Abstract
Dynamics of processes of moisture redistribution in water balance of agrolandscapes was studied with the use of analytical modeling. Water balance is represented as the result of changes in its components with time. Atmospheric precipitation and its interception on the surface by plants, water accumulation in depressions on the slope, infiltration, and slope runoff are simulated in combination with the processes of vertical water flow to groundwater in the context of system dynamics. Analytical modeling is used as a basis for the representation of the system dynamics in the mode of a simulation modeling of hydrological processes of soil moisture accumulation. Modeling of vertical water flow is based on the semiempirical description of moisture conductivity and retention in the aeration zone.
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.
