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© NERC All rights reserved Environmental Protection Scotland: 24th March 2014
Potential shale gas/oil resources in Scotland
Hugh Barron
Responsive Surveys Scotland
© NERC All rights reservedEnvironmental Protection Scotland: 24th March 2014
The British Geological Survey (BGS)
− world's oldest national geological survey (1835)
− public sector organisation
− the UK’s No.1 centre for geoscience information & expertise
− geoscience advisors to UK Government (and Scottish Govt)
− impartial geological advice to industry, academia & the public
− part of NERC, which reports to BIS
− 50% funded (c. £45m) from NERC, rest from public and private commissioned research
© NERC All rights reservedEnvironmental Protection Scotland: 24th March 2014
BGS Edinburgh office
Murchison House
© NERC All rights reservedEnvironmental Protection Scotland: 24th March 2014
BGS expertise on shale gas issues− 3D geological modelling
− Hydrocarbon prospectivity
− Organic geochemistry
− Groundwater sustainability and quality
− Seismicity, earthquake hazard & rock stress
© NERC All rights reservedEnvironmental Protection Scotland: 24th March 2014
What is shale?
− Grey or black, soft
− Fine grained
− Low porosity and permeability
− 70% of the world’s surface rocks are sedimentary; 50% of those are shale
− Contain ~95 % of the organic matter in sedimentary rocks
P521295
Lower Devonian shale, Margie Burn, Edzell
© NERC All rights reservedEnvironmental Protection Scotland: 24th March 2014
P219686Shales, siltstones and thin sandstones in the Gullane Formation, Linhouse Water, Mid Calder, West Lothian
What is shale?
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Land plant material and seawater algae collect in mud
Older, deeper shale layer
Where does the organic material come from?
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500 m
0 mOld deep shale layer
Burial over millions of years
− Shale buried
− Biological decay –biogenic methane
− Organic matter ‘cooked’ – thermogenic methane
Shale formation
© NERC All rights reservedEnvironmental Protection Scotland: 24th March 2014
© NERC All rights reservedEnvironmental Protection Scotland: 24th March 2014
Oil and gas maturation
Geothermal gradient in Scotland = 30 to 45oC/km
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Kerogen types and their hydrocarbon potentialEnvironment Kerogen
typeKerogen form Origin HC potential
Aquatic
I
Alginite Algal bodiesOil
Amorphous Kerogen
Structureless debris of algal origin
Oil
IIStructureless planktonic material,primarily of marine origin
Terrestrial
II
Exinite Skins of spores and pollen, cuticle of leaves and herbaceous plants
Oil
III
Vitrinite Fibrous and woody plant fragments and structurelesscolloidal humic matter
Gas, some oil
Mainly gas
IVInertinite Oxidised, recycled woody debris
None
© NERC All rights reservedEnvironmental Protection Scotland: 24th March 2014
Petroleum accumulates instructural closure
Cap rock
Oil
Gas
Water
Reservoir
rock
Source
rock
www.aapg.org
Cap Rock
Reservoir
Source
Conventional Petroleum System
© NERC All rights reservedEnvironmental Protection Scotland: 24th March 2014
PERMEABLE
RESERVOIR
ROCKS
What is a Gas Shale ?
LOMPOC Quarry Sample
Monterey Formation, CA
10 cm
It´s all together:
the source
the reservoir
the seal
and:
it is rich in organic carbon
!! Shale gas is self-contained HC system !
Unconventional Petroleum System− Regionally extensive
− Dry holes are rare
− No HC/H2O contacts
− Poor reservoir
− Production difficult
− Performance unpredictable
− High OPEX
© NERC All rights reservedEnvironmental Protection Scotland: 24th March 2014
Sand grain
Sand grain
gas
gas
0.25mm
shalesandstone
Conventional − Unconventional
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iMethane gas is stored……
In sorbedstate
On the surface of the organic fraction
On the surface of clay minerals
As free gas
Matrix porosity (blue)
Fracture porosity
− Fracture gas is produced immediately
− Adsorbed gas is released as pressure declines
© NERC All rights reservedEnvironmental Protection Scotland: 24th March 2014
PERMEABLE
RESERVOIR
ROCKS
Unconventional Petroleum Systems
− Shale gas
− Shale oil
− Tight gas sands
− Heavy oil
− Coalbed methane
− Gas hydrates
− Oil shale
© NERC All rights reservedEnvironmental Protection Scotland: 24th March 2014
Oil shale
− Organic rich
− Immature for oil & gas
− Produces oil and gas when pyrolyzed at around 500°C
P528095Oil-shale from West Lothian
© NERC All rights reservedEnvironmental Protection Scotland: 24th March 2014
From: frontispiece of Bibliotheca Chemica (Volume 2), 1906, edited by John Ferguson
Scotland − birthplace of the oil industryJames “Paraffin” Young
1811 − 1883− 1850 Patent: distillation of
oil and paraffin wax from cannel coal
− 1851, Bathgate: first commercial oil-works in the world
− Initially torbanite & cannel coal, then oil shale used
− Scotland was the worlds largest oil-producing nation for a few years!
− In production until 1960
© NERC All rights reservedEnvironmental Protection Scotland: 24th March 2014
P000194
West Lothian oil-shale works
Retorts, distillation plant and condensers in 1927
− Estimated total oil production = 75m barrels (10m tonnes)
− 37m barrels remaining (5m tonnes)
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Oil-shale products
P528115
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P000199
Spent shale…
Westwood Bing 'The Five Sisters', West Calder, West Lothian
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What makes a successful shale play?
− Conventional oil & gas production
− Depth range: 1000 – 3500 m
− TOC; Tmax; HI (maturity)
− Kerogen type (I & II)
− Target unit thickness/volume
− Overpressured zones
− Maturity within the gas/oil window
− Petrography: non-clay minerals
− Good geophysical data
© NERC All rights reservedEnvironmental Protection Scotland: 24th March 2014
Risk Period Target Basin/setting
Lower
Carboniferous Bowland Shale Pennine
Jurassic Kimmeridge Clay Weald
Higher
Carboniferous Dinantian shales Pennine
Jurassic Lias Weald
Carboniferous Oil Shale Group Midland Valley, Scotland
Cambrian Upper Cambrian Midland Microcraton
UK exploration targets
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Conventional oil & gas wells
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Midland Valley PEDL licences
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© NERC All rights reservedEnvironmental Protection Scotland: 24th March 2014
Resources and reserves ‒ definitions
Resources refers to an estimate of the amounts of oil and gas that are believed to be physically contained in the source rock
Reserves refer to an estimate of the amount of oil or gas that can technically and economically be expected to be produced from a geological formation. Estimates of reserves will develop and improve with increasing exploration drilling
© NERC All rights reservedEnvironmental Protection Scotland: 24th March 2014
SPE Oil & Gas Reserves Committee (OGRC)
Resources and reserves
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ResourceTechnically recoverableresource
Economic reserve ?
Resources and reserves
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Resources and reserves
Bowland Shale resources
Total Gas in Place (GIP)
= 1,329 tcf (2013)
Midland Valley resources
= ? (2014)
© NERC All rights reservedEnvironmental Protection Scotland: 24th March 2014
− Bottom-up – In place figure based on geological model, volumetrics and gas contents-BGS approach
− Top-down – Technically recoverable estimate based on well technology, well density, well performance* USGS approach
*more reliable figure but requires production data that we don’t have in the UK
How to estimate
© NERC All rights reservedEnvironmental Protection Scotland: 24th March 2014
Core and cuttings for:Mineralogy
Organic geochemistry
Vitrinite reflectance
Porosity and permeability
Subsurface models:of shale thicknesses
of underground stress
Downhole data:Geophysical log: Natural/spectral gamma;
resistivity; sonic, nuclear, image etc.
Geothermal gradient
Interpreted 2D/3D seismic
Datasets to aid resource estimations
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Workflow
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Bowland Shale (lower unit)
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− Correlation and dating: establish a geological framework
− Variations in TOC and kerogen types
− Variations in shale mineralogy
− Geological controls on variables:
• Depositional
• Diagenetic
• Basin evolution; Maturation, inversion
− Resource assessment‒ resource to reserve
Geological challenges
© NERC All rights reservedEnvironmental Protection Scotland: 24th March 2014
− Cracks the shale
− High pressure water or nitrogen, 350-700 bar (350 to 700 atmospheres)
Fracking basics
© NERC All rights reservedEnvironmental Protection Scotland: 24th March 2014
hfb@bgs.ac.uk
www.bgs.ac.uk/research/ukgeology/scotland.html