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Theme 3 Analysis of Transient Flow Through Porous Sediments at Different Levels of Aggregation. Theme leaders Prof. Van den Akker & Prof. Verruijt. Projects in Theme 3.
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Theme 3Analysis of Transient Flow Through Porous Sediments at Different Levels of Aggregation Theme leaders Prof. Van den Akker & Prof. Verruijt
Projects in Theme 3 • Project 3.1 Transient Flow Through Chemically Interactive Porous Sediments(Dr. ir. Amro Elfeki). Physical and Chemical Processes Modelling+Uncertainty Modelling. • Project 3.2 Transient Field Properties and Boundary conditions (Ir. C. Zwanenburg). Measurements+Physical Process Modelling. • Project 3.3 Fundamental description of hysteresis of capillary pressure (Ir. W.J. Plug). Physical Process Modelling +Measurements • Project 3.4 Optimum groundwater monitoring network design at landfill sites (Ir. N. Yenigul). Monitoring+Physical Process Modelling. • Project 3.6 Catalytic and dynamic impact of mico-organisms on soil water interaction (Dr. J. Geelhoed). Biological Process modelling+Measurements. • Project 3.7 Iron oxidizing and iron reducing bacteria. ( R. Kumaraswamy). Biological Process modelling+Measurements.
Transient Flow Through Chemically Interactive Porous Sediments Dr. Ir. Amro Elfeki Section Hydrology and Ecology, Dept. of Water Management TU Delft
Research Directions and Collaborations • Heterogeneity Modelling and Uncertainty by Coupled Markov Chains (CMC): -2D CMC: Elfeki (CiTG) and Dekking (EEMC). -3D CMC: (2-years postodc NWO Project: Park, Elfeki, Dekking. • Transient Flow and Transport Modelling: - Gradient Magnitude Variability: MSc. thesis (Lebreton, Elfeki and Uffink). - Gradient Direction Variability: (not yet). • Modelling Chemical Interaction with • Porous Sediments: 2-State PTRW method: (Elfeki, Bruining, Dekking, Kraaikamp and Uffink)
Research Output • Heterogeneity Modelling and Uncertainty : - 2D CMC: Article in review (Elfeki and Dekking). -2D CMC uncertainty: Article in preparation (Elfeki and Dekking). - 3D CMC: Article published in UIST Conf. Oct., 2003. (Park, Elfeki and Dekking) • Transient Groundwater Flow and Transport Modelling: -MSc. Thesis by Sophie Lebreton (Supervisors: Elfeki and Uffink). -Poster for the DIOC meeting Dec. 2003. -Article published at MEJ, March, 2003 (Elfeki). -Articles are foreseen from Sophie thesis. • Modelling Chemical Interaction with Porous Sediments: - Article in Preparation “Linear Adsorption” (Elfeki, Bruining, Dekking, Kraaikamp and Uffink). - Non-linear Adsorption Case.
Influence of the period of Oscillation Head profiles along the aquifer length. T he downstream water level is a cosine function with an amplitude of 5m and with different periods: 1, 5, 10 days. The length of the aquifer is 300m, the storativity S=0.01. Penetration length : controls the propagation of oscillations within the aquifer. When the period P increases, the penetration length increases
Geological Uncertainty Quantification by CMC Data 19 boreholes Stochastic simulation of the longitudinal Section of afsluitdijk-Caspar de Roblesdijk, a part of Waddenzeedijken conditioned on 13 boreholes. Simulation conditioned on 13 boreholes
Modelling Chemical Interaction with Porous Sediments: Non-linear Adsorption