Abstract: Leary Weber Ditch Basin, Hancock County, Indiana, is one of seven first-order basins selected from across the United States as part of the Agricultural Chemicals: Source, Transport, and Fate study conducted by the National Water-Quality Assessment Program of the U.S. Geological Survey. The nationwide study was designed to increase the understanding of the links between the sources of water and agricultural chemicals (nutrients and pesticides) and the transport and fate of these chemicals through the environment. Agricultural chemicals were detected in Leary Weber Ditch and in every associated hydrologic compartment sampled during 2003 and 2004. Pesticides were detected more frequently in samples collected from overland flow and from the ditch itself and less frequently in ground-water samples. The lowest concentrations of pesticides and nutrients were detected in samples of rain, soil water, and ground water. The highest concentrations of pesticides and nutrients were detected in samples of tile-drain water, overland flow, and water from Leary Weber Ditch. Samples collected from the tile drain, overland flow and Leary Weber Ditch soon after chemical applications to the fields and coincident with rainfall and increased streamflow had higher concentrations of pesticides and nutrients than samples collected a longer time after the chemicals were applied. A mass-balance mixing analysis based on potassium concentrations indicated that tile drains are the primary contributor of water to Leary Weber Ditch, but overland flow is also an important contributor during periods of high-intensity rainfall. When maximum rainfall intensity was 0.5 inches per hour or lower, overland flow contributed about 10 percent and tile drains contributed about 90 percent of the flow to Leary Weber Ditch. When maximum rainfall intensity was 0.75 inches per hour or greater, overland flow contributed about 40 percent and tile drains contributed about 60 percent of the flow to the ditch. Ground-water flow to Leary Weber Ditch was negligible. Tile drains are an important agricultural-chemical transport path to Leary Weber Ditch, based on the hydrologic contributions of overland flow and tile drains to the ditch. Overland flow is also an important agricultural-chemical transport pathway during high-intensity rainfall; however, storms with high-intensity rainfall are sporadic throughout the year. Tile drains and the soil water moving to the tile drains are the primary transport pathway for agricultural-chemical transport to Leary Weber Ditch during most storms as well as between storms. Introduction Leary Weber Ditch Basin in Hancock County, Indiana, is one of seven first-order basins selected from across the United States as part of the Agricultural Chemicals: Source, Transport, and Fate Team (ACT) study (Capel and others, 2004) conducted by the National Water-Quality Assessment (NAWQA) Program of the U.S. Geological Survey (USGS). The goal of the ACT study is to assess the fate and transport of chemicals applied to crops in agricultural basins across the Nation. Chemicals selected for nationwide ACT study include nutrients (nitrogen and phosphorus), major ions, and about 43 commonly used pesticides and 39 degradation products (including triazine herbicides such as atrazine and simazine, acetanilide herbicides such as acetochlor and metolachlor, and organophosphorus insecticides such as chlorpyrifos and diazinon). Because the herbicide glyphosate is so important in the Midwest, glyphosate and its degradate aminomethylphosphonic acid (AMPA) also were selected for analysis in the Leary Weber Ditch study in 2004 as part of the USGS Toxic Substances Hydrology Program. The basins in the ACT study represent a variety of agricultural settings with different crop types and agricultural practices related to tillage, irrigation, artificial drainage, and chemical use, as well as a range of landscapes with different geology, soils, topography, climate, and hydrology (Capel and others, 2004). Leary Weber Ditch Basin was selected for study because it is typical of an artificially drained (subsurface tile drains) Midwestern basin with corn and soybean row cropping. In areas with poorly drained soils, tile drains are used to Occurrence and Transport of Agricultural Chemicals in Leary Weber Ditch Basin, Hancock County, Indiana, 2003–04 By Nancy T. Baker, Wesley W. Stone, John T. Wilson, and Michael T. Meyer facilitate access to and cultivation of agricultural land. During the 1980s, the U.S. Department of Agriculture (USDA) estimated that approximately 50 percent of all cropland in Indiana was drained; tiles drain approximately 70 percent of that cropland. The USDA estimated that Indiana ranked second in the U.S. in total land area where artificial surface and subsurface drainage is used (U.S. Department of Agriculture, 1987). The ACT study is designed to increase the understanding of the links between the sources of water and agricultural chemicals (nutrients and pesticides) and the fate and transport of these chemicals through the environment. Understanding the fate and transport of these chemicals in the study basins may help predict the fate and transport of agricultural chemicals in other agricultural areas. This information will help managers target the implementation of best management practices to those hydrologic compartments that are the most conducive to the transport of agricultural chemicals. Purpose and Scope This report documents the occurrence of agricultural chemicals in Leary Weber Ditch and in the major hydrologic compartments of the Leary Weber Ditch Basin during 2003 and 2004. Hydrologic compartments that contribute water and agricultural chemicals to Leary Weber Ditch are rain water, overland-flow water, soil water, tile-drain water, and ground water. Water samples were collected during four storms in 2003 and three storms in 2004 from the Tile Drain, Overland Flow, and Leary Weber Ditch sites. In addition, stable-flow samples were collected between storms at the Tile Drain and Leary Weber Ditch sites. Weekly composite rain samples were collected for 13 weeks in 2003 and 2004. Soil-water and ground-water samples were collected at selected times during 2003 and 2004. The samples were analyzed for selected pesticides, nutrients, and major ions. This report also describes the transport of water and chemicals from the major hydrologic compartments to Leary Weber Ditch based on a mass-balance mixing analysis and analyses of hydrologic and chemical data from each of the hydrologic compartments. Description of Basin and Sampling Sites Leary Weber Ditch is a 2.73 mi intensively farmed drainage basin dominated by poorly drained soils in Hancock County, east-central Indiana (fig. 1). The USGS maintains streamflow gaging station 03361638, Leary Weber Ditch at Mohawk, IN (hereafter referred to as the gaging station). Agriculture is the principal land use, with 87 percent of the total land area in row crops. Leary Weber Ditch is an intermittent stream and a tributary to Sugar Creek. The ditch has been dredged along much of its reach to facilitate drainage of the shallow water table. Successful farming requires lowering the water table and removing ponded water by artificially draining the fields through tiles. Flow in Leary Weber Ditch is sustained primarily from tile-drain contributions. Large changes in flow are tied to snowmelt and rainfall, with flow diminishing quickly between periods of precipitation. A more complete description of the basin can be found in Lathrop (2006). Tile-drain systems are extensive in the basin; field reconnaissance showed 58 tile-drain outlets along the 2.86-mi length of Leary Weber Ditch. This number of outlets is conservative because 0.3 mi of the ditch was not accessible during the reconnaissance. The drains typically are installed 3 to 4 ft below the land surface, with an average outlet spacing of 200 ft. Tile-drain outlets represent individual tiles or collector tiles that combine discharge water from a network of tiles that may drain several fields. Approximate locations of tile drains in the basin are shown in figure 2. Tile locations were derived from landowner recollection, tile-drain outlets, and infrared aerial photography. Because it was not possible to verify tile locations derived from infrared aerial photography, precedence for estimating locations was given to landowner recollection and tile-drain outlets. The Leary Weber Ditch Basin is topographically flat. A few land areas adjacent to the ditch have overland runoff; areas farther away hold ponded water, unless they too are drained by tile drains. The areas where overland runoff can occur are usually small field-size depressions that drain directly into the ditch, commonly through a culvert that runs beneath the berm of the ditch bank. The Overland Flow site is one of 17 overland flow culverts along the length of Leary Weber Ditch. The Overland Flow site is a 3.5-acre depression with a culvert for drainage at the mouth. The contributing area for runoff is variable and dependent upon the magnitude and intensity of rainfall. Field observations during rainfall indicate that runoff occurs mainly as sheet and rivulet flow to the discharge point. The potential contributing areas of the other 16 culverts were not determined. A sampling plan was established so that chemicals in Leary Weber Ditch Basin could be accounted for from their point of entry into the basin, their storage or degradation within the basin, or until their departure by flow out of the basin through Leary Weber Ditch (Lathrop, 2006). A wide variety of water-quality sampling sites were established throughout the basin to evaluate the occurrence and movement of water and chemicals into Leary Weber Ditch and between the hydrologic compartments: rain, soil water, ground water, tile-drain water, and overland-flow water. Five monitoring sites were established to characterize Leary Weber Ditch and th