02.12.2014 Views

Presentation - UC Davis Geology

Presentation - UC Davis Geology

Presentation - UC Davis Geology

SHOW MORE
SHOW LESS

You also want an ePaper? Increase the reach of your titles

YUMPU automatically turns print PDFs into web optimized ePapers that Google loves.

Identifying Blind Geothermal Systems through<br />

Integrated Geologic, Geochemical,<br />

and Geophysical Studies<br />

James Faulds, UNR<br />

Nevada Bureau of Mines & <strong>Geology</strong><br />

• Basin and Range – Region of high heat flow<br />

• Ironic that what little water region has is hot<br />

• Difficult to find sufficient fluid flow<br />

• Permeability more important than temperature<br />

• Most geothermal resources are blind<br />

• Need multi-disciplinary studies to discover new<br />

resources<br />

Desert Peak – Blind System


Challenges, Barriers, and Needs<br />

• Current technology cannot identify best<br />

geothermal sites with a high degree of<br />

certainty without drilling.<br />

– Permeability<br />

– Temperature<br />

• Drilling is expensive and generally has high<br />

risks.<br />

• Inadequate knowledge precludes low-risk<br />

options to effectively select sites and<br />

characterize their physical parameters as<br />

potential geothermal reservoirs before<br />

drilling.<br />

• Better characterization of known systems<br />

needed to address these problems.<br />

• Our approach – Characterize settings<br />

favorable for geothermal activity and develop<br />

more comprehensive, conceptual models that<br />

can facilitate exploration.<br />

Beowawe<br />

Fly Ranch Geyser – Blind system


Exploration Challenges<br />

• Exploration Challenges<br />

– Spring directly above upflow from<br />

deep source (uncommon)<br />

– Outflow from source (common)<br />

– Hidden or blind systems (most<br />

common)<br />

• Results – significant drilling risk<br />

– Hot dry wells<br />

– Overturn in down-hole temperatures<br />

• Need better conceptual models to:<br />

– Locate areas of upflow<br />

– Avoid typically less productive<br />

outflow zones<br />

Non-Productive Well<br />

Blue Mt., Nevada<br />

Productive Well<br />

Productive wells commonly proximal<br />

to non-productive wells<br />

Productive<br />

Non-Productive Well<br />

Productive Well<br />

Non-Productive<br />

Non-Productive<br />

Desert Peak, Nevada<br />

From Richards and<br />

Blackwell, 2002


Project Goals<br />

Gravity Data<br />

Geologic-Structural Data<br />

• Identify multi-faceted characteristic<br />

signature of known, high-enthalpy,<br />

productive geothermal systems based<br />

on several methods and techniques:<br />

– Structural geology and geologic maps<br />

– Gravity<br />

– Seismic reflection-refraction<br />

– Magnetotellurics (MT)<br />

– Soil gas flux<br />

– Geochemistry<br />

• Integrate data into one geodatabase<br />

• Generate 3D models of systems<br />

Magnetotelluric Data<br />

Seismic Reflection Data<br />

3D Model


Project Objectives<br />

• Determine characteristic geologic and<br />

geophysical signature for productive<br />

geothermal systems<br />

• Relate these findings to tectonic setting<br />

and regional strain rates<br />

• Later apply these methods in a Phase<br />

II to discovering blind geothermal<br />

systems<br />

– Estimates suggest that ~3/4 of systems in<br />

Great Basin region are blind or hidden<br />

– Example below from Hot Springs Mts, NW<br />

Nevada – 2 of 3 high-temp systems blind<br />

Structural Settings of Geothermal<br />

Systems (Faulds et al., 2013)


Approach<br />

• Review all available data sets for several<br />

operating geothermal systems in<br />

different structural settings<br />

• Integrate geologic, geophysical, and<br />

geochemical data from productive<br />

geothermal fields in Great Basin region,<br />

(e.g., systems with existing power plants):<br />

– Dixie Valley<br />

– Steamboat<br />

– Desert Peak<br />

• Phase I relies on existing data due to<br />

limited funding for data acquisition and<br />

is collaborative with industry at these<br />

sites<br />

• Very limited new data acquisition<br />

possible in some areas<br />

• Variety of settings selected for study to<br />

best characterize range of values for<br />

productive systems


• Integrated geodatabases<br />

contributed to NGDS.<br />

• Descriptions of characteristic<br />

signatures.<br />

• Final report.<br />

Outcome/Deliverables<br />

• Peer-reviewed published paper.<br />

Steamboat, Reno


Impact<br />

• Project has potential of making critical<br />

breakthroughs<br />

– Identifying characteristic signatures of<br />

geothermal systems<br />

– Developing techniques for identifying blind<br />

geothermal systems<br />

• May significantly expand the overall<br />

geothermal potential of the Great Basin<br />

• May lower costs of geothermal development<br />

• May foster economic development in rural<br />

areas<br />

• Project will help educate next generation of<br />

geothermal geoscientists<br />

Strain rates reflect the<br />

second invariant strain<br />

rate tensor (10 -9 /yr)<br />

Faulds et al. (2012)<br />

Fairway 3D Mapping of Geothermal System<br />

(Siler and Faulds, in press)


Project Duration/Proposed Budget<br />

• Project duration – October 1, 2013<br />

to September 30, 2014.<br />

• Proposed Budget - $59,990<br />

– Non state-funded faculty salaries - $11,000<br />

– Graduate student salaries - $30,000<br />

– Fringe – $8,240<br />

– Travel - $2,750<br />

– Operating - $2,000<br />

– Overhead (10%) - $6,000<br />

Neal Hot Springs, Oregon<br />

Temperature Anomaly,<br />

Desert Peak, NV


Questions?<br />

Please fill out Level of Interest Evaluation Form (L.I.F.E.)<br />

Roosevelt, Utah

Hooray! Your file is uploaded and ready to be published.

Saved successfully!

Ooh no, something went wrong!