Initial chemical composition and temperature can vary across the domain. Click on a “+” button to enter heterogeneity data for any field variable: ● enter.

Slides:



Advertisements
Similar presentations
Model water-rock interaction Enter your initial fluid composition on the Basis pane, then go to the Reactants pane to create a reaction path. Titrate in.
Advertisements

Carbon Deposition in Heterogeneous Catalysis
Simulation lasts 30 years Aquifer is 70% Quartz Specify domain’s starting fluid composition on the Initial pane Initial fluid in equilibrium with Quartz.
Finite Element Method (FEM) Different from the finite difference method (FDM) described earlier, the FEM introduces approximated solutions of the variables.
Chapter 3 Steady-State Conduction Multiple Dimensions
Scripts and Flow Control. Scripts So far we have been entering commands directly into the command line But there is a better way Script files (and functions)
REVIEW. What processes are represented in the governing equation that we use to represent solute transport through porous media? Advection, dispersion,
Variance and Standard Deviation The Expected Value of a random variable gives the average value of the distribution The Standard Deviation shows how spread.
Non Isothermal Chemical Reactor ChE 479 Alexander Couzis.
Thermal Energy and Heat Temperature, Thermal Energy, and Heat The Transfer of Heat Thermal Energy and States of Matter Uses of Heat Table of Contents.
Combined Geological Modelling and Flow Simulation J. Florian Wellmann, Lynn Reid, Klaus Regenauer-Lieb and the Western Australian Geothermal Centre of.
How to use WhoIs.Net Click to Continue Begin by typing your desired Domain Name in the Entry Field Mychurch.org Click on GO.
Two-Dimensional Conduction: Flux Plots and Shape Factors
Poisson Random Variable Provides model for data that represent the number of occurrences of a specified event in a given unit of time X represents the.
Standard Normal Distribution
Clean water Start and end times of two reaction intervals Specify domain’s starting fluid composition on the Initial pane.
PAT328, Section 3, March 2001MAR120, Lecture 4, March 2001S16-1MAR120, Section 16, December 2001 SECTION 16 HEAT TRANSFER ANALYSIS.
Porosity m. Field variables are constant in space (homogeneous) by default. Click + to expand, then to select options. Porosity is 30% throughout.
X1t models reactive transport in groundwater flows in one linear or radial coordinate. Set initial fluid composition and mass of sorbing mineral Fe(OH)
Copyright 2008 McGraw-Hill Ryerson 1 TECHNOLOGY PLUG-IN T7 PROBLEM SOLVING USING ACCESS.
Applications of Spatial Statistics in Ecology Introduction.
Specify chemical composition of fluid and formation minerals from the Initial pane. Set initial temperatureSet starting and ending times.
Specify domain’s starting fluid temperature on the Initial pane Porewater temperature is 40 °C.
McGraw-Hill/Irwin © 2008 The McGraw-Hill Companies, All Rights Reserved Plug-In T7: Problem Solving Using Access 2007 Business Driven Technology.
Advection-Dispersion Equation (ADE)
Convective Heat Transfer in Porous Media filled with Compressible Fluid subjected to Magnetic Field Watit Pakdee* and Bawonsak Yuwaganit Center R & D on.
19 Basics of Mass Transport
Copyright © 2010 Altair Engineering, Inc. All rights reserved.Altair Proprietary and Confidential Information Section 20 Flux and Convection.
Engineering Analysis – Computational Fluid Dynamics –
T7-1 LEARNING OUTCOMES – ACCESS PROBLEM SOLVING 1.Describe the process of using the Simple Query Wizard using Access 2.Describe the process of using the.
Decouple reaction between carbonate and Benzene(aq), other forms of carbon. Config → Redox Couples… Default setting: all redox reactions are coupled.
(Z&B) Steps in Transport Modeling Calibration step (calibrate flow & transport model) Adjust parameter values Design conceptual model Assess uncertainty.
Measures of Central Tendency and Dispersion from Grouped Data.
Porewater temperature is 40°C Specify domain’s starting fluid temperature on the Initial pane.
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.
The Laplace Transform.
Pulse of Benzene contaminated water is attenuated by biodegradation. X1t models reactive transport in groundwater flows in one linear, radial, or spherical.
3/23/05ME 2591 Numerical Methods in Heat Conduction Reference: Incropera & DeWitt, Chapter 4, sections Chapter 5, section 5.9.
McGraw-Hill/Irwin © 2008 The McGraw-Hill Companies, All Rights Reserved Plug-In T7: Problem Solving Using Access 2007 Business Driven Technology.
Innovation Intelligence ® Section 20 Flux and Convection.
KKEK 3152 MODELLING of CHEMICAL PROCESSES. Lumped vs Distributed parameter model.
1 Variational and Weighted Residual Methods. 2 Introduction The Finite Element method can be used to solve various problems, including: Steady-state field.
Quick recap.... Heat, Temperature and Internal energy Define: 1. Heat Defined as the transfer of energy across a boundary due to a temperature difference.
Clean water Specify starting fluid composition on the Initial pane.
Click + to expand, then to select options.
Chapter 2: Introduction to Conduction
Finite Element Application
Analyzing Data Using Access
Date of download: 10/24/2017 Copyright © ASME. All rights reserved.
Plug-In T7: Problem Solving Using Access 2007
Chapter 2. Mathematical Expression of Conduction
Access Maintaining and Querying a Database
You control discretization on the Domain 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
A First Course on Kinetics and Reaction Engineering
The Initial fluid has negligible Pb2+ everywhere but the central node
Specify domain’s starting fluid composition on the Initial pane
Default setting: all redox reactions are coupled.
Concentrations and activities
Effects of Free and Forced Convection on the Convection Coefficient and Time to Steady State for Various Objects Christian Roys, Jon Zywusko, and Julie.
What would be the typical temperature in Atlanta?
Config → Dual Porosity… Run → Go
Thermal Energy & Heat Capacity:
1 To go to the next slide, click this button instead. A random slide will come up.
Na-Cl fluid in equilibrium with four minerals at 300°C
Research Project Mean vulnerability to drought 1990–2005 for wheat production. Vulnerability to drought is low (high) when crop failures are small (big)
[6.1] Patterns Describe the T-Block pattern
EQUATION 5.1 The Production Function
Presentation transcript:

Initial chemical composition and temperature can vary across the domain. Click on a “+” button to enter heterogeneity data for any field variable: ● enter data node by node ● import a table ● use a script, equation, or function ● enter an average value and standard deviation

Nodal block spacing can be regular or refined in the areas of greatest interest.

Choose to enter porosity data node by node.

Import a table with porosity values for each node. Alternatively you can enter tables in-line from the command pane.

Use a simple equation to describe the porosity field. Or write a BASIC script or C++ function for the most flexibility. Thermal conductivity and internal heat sources can vary in space, as can longitudinal and transverse dispersivity.

Porosity is set in this run to vary randomly according to a Gaussian distribution. Permeability is set to vary with porosity.

Br − enters the fluid through the left boundary. The random porosity and permeability structure create a “fingering” pattern of infiltration.