background characterization and monitoring at the ... recap the homestake gold mine, an ......
TRANSCRIPT
1DUSEL ISE 30 Sept - 3 Oct 2009 Rohit Salve
Homestake DUSEL
DEDC Workshop for the ISE
Rohit SalveUniversity of California, Berkeley
Lawrence Berkeley National Laboratory
Lead, South Dakota, September 30, 2009
Background Characterization and Monitoring at the Homestake Mine
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To maintain a safe working environment, while providing
engineers and scientists with fundamental information to enhance the quality and reliability of their activities
The Need
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Talk Outline
• Geology
• Monitoring and Characterization
o Radiometric
� Rock
� Air
o Microclimate
� Temperature
� Relative Humidity
� Barometric Pressure
• Resources
o Vulcan Database
o Core library
o 3D-Geology Model
Carbonate straws
at 1700L
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• Located in Northern Black Hills of
western South Dakota
• Homestake hosted in Precambrian
rock ~2 billion years old
• Precambrian core of the Black Hills
uplift exposed as a dome ~100 km
long and ~60 km wide.
• The rocks are metamorphic and
subdivided into three distinct units
Poorman, Homestake, Ellison
• Subsequently intruded by Tertiary
volcanic rocks
• Complex deformed geologic terrain
Caddey, e
t al. (1
991)
Geology General
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Geology Vertical x-section
Near vertical ~60 cm wide
Rhyolite sill (2000L)
Tertiary intrusive rock
Northwestern Formation
Ellison Formation
Homestake Formation
Poorman /Yates Unit
Ross Shaft
NorthwestSouthwest
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• Pertinent formation/unitsEllisonHomestakePoormanYates
• Tertiary volcanic rocks present
• The geologic structure is nearly vertical
• Nearly every subsurface rock type encountered at surface
Geology Recap
The Homestake Gold Mine, an
Early Proterozoic iron-formation-
hosted gold deposit
Stanton W. Caddey ... [et al.].
U.S. Geological Survey ([Washington, D.C.], Denver, CO)
Useful Reference
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Homestake Mine Infrastructure
Mine workings ~40.5 km3
Volume occupied by drifts
0.006%
~3.0
km~5.0 km
~2.7
km
More than 500 km drifts
50 levels (150’ between levels)
Total depth 8000 ft
Water at 5000L since July 2009
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Radiometric Measurements
Natural radioactivity is the spontaneous decay of atoms of certain isotopes into other isotopes.
Decay process usually accompanied by emission of alpha, beta, and gamma radiation.
Measuring radioactivity important for low-energy neutrino and dark matter experiments
Sources of background radioactivity
Rock
Gamma-rays, alpha, neutrons
radon
Muon-induced processes
Neutrons
Bremsstrahlung
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Characterization of the rock required to:
• Evaluate placement of laboratory rooms
• Identify concrete constituents to be used
• Estimate shielding from the country rock
U, Th & K Radiometric Measurements
Uranium, Thorium, and Potassium (U, Th, K)
affect radioactive backgrounds experienced by
detectors
Measurement with Low-BKG high-resolution HPGe detector gamma ray spectrometer to
identify gamma-emitters in sample materials
10DUSEL ISE 30 Sept - 3 Oct 2009 Rohit Salve
Analy
sis
by A
l Sm
ith (L
BN
L)
Aggregates
Poorman
Fm
Tertiary
Rhyolites
Cement
(local)
Limestone Crushed
Limestone
Sioux
Quartzite
Central
Black Hills
SNO Lab.
U (ppm) 0.24 8.60 3.00 1.75 1.49 1.06 3.37 1.10
Th (ppm) 0.25 10.80 3.40 0.30 0.36 4.68 10.40 4.90
K (%) 0.77 3.60 0.04 0.05 0.09 0.07 1.16 1.00
U,Th & K Radiometric Measurements
Tertiary intrusive rock
Ellison Formation
Homestake Formation
Poorman Formation
Yates memberYm
Pf
Ef
Hf
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� Colorless, odorless, tasteless, naturally occurring, radioactive noble gas
with no stable isotopes
� Once the parent nuclei decay into gaseous radon, it will diffuse through
the bulk matrix and may reach the open air
Concerns about radon underground:o Contributions to background radiation from the short and long-
lived daughters of radon. (210Pb a 222Rn daughter has a 22 year
half life)
o Leading cause of lung cancer among non-smokers
US EPA action level for radon 4 pCi/L…at or above corrective measures recommended.
Radon Radiometric Measurements
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Davis Cavern
Radon Radiometric Measurements
Note: Current ventilation is 33-50% of former
production levels
Jare
tH
eis
eet a
l (Sanfo
rd L
ab.), D
onm
ing
Meiet a
l (US
D)
Level Location (Formation) Bq/m3
300 Ross Station (Ellison) 66
800 Cap magazine room (Ellison, some Homestake) 444
2000 1st Transformer Substation (Ellison) 792
4550 #6 WINZE Hoist Rm. (Poorman) 335
4850 Yates Station 755
4850 Davis Cavern- NE (Yates + Rhyolite) 659
4850 Davis Cavern- Center (Yates + Rhyolite) 585
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Total Gamma-ray fluxes
(> 0.1 MeV@ 800L): 2.36 Hz/cm2
40K
208Tl
Alphas from decays inside detector
Gammas from neutroncapture in surrounding
rock
Gamma-Ray Radiometric Measurements
Measured Gamma-Ray FluxExample 800L
Donm
ing
Meiet a
l. (US
D), R
ichard
Kadel(L
BN
L)
14DUSEL ISE 30 Sept - 3 Oct 2009 Rohit Salve
Measured Muon FluxExample 2000L
3 or 4-fold muon coincidence rate:
3.11 ± 0.35 x 10-7 Hz cm-2sr-1
1
4
3
2
4-Fold Scintillation counter assembly
Comparison with historic data
M.F. Crouch, in
Proceedings of the 20th
International Cosmic Ray Conference, Vol. 6,
p. 165.
Muon-Flux Radiometric Measurements
Donm
ing
Meiet a
l (US
D), R
ichard
Kadel(L
BN
L)
15DUSEL ISE 30 Sept - 3 Oct 2009 Rohit Salve
Radiometric Measurement Recap
Most country rocks have low levels of U,Th, K
Rhyolite intrusive rocks have substantially higher U,Th, K
Locally available cements also have higher U,Th, K contents than the country rocks
Manufactured sand derived from local limestones have the lowest U,Th, K contents
Radon levels may be higher than when ventilation system working at full capacity
Muon flux (at 2000L) compares well with historical data
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Microclimate Location of stations
Sensor in drift
Sensor in rock
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10
12
14
16
18
20
22
24
26
28
30
10-Jun-09 17-Jun-09 24-Jun-09 1-Jul-09 8-Jul-09 15-Jul-09 22-Jul-09 29-Jul-09
800' Drif t T 800' Rock T
2000' Drift T 2000' Rock T
4850' Drift T 4850' Rock T
Tem
pera
ture
(0C
)
Salv
e a
nd D
obson (L
BN
L)
Microclimate Temperature
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Rela
tive h
um
idity
(%)
Sa
lve
an
d D
ob
so
n (L
BN
L)
Microclimate Relative humidity
55
60
65
70
75
80
85
90
95
100
105
10-Jun-09 17-Jun-09 24-Jun-09 1-Jul-09 8-Jul-09 15-Jul-09 22-Jul-09 29-Jul-09
800' Drift RH 800' Rock RH
2000' Drift RH 2000' Rock RH
4850' Drift RH 4850' Rock RH
19DUSEL ISE 30 Sept - 3 Oct 2009 Rohit Salve
Tem
pera
ture
measure
ments
(1973 v
ers
us 2
009)
Microclimate Temperature
0 level
-600’
-2000’
-3800’
-4850’
-6500’
400 500 600 800 900 1000700Fahrenheit 1100
40 100 160 270 320 380210 430Celsius
Yates
No.5
No. 4
Ore bodies
July 2009
Geothermal Gradients
at Principal Shafts
By S.W.H. (retired)
4/3/1973
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Microclimate Recap
• Mine temperature:
� Influenced by ventilation (near drift environment)
� A function of depth
• Non-ventilated areas have high relative humidity
Larry. D. Stetler, SDMST Jaret Heise, Sanford Laboratory Salve & Dobson LBNL
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Resources
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Workingsa. Sills (drifts)
b. Ramps (drifts between levels)
c. Stopes (all mined out areas)
Geologya. Diamond drill holes: Approximately 24,000 holes
b. Geologic mapping: 1996-2001, additional old mapping has been
digitized as deemed necessary
c. Geologic Interpretations: Plan maps, every level-surface
Cross-section maps, entire length of mine at 50 foot intervals
Reference Systema. Boreholes, sandlines, electrical system, walls
Available Data and Information
Resources Vulcan DatabaseK
ath
y H
art S
anfo
rd L
ab.
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Generalized Geology Plan View
Tertiary RhyoliteEllison FormationHomestake FormationPoorman FormationYates Member
NORTH
Resources Vulcan DatabaseK
ath
y H
art S
anfo
rd L
ab.
4850L
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Long-section view looking
east showing solids
NORTH
Resources Vulcan Database
Kathy Hart Sanford Lab.
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Resources Core repository
Repository Contents
Estimated ~400K feet of core drilled within the Homestake Mine and Northern Black Hills
Consists of underground cores drilled from the 1930’s to the late 1990’s
Represents core extending from the surface to the 12,000+ equivalent level within the Homestake Mine
Ongoing drilling (2009) at 4850L will add another ~6K feet of core
Tom Haggar South Dakota Geological Survey-DENRWilliam Roggenthen SDSMT
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3-D Structural Geology Model For
Location Of Large Cavities
To locate:
• Main rock types
• Shear zones and fault zones
• Contacts between Rhyolite dikes-host rock
• Foliation and/or any cross-cutting features
• Main joint sets
Area of Interest
• Between 4100 and 5000 Levels
• Between, and northwest of, the Yates
and Ross shafts
Geology 3D Structural Model(L
isenbee
and T
erry
, 2009
)
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Ross Shaft
Yates Shaft
Poorman Fm
Strongly folded zone
4850
4700
Yates
Unit
(Am
phibolite
)
Rhyolite Dyke
Swarm
3D Geology of Large Cavity Study Area
Geology 3D Structural Model(L
isenbee
and T
erry
, 2009
)
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In conclusion…
� Extensive information available about regional and local
geology……..Additional information being collected (e.g.
Yates unit at the 4850L)
� Ongoing characterization and monitoring activities are useful
for engineering design, development of experiments and mine
safety strategies
� Resources such as the Vulcan database and core library
provide relatively easy access to a wide range of information
about the subsurface environment
� There are other efforts, both ongoing (e.g., seismic studies
[Roggenthen et al.], environmental magnetic surveys [Bryam
et al.]), and planned