IODP Expedition 301: The Hydrogeologic Architecture of Basaltic Oceanic Crust: Compartmentalization,...
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IODP Town Hall Meeting 2004 Fall AGU Meeting San Francisco, CA 14 December 2004 PowerPoint PPT Presentation


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IODP Expedition 301: The Hydrogeologic Architecture of Basaltic Oceanic Crust: Compartmentalization, Anisotropy, Microbiology, and Crustal-scale Properties on the Eastern Flank of Juan de Fuca Ridge. IODP Town Hall Meeting 2004 Fall AGU Meeting San Francisco, CA 14 December 2004.

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IODP Town Hall Meeting 2004 Fall AGU Meeting San Francisco, CA 14 December 2004

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Iodp town hall meeting 2004 fall agu meeting san francisco ca 14 december 2004

IODP Expedition 301: The Hydrogeologic Architecture of Basaltic Oceanic Crust: Compartmentalization, Anisotropy, Microbiology, and Crustal-scale Properties on the Eastern Flank of Juan de Fuca Ridge

IODP Town Hall Meeting

2004 Fall AGU Meeting

San Francisco, CA

14 December 2004

T. Fisher1 and Tetsuro Urabe2

and the IODP Expedition 301 Scientific Party

1 University of California, Santa Cruz

2 University of Tokyo


Expedition 301 science party

Expedition 301 Science Party:

A. Fisher, T. Urabe, A. Klaus, A. Bartetzko, K. Becker, R. Coggon, M. Dumont, B. Engelen, S. Goto, V. Heuer, S. Hulme, M. Hutnak, F. Inagaki, G. Iturrino, S. Kiyokawa, M. Lever, S. Nakagawa, M. Nielsen, T. Noguchi, W. Sager, M. Sakaguchi, B. Steinsbu, T. Tsuji, C. G. Wheat

Additional proponents and collaborators:

J. Alt, W. Bach, J. Baross, J. Cowen, S. D’Hondt, E. E. Davis, D. Kadko, M. McCarthy, J. S. McClain, M. J. Mottl, M. Sinha, G. Spinelli, V. Spiess, R. Stephen, D. Teagle, H. Villinger, L. Zühlsdorff


Fundamental questions addressed by iodp expedition 301 and related experiments

Fundamental questions addressed by IODP Expedition 301 and related experiments

  • What are the magnitude and nature (distribution, extent of channeling) of permeability in crustal fluid-rock systems, variations, scaling (temporal, spatial)?

  • What are the magnitudes and directions of driving forces, fluid fluxes, and associated solute and heat transport?

  • What are the magnitude and nature of storage properties, variations with fluid pressure, scaling (temporal, spatial)?

  • What are relations between fluid flow, vertical and horizontal compartmentalization, microbiological communities, seismic properties, alteration, structure, and primary crustal lithology?

  • How large are distinct fluid reservoirs, what are fluid residence times and fluid velocities, and how do these respond to transient processes (tides, seismic events)?


Permeability is at the center of many of these questions

Permeability is at the center of many of these questions…

Things we want to understand

Things we measure

Permeability links observation and process


And so is the subseafloor biosphere

…and so is the subseafloor biosphere!

• What is the diversity, distribution, and size of ecosystems?

• What happens when we move from oceanic sediments to basement?

• How does microbiology relate to other aspects of water/rock?

modified from Parkes et al. (1994), D’Hondt et al. (2003)


Why work on the eastern flank of juan de fuca ridge

Why work on the eastern flank of Juan de Fuca Ridge?

  • The geology is typical in many ways.

  • Young crust, thick sediments, create extreme conditions we can measure and sample.

  • Existing boreholes/CORKs help us understand the system, save time in creating a network of observatories.

  • Link with future cabled observatory system: NEPTUNE.

Eventually, we will need to test several areas,

but this is the best place to start.


Expedition 301 and follow up expeditions will provide many new opportunities and results

Expedition 301 and follow-up expeditions will provide many new opportunities and results…

• First controlled, cross-hole seafloor experiment;

• First multi-directional hydrogeologic experiment (both vertical and multi-azimuth);

• First active large-scale assessment of storage properties and effective porosity;

• First combined (simultaneous, co-located) hydrogeologic, microbiological, tracer, seismic experiment;

• First long-term active experiment (hours to multi-year);

• First attempt to measure multiple scales (temporal, spatial) with the same techniques, link to primary lithology, alteration, etc.


Summary of iodp 301 operational plans

Summary of IODP 301 Operational Plans

• Create/modify a network of boreholes (two existing, two new), penetrating up to ~300-400 m of permeable basement;

• Conduct wireline logging, VSP, short-term packer tests;

• Install long-term observatories (CORKs) to monitor pressure, temperature, collect fluid samples, colonize microbes; and

• Collect sediment and rock samples and evaluate lithology, alteration, microbiology, fluid chemistry.

• Prepare for installation of additional holes to conduct cross-hole hydrogeologic, microbiological, geochemical, and seismic experiments at a range of spatial and temporal scales (meters to kilometers, minutes to years) in the same holes.


Iodp 301 site locations

IODP 301 site locations…

Second Ridge area

Second Ridge (SR): Primary Sites

First Ridge (FR), Deep Ridge (DR): Secondary Sites


Planned sr operations

Planned SR operations

• Replace CORKs at 1026B (higher priority), 1027C (lower priority)

• Drill holes at Site 1301, ≤400 m into basement, core, log, BHTV, VSP, packer, CORK multiple intervals, additional sediment coring

• Drill Hole SR-2A, ≤200 m into basement, core, sample, log, BHTV, VSP (offset), packer, CORK multiple intervals

• Long-term testing (1-3 years) within and between holes


Simultaneous and co located hydrogeologic microbiological seismic tracer experiments

Simultaneous and Co-located Hydrogeologic, Microbiological, Seismic, Tracer Experiments

(1) Hydrogeologic Experiments:

• Single-hole tests

• Use CORK’ed wells as observation points, pump across wells

• Pump for 24 hours, let equilibrate for 6-12 months, open valve(s) to overpressured interval(s), allow to flow for 12-24 months = "artesian well" test

• Test multiple scales, directional properties, differences in properties and relations


Simultaneous and co located hydrogeologic microbiological seismic tracer experiments1

Simultaneous and Co-located Hydrogeologic, Microbiological, Seismic, Tracer Experiments

(2) Microbiological Experiments:

• Which microbes live where, how?

• Three main stages of analysis:

(a) Sediment coring, sampling

(b) Basement coring, sampling

(c) Long-term fluid sampling, incubation

• Long-term samplers and colonization substrate deployed within sealed boreholes

• Vent overpressured system at seafloor, time-series sampling, additional seafloor experiments


Simultaneous and co located hydrogeologic microbiological seismic tracer experiments2

Simultaneous and Co-located Hydrogeologic, Microbiological, Seismic, Tracer Experiments

(3) Seismic Experiments:

• Collect wireline logs in deep basement holes

• Single-hole VSP in Holes 1301B and SR-2A

• Offset VSP, shoot from another ship to the hole

• Determine directional basement seismic properties, relations to hydrogeologic and other properties


Simultaneous and co located hydrogeologic microbiological seismic tracer experiments3

Simultaneous and Co-located Hydrogeologic, Microbiological, Seismic, Tracer Experiments

(4) Tracer Experiments:

• Thermal, modeling, and geochemical studies suggest fluid velocities on the order of kilometers per year

• Pump multiple tracers in multiple holes and depths during hydrogeologic tests

• Monitor individual holes and depths for tracer return patterns (single-hole tests)

• Monitor for across-hole tracer appearance, also monitor natural discharge on Baby Bare outcrop


Expedition 301 cork system features

Expedition 301 CORK system features

• In new holes: four nested casing strings (three to hold open hole, one for CORK)

• Multiple sealing systems: cement, packer(s), CORK body, CORK casing (top and bottom)

• Tubing extends to depth for fluid and microbio sampling, pressure monitoring, several kinds of umbilicals used

• Autonomous temperature loggers, OsmoSamplers, microbio cells within/below CORK, hung on Spectra cable

• Pressure logger attached to CORK head by ROV/sub after CORK deployment

• System allows monitoring of formation and cased intervals, to evaluate CORK performance


Expedition 301 corks casing hangers

Expedition 301 CORKs,casing hangers


Hoisting cork onto rig floor

Hoisting CORK onto rig floor

Sampling/

monitoring

bay

Top seal


Attaching cork running tool

Attaching CORK running tool


Raising cork in the rig in preparation for deployment through the moon pool

Raising CORK in the rig in preparation for deployment through the moon pool


Running tubing protective centralizers

Running tubing, protective centralizers


Attaching umbilicals to pass throughs on main cork seal

Attaching umbilicals to pass-throughs on main CORK seal

Hero

Hero

Hero

Hero


Autonomous temperature loggers attached to downhole instrumentation and cables

Autonomous temperature loggers, attached to downhole instrumentation and cables


Preparing osmosamplers and microbiological substrate cells

Preparing OsmoSamplers and microbiological substrate cells


Downhole microbiological instrumentation

Downhole microbiological instrumentation


Three bays on cork head for uphole instrumentation and access to samples

Three bays on CORK head for uphole instrumentation and access to samples


Three corks deployed during iodp expedition 301

Three CORKs deployed during IODP Expedition 301


Iodp 301 collected and tested many basement and sediment samples

IODP 301 collected and tested many basement and sediment samples


Extensive microbiological sampling and analysis 9 of basement rock much of the sediment

Extensive microbiological sampling and analysis (9% of basement rock, much of the sediment)


Summary of iodp 301 basement results

Summary of IODP 301 basement results


Post iodp 301 operations

Post-IODP 301 operations

• E. Davis (PGC) and R. Dixon (US-IO) returned to Exp. 301 CORKs on R/V Thomas G. Thompson in September 2004

• Installed pressure loggers, closed valves

• Recovered some OsmoSamplers from CORK heads

• Inspected CORK installations


Ropos operations september 2004

ROPOS operations: September 2004


Expedition 301 achieved critical objectives

Expedition 301 achieved critical objectives

• Successes are remarkable considering limited time available to prepare…

• Now poised to finish drilling and related work, conduct long-term, active tests in the crust…

• Appropriate for the first expedition of IODP - a new kind of experiment


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