Objectives and Goals. What this course is Basic ground water physics and chemistry Introduction to ground water flow and solute transport modeling Ground.

Slides:



Advertisements
Similar presentations
Lake Ponchartrain Normal WS EL = 0.0 Normal Operation Before Gates City of New Orleans Storm Water Pumping Station Levee Top of Levee EL = 11.5 Maximum.
Advertisements

Introduction to EE 327. Pop Quiz Grading 5Correct 4Close 3Legitimate Attempt 2Attempt (but not close) 0No Attempt All quiz grades will be out of 5 points.
Introduction to Physical and Chemical Hydrogeology (GEO 346C) Instructor: Bayani Cardenas TAs: Travis Swanson and John Nowinski
Boundaries and Superposition
Numerical Simulations of Multi-Species Contaminant Transport in Variably Saturated Aquifers in Coastal Areas Presenter : Yi-Ming Wei Adviser : Chuen-Fa.
Subsurface Hydrology Unsaturated Zone Hydrology Groundwater Hydrology (Hydrogeology )
Subsurface Hydrology Unsaturated Zone Hydrology Groundwater Hydrology (Hydrogeology )
The Valley Network Record on Mars (Class 2). LPSC Key Sessions on the Mars Hydrological Cycle Tuesday Afternoon, Sess 251. Ground Ice and Climate Change.
Exam Preparation Fall 2008 CSCE 235 Introduction to Discrete Structures Course web-page: cse.unl.edu/~cse235 Questions:
GLY 521- Hydrogeology Modflow Packages. Block Center Flow (BCF) Package The BCF package is the central package for all solutions Specify the way each.
Water Above and Below Ground
Course Introduction. Math is an important subject:  We live in a changing world. The need to understand Math in everyday life has never been greater.
ESS 454 Hydrogeology Module 1 Course Overview, Hydrogeology History, Hydrologic Cycle, Sustainability I & II.
Watershed Assessment and Diagnosis of Condition for August 20, 2007 Joe Magner and Greg Johnson MPCA.
GEO/ENV 315/GEO 514 Hydrogeology Class meets: Time: Mondays: 5:30 pm – 8:30 pm. Location: ESS 183 Office Hours: Wednesdays and Fridays 3:00 – 4:00 pm ESS.
Fluid Mechanics –I Surveying –I Mechanics of Solids Building Materials
Tempus CD-JEP Education and Culture Assiut University Coordinator Prof.Esmat Keheila Grant Holder.
Storage Coefficients/Specific Yield. Storage Coefficient/Storativity S: storage coefficient or storativity: The amount of water stored or released per.
Dr. James M. Martin-Hayden Associate Professor Dr. James M. Martin-Hayden Associate Professor (419)
Understanding Ground Water Modeling Gary Johnson Donna Cosgrove Idaho Water Resources Research Institute University of Idaho Idaho Falls.
GROUND-WATER AVAILABILITY Planning for Sustainable Future Water Supplies South of the C&D Canal Delaware Geological Survey – January 2007.
RAP 1._____ layer of atmosphere that weather occurs in (atm layers) 2._____ most abundant gas in the atmosphere (atmosphere) 3._____changes from water.
Groundwater David R. Maidment CE 394K.2 Spring 2005 Reading: Handbook of Hydrology, Chapter 6, Sec 6.1 to 6.7.
Dave Watkins BSc 3 AG, EGG, EST, CZEM MSc Geotechnical Engineering
Loren McClung. Work Description  Discover the impact of water on elements & how elements affect the quality of water.
Civil and Environmental Engineering
MATH | First Day of Class Introduction Course Name, Course Number College Date.
HOW DOES PRECIPITATION MAKE ITS WAY BACK TO THE OCEANS? Notebook Question.
Calculator Questions & Answers. When can I use a calculator?
The Islamic University of Gaza Faculty of Engineering Civil Engineering Department EENV 5326 Groundwater Modeling.
ME 475/675 Introduction to Combustion Lecture 26 Plug flow reactor, Problem X5:Constant area and pressure equations.
Hydrogeological Background Study Proposed Gravel Pit SE W5M Brent Lennox, M.Sc., P.Geol. Waterline Resources Inc. December 10, 2012.
Fresh Water Notes Pages What is Water? Water is a compound. 1 water Molecule is made of: 2 Hydrogen Atoms 1 Oxygen Atom.
Chemical Hydrogeology GLY What this course is: Diffusion equation Dispersion Convection-Dispersion equation Boundary conditions Sorption Production.
An Analytical Solution for Groundwater Flow to Various Wells in a Finite Unconfined Aquifer near a Stream National Chiao Tung University Adviser:Hund-Der.
Geochemistry of prairie wetlands. CWB Produces 50 to 80% of nation’s waterfowl.
CE 3354 Engineering Hydrology Lecture 2: Surface and Groundwater Hydrologic Systems.
Course Title. N2 - Attention Getter Enter information on screen to serve as the “attention- getter” portion of the course.
Modeling with WEAP University of Utah Hydroinformatics - Fall 2015.
Groundwater movement Objective To be able to calculate the hydraulic conductivity of a sample given measurements from a permeameter To be able to evaluate.
Lesson 3: An exploration of stakeholders and where we fit in.
CEE 3430, Engineering Hydrology David Tarboton. Overview Handouts –Syllabus –Schedule –Student Information Sheet –Homework 1 Web:
Florida Water Cycle© /07/2002.
Test Rules Answer all questions. Please answer on separate sheets of paper. Reference material. You may refer to one 8.5 x 11 inch page of notes, hand.
Radial Flow to an Unconfined Aquifer From Mays, 2011, Ground and Surface Water Hydrology.
THE HYDROLOGIC CYCLE.
Water Cycle and Groundwater
CEE 3430, Engineering Hydrology David Tarboton
Chapter 3 The Conceptual Model
Test 1 Review Chapter 1, Hydrologic cycle and the water balance
Objectives, Format, and Goals
D. The Hydrosphere 1. 70% of the Earth is water
Human dependence Practice questions Human.
Welcome to Chemistry Ms. Ose
نجاح وفشل المنشآت الصغيرة
Transport Modeling in Groundwater
Anisotropy – Key ideas Effective conductivity that represents aggregate effect of flow through a layered system Effective conductivity is different parallel.
Determine the storage coefficient
Developing a Community of Scholars and Teaching Modules for Water Resource Courses at KU, University of California, Davis, and the University of Alabama.
Determine the storage coefficient
Introduction to EE 327.
The hydrologic cycle.
MATH 1310 Section 2.8.
Transport Modeling in Groundwater
MATH 1310 Section 2.8.
MATH 1310 Section 2.8.
Welcome to Principles of
Welcome 12/10/14   Find the equation in standard form given the following information: Zeros x = 5 ± 3i, f(2) = 27.
Name __________________________
MATH 1310 Section 2.8.
Presentation transcript:

Objectives and Goals

What this course is Basic ground water physics and chemistry Introduction to ground water flow and solute transport modeling Ground water in hydrologic and geologic framework Aquifer testing Math sharpening

What this course is not Large modeling package training Numerical methods Aqueous geochemistry

What I Expect Class participation –Attendance –Attention –Questions (and answers) –Homework –Full preparation for quizzes Knowledge/Skills –Understand and apply basic flow and transport equations –Be able to analyze head, breakthrough, and aquifer test data –Understanding is key

Semester Project Individual or group Group project proposal: FIU Hydrogeology –Collect available well, canal, lake, precipitation, transmissivity, pumping, ET etc. data. –Present data –Application?