The water balance at a low-level radioactive-waste disposal site in northwestern Illinois was studied from July 1982 through June 1984. Continuous data collection allowed estimates to be made for each component of the water-balance... more
The water balance at a low-level radioactive-waste disposal site in northwestern Illinois was studied from July 1982 through June 1984. Continuous data collection allowed estimates to be made for each component of the water-balance equation independent of other components. The average annual precipitation was 948 millimeters. Average annual evapotranspiration was estimated at 637 millimeters, runoff was 160 millimeters, change in
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Current distribution patterns of oxygen-18 concentration in meteoric waters (rain and snow) reveal a close relationship among some climatic parameters such as air temperature or amount of precipitation and the isotopic composition of... more
Current distribution patterns of oxygen-18 concentration in meteoric waters (rain and snow) reveal a close relationship among some climatic parameters such as air temperature or amount of precipitation and the isotopic composition of precipitation. These relationships have been used to extract paleoclimatic information from records of past precipitation preserved in tropical Andean ice cores, even though very little is known
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Go to AGRIS search. Soil Science Society of America journal (Jul-Aug 1991). Variability of an unsaturated sand unit underlying a radioactive-waste trench. ...
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JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 106, NO. D14, PAGES 14,783-14,803, JULY 27, 2001 Hypothesized climate forcing time series for the last 500 years A. Robertson,1 J. Overpeck,2 D. Rind,3 E. Mosley-Thompson,4 G. Zielinski,5 J. Lean,6 D.... more
JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 106, NO. D14, PAGES 14,783-14,803, JULY 27, 2001 Hypothesized climate forcing time series for the last 500 years A. Robertson,1 J. Overpeck,2 D. Rind,3 E. Mosley-Thompson,4 G. Zielinski,5 J. Lean,6 D. Koch,1 J. ...
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Research Interests: Climate variability, Data Assimilation, Peru, Multidisciplinary, Sea surface temperature, and 14 moreGlobal change, Seasonality, Stable Isotope, South America, Ice Cores, Evaluation Model, Atmospheric Circulation, Geophysical, Numerical Model, Amazon basin, El Nino, Water Vapor, Low Resolution, and Interannual Variability
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Pesticide leaching through variably thick soils beneath agricultural fields in Morgan Creek, Maryland was simulated for water years 1995 to 2004 using LEACHM (Leaching Estimation and Chemistry Model). Fifteen individual models were... more
Pesticide leaching through variably thick soils beneath agricultural fields in Morgan Creek, Maryland was simulated for water years 1995 to 2004 using LEACHM (Leaching Estimation and Chemistry Model). Fifteen individual models were constructed to simulate five depths and three crop rotations with associated pesticide applications. Unsaturated zone thickness averaged 4.7 m but reached a maximum of 18.7 m. Average annual recharge to ground water decreased from 15.9 to 11.1 cm as the unsaturated zone increased in thickness from 1 to 10 m. These point estimates of recharge are at the lower end of previously published values, which used methods that integrate over larger areas capturing focused recharge in the numerous detention ponds in the watershed. The total amount of applied and leached masses for five parent pesticide compounds and seven metabolites were estimated for the 32-km2 Morgan Creek watershed by associating each hectare to the closest one-dimensional model analog of model depth and crop rotation scenario as determined from land-use surveys. LEACHM parameters were set such that branched, serial, first-order decay of pesticides and metabolites was realistically simulated. Leaching is predicted to be greatest for shallow soils and for persistent compounds with low sorptivity. Based on simulation results, percent parent compounds leached within the watershed can be described by a regression model of the form e(-depth) (a ln t1/2-b ln K OC) where t1/2 is the degradation half-life in aerobic soils, K OC is the organic carbon normalized sorption coefficient, and a and b are fitted coefficients (R2 = 0.86, p value = 7 x 10(-9)).