UT GeoFluids News
UT GeoFluids Group Research Day
On August 15th, the UT GeoFluids group had a day-long meeting reviewing our research advancements over the summer. The group has been hard at work! Afterwards, we celebrated in Peter’s back yard.
posted August 2015
UT GeoFluids 2015 Annual Meeting
The 2015 Annual UT GeoFluids Consortium Review Meeting was enthusiastically attended by approximately 95 representatives from 13 companies. We held a poster session, gave 24 presentations, taught a fluid flow workshop, and had many lively discussions and recommendations for future work.
The PowerPoint presentations, posters, and workshop materials from the 2015 meeting are available for download in the Members’ Area of the UT GeoFluids website. http://www.beg.utexas.edu/geofluids/g4/g4talks.php
Posted March 2015
UT GeoFluids Workshop 2015
January 2015 UT GeoFluids personnel gathered in Marble Falls, TX for the annual GeoFluids workshop. The students and staff worked hard on presentations, posters, and the workshop for the upcoming 2015 UT GeoFluids Consortium Meeting.
Registration is open for the 2014 UT GeoFluids Consortium Meeting. Details can be found here: http://www.cvent.com/d/j4qb49
Posted January 2015
Polito Gives Talk at Workshop in France
Peter Polito gave a talk entitled, “Characterizing matrix permeability and porosity in Barnett Shale” at The Challenge of Studying Low Permeability Materials workshop at Université de Cergy-Pontoise on 1 December 2014. This workshop provided an opportunity for experimentalists, theorists, and field-based scientists to discuss the state of the low-permeability field and lay the groundwork for a benchmark study, which will involve the collaboration of over twenty-five international laboratories.
For more information on the workshop see thier flyer here: http://www.cfmr-roches.org/sites/default/files/manifestations/flyer-LowPermeabilityMaterials-Workshop-Cergy-2-3dec2014.pdf
posted December 2014
Registration Open for 2015 UT GeoFluids Consortium Meeting
We will hold the 2015 UT GeoFluids Consortium Meeting Wednesday, February 25, 2015 to Friday, February 27, 2015 on the downtown UT Campus at the AT&T Executive Education and Conference Center. We hope you will consider attending the 2015 meeting. Details can be found on the event website here: http://www.cvent.com/d/j4qb49.
Poster session reception: Wednesday, Feb. 25
Meeting sessions:Thursday, Feb. 26 - Friday, Feb. 27
Workshop: Friday, Feb 27
The University of Texas
AT&T Executive Education and Conference Center, 1900 University Ave, Austin, TX 78705
Registration is open. Please respond at the event website . We look forward to your response.
The AT&T Executive Education and Conference Center room block is open. This year's rate is $179 per night. To guarantee this rate you must make your room reservation before January 26, 2015. However the room block sells out quickly so to guarantee you have a room we suggest you make your reservation early.
Booking website: https://resweb.passkey.com/go/UTGEOF0215
We hope to see you at UT GeoFluids 2015,
Co-Director UT GeoFluids
Co-Director UT GeoFluids
posted November 2014
Dylan Meyer at Sea on R/V Endeavor
Dylan Meyer is currently on board the R/V Endeavor participating in the Eastern North American Margin Community Seismic Experiment (ENAM CSE) offshore Cape Hatteras. He and the rest of the scientific crew are working on deploying short-term ocean bottom seismometers (OBS) in time for the active-source seismic portion of the experiment. Information about the experiment and a blog concerning the experiment’s progress can be found at the links below.
Image: Research scientists and graduate students of the scientific party aboard the R/V Endeavor. From left to right - Pamela Moyer, Jennifer Harding, Afshin Aghayan, Dylan Meyer, Kathryn Volk, Brandon Dugan, Harm van Avendonk, and Gard Linkevich. (Photo Credit: Gary Linkevich)http://enamseismic.blogspot.com
posted September 2014
Maria Nikolinakou attends 48th US Rock Mechanics/Geomechanics Sympossium
June 1 - 4, Maria Nikolinakou Attended the 48th U.S. Rock Mechanics/Geomechanics Symposium, in Minneapolis MN, and presented the talk: "Comparison of evolutionary and static modeling of stresses around a salt dome: The importance of modeling the past.” (paper 14-7027). Maria was co-organizer for the career center and student trivia contest events, as well as the “how to give an effective presentation” workshop. She represented the ARMA Future Leader during the Board meeting. She also participated in the Soudan Mine technical tour.
posted August 2014
Gang Luo Leaving UT GeoFluids
Gang Luo has accepted a professorship in Beijing, China. This is wonderful news for him. However, this means he will be leaving our group at the end of May. We have greatly enjoyed working with him and are sad to see him go. We gathered at Peter's house to celebrate the contributions Gang has made to the GeoFluids group.
posted May 2014
Dear UT GeoFluids Colleague,
The 2014 Annual UT GeoFluids Consortium Review Meeting was enthusiastically attended by approximately 92 representatives from 11 companies. We held a poster session, gave 23 presentations, taught a Modeling workshop, and had many lively discussions and recommendations for future work.
The PowerPoint presentations, posters, abstracts, and workshop materials from the 2014 meeting are available for download in the Members’ Area of the UT GeoFluids website. http://www.beg.utexas.edu/geofluids/g4/g4talks.php
You will be prompted for a Log in and Password. Enter your company’s 2014 username and password. This information was provided in your booklet. If you don’t know these, please contact Tessa Green (email@example.com)
Dates for the 2015 meeting are set so please mark your calendar: February 25 – 27, 2015
The reviews of the meeting were general positive and can be found here: http://www.beg.utexas.edu/geofluids/g4/Meetings/Meet14/2014_Evaluation_Results.pdf. From these reviews we interpret the following guidance for next year: 1) we will try another place for dinner that is a little quieter; 2) Peter and Jack will present on the achievements, state, and direction of the consortium; 3) we will emphasize linking our experimental work with our geomechanical modeling.
Thank you as always for participating in UT GeoFluids. Your support is critical to our effort,
Peter Flemings, Jack Germaine, & Tessa Green
posted March 2014
Register for 2014 Consortium MeetingDear UT GeoFluids Consortium Members,
The 2014 GeoFluids Consortium meeting will be held Feb. 19 (evening poster session), Feb 20, & 21. We currently have 79 participants registered. We have terrific representation from most of our companies (http://www.cvent.com/d/wcqtf4/3A). However, we have room for more, if you would still like to sign up.
An executive summary of the meeting is available here: http://www.cvent.com/d/wcqtf4/3K?cpc=M4N3MSJHMHC Highlights of the meeting include:
- Modeling: Geomechanical modeling of stress and pressure around evolving salt domes with illustrations of how conventional pore pressure prediction fails near salt domes.
- Experimental: Presentation of a Gulf of Mexico rock property model and a comparison of model behavior to intact behavior
- Field Study: Testing centroid pressure predictions at Bullwinkle and exploring column height at Mad Dog
- Workshop: On Friday afternoon (12:30-2:30) we will present a modeling workshop to drive home some of the practical applications of our work. We will summarize three applications:
- UTCENDROID: is an online package to calculate an area-based and a permeability based centroid. We will demonstrate the software and have participants pursue an exercise.
- PRESSURE-STRESS COUPLING: UT GeoFluids developed an excel spread sheet to illustrate how pore pressure impacts horizontal and vertical stresses around dipping structures.
- Salt-Induced Stress Perturbation: It is now routine to use complicated numerical models to predict stress near salt. We will review and practice core conceptual outcomes of these models.
1. The list of attendees can be found on the attendees tab: http://www.cvent.com/d/wcqtf4/3A
2. To view the current agenda with abstracts: http://www.cvent.com/d/wcqtf4/6X
3. If you haven’t yet registered and plan to attend the meeting please do so today: http://www.cvent.com/d/wcqtf4/4W
4. Please remember that the meeting is at the UT campus (downtown Austin): http://www.cvent.com/d/wcqtf4/1K
posted February 2014
Michael Cronin Wins Best Poster Award at 3rd Annual Jackson School Student Research Symposium
Each spring semester the Jackson School hosts a research symposium where student present their research in a poster competition. Congratulations to Michael Cornin, who recieved the 2nd place Late-Career M.S. Best Poster Award for his poster titled: "Core-scale heterogeneity and dual-permeability pore structure in the Barnett Shale." Michael presented his poster at the 3rd Annual Jackson School Student Research Symposium January 25th.
For more details on the symposium please visit http://www.jsg.utexas.edu/research_symposium/.
posted January 2014
UT GeoFluids Workshop 2014
January 7-11 the UT GeoFluids personnel gathered in Burnett TX for the annual GeoFluids workshop. The students and staff worked hard on presentations, posters, and the workshop for the upcoming 2014 UT GeoFluids Consortium Meeting.
Registration is open for the 2014 UT GeoFluids Consortium Meeting:
AGENDA: The meeting agenda with talk/poster titles and workshop details can be found here http://www.cvent.com/d/wcqtf4/6X.Regrets
HOTEL: Now is the time to book your hotel room. A room block has been set up at the AT&T Executive Education and Conference Center. The rate is $174 per night. To guarantee this rate you must make your room reservation no later than January 20, 2014. However the room block is quickly filling up so please book your room early.
UT GeoFluids hotel booking website: https://resweb.passkey.com/go/GEOSCI0114
REGISTRATION: Registration is open for the 2014 UT GeoFluids Consortium meeting. If you have not already done so, please register today here:
Posted January 2014
2013 annual conference for the Society of Petrophysicists and Well Log Analysts (SPWLA) attended by Dylan Meyer
UT GeoFluids student Dylan Meyer attended the 2013 annual conference for the Society of Petrophysicists and Well Log Analysts (SPWLA) in New Orleans, LA from June 23 – 25th this year. Along with making many important contacts within the industry, Dylan presented his work on a method for determining the thermodynamic state of hydrate systems in the student poster symposium on the 25th of June.
Poster Title: "In situ gas hydrate saturation and salinity of hydrate-bearing sediments through well log analysis"
Posted October 2013
MIT Students Chunwei Ge and Taylor Nordquist Join UT GeoFluids Group
Chunwei is a graduate student seeking SM at MIT. He graduated from University of Minnesota - Twin Cities with a B.S. degree in Civil Engineering December 2012. While at UMN, Chunwei, did UROP research on damage detection in sandstone by acoustic emission with Prof. Labuz. After graduating from UMN, Chunwei worked for a central A/C install company in China. Chunwei joined the UT GeoFluids group in 2013 and will be doing some basic material characterization testing and researching on the possibility of resedimentation and semectite/illite transformation
Taylor is a Masters student studying Geotechnical Engineering at MIT. While earning a BS degree in Civil Engineering from Brigham Young University, he spent summers doing lab & quality assurance testing for a small consulting firm in Utah, Applied Geotechnical Engineering Consultants. He joined the UT Geofluids group in 2013, and plans to work with permeability & resistivity anisotropy in resedimented clays.
Posted September 2013
Maria Nikolinakou Invited Speaker for the 3rd Geoqus Conference
This August 21-23, 2012 Maria Nikolinakou was an invited speaker for the 3rd Geoqus conference in Potsdam, Germany. Her talk was titled: "Geomechanical modeling of stresses and pore pressures in mudstones adjacent to salt bodies"
Posted August 2013
Maria Nikolinakou Attends 5th Biot Conference on Poromechanics
This July 9-12, Maria Nikolinakou attended the 5th Biot Conference on Poromechanics, in Vienna, Austria, and presented the talk: "Pore pressure and stress around dipping structures". The conference was a reunion of sorts for the poromechanical community, as it marked the 50 year anniversary of Karl von Terzaghi's death. Maria particularly enjoyed a visit to the Geotechnical Lab of the Technical University of Vienna, where Terzaghi spent some years between the 2 world wars. Housed here are Terzaghi's original device on measuring pore pressure during triaxial loading, and his original notes on the theory of consolidation.
Also, congratulations are in order for Maria Nikolinakou. This July she became a member of the MIT Educational Council for Central Texas
Posted July 2013
Flemings and Nikolinakou Present at 47th U.S. Rock Mechanics/Geomechanics Symposium
This June 23-27 Peter Flemings and Maria Nikolinakou attended the 47th U.S. Rock Mechanics/Geomechanics Symposium in San Francisco, CA. Peter was an invited speaker and gave the opening talk titled "The Science of Pore Pressure Prediction in the Deepwater". Maria Nikolinakou presented her talk: Geomechanical modeling of the Mad Dog salt, Gulf of Mexico. Maria was also a member of the organizing committee for ARMA 2013, chair of the paper awards committee, and co-organizer for the career center and student trivia contest events. She also participated in "The Geysers" technical tour.
Posted June 2013
GeoFluids Student Dylan Meyer Attends MG&G Field Course
Dylan Meyer attended the Marine Geology and Geophysics (MG&G) Field Course offered this summer 2013 semester. The MG&G Field Course consists of three, one-week long intensive components: week one in the classroom, week two at the field site, and week three post-processing and interpretation of data. The MG&G Field Course 2013 took place during the end of May and into early June and focused on Galveston Bay and Heald Bank (approx. 20nm offshore Galveston). While at the field site, the class collected data at Boliver Roads, the Bolivar Peninsula shoreface, the Bolivar Peninsular washover fan, the salt dome south of Bolivar Roads, and Heald Bank, a buried barrier island system.
Dylan's team spent a total of three days on the Manta, one day on the Itasca, and one day onshore. During their time in the field they worked with a variety of equipment, including the box core, and processed the data that was collected. After returning from Galveston, Dylan's team was assigned the data from Heald Bank and spent the next six days interpreting that data. They used DecisionSpace and Fledermaus to pick seismic lines from both the MCS and CHIRP data, create time-thickness surface maps, and produce 3-D visualizations maps. These were used to produced a professional presentation covering the study site and results.
This field course provided Dylan with an inarguably unique opportunity to work with some of the most sophisticated scientific equipment available and a better understanding of how this equipment can be used to produce quality results.
Posted June 2013
Pore Pressure Prediction and Modeling (Anadarko 2013)
Welcomed by custom made posters Peter Flemings and Maria Nikolinakou were honored as they arrived at Anadarko. May 7th Peter and Maria traveled to Anadarko offices in Houston to present talks around pore pressure prediction and modeling. The talks were well received by a large audience.
"Predicting Reservoir Overpressure: Implications for Trap Integrity and Wellbore Design" (Flemings)
" Modeling Stress Evolution Around a Rising Salt Dome" (Nikolinakou)
" Fundamentals of Pore Pressure Prediction and Geopressure" (Flemings)
Posted May 2013
Statoil Fellowships Awarded to Baiyuan Gao and Michael Cronin
International energy company Statoil awarded fellowships to two of our GeoFluids students, Baiyuan Gao and Michael Cronin. These fellowships were awarded based on proposals submitted by the students and their advisor, Peter Flemings. This was a competitive field and we congratulate Baiyuan and Michael for their hard work at writing quality proposals. This money will go to fund their research at UT Austin.
Statoil Fellowship – "Trap integrity in salt basins; sub‐salt imaging and seal vs. pore pressure challenges"
Statoil Fellowship – "Multi-scale Pore Structure at the Core Scale in Shales: Experimental and Numerical Investigation of Mass Transport Implications"
Posted April 2013
Mark your calendar for UT GeoFluids 2014
Dear GeoFluids Members,
The 2013 UT GeoFluids Consortium Meeting, held Feb. 2013, was well received as evident by the evaluation responses. If you would like to read this year’s evaluations we have compiled and posted them here
To those of you that were able to join us this year, we appreciate your attendance and participation in the meeting. For those that were not able to join we hope you will join us in 2014. The dates of our 2014 meeting are set, please put these on your calendar. You will see that this year we have blocked off three dates. Based on feedback at the 2013 meeting we will have a session on the evening of Feb. 19th to kick off the meeting.
UT GeoFluids 2014 Consortium Meeting
Feb. 19-21, 2014
University of Texas Campus at the AT&T Executive Education and Conference Center, 1900 University Ave, Austin, TX
The PowerPoint presentations, and abstracts from the 2013 UT GeoFluids Consortium meeting are available for download on the UT GeoFluids 2013 meeting website http://www.beg.utexas.edu/geofluids/Meetings/meet2013.php
Data available to Consortium members can be found on our data site http://www.beg.utexas.edu/geofluids/g4/g4database.php
You will be prompted for a Log in and Password. Enter your company’s 2013 username and password. If you don’t know these, please contact Tessa Green (firstname.lastname@example.org)
Finally, each year many of you are disappointed that you do not get a room in the AT&T conference center. We urge you to book early (and cancel later if you can’t join us). Tessa will send out hotel details as soon as the room block is available so keep an eye on your email.
Peter Flemings & Jack Germaine
Posted March 2013
UT GeoFluids Consortium Meeting 2013
The 2013 UT GeoFluids Consortium Review Meeting, held February 21 – 22, was enthusiastically attended by approximately 90 representative from 11 different companies. We had 26 presentations and many lively discussions and recommendations for future work.The PowerPoint presentations from the 2013 UT GeoFluids Consortium Annual meeting are now available for download in the Members' Area of the UT GeoFluids website. Visit the UT GeoFluids 2013 meeting site.
You will be prompted for a Log in and Password. Enter your company's 2013 username and password. This information was provided on the second page of your booklet. If you don't know these, please contact Tessa Green (email@example.com)
Mark your calendar for the 2014 meeting Feb. 20 and 21, 2014 on the downtown U.T. Campus at the AT&T Executive Education and Conference Center.
Flemings, P.B., Germaine, J.T., Adams, A., Alberty, M., Betts, W., Bhandari, A.R., Casey, B., Coleff, D., Deirieh, A., Fahy, B., Gao, B., Hermanrud, C., Hurd, G., Luo, G., Marjanovic, J., Merrell, M., Meyer, D., Nikolinakou, M., Reece, J.S., and You, Y., 2013, UT GeoFluids annual report to Industrial Associates for 2013: slide set 4, annual report prepared for Anadarko, BHP, BP, Chevron, ConocoPhillips, ExxonMobil, Hess Corp, Schlumberger, Shell, Statoil, Total The University of Texas at Austin, Bureau of Economic Geology.
Posted February 2013
UT GeoFluids Workshop 2013
January 13-19 the UT GeoFluids personnel gathered in Burnett TX for the annual GeoFluids workshop. Lots of progress was made in preparation for the upcoming 2013 UT GeoFluids Consortium Meeting. Students were able to practice their talks and work on current projects.
Registration is open for the 2013 UT GeoFluids Consortium Meeting:
Thursday, February 21 - Friday, February 22, 2013
The University of Texas
AT&T Executive Education and Conference Center, 1900 University Ave, Austin, TX 78705
Travel & Hotel Logistics
Please register for the 2013 meeting HERE
Posted January 2013
Brendan Casey Winner of the 2012 Northeast Geotechnical Research Symposium Abstract Competition
The Geotechnical Engineering Group at the University of Massachusetts Amherst, in collaboration with Geosyntec Consultants, hosted the 2012 Northeast Geotechnical Engineering Graduate Research Symposium at UMass Amherst on Friday, 26 October 2012. Graduate students at all stages of research were invited to submit abstracts providing an overview of their research and the anticipated contribution to the geotechnical and geoenvironmental engineering industry. UT GeoFluids student Brendan Casey won the 2012 award with his abstract "Liquid Limit as a Predictor of Fine-Grained Soil Strength."
Posted November 2012
Registration is open for the 2013 UT GeoFluids Consortium Meeting
2013 UT GeoFluids Consortium Meeting
Registration is open for the 2013 UT GeoFluids Consortium meeting and workshop Feb. 21 and 22, 2013 on the downtown U.T. Campus at the AT&T Executive Education and Conference Center.
Posted October 2012
Andrew Smith Joined Successful Mission for AMGG Research School
Andrew Smith is currently working with Juergen Meinert and Stefan Buenz in the arctic marine geology and geophysics group at the University of Tromsø. He recently participated in scientific cruises to acquire high-resolution 3D seismic and multi-component data using University of Tromsø's research vessel FF Helmer Hanssen. Below is a picture of Andrew on his voyage. For more information on the cruise visit the University of Tromso site.
Posted August 2012
Peter Polito gives talk on JR field test of Downhole tools
On June 27th Peter Polito gave a talk titled "Curacao to Bermuda to the Jersey Slope to Central Park: The trials and tribulations of developing IODP technologies" to the researchers and staff of the Bureau of Economic Geology.
Summary: Over the past decade the GeoFluids group has been developing and testing a penetrometer and corresponding delivery system to be deployed on the JOIDES Resolution. Over the past year we have undergone an extensive stretch of land based bench testing in preparation for sea trials. For two weeks in May and June we were deployed on the JR in preparing for our tests while the ship transited from Curacao to Bermuda to our test site. For 48 hours straight we ran a series of tests on the New Jersey Slope with some success, a healthy dose of humility, and an education on working at sea. On June 8, at approximately 4pm I sat in Central Park, exhaled, and had a beer.
You can view Polito's powerpoint presentation here.
Visit http://www.ig.utexas.edu/research/facilities/downhole/ for more information on the Down-hole Technologies for Ocean Drilling
Posted July 2012
New Data Posted: Compression and permeability behavior of resedimented Nankai - Silt mixtures
Julia Schneider Reece performed an experimental study similar to the one on Boston Blue Clay (BBC) - Silt mixtures. However, here Julia used a marine, deepwater mudstone from offshore Japan, that was drilled during Integrated Ocean Drilling Program (IODP) Expedition 322, as the baseline mudstone instead of BBC. Then she added the same silt-sized silica to the Nankai mudstone in five varying proportions in order to analyze how grain size and also mineralogy affect compression and permeability behavior over a large range in stress (up to 21 MPa). The mineralogy of the Nankai mudstone is significantly different from BBC. The Nankai mudstone consists of almost 50% of smectite (weight %).
Julia prepared these homogeneous mudstone mixtures in the laboratory using the resedimentation technique. After pre-loading the samples to 100 kPa in the resedimentation tests, she conducted constant-rate-of-strain consolidation tests to a maximum vertical effective stress of 21 MPa, equivalent to about 2 km of burial under hydrostatic conditions. Microstructure and fabric of all samples were analyzed at two different stress states in scanning electron microscope images.
Find all UT GeoFluids data on the Member's Data Page.
Posted July 2012
Andrew Smith Awarded Master's Degree
On May 19th Andrew Smith was awarded his Master's degree. His thesis was entitled "Observations and Models of Venting at Deepwater Gulf of Mexico Vents". Andrew's work focused on the process of venting and associated hydrate formation at deepwater vents in the Gulf of Mexico. After completing his MS, he will join the marine geology and geophysics research group at the University of Tromsø in Norway as a Fulbright scholar. We wish Andrew the best of luck in his new adventure.
Posted June 2012
Athma Bhandari Joins UT GeoFluids Group
We are excited to welcome Athma Bhandari to the UT GeoFluids group as a postdoctoral fellow. Athma earned his Ph.D. from University of Southampton, and M. Eng degree in Civil Engineering from the University of Tokyo. Athma's main research interests lie in experimental geomechanics, more specifically, laboratory study of deformation and flow in geomaterials (soils and rocks). During his PhD, he developed a novel digital image-based deformation measurement system for triaxial tests and used it to study the initiation and evolution of failures in a naturally locked sand. He examines the underlying mechanics of observed macro-scale behavior of geomaterials. In his work with UT GeoFluids Athma will will focus on measuring and interpreting mass transport in low permeability shales.
Posted May 2012
Andrew Smith Awarded Best Student Presentation at the Gordon Research Conference on Natural Gas Hydrate Systems 2012
The 2nd Annual Gordon Research Conference on Natural Gas Hydrates was held March 18-23 in Ventura, CA. Andrew Smith presented his poster titled "Multiphase heat and salt transport at a deepwater gulf of Mexico vent." Andrew was honored with the Best Student Presentation Award.
Deepwater vents in the Northern Gulf of Mexico are actively releasing water and hydrocarbons. They are ubiquitous across the continental slope, and we focus on one in the Ursa Basin at lease blocks MC852/853. The vent is elevated ~75 meters relative to the surrounding seafloor, and its core is ~1.6 km in diameter. It is bounded by a strong negative polarity seismic reflection. We interpret that this reflection records a negative impedance contrast marking the boundary between hydrate above and gas below: it is the Bottom Simulating Reflector (BSR). This BSR rises sharply at the boundaries of the vent and is horizontal within a few meters of the seafloor beneath the vent edifice. High temperature gradients and elevated salinities are present within the vent (Ruppel et al., 2005; Paull et al., 2005). We model the coexistence of elevated temperature gradients, saline fluids, and an uplifted BSR by assuming that warm, salty fluids are sourced from depth and expelled vertically through the vent conduit. We show that both the observed temperature gradients and salinities cannot be reconciled with a single-phase flow model. They can, however, be reconciled if gas and water are flowing upwards together, and if the flux of gas is large relative to the flux of water. A better understanding of the hydrogeological processes at vents is important for estimating the fluxes of water and gas from vents and for understanding the conditions under which deep-sea biological communities exist at vent locations.
Smith, A. J., Flemings, P.B., Fulton, P.M. , in review, Hydrocarbon flux from natural deepwater Gulf of Mexico vents, Science
Posted April 2012
UT GeoFluids Consortium Meeting
The 2012 UT GeoFluids Consortium Meeting, held February 16 – 17, was enthusiastically reviewed by approximately 70 attendees representing 10 different companies. Some of the meeting highlights included preliminary observational and modeling results from the new field study at Mad Dog, the first demonstration of experimental capability in resistivity measurements, and a synthesis talk on our work on resedimented mudstones around the world.
The newly developed experimental database for consortium members was launched at this years' meeting. This database gives members immediate access to laboratory test results, analysis and scanning electron microscope (SEM) images of the various substrates tested within the GeoMechanics Laboratory.
Presentation are available to consortium members on the 2012 meeting site.
Mark your calendar for the 2013 meeting Feb. 21 and 22, 2013 on the downtown U.T. Campus at the AT&T Executive Education and Conference Center.
Peter B. Flemings presentation to 2012 Consortium Members
Posted March 2012
UT GeoFluids Workshop
January 10 - 14 the UT GeoFluids personnel gathered in Burnett TX for the annual GeoFluids workshop.
Posted January 2012
Julia Schneider Awarded Doctoral Degree
On December 3rd Julia Schneider was awarded her doctoral degree. Her dissertation was entitled "Compression and permeability behavior of natural mudstones". Julia will continue her research with the UT GeoFluids Consortium as a Postdoctoral Fellow. We are excited to have her stay on and look forward to her talks at the upcoming UT GeoFluids Consortium Meeting.
Posted December 2011
Gang Luo and Maria Nikolinakou have two upcoming publications in the AAPG Bulletin on geomechanical modeling and pore pressure response in salt-sediment systems. You may access their publications at the following links with your company log in.
Luo, G., Nikolinakou, M.A., Flemings, P.B., Hudec, M.R., Geomechanical modeling of s tresses adjacent to salt bodies: 1. Uncoupled models, AAPG Bulletin, (in press)
Nikolinakou, M.A., Luo, G., Hudec, M.R., Flemings, P.B., 2011, Geomechanical modeling of stresses adjacent to salt bodies: 2. Poro-Elasto-Plasticity and Coupled Overpressures, AAPG Bulletin (in press).
Posted November 2011
Andrew Smith Attends ICGH
In July 2011, Andrew Smith traveled to Edinburgh, Scotland to present ongoing research on a gas vent in the Gulf of Mexico at the 7th International Conference on Gas Hydrates. His oral presentation focused on identifying the hydrogeological process of gas venting and the associated hydrate formation. He discussed his research with experts in the field of natural gas hydrates and received invaluable feedback that will help him as he completes his Master's thesis this year.
Posted July 2011
Congratulations to Julia Schneider
Julia received an ‘Outstanding Student Paper Award’ from the Mineral and Rock Physics Section of AGU. Her poster was presented at the Fall 2010 AGU meeting in San Francisco and was entitled “Experimentally derived model to predict permeability behavior of mudstones.”
Posted April 2011
Yao You Receives 'Best Poster' Award
Congratulations to Yao You (Doctoral Candidate) for receiving a 'Best Poster' award for his presentation "Coupling of the evolution of pore pressure and the retrogressive slope failure during breaching " at the recent SIAM Conference on Mathematics & Computational Issues in the Geosciences held in Long Beach California.
Posted March 2011
New Consortium Member
Statoil has joined the UT GeoFluids consortium and will attend the 2011 consortium meeting. We are excited to welcome Statoil to the UT GeoFluids Consortium.
Posted February 2011
UT GeoFluids Workshop
On Jan 12 - 16, the GeoFluids Team had a research workshop at Canyon of the Eagles on Lake Buchanan. They practiced presentations, worked on research, and spent quality time as a group.
Posted January 2011
Derek Sawyer Awarded Doctoral Degree
Derek Sawyer was awarded his doctoral degree from The University of Texas December 4, 2010. His dissertation was entitled "Failure mechanics, transport behavior, and morphology of submarine landslides".
Derek studied sedimentation, deformation, and fluid flow on continental margins. His study area was the Mars-Ursa region outboard of the Mississippi River on the upper Mississippi Fan, Gulf of Mexico. Rapid Pleistocene sedimentation of a sand-rich basin-floor fan, two channel-levee systems, and numerous submarine landslides created a fascinating hydrodynamic system. He participated on Integrated Ocean Drilling Program Expedition 308 as a shipboard sedimentologist and has had summer internships at BP and Shell as a graduate student.
Derek has joined ExxonMobil in Houston, Texas in the Operations Geology group.
Posted December 2010
Message from the Director
UT GeoFluids Update: GEOFLUIDS MEETING Feb. 17-18, 2011 in Austin Texas
This is an update on the UT GeoFluids Consortium. We have been hard at work here in Austin Texas!
- Our annual meeting will be held on February 17-18, 2011 in Austin, Texas. Please hold the date. Details will be forthcoming
- As always, our website can be found here: http://www.beg.utexas.edu/geofluids/. There is a 'members only' button that you can access with your companies username and password. If you don't know the username and password, please contact me (firstname.lastname@example.org) and I will forward it to you.
- I am very pleased to announce that Tessa Green has accepted a position as Program Coordinator for UT GeoFluids. Many of you will meet her in person or by email.
- Recent publications:
- Our online software (Frac, McFrac, and Pstar) have been modified to work on the web and may be accessed here: http://www.beg.utexas.edu/geofluids/g4/software.php
- Student news:
Please drop me a note if you have any questions.
I look forward to seeing many of you in February.
Peter B. Flemings
Jackson Professor of GeoSystems
Jackson School of Geosciences
Posted November 2010
Flemings Presents Talk at BEG Seminar
Dr. Peter Flemings presented a talk entitled Deep pore pressures and seafloor venting in the Auger Basin, Gulf of Mexico as part of the Bureau of Economic Geology seminar series. You can view the streaming video of the presentation online at: http://www.beg.utexas.edu/abs/Flemings_040910.php
Abstract: Pore fluid overpressures in four reservoir sandstones in the Auger Basin, deepwater Gulf of Mexico, are similar across the basin, suggesting that these sandstones are hydraulically connected over distances >20 km. Small overpressure gradients within them suggest upward flow rates between 1 and 20 mm/yr. At the crest of these sandstones, pore pressure equals or exceeds the least principal stress, and we interpret that high fluid pressure is fracturing the caprock and driving flow vertically. A well drilled into the crest of the Auger sandstones confirmed the presence of extreme overpressures that converge on both the least principal stress and the overburden stress. Above these zones, spectacular mud volcanoes are venting fluids today. Overpressured aquifers with significant structural relief may drive fluid vents and mud volcanoes around the world.
Posted May 2010
2010 Consortium Meeting
The UT GeoFluids Annual Meeting 1.0 was held on February 11-12, 2010 at the University of Texas at the Pickle Research Campus. More than 40 industry attendees represented the 10 members of the consortium. The UT team presented more than 20 talks on their cutting-edge research. A special thank you to Neil Braunsdorf and Brent Couzens of Shell for also giving presentations. For more information on the meeting, including the presentations and attendees, please see the meeting website at the link above.
Posted March 2010
October 16, 2009 - Following are the abstracts for the papers that have been accepted from UT GeoFluids researchers for the upcoming 4th International Symposium of Submarine Mass Movements and Their Consequences in Austin, Texas, November 7 – 12, 2009.
For more information on this conference, visit http://www.beg.utexas.edu/indassoc/dm2/Conference2009/home.htm
Subaqueous Landslides in Clay-Rich Systems
Derek E. Sawyer, Peter B. Flemings, David Mohrig
We simulated subaqueous landsliding within sedimented beds of clay-rich material. We deposited beds inside a flume and gradually increased the bed angle until failures developed. In a preliminary experiment, localized debris flows developed at bed angles of ~25° in a thin (2 cm thick) bed of kaolinite clay (60% by weight) and silica silt (40% by weight). Failure surfaces were confined to the upper 0.5cm. In one flow we observed outrunner blocks that accelerated away from the main flow and created linear grooves along the upper bed surface. In future experiments we aim to understand: 1) how landslide rates and styles vary as a function of material properties (clay mineralogy, grain size, and presence of thin interbeds of sand); and 2) the process of retrogression by measuring pore pressure in several locations behind retrograding headscarps. This work will illuminate the processes that drive subaqueous landsliding on continental slopes.
Exploring the Origin and Characteristics of Mass Transport Deposits
Ursa Basin, Gulf of Mexico
Hilary E Strong, Peter B Flemings, Ruarri J. Day-Stirrat, Derek E. Sawyer, Julia Schneider
Seismic, core, and logging data from Integrated Ocean Drilling Program (IODP) Expedition 308 record multiple Mass Transport Deposits (MTDs) within the upper 600 meters below seafloor (mbsf) of the Ursa Basin, northern Gulf of Mexico. The most prominent, MTD-2, is 35 to 100m thick, spans all three drill sites – U1324, U1323 and U1322 – and is located approximately 100 mbsf. MTD-2 is seismically imaged with a positive, low-amplitude top reflection, and negative, high-amplitude basal reflection. MTD-2 is identified in core and logging data as a low porosity, high bulk density, zone. At U1324, the basal sediments of MTD-2 are 7 porosity units less than those immediately below, while at U1322, the basal sediments are 10 porosity units less. This decline in porosity corresponds to a 5% increase in bulk density from overlying bounding sediments to MTD-2. We hypothesize that MTD densification is a result of sediment remolding during debris flow. Remolding is defined as shearing sediment at unaltered water content, thus removing the original fabric and resulting in weaker, more compressible material. We also suggest that the arrested flow is buried and consolidated under uniaxial strain. Initial high resolution X-ray texture goniometry (HRXTG) fabric analysis shows greater basal plane alignment of smectite and chlorite in a MTD specimen, compared to a non-MTD specimen. Mercury Injection Capillary Pressure (MICP) tests confirm a reduction in pore throat size within the MTD-2; however this is a function of decline in porosity, not position within the MTD. Consolidation curves from initial uniaxial experiments show that at a given porosity, a synthetically remolded specimen has on average a 2MPa lower vertical effective stress than the original intact specimen. Pre-consolidation effective stresses measured for Constant Rate of Strain (CRS) consolidation tests on 11 MTD and 13 non-MTD Ursa specimens suggest that the pre-consolidation stresses are approximately the same whether within or outside of an MTD. We further explored these hypotheses through CRS tests on 3 intact Ursa core specimens above MTD-2 (75mbsf), below MTD-2 (125mbsf) and within MTD-2 (115mbsf). Our results show (1) Weaker consolidation curves for MTD vs. non-MTD specimens; (2) Decreased sediment compressibility correlating with decline in porosity, irrespective of location within MTD vs non MTD; (3) Slightly higher permeability within the MTD, but still within the range of Ursa mudstones; and (4) No distinction in linear pre-consolidation stress trend between MTD and non-MTD specimens. Ultimately, MTDs pose a hazard because it takes longer for suction anchor piles and jetted conductors – installed for production platforms – to penetrate MTDs relative to bounding sediment.
History of pore pressure build up and slope instability in mud-dominated
sediments of Ursa Basin, Gulf of Mexico continental slope
Roger Urgeles, Jacques Locat, Derek E. Sawyer, Peter B. Flemings, Brandon Dugan4 and Nguyen Thi Thanh Binh
The Ursa Basin, at ~1000 m depth on the Gulf of Mexico continental slope, contains numerous Mass Transport Deposits (MTDs) of Pleistocene to Holocene age. IODP Expedition 308 drilled three sites through several of these MTDs and encompassing sediments. Logs, sedimentological and geotechnical data were collected at these sites and are used in this study for input to basin numerical models. The objective of this investigation was to understand how sedimentation history, margin architecture and sediment properties couple to control pore pressure build-up and slope instability at Ursa. Measurements of porosity and stress state indicate that fluid overpressure is similar at the different sites (in the range of 0.5 to 0.7) despite elevated differences in sedimentation rates. Modeling results indicate that this results from pore pressure being transferred from regions of higher to lower overburden along an underlying more permeable unit: the Blue Unit. Overpressure started to develop at ~53 ka, which induced a significant decrease in FoS from 45ka, especially where overburden is lower.
Failure caused by breaching in subaqueous sand
Yao You, Peter B. Flemings, David Mohrig
Submarine failures can be divided into two categories: liquefaction failure and breaching failure. During liquefaction failure the sediment matrix contracts while during breaching failure the sediment matrix dilates. Dilation causes the pore pressure in the sediment deposit to decrease, thereby temporarily increasing its shear strength. The tangent of failure angle increases in proportion with the ratio of effective stress to total stress: . Degree of dilation is greatest near the failure front and decays quadratically with distance away from failure. Finer sand or poorly sorted sand creates a higher failure angle and slower erosion rate during breaching because of stronger dilative response and lower diffusivity. In preliminary experiments we have documented pressure drawdown and identified the fraction due to dilation and the part due to change in stresses. We will present recent results from laboratory experiments and a numerical model that characterize how the behaviors of the dilative failures vary with different sand compositions.
Posted October 2009
June 10, 2009 - Hilary Strong, an M.S. student with the UT GeoFluids Consortium, received third place in the AAPG student poster competition for her Poster entitled, Consolidation Characteristics of Mass Transport Deposits in Ursa Basin, Northern Gulf of Mexico
ABSTRACT: Seismic, core, and logging data from Integrated Ocean Drilling Program (IODP) Expedition 308 record multiple Mass Transport Deposits (MTDs) within the upper 600 meters below seafloor (mbsf) of the Ursa Basin, northern Gulf of Mexico. The most prominent, MTD-2, is 35 to 100m thick, spans all three drill sites – U1324 U1323 and U1322 – and is located approximately 100mbsf. MTD-2 is seismically imaged with a positive, low-amplitude top reflection, and negative, high-amplitude basal reflection. MTD-2 is identified in core and logging data as a low porosity, high bulk density, zone. At U1324, the basal sediments of MTD-2 are 7 porosity units less than those immediately below, while at U1322, the basal sediments are 10 porosity units less. This decline in porosity corresponds to a 5% increase in bulk density from overlying bounding sediments to MTD-2. We hypothesize that MTD densification is a result of sediment remolding during debris flow. Remolding destroys the original chaotic fabric, resulting in shear-aligned grains that have lower porosity. We also suggest that the arrested flow is buried and consolidated under uniaxial strain. Initial high resolution x-ray texture goniometry (HRXTG) fabric analysis shows greater basal plane alignment of smectite and chlorite in a MTD specimen, compared to a non-MTD specimen. Consolidation curves from initial uniaxial experiments show that at a given porosity, a synthetically remolded specimen has on average a 2MPa lower vertical effective stress than the original intact specimen. Pre-consolidation effective stresses measured for Constant Rate of Strain (CRS) consolidation tests on 11 MTD and 13 non-MTD Ursa specimens suggest that the pre-consolidation stresses are approximately the same whether within or outside of an MTD. We will further explore these hypotheses through HRXTG fabric analysis and CRS tests on natural and synthetically remolded Ursa core specimens. If our hypotheses are correct, we expect (1) weaker consolidation curves for MTD vs. non-MTD specimens; (2) Similar consolidation curves for MTD and remolded specimens; (3) No distinction in linear pre-consolidation stress trend between MTD and non-MTD specimens; and (4) Chaotic fabric in non-MTDs, and shear-aligned fabric in remolded and MTD specimens. Ultimately, MTDs pose a hazard because it takes longer for suction anchor piles and jetted conductors – installed for production platforms – to penetrate MTDs relative to bounding sediment.
Posted June 2009