, 1990. Transport of soluble pesticides through drainage networks in large agricultural river basins. In: Long Range Transport of Pesticides: Lewis Publishers, Ann Arbor, MI. p 241-271.
Battaglin, W. A. and D. A. Goolsby, 1995. Spatial Data in Geographic Information System Format on Agricultural Chemical Use, Land Use, and Cropping Practices in the United States. U. S. Geol. Surv. Water-Resour. Invest. Rep. 94-4176.
Battaglin, W. A. and L. E. Hay, 1996, Effects of Sampling Strategies on Estimates of Annual Mean Herbicide Concentrations in Midwestern Rivers. Environ. Sci. Technol., 30(3), p 889-896.
Coupe, R. H., D. A. Goolsby, J. L. Iverson, S.D. Zaugg and D. J. Markovchick, 1995. Pesticide, Nutrient, Streamflow and Physical Property Data for the Mississippi River, and Major Tributaries, April 1991- September, 1992. U.S. Geol. Surv. Open-File Rep. 93-657.
Goolsby, D. A., W. A. Battaglin, J. D. Fallon, D. S. Aga, D. W. Kolpin and E. M. Thurman, 1993. Persistence of Herbicides in Selected Reservoirs in the Midwestern United States: Some Preliminary Results. U.S. Geol. Surv. Open-File Rep. 93-418, p 51-63.
Goolsby, D. A. and W. A. Battaglin, 1995. Occurrence and Distribution of Pesticides in Rivers of the Midwestern United States. In: Agrochemical Environmental Fate: State of the Art; CRC Press, Boca Raton, FL, p 159-173.
Helsel, D. R. and R. M. Hirsch, 1992. Statistical Methods in Water Resources. Elsevier, New York.
Kalkoff, S. J. 1993. Water Quality of Corydon Reservoir Before Implementation of Agricultural Best-Management Practices in the Basin, Wayne County, Iowa, September 1990 to September 1991. U.S. Geol. Surv. Water-Resour. Invest. Rep. 93-4099.
Leung, S. T., R. V. Bulkley and J. J. Richard, 1982. Pesticide Accumulation in a New Impoundment in Iowa. Wat. Resour. Bull. 18 (3), p 485-493.
Miller, J. G. and J. O. Kennedy, 1995. Study of Herbicides in Water and Sediment from 19 Iowa Water Supply Reservoirs January - February, 1995. Univ. of Iowa Hyg. Lab. Rep. No. 95-1.
Rea, A. and J. R. Cederstrand, 1994. GCIP reference data sets (GREDS). U.S. Geol. Surv. Open-File Rep. 94-388, CD-ROM.
Schottler, S. P., S. J. Eisenreich and P. D. Capel, 1994, Atrazine, Alachlor, and Cyanazine in a Large Agricultural River System. Environ. Sci. Technol., 28, p 1079-1089.
Scribner, E. A., D. A. Goolsby, E. M. Thurman, M. T. Meyer and M. L. Pomes, 1994. Concentrations of Selected Herbicides, Two Triazine Metabolites, and Nutrients in Storm Runoff From Nine Stream Basins in the Midwestern United States, 1990-92. U.S. Geol. Surv. Open-File Rep. 94-396.
Scribner, E. A., D. A. Goolsby, E. M. Thurman, M. T. Meyer and W. A. Battaglin, 1996 (in press) Concentrations of Herbicides, Herbicide Metabolites, and Nutrients in the Outflow from Selected Midwestern Reservoirs, 1992-93. U.S. Geol. Surv. Open-File Rep. 96-393.
Stamer, J. K., K. D. Gunderson and B. J. Ryan, 1995, Atrazine Concentrations in the Delaware River, Kansas. U.S. Geol. Surv. Fact Sheet FS-001-94.
Steeves, P. and D. Nebert, 1994. Hydrologic Units Maps of the Conterminous United States, 1:250,000-scale (nominal), ARC/INFO format, 1994.
U.S. Army Corps of Engineers, 1982. National Inventory of Dams Database. National Technical Information Service, Springfield, VA, digital file.
U.S. Department of Agriculture, 1993, State Soil Geographic Data Base (STATSGO) --Data Users Guide. U.S. Department of Agriculture, Soil Conservation Service, Misc. Pub. Num. 1492.
U.S. Department of Commerce, 1990. Census of Population and Housing, 1990. U.S. Department of Commerce, Bureau of Census, Data Users Division, Washington, D.C.
U.S. Environmental Protection Agency, 1989. Drinking Water Health Advisory: Pesticides. Office of Drinking Water Health Advisories, Lewis Publishers, Inc., Chelsea, Michigan.
U.S. Environmental Protection Agency, 1995. Drinking Water Regulations and Health Advisories. U.S. Environmental Protection Agency, Office of Water, Washington, D.C.
Wolock, D.M., 1993, Simulating the Variable-Source-Area Concept of Streamflow Generation with the Watershed Model TOPMODEL. U.S. Geol. Surv. Water-Resour. Invest. Rep. 93-4124.
2.
Donald A. Goolsby
GIS Data

Statistical Techniques
Herbicide Concentrations
figure 2.
Shown are concentrations in outflow from reservoirs with short residence times
(Lake Vermillion, IL; 3 months), moderate residence times (Turtle Creek, KS; 1.5
months)and long residence times (Hillsdale Lake, KS; 8 months). Multiple Linear Regression Models

A chemical use,
chemical expense, or cropland variable is significant in every model, always having a
direct relation to annual mean herbicide concentration. Subsurface contact time (CNCT)
is significant in every model, always having a direct relation to annual mean herbicide
concentration. Soil hydrologic group (HYGP) is significant in a several models, having
a direct relation to atrazine and total herbicide concentration. Percentage of basin
as pastureland (PSTP) is significant in several models, always having a direct
relation to herbicide concentrations. TOPM is significant in all cyanazine models,
having an inverse relation to annual mean concentration. Soil thickness (SLTK) is
significant in two models and potential evapotranspiration rate (PET) and soil
permeability (PERM) are each significant one model. All of the MLR models listed
in table 3 have moderate predictive power and could only be expected to estimate
annual mean herbicide concentrations values with a limited degree of confidence.
The overall accuracy of the best LGR models, defined as the number of correct
classifications (modeled concentration category matches observed category) divided
by the number of attempted classifications, averaged about 76% (Table 4). LGR models
are most effective at estimating when herbicide concentrations are in the lowest
category (average accuracy of 86%), but had more difficulty predicting concentrations
in the intermediate category (average accuracy of 67%), and concentrations in the
highest category (average accuracy of 66%). Authors
1.
William A. Battaglin
U.S. Geological Survey, WRD
Box 25046, MS 406
Building 53, Wing F-1200, DFC
Denver, Colorado 80225
Email: wbattagl@usgs.gov
U.S. Geological Survey, WRD
Box 25046, MS 406,
Building 53, Wing F-1200, DFC
Denver, Colorado 80225
Email: dgoolsby@usgs.gov
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