Abstract
Abstract Detailed investigations of the unsaturated zone in regard to water and tritium balance and tritium input into groundwater are necessary especially in the case of thick and inhomogeneous aeration zone (different soil layers, clay horizons etc.) and inhomogeneous land utilization. The paper shows a method to quantify water and tritium movement and storage in unsaturated zone by means of a two-dimensional conceptual box model called BOWAM(T). The model was tested on 4 sandstone aquifers in the Finne region (brink of the Thuringia basin). The results show that water balance depends strongly on surface morphology and infiltration capacity, non- or semiconducting layers within aeration zone, land usage (forest, agriculture, meadow…) and atmospheric conditions. Especially runoff, evapotranspiration and groundwater recharge at Finne region have a sensitive variation. Naturally, the tritium balance is connected with water balance. There is a difference in tritium input functions into groundwater between c...
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Disclaimer: 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.