Moving Boundary Problems are Us The development and application of numerical methods for transport models towards an integrated frame-work for modeling.

Slides:



Advertisements
Similar presentations
Introduction to Plasma-Surface Interactions Lecture 6 Divertors.
Advertisements

Subsurface Fate and Transport of Contaminants
Numerical Simulation of Wave-Seawall Interaction Clive Mingham, Derek Causon, David Ingram and Stephen Richardson Centre for Mathematical Modelling and.
Oceans.
2L 2aL s h T Introduction Zach Frye, University of Wisconsin-Eau Claire Faculty Advisors: Mohamed Elgindi, and John Drost, Department of Mathematics Funded.
Moving Boundaries in Earthscapes Damien T. Kawakami, V.R. Voller, C. Paola, G. Parker, J. B. Swenson NSF-STC
National Center for Earth-surface Dynamics Modeling physical and ecological dynamics of channel systems that shape Earth’s surface Moving boundary problems.
National Center for Earth-surface Dynamics Modeling physical and ecological dynamics of channel systems that shape Earth’s surface Moving boundary problems.
Validation and Verification of Moving Boundary Models of Land Building Processes Vaughan R. Voller National Center for Earth-surface Dynamics Civil Engineering,
Influence of Geomorphic Complexity on Hyporheic Flow and Nutrient Processing Prepared by Dan Baker for CE 413.
Scouring—↑flashiness of the hydrograph → scour and gravel shift.
Numerical analysis of simultaneous heat and mass transfer during absorption of polluted gases by cloud droplets T. Elperin, A. Fominykh and B. Krasovitov.
Non-local Transport in Channel Networks Vaughan Voller Civil Engineering University of Minnesota Tetsuji Muto, Wonsuck Kim, Gary Parker, John Swenson,
10.2 Oxygen Dissociation Curves
Chapter 20 Section 1 Review Page 500
Chapter 20 Section 1 Review Page 500
Unit 2.4: Currents and Tides. Vocabulary: 1.Current: a large stream of moving water that flows through oceans Unlike waves, currents carry water from.
OPTIMAL STRATEGIES FOR ECOLOGICAL RESTORATION UNDER CLIMATE CHANGE Koel Ghosh, James S. Shortle, and Carl Hershner * Agricultural Economics and Rural Sociology,
What Causes Acid Precipitation?
Ryan Johnson Earth and Physical Science Department Western Oregon University Monmouth, Oregon
Ocean Circulation Winds and Currents. The __________________ and the ___________________ interact The ocean and atmosphere transport heat from the ______________________________.
Channel Modification Washington Dept. Forestry, 2004, Channel Modification Techniques Katie Halvorson.
Lesson 9 Channel characteristics
Jeopardy Q 1 Q 2 Q 3 Q 4 Q 5 Q 6Q 16Q 11Q 21 Q 7Q 12Q 17Q 22 Q 8 Q 13 Q 18 Q 23 Q 9 Q 14 Q 19Q 24 Q 10 Q 15 Q 20Q 25 Final Jeopardy Oceans.
Section 3: Acid Precipitation
The Structure of Hydrosphere. Oceans—96.5% of water found here Fresh water—3.5% of water found here Fresh water distribution:  Ice: 1.762%  Groundwater:
Tracers for Flow and Mass Transport
National Center for Earth-surface Dynamics an NSF Science and Technology Center V.R. Voller+, J. B. Swenson*, W. Kim+ and C. Paola+ +
Rivers and Streams. River Systems A river or stream: any body of water flowing downhill in a well defined channel A river or stream: any body of water.
Dmitry Arkhipov and Georgy Khabakhpashev New equations for modeling nonlinear waves interaction on a free surface of fluid shallow layer Department of.
Oceans. Why is the Ocean Salty? 1. The ocean is salty because of dissolved chemicals eroded from the Earth's crust and washed into the sea. 2. Ejections.
Governing Equations II
Transpiration Similar to evaporation, this is the loss of water through plants. – Pores in leaves (stomata) are opened to release oxygen and water vapor.
Salinity. What is the difference between a fish and a piano? You can't tuna fish.
Biological biodiversity Is the term given to the variety of life on Earth and the variety within and between all species of plants, animals and micro-organisms.
OCEANS INTRO AND ESTUARY REVIEW Module 7. THE OCEAN IS A DYNAMIC SYSTEM- ALWAYS CHANGING!  The ocean is an important source of food and mineral resources.
The shallow water equations in geomorphic modeling
Section 3: Acid Precipitation
Waves and Currents.
A Mesh-less method for solutions of the Stefan Problem
delta landform model river channel sediments.
Section 3: Acid Precipitation
Section 3: Acid Precipitation
Section 3: Aquatic Ecosystems
Direction and Non Linearity in Non-local Diffusion Transport Models
Section 3: Aquatic Ecosystems
Advanced Contaminant-Transport Techniques
Modeling tools Training Module
Lotic vs. Lentic Systems
Chapter 4.5 – Aquatic Ecosystems
Aquatic Ecology Ocean Life Zones.
Example: Micromixer.
A World of Water “Living in water”
Oceans.
Waves, Currents, and Tides (S6E.3.d)
Transport Modeling in Groundwater
Section 3: Aquatic Ecosystems
Waves and Currents.
How are lakes and streams similar? How are they different?
Objectives Explain the causes of acid precipitation.
Section 3: Acid Precipitation
Transport Modeling in Groundwater
Salinity.
Chapter 54: Ecosystems.
Ocean Characteristics and Technology
Waves and Currents.
Section 3: Acid Precipitation
Section 3: Acid Precipitation
Classroom Catalyst.
Modeling Water Treatment Using the Contaminant Transport Module
Presentation transcript:

Moving Boundary Problems are Us The development and application of numerical methods for transport models towards an integrated frame-work for modeling earth surface dynamics from source to sink Voller, Paola, Mohrig, Parker Wolinsky, Jerolmack Kim, Qian, Sittoni Stefan, Swenson SA2Reconstructing delta dynamics from cores and other records SR2Determine how physical channel attributes affect nutrient & contaminant dynamics, productivity, and species diversity

Interactions Between Flow and Fan Topography Some JT Questions: How Does topography influence the flow over fans? Is there fan geometry that crates a bypassing condition ? Investigate by solving Exner + Shallow Water Eq Over Different Tops. FlatLong ComboTran. SA2Reconstructing delta dynamics from cores and other records

Transport exchange between a stream and its gravel bed is greatly enhanced by surface waves and/or bed forms. 2-D Advection Dispersion A Depth dependent dispersion can Be obtained from problem par. Hence an easy to use meaningful management tool Can be used to answer questions What restoration devices can be in place to create conditions to increase (dissolved oxygen for fish eggs) or decrease (organic carbon) exchange with the bed. Further work compare with Clark Stream-Lab exp. SR2Determine how physical channel attributes affect nutrient & contaminant dynamics, productivity, and species diversity Through Solution of a transient advection-dispersion can be shown that the laterally averaged concentration penetration CAN Be described by a 1-D Dispersion Equation y

Increasing Flexibility GRID---FIN-DIFF Efficient solution Ax=b — Difficult to Fit Geometry MESH---FEM Less Efficient solution Ax=b — Easy to Fit Geometry Difficult to adapt “CLOUD”---SPH Even Less Efficient solution Ax=b — Very Easy to Fit Geometry Easy to adapt Application of Meshless Methods