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Atrazine in a Stream‐Aquifer System: Estimation of Aquifer Properties from Atrazine Concentration Profiles
Author(s) -
Davis Ralph K.,
Pederson Darryll T.,
Blum Darryl A.,
Carr James D.
Publication year - 1993
Publication title -
groundwater monitoring and remediation
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.677
H-Index - 47
eISSN - 1745-6592
pISSN - 1069-3629
DOI - 10.1111/j.1745-6592.1993.tb00445.x
Subject(s) - aquifer , hydrology (agriculture) , groundwater recharge , surface runoff , environmental science , transect , geology , streamflow , atrazine , groundwater , drainage basin , pesticide , geography , ecology , agronomy , oceanography , geotechnical engineering , cartography , biology
Lincolns municipal wellfield consists of 44 wells developed in an alluvial aquifer adjacent to the Platte River near Ashland, Nebraska Induced recharge from the river is the primary source of water for the wellfield. Wafer samples were collected on a periodic basis from the Platte River arid two transects of monitoring wells. These samples were analyzed for the herbicide atrazine, which was used as a tracer of induced recharge in this stream‐aquifer system. Atrazine concentrations in the river and aquifer were much less than 1.0 ppb during late fall and winter, but increased to as high as 18.9 ppb during spring and summer, associated with runoff from upgradient agricultural lands. There was approximately a 21‐day lag time from the first detection of increasing atrazine concentration in the river to the first detection in monitoring wells immediately adjacent to the river. This lag time was relatively constant throughout the year and from one year to the next, even with major fluctuations of river stage and wellfield production. This consistency of lag time indicated that the travel times from the river to the first set of monitoring wells immediately adjacent to the river were fairly constant. Paths of preferential flow were identified in the aquifer at a depth of 25 to 35 feet below land surface. This aquifer zone appeared to play a significant role in movement of water from beneath the river into the wellfield. Aquifer dispersivity was calculated using a method described by Hoehn and Santschi (1987). Macrodispersivity (A L ) was shown to increase linearly over the scale of the wellfield. Calculated values of A L were within limits of other reported values for this type of aquifer material and agreed well with values reported by Hoehn and Santschi (1987); These findings will be extremely beneficial for planning and management of the municipal wellfield.