Abstract: The use of glyphosate has increased rapidly, and there is limited understanding of its environmental fate. The objective of this study was to document the occurrence of glyphosate and the transformation product aminomethylphosphonic acid (AMPA) in Midwestern streams and to compare their occurrence with that of more commonly measured herbicides such as acetochlor, atrazine, and metolachlor. Water samples were collected at sites on 51 streams in nine Midwestern states in 2002 during three runoff events: after the application of pre-emergence herbicides, after the application of post-emergence herbicides, and during harvest season. All samples were analyzed for glyphosate and 20 other herbicides using gas chromatography/mass spectrometry or high performance liquid chromatography/mass spectrometry. The frequency of glyphosate and AMPA detection, range of concentrations in runoff samples, and ratios of AMPA to glyphosate concentrations did not vary throughout the growing season as substantially as for other herbicides like atrazine, probably because of different seasonal use patterns. Glyphosate was detected at or above 0.1 μg/l in 35 percent of pre-emergence, 40 percent of post-emergence, and 31 percent of harvest season samples, with a maximum concentration of 8.7 μg/l. AMPA was detected at or above 0.1 μg/l in 53 percent of pre-emergence, 83 percent of post-emergence, and 73 percent of harvest season samples, with a maximum concentration of 3.6 μg/l. Glyphosate was not detected at a concentration at or above the U.S. Environmental Protection Agency’s maximum contamination level (MCL) of 700 μg/l in any sample. Atrazine was detected at or above 0.1 μg/l in 94 percent of pre-emergence, 96 percent of postemergence, and 57 percent of harvest season samples, with a maximum concentration of 55 μg/l. Atrazine was detected at or above its MCL (3 μg/l) in 57 percent of pre-emergence and 33 percent of postemergence samples. (KEY TERMS: glyphosate; water quality; nonpoint source pollution; herbicides; runoff.) Battaglin, William A., Dana W. Kolpin, Elizabeth A. Scribner, Kathryn M. Kuivila, and Mark W. Sandstrom, 2005. Glyphosate, Other Herbicides, and Transformation Products in Midwestern Streams, 2002. Journal of the American Water Resources Association (JAWRA) 41(2):323-332. INTRODUCTION Herbicide Chemistry, Use, and Toxicity Glyphosate is a nonselective, systemic herbicide that controls most annual and perennial weeds (and other plants) by inhibiting the synthesis of aromatic amino acids needed for protein formation. The use of glyphosate is increasing rapidly, and there is limited understanding of its environmental fate. Glyphosate is highly water soluble and could be mobile in aquatic systems. However, glyphosate binds strongly to cations that are adsorbed to soils (Carlisle and Trevors, 1988). This binding is unlike other organic compounds that primarily adsorb to organic matter in soils. Glyphosate binding is similar to phosphate binding, and it is possible that phosphate accumulation in soils could reduce the capacity for glyphosate binding (Gimsing et al., 2004). The reported organic carbon partition coefficient (Koc) values for glyphosate span several orders of magnitude (Table 1). USDOE (2003) lists the relatively low Koc value of 18.8, while the manufacturer suggests a much higher Koc of 24,000 (Monsanto, 2003). It may be difficult to determine reliable physical and chemical property data for some organic compounds (Pontolillo and Eganhouse, 2001). For many organic compounds, low Koc and Kow values imply that limited binding to soils will occur. For glyphosate, however, it appears that binding to soils is not directly to carbon. Glyphosate has low vapor pressure, suggesting that loss to the 1Paper No. 04024 of the Journal of the American Water Resources Association (JAWRA) (Copyright © 2005). Discussions are open until October 1, 2005. 2Respectively, Hydrologist, U.S. Geological Survey, Box 25046, MS 415, Lakewood, Colorado 80225; Hydrologist, U.S. Geological Survey, P.O. Box 1230, Iowa City, Iowa 52244; Research Assistant, U.S. Geological Survey, 4821 Quail Crest Place, Lawrence, Kansas 66049; Hydrologist, U.S. Geological Survey, Placer Hall, 6000 J Street, Sacramento, California 95819; and Chemist, U.S. Geological Survey, Box 25046, MS 407, Lakewood, Colorado 80225 (E-Mail/Battaglin: wbattagl@usgs.gov). JOURNAL OF THE AMERICAN WATER RESOURCES ASSOCIATION 323 JAWRA JOURNAL OF THE AMERICAN WATER RESOURCES ASSOCIATION APRIL AMERICAN WATER RESOURCES ASSOCIATION 2005 GLYPHOSATE, OTHER HERBICIDES, AND TRANSFORMATION PRODUCTS IN MIDWESTERN STREAMS, 20021 William A. Battaglin, Dana W. Kolpin, Elizabeth A. Scribner, Kathryn M. Kuivila, and Mark W. Sandstrom2