Jf. Walker et Dj. Graczyk, PRELIMINARY EVALUATION OF EFFECTS OF BEST MANAGEMENT-PRACTICES IN THEBLACK EARTH CREEK, WISCONSIN, PRIORITY WATERSHED, Water science and technology, 28(3-5), 1993, pp. 539-548
Citations number
16
Categorie Soggetti
Water Resources","Environmental Sciences","Engineering, Civil
Nonpoint-source contamination accounts for a substantial part of the w
ater quality problems in many watersheds. The Wisconsin Nonpoint Sourc
e Water Pollution Abatement Program provides matching money for volunt
ary implementation of various best management practices (BMPs). The ef
fectiveness of BMP s on a drainage-basin scale has not been adequately
assessed in Wisconsin by use of data collected before and after BMP i
mplementation. The U.S. Geological Survey, in cooperation with the Wis
consin Department of Natural Resources, monitored water quality in the
Black Earth Creek watershed in southern Wisconsin from October 1984 t
hrough September 1986 (pre-BMP conditions). BMP implementation began d
uring the summer of 1989 and is planned to continue through 1993. Data
collection resumed in fall 1989 and is intended to provide informatio
n during the transitional period of BMP implementation (1990-93) and 2
years of post-BMP conditions (1994-95). Preliminary results presented
for two subbasins in the Black Earth Creek watershed (Brewery and Gar
foot Creeks) are based on data collected during pre-BMP conditions and
the first 3 years of the transitional period. The analysis includes t
he use of regressions to control for natural variability in the data a
nd, hence, enhance the ability to detect changes. Data collected to da
te (1992) indicate statistically significant differences in storm mass
transport of suspended sediment and ammonia nitrogen at Brewery Creek
. The central tendency of the regression residuals has decreased with
the implementation of BMPs; hence, the improvement in water quality in
the Brewery Creek watershed is likely a result of BMP implementation.
Differences in storm mass transport at Garfoot Creek were not detecte
d, primarily because of an insufficient number of storms in the transi
tional period. As practice implementation continues, the additional da
ta will be used to determine the level of management which results in
significant improvements in water quality in the two watersheds. Futur
e research will address techniques for including snowmelt runoff and e
arly spring storms.