J
John T. Wilson
Researcher at United States Geological Survey
Publications - 28
Citations - 1078
John T. Wilson is an academic researcher from United States Geological Survey. The author has contributed to research in topics: Aquifer & Surface water. The author has an hindex of 10, co-authored 28 publications receiving 1031 citations.
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New Social Movements: From Ideology to Identity
TL;DR: In this paper, the authors discuss culture and identity in contemporary social movements and the role of actors in new social movements, as well as the relationship between identity fields and the social construction of movement identities.
Journal ArticleDOI
Preferential Flow Estimates to an Agricultural Tile Drain with Implications for Glyphosate Transport
Wesley W. Stone,John T. Wilson +1 more
TL;DR: Positive relations between glyphosate [N-(phosphonomethyl)glycine] concentrations and preferential flow for the two storms suggest that preferential flow is an important transport pathway to the tile drain.
Journal ArticleDOI
Transport and fate of nitrate at the ground-water/surface-water interface.
Larry J. Puckett,Celia Zamora,Hedeff I. Essaid,John T. Wilson,Henry Johnson,Michael J. Brayton,Jason R. Vogel +6 more
TL;DR: The results show that in these low hydrologic-gradient systems, storm and other high-flow events can be important factors for increasing surface-water movement into streambeds.
Journal ArticleDOI
Using heat to characterize streambed water flux variability in four stream reaches.
TL;DR: Streambed water flux was influenced by physical heterogeneity of the stream channel and temporal variability in stream and ground-water levels, and water flow through the streambed was roughly an order of magnitude larger in the humid basins of IN and NE than in the arid basins (WA and CA).
OtherDOI
Occurrence and Transport of Agricultural Chemicals in Leary Weber Ditch Basin, Hancock County, Indiana, 2003-04
TL;DR: Capel et al. as mentioned in this paper found that the highest concentrations of pesticides and nutrients were detected in samples of tile-drain water, overland flow, and water from Leary Weber Ditch.