Dr. Van Wagoner graduated from the University of Texas Southwestern Medical Center at Dallas in 1996. He works in McKinney, TX and 1 other location and specializes in Allergy & Immunology and Pediatric Allergy/Immunology. Dr. Van Wagoner is affiliated with Denton Regional Medical Center, Medical Center Of Plano, Texas Health Presbyterian Hospital Denton and Texoma Medical Center.
Dr. Wagoner graduated from the Oregon Health & Science University School of Medicine in 1999. He works in Olympia, WA and 2 other locations and specializes in Cardiovascular Disease and Nuclear Cardiology. Dr. Wagoner is affiliated with Providence Centralia Hospital, Providence St Peter Hospital, Saint Clare Hospital, St Elizabeth Hospital, St Francis Hospital and St Joseph Medical Center.
Wagoner Medical Group 800 N Alpha St, Grand Island, NE 68803 308 382-2010 (phone), 308 382-9549 (fax)
Education:
Medical School University of Nebraska College of Medicine Graduated: 1978
Procedures:
Arthrocentesis Cardiac Stress Test Electrocardiogram (EKG or ECG) Skin Tags Removal Vaccine Administration
Conditions:
Anemia Atrial Fibrillation and Atrial Flutter Disorders of Lipoid Metabolism Gastroesophageal Reflux Disease (GERD) Hypertension (HTN)
Languages:
English Spanish
Description:
Dr. Wagoner graduated from the University of Nebraska College of Medicine in 1978. He works in Grand Island, NE and specializes in Internal Medicine. Dr. Wagoner is affiliated with CHI Health Saint Francis.
Max Deffenbaugh - Houston TX, US John Van Wagoner - Houston TX, US Chun Huh - Austin TX, US Tao Sun - Missouri City TX, US
Assignee:
EXXONMOBIL UPSTREAM RESEARCH COMPANY - Houston TX
International Classification:
G06F019/00
US Classification:
702/002000
Abstract:
The internal properties of a water-lain sediment body can be determined from the shape of the deposit. One method comprises solving equations relating the shape of a sediment body to the flow field that produced the body and using the flow field to solve for the sediment body properties in at least one point within the body. The flow field properties include flow velocity, suspended sediment volume fractions, deposition time, and flow height. The properties of the water-lain sediments include, in addition to the flow properties associated with deposition of the sediments, the thickness of the sediment body, the size of the body, the shape of the body, and the grain size distribution at points within the body.
Method For Predicting Properties Of A Sedimentary Deposit From A Thickness Contour Of The Deposit
Max Deffenbaugh - Houston TX, US John Van Wagoner - Houston TX, US Neal Adair - Sugar Land TX, US
Assignee:
EXXONMOBIL UPSTREAM RESEARCH COMPANY - Houston TX
International Classification:
G01V003/00 G01V007/00 G06F019/00
US Classification:
702/002000
Abstract:
The properties of a water-lain sedimentary deposit may be predicted at any location from a contour of constant deposit thickness. One embodiment of the method comprises (a) determining an outline of constant deposit thickness in a measured deposit, (b) determining the fluid flow properties at the inlet of the measured deposit, (c) determining a property of the deposit at any point inside the deposit from modeling the fluid flow. The properties of the deposit at any point may include the thickness of the sediment body, the size of the body, the shape of the body, and the grain size distribution at each point within the body, and any combination thereof.
Method For Geologic Modeling Through Hydrodynamics-Based Gridding (Hydro-Grids)
Dachang Li - Katy TX, US Tao Sun - Missouri City TX, US Chun Huh - Austin TX, US Chris Donofrio - The Woodlands TX, US John Van Wagoner - Houston TX, US Max Deffenbaugh - Califon NJ, US
International Classification:
G01V 1/28 G06F 19/00
US Classification:
702012000
Abstract:
The present invention is a method of hydrodynamics-based gridding (Hydro-Grids) for creating geologic models of subsurface volumes, such as reservoirs. Vertical grid surfaces may be chosen in an unstructured fashion to provide lateral resolution where needed. Lateral grid surfaces are created to represent surfaces of constant geologic time based on simulation of the depositional processes that created the subsurface volume. The values of geologic properties are then specified within each cell created by the intersections of the vertical and lateral surfaces. The geologic data may include, for example, seismic data, outcrop studies, well log data, core data, numerical modeling data, and interpreted stratigraphic surfaces based on seismic data. The modeled geologic properties of the subsurface volume may include, for example, grain size distribution, connectivity, net-to-gross, porosity, permeability and pore pressure.
Method For Evaluating Sedimentary Basin Properties By Numerical Modeling Of Sedimentation Processes
Tao Sun - Missouri City TX, US Dachang Li - Katy TX, US Max Deffenbaugh - Califon NJ, US Chun Huh - Austin TX, US David Hoyal - Houston TX, US Neal Adair - Sugar Land TX, US Xiao-Hui Wu - Sugar Land TX, US Timothy Chartrand - Spring TX, US John Van Wagoner - Houston TX, US
International Classification:
G06F 19/00
US Classification:
702013000
Abstract:
A method is disclosed for simulating the formation of sedimentary deposits. In one embodiment, this method involves, (a) solving a two-dimensional time-dependent map view system of equations for at least flow momentum, flow height, suspended sediment concentration, and entrainment of overlying water, (b) calculating net sediment deposition at each map view location using the flow properties, (c) recording the time-variability of the net sediment deposition.
Overlapped Multiple Layer Depth Averaged Flow Model Of A Turbidity Current
Tao Sun - Missouri City TX, US Dachang Li - Katy TX, US John Van Wagoner - Houston TX, US Xiaohui Wu - Sugar Land TX, US
International Classification:
E21B 43/00 G06F 17/10 G06G 7/57
US Classification:
166369, 703 9, 703 10
Abstract:
A method of generating a model of a turbidity current in a fluid is disclosed. A first flow layer in the turbidity current is defined. The method successively defines at least one more flow layer in the turbidity current. Each successive flow layer includes the previously defined flow layer. A set of depth-averaged flow variables for each flow layer is defined. A model is developed that describes the turbidity current. The model uses fluid flow equations and the set of depth-averaged flow variables for each flow layer to predict fluid flow in each flow layer. The model is then output.
Name / Title
Company / Classification
Phones & Addresses
John E. Wagoner
PLANET HARMON, INC
John M Wagoner
WAGONER'S RENTALS, LLC
John E. Wagoner
FAVER, INC
John E. Wagoner
ROACH ENTERPRISES OF OHIO, LTD
John E. Wagoner
JAMES G. O'BRIEN AND ASSOCIATES, LLC
John E Wagoner
TIMBERSTONE MORTGAGE, LTD
John E. Wagoner
COLONY & COLONY, LTD
John E. Wagoner
MON AMI LIMOUSINE SERVICE, INC
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