Zobrazeno 1 - 10
of 22
pro vyhledávání: '"J Kent Mitchell"'
Publikováno v:
Journal of Environmental Quality. 20:663-670
Runoff, soil loss and sediment bound total Kjeldahl nitrogen (TKN) and Bray P-l phosphorus losses from simulated rainfall were measured from five alternative corn and soybean tillage systems. Runoff and soil loss were influenced by contouring and til
Publikováno v:
Journal of Environmental Quality. 19:539-545
Publikováno v:
Hydrological Sciences Journal. 50
River basin lag time (LAG), defined as the elapsed time between the occurrence of the centroids of the effective rainfall intensity pattern and the storm runoff hydrograph, is an important factor in determining the time to peak and the peak value of
Publikováno v:
2005 Tampa, FL July 17-20, 2005.
The Little Vermilion River (LVR) watershed in east central Illinois is an example of a watershed with altered hydrology from subsurface drainage systems. A continuous monitoring study has been conducted from 1991 to 2004 on this watershed to evaluate
Publikováno v:
2001 Sacramento, CA July 29-August 1,2001.
Agriculture is the leading source of non-point source pollution on a national scale. The driving force of non-point source pollution is the rainfall-runoff process, which is the transformation of rainfall to direct streamflow. This is a complex, nonl
Publikováno v:
ACS Symposium Series ISBN: 9780841224803
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9142d670a80d71477b490371dac840b1
https://doi.org/10.1021/bk-1992-0510.ch022
https://doi.org/10.1021/bk-1992-0510.ch022
Autor:
Benjamin A. Jones, J. Kent Mitchell
Publikováno v:
Journal of the American Water Resources Association. 14:777-802
Micro-relief surface depression storage is one of the dynamic components of the rainfall-runoff process. The quantification of the effect of rainfall intensity and duration on the micro-relief was the subject of this study. Micro-relief measurements
Autor:
Benjamin A. Jones, J. Kent Mitchell
Publikováno v:
Journal of the American Water Resources Association. 12:1205-1222
Micro-relief surface depression storage is one of the components of the rainfall-runoff process. The quantification of surface depression storage values and a depth-storage model to describe the storage was the subject of this study. Point measuremen