Specify domain’s starting fluid temperature on the Initial pane Porewater temperature is 40 °C.

Slides:



Advertisements
Similar presentations
INRNE-BAS MELCOR Pre -Test Calculation of Boil-off test at Quench facility 11th International QUENCH Workshop Forschungszentrum Karlsruhe (FZK), October.
Advertisements

Institute of Energy and Sustainable Development Improvement of a Two-Dimensional (2D) Borehole Heat Exchanger (BHE) Model Miaomiao He, Simon Rees, Li Shao.
Author: Cliff B. Davis Evaluation of Fluid Conduction and Mixing Within a Subassembly of the Actinide Burner Test Reactor.
Simulation lasts 30 years Aquifer is 70% Quartz Specify domain’s starting fluid composition on the Initial pane Initial fluid in equilibrium with Quartz.
MuCool Absorber Review meeting FermiLab, Chicago 21 – 22 February 2003 Fluid Flow and Convective Heat Transfer Modelling by Wing Lau & Stephanie Yang Oxford.
Convection Convection: transfer of heat by a flowing liquid or gas
Specific Heat. Names Specific Heat Capacity Specific Heat Heat Capacity.
Feasibility Analysis h T1 T2 T3 T4 T5 One Dimensional Transient Analysis One Dimensional Finite Difference Steady State Analysis T1 and T5 will be known.
The governing equation for groundwater flow can be written using total head (h) or pressure (p). Why do we typically use head (h) as the dependent variable?
CONVECTION: THE TRANSFER OF THERMAL ENERGY BY THE MOVEMENT OF THE PARTICLES FROM ONE PART OF A MATERIAL TO ANOTHER; TRANSFER OF THERMAL ENERGY IN A FLUID.
1 CHAPTER 5 POROUS MEDIA Examples of Conduction in Porous Media component electronic micro channels coolant (d) coolant porous material (e) Fig.
EGEE 520: Spring 2008 Instructor: Dr. Derek Elsworth By: Sylvain-Didier Kouame A Study of Fluid displacement in Porous Medium using Nitrogen/CO2 injection.
The oven given in the figure is heated with a heat source having the heat flow rate Q. The total heat capacity of all objects in the oven is C and the.
Clean water Start and end times of two reaction intervals Specify domain’s starting fluid composition on the Initial pane.
Numerical simulation of the Alum lakes geothermal outflow J. Newson and M. J. O’Sullivan.
X1t models reactive transport in groundwater flows in one linear or radial coordinate. Set initial fluid composition and mass of sorbing mineral Fe(OH)
Heat Transfer.
Thermal Conductivity. Influence of Fluid Velocity on the Longitudinal Thermal Dispersivity of a Porous Medium.
ICP 12/4/12 Heat and Temperature Notes Video: Classroom Video: Methods of Heat Transfer.
Applied Geothermics Aachen 0ct Numerical Simulation of a Thermal Response Test (TRT) Experiment R. Wagner Applied Geophysics, Aachen University.
Heat Transfer. Heat is the transfer of thermal energy between substances that are at different temperatures.
In Class Examples CME 370: Heat & Mass Transfer Spring
Initial chemical composition and temperature can vary across the domain. Click on a “+” button to enter heterogeneity data for any field variable: ● enter.
Chapter 4.4 Notes Resistance in Thermal Systems. In fluid systems, resistance opposes the flow of Fluid. In thermal systems, resistance opposes the flow.
Conduction C ontents: Basic Concept Example Whiteboards.
Decouple reaction between carbonate and Benzene(aq), other forms of carbon. Config → Redox Couples… Default setting: all redox reactions are coupled.
O o Problem HOMEWORK-01 Establish the closed loop block diagram. G c (s)=K p Answer: The oven shown in the figure is heated with a source having.
Moving Thermal Energy. CONDUCTION ► Is the transfer of energy through matter by direct contact of particles.
Microwave Cooking Modeling Heat and moisture transport Andriy Rychahivskyy.
MULTLAB FEM-UNICAMP UNICAMP Workshop on Thermal Boundary Conditions Several thermal boundary conditions will be explored in this workshop modifying the.
Porewater temperature is 40°C Specify domain’s starting fluid temperature on the Initial pane.
Finite-Difference Solutions Part 2
Variable inlet chemistry. Inlet fluid “contaminated” enters the domain from t = 0 to 2 years Inlet fluid “flush” enters the domain from t = 2 to 10 years.
Pulse of Benzene contaminated water is attenuated by biodegradation. X1t models reactive transport in groundwater flows in one linear, radial, or spherical.
Standards 3: Thermal Energy How Heat Moves  How heat energy transfers through solid.  By direct contact from HOT objects to COLD objects.
* Materials that allow heat, electricity, or sound waves to pass through them.
Decouple reaction between carbonate and acetate, carbonate and methane, and sulfate and sulfide. Config → Redox Couples… Default setting: all redox reactions.
Clean water Specify starting fluid composition on the Initial pane.
Conduction Convection Radiation
Heat Transfer.
Specify coordinate system on the Domain pane.
Chain together kinetic reactions
14-6 Heat Transfer: Conduction
Date of download: 12/25/2017 Copyright © ASME. All rights reserved.
What is it and how do we measure it?
Convective Thermo-Poroelasticity in Non-Boiling Geothermal Reservoirs
Understanding Heat Transfer, Conduction, Convection and Radiation
Physics 202 Lecture 4 Heat and Temperature.
Specify domain’s starting fluid composition on the Initial pane
Specify domain’s starting fluid composition on the Initial pane
Specify domain’s starting fluid composition on the Initial pane
Specify domain’s starting fluid composition on the Initial pane
X position (m) I s o t p i c m n C , d a y Bulk fluid CO (aq)
The Intervals pane sets the total duration of the simulation.
The Initial fluid has negligible Pb2+ everywhere but the central node
Earth’s Energy Balance
Specify domain’s starting fluid composition on the Initial pane
Reading Materials: Chapter 9
Default setting: all redox reactions are coupled.
Convective Thermo-Poroelasticity in Non-Boiling Geothermal Reservoirs
Config → Dual Porosity… Run → Go
Chapter Four: Energy transfer by Heat, Work and Mass
Heat Transfer Science Vocabulary
Energy & Transformations
Temperature Is a property of an object which determines the direction of net heat flow when an object is placed in contact with some other object. Heat.
Heat Transfer.
Heat Temperature Conduction Convection Radiation
12. Heat Exchangers Chemical engineering 170.
The Sun is the source of energy for the Earth.
Presentation transcript:

Specify domain’s starting fluid temperature on the Initial pane Porewater temperature is 40 °C

Initial fluid displaced by 200 °C injectate Inlet fluid enters the domain from t = 0 to 20 days

Specify domain size, gridding, and flow rate on the Domain pane. Domain is 2000 cm long, divided into 40 nodal blocks Radial domain set in this example

Set various thermal properties on the Medium pane. Can include transient heat sources or sinks within the domain. Set thermal conductivity of porous medium to model heat conduction. Run → Go traces the model Set heat capacity of the fluid and rock to simulate heat transfer by advecting groundwater.

Hot water is injected into the domain’s inlet. Heat transported by advection and conduction.