geosciences in an underground laboratory: earthlab w. m. roggenthen sd school of mines &...
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Geosciences in an Underground Laboratory:
EarthLab
W. M. RoggenthenSD School of Mines & Technology
EarthLab:A Subterranean Laboratory and Observatory to Study Microbial Life, Fluid Flow, and Rock Deformation
Brian McPherson, New Mexico Institute of Mining and TechnologyDerek Elsworth, Pennsylvania State UniversityCharles Fairhurst, University of MinnesotaStephen Kesler, University of MichiganTullis Onstott, Princeton UniversityWilliam Roggenthen, SDSMTHerb Wang, University of Wisconsin
http://www.earthlab.org
Requirements – what Geosciences need:
1. A large (~20+ km3) volume of rock with interesting geology.
2. Drill holes and underground workings in rocks reaching temperatures of 120°C - water-filled fracture systems.
3. Ability to introduce materials into holes, workings, or fractures to modify the geochemistry of the rock.
4. Existing geologic data and samples.
Homestake Mine, Lead, SD
•EarthLab:
• A “window” into the basement of North America
•Microbial Life at Depth
•Hydrologic Cycle
•Rock-Water Chemistry
•Rock Deformation and Fluid Flow
•Deep Seismic Observatory
Microbial Life at Depth
The Ultradeep Life and Biogeochemistry Observatory
Purpose:
to search for the limits of life
•what is living at depth?•how does it take advantage of its environment?•what is its metabolic rate/how does it grow?
Methods:
use closely spaced boreholes that:
• attain depths up to 5 km
• have bottom-hole temperatures of 110-120°C, the maximum known temperature for life
Homestake Mine, Lead, SD
~16,000 ft
Hydrologic Cycle
The Deep Flow and Paleoclimate Laboratory and Observatory
Purpose:
to search for continental paleoclimate recordsand document deep transport processes
Methods:
instrument a fracture zone extending from the surface to the maximum depth of the laboratory.
Deep Flow Hydrologic Experiments
will provide information on the movement of groundwater in the crust and its relationship to Earth’s changing climate.
The Induced Fracture and Deformation Processes Laboratory
Purpose:
to conduct extensive studies of three-dimensionalrock deformation in heterogeneous rock formations
Methods:
Instruments in boreholes will measure:
•Rock deformation associated with mining out a large cavity
•Creation of fractures using high-pressure fluid
•Deformation resulting from heating small volumes of rock
Data are critical to scaling-up models used to predict long-term stability of subsurface excavations.
Induced Fracture and Deformation
The Deep Seismic Observatory
Purpose:
To make the largest and best seismometer in the world.
Method:
•The laboratory will become the instrument.
•Will use a fully three-dimensional array consisting of at least 60 broadband seismometers in tunnels and boreholes.
Key Numbers for EarthLab
Anticipated total tunnel length: ~ 10 kmGreatest tunnel depth: ~ 2 - 2.5 kmnumber of instrumented boreholes: ~ 140total length of rock core to collect: ~ 15,000 m
Genetic materials - novel microorganisms
Analytical techniques for geomicrobiology
Environmental remediation
Subsurface imaging
Natural resource recovery