Magma-Hydrothermal Research at Georgia Tech

Introduction

Personnel

Publications

GTH code

GTHSW code

Hydrothermal Modeling

Projects

Related Links

Introduction

Research on magma-hydrothermal processes has been an integral part of the geophysics program at Georgia Tech since 1971. The program focuses mainly on the development of analytical solutions and numerical simulations that address fundamental processes in seafloor hydrothermal systems, and related magmatic processes.

Early research on seafloor hydrothermal systems addressed the role of hydrothermal circulation in causing conductive heat flow anomalies on the seafloor. More recent work has addressed: (1) the operation of high temperature systems at ocean ridge crests (black smokers), (2) heat transfer across magma-hydrothermal boundary layers, (3) the role of thermoelastic stresses and mineral precipitation on the evolution of permeability, (4) the formation of event plumes, (5) the relationships between focused and diffuse venting, (6) the role of serpentinization reactions in driving hydrothermal circulation, (7) two-phase flow and phase separation, and (8) has also been extended laboratory experiments in fractured geomaterials to Archean hydrothermal processes and hydrothermal activity on Jupiter's moon Europa.

Early work on magmatic processes included studies of double diffusive convection during magma generation and crystallization. More recent work has addressed phreatic eruption mechanisms. Current research on magmatic processes is primarily concerned with the coupled problem crack propagation and magma-hydrothermal heat transfer, the emplacement of magma at ocean ridge axes, and the connections between magma lenses, dike emplacement, and the location of hydrothermal vent sites.

Personnel

The magma-hydrothermal research program at Georgia Tech is a collaborative effort led by Dr. Robert P. Lowell(full CV), Professor, School of Earth and Atmospheric Sciences and Dr. Leonid Germanovich, Professor, School of Civil and Environmental Engineering. In addition, the group includes:

Research Collaborators:

Dr. Wenyue Xu (wenyue.xu@eas.gatech.edu), Office of Information Technology and School of Earth and Atmospheric Sciences, Research Scientist II

Graduate Students:

Ms. Yufeng Yao (gt6906a@prism.gatech.edu), Research and Web Development Assistant, and Ph.D. student, School of Industrial and Systems Engineering.

Ms. Kayla Lewis (geofleur@sbcglobal.net), Ph.D. student, School of Earth and Atmospheric Sciences

Mr. Sawyer Gosnell (gtg590s@mail.gatech.edu), M.S. student, School of Earth and Atmospheric Sciences.

Mr. Pierre Ramondenc (pierre.ramondenc@ce.gatech.edu), Ph.d student, School of Civil and Environmental Engineering, Rock and Fracture Group.

Mr. Yang Yang (yang.yang@eas.gatech.edu), Ph.d student, School of Earth and Atmospheric Sciences.

Undergraduate Students:

The group has from time to time involved a number of undergraduate research assistants in the School of Earth and Atmospheric Sciences

Recent Alumni:

 

Recent Publications

 

GTH Source Code and Documentation

GTH is a finite difference code for studying two-phase flow in pure water hydrothermal systems. The code was developed by Dr. Wenyue Xu (wenyue.xu@eas.gatech.edu). The code can be downloaded by clicking either of the download links below. These link to "tar" files that contain the directory structure, source files, Makefile, and example data files. The compressed version (gth.tar.Z) is smaller than 2 Mb and the uncompressed version (gth.tar) is smaller than 7 Mb. The compressed version can be expanded using the "uncompress" command, standard on most versions of unix. Once the file is saved onto the target machine and uncompressed, its files need to be extracted (using "tar -xvf gth.tar") The user manual can be viewed by following the "documentation" link below.

GTH (compressed) Download

GTH (uncompressed) Download

Documentation

GTHSW Source Code and Documentation

GTHSW is a finite difference code for studying two-phase flow and phase separation in a NaCl-H2O hydrothermal system. Equations of state for the system over the P-T range of 1-1000 bars and 0- 1000°C will be available soon. The code is currently under development by Dr. Wenyue Xu (wenyue.xu@eas.gatech.edu). A downloadable version and necessary documentation will be posted to this site when available.

 

 

Hydrothermal Modeling

To help educate scientists and students in the basics of modeling seafloor hydrothermal systems, we have constructed a simple interactive modeling website based on the single pass hydrothermal model depicted above.

 

Some Projects Planned and Currently Underway

  1. Two-phase flow in NaCl-H2O hydrothermal systems and phase separation in seafloor hydrothermal systems
  2. The response of seafloor hydrothermal systems to earthquakes
  3. Thermoelastic stresses and the stability of seafloor hydrothermal systems
  4. Precipitation of anhydrite and the evolution of permeability in seafloor hydrothermal systems
  5. Dike propagation from subseafloor magma chambers and shallow crustal structure at ocean ridge axes
  6. Laboratory experiments on flow in fractured geomaterials
  7. Hydrothermal activity driven by serpentinization of peridotite
  8. Archean hydrothermal systems and Banded Iron Formations
  9. Hydrothermal systems on Europa
  10. Near axis hydrothermal circulation

 

Related LINKS

RIDGE 2000 website

InterRIDGE website

AGU

Deap Ocean Exploration Institute

 


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