Joshua K. Miller, Christian Haselwimmer, Anupma Prakash Geophysical Institute, University of Alaska Fairbanks
Joshua K. Miller , Christian Haselwimmer, Anupma Prakash Geophysical - - PowerPoint PPT Presentation
Joshua K. Miller , Christian Haselwimmer, Anupma Prakash Geophysical - - PowerPoint PPT Presentation
INVESTIGATING LOW-TEMPERATURE HYDROTHERMAL ALTERATION IN DRILL CUTTINGS FROM PILGRIM HOT SPRINGS, ALASKA, USING A SUITE OF LOW COST ANALYTICAL TECHNIQUES Joshua K. Miller , Christian Haselwimmer, Anupma Prakash Geophysical Institute, University
Acknowledgements
Research funding provided by Department of Energy Geothermal Technologies Programme (CID: DE-EE0002846) and the Alaska Energy Authority Renewable Energy Fund Round III Project team headed by Gwen Holdmann (ACEP, Director), consultants William (Bill) Cumming and Dick Benoit, as well as many other organizations:
Overview
- Pilgrim Hot Springs Geothermal System
– Conceptual Model
- Analytical Methods
– Reflectance Spectroscopy – Methylene Blue Titration – X-ray Diffraction
- Summary of Results
- Conclusions
Pilgrim Hot Springs
- 1.5 km2
- 91°C at 12 m
depth
- 26-28 MWthermal
- 2.6-2.8 MWelectric
(Chittambakkam et al., 2013)
Conceptual Model
Reflectance Spectroscopy
- Reflectance spectroscopy is the
interaction of light with a medium that absorbs specific wavelengths that produces characteristic spectrums.
(Ruitenbeek et al., 2005)
Montmorillonite USGS Reference Sample Absorption Reflection
Reflectance Spectroscopy
- 120 sediment
samples
- 7 cm intervals
- ver 15 m of core
- Bandwidth
– R: 2145 nm – G: 2205 nm – B: 2235 nm PS-12-2 Hyperspectral Cube
(Calvin et al., 2010)
Reflectance Spectroscopy
5 10 15 20 25 30 MgChlorite Muscovitic Illite Muscovite FeMgChlorite Siderite Kaolinite Montmorillonite
5 10 15 20 25 30
Hornblende Biotite Ankerite Siderite Calcite Muscovite Muscovitic Illite Montmorillonite MgChlorite Phlogopite FeMgChlorite
PS-12-2 Sediments PS-12-2 Core Micas Clays
Methylene Blue Titration
- Determining presence of smectite
clay
- Conductive signature
- 28 sediment and bedrock samples
for PS-12-2
X-ray Diffraction
- 4, 20 m vertically-spaced
samples
- Reflectance Spectroscopy &
Methylene Blue results comparison
- Oriented <2 µm clay
particles and saturated with ethylene glycol
- (M)ontmorillonite, (I)llite,
(B)iotite, (K)aolinite detected
Conclusions
- Abundant montmorillonite, kaolinite, white
micas, and illite detected
- Possible indicators of hydrothermal alteration
assemblages
- Techniques applicable as quick, cheap
assessment of alteration in low-temperature geothermal systems
Extra Slides
S N W E
Temperate Modeling
S N W E
Geologic Data
Groundwater flow
Biotite schist Pegmatitic dike Diabase dike Biotite schist/pegmatitic dike contact