Abstract
The purpose of this paper is to separate the total storm runoff into runoff components of overland flow, interflow and groundwater flow. The hourly storm hydrograph is separated into runoff components by the following two methods and the results are compared with each other: 1. (1) The first method is to separate the time series of the total flow into overland flow, interflow, and groundwater flow by using numerical filters determined by the slope of the semi-logarithmic plot of the recession curve. 2. (2) The second one is to separate the total storm runoff, using the geochemical data, into each component by the simultaneous solution of the mass balance equations describing the fluxes of water and the tracer isotope in the stream. 3. (3) Both results compare relatively well with each other.
Sign-in/Register to access full text options 
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
