PLANETARY EMISSIONS MANAGEMENT INC. · PDF file1 Planetary Emissions Management, Inc....

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Planetary Emissions Management, Inc. 1 PLANETARY EMISSIONS MANAGEMENT INC. Near Surface Leakage Monitoring for the Verification & Accounting of Geologic Carbon Sequestration Using a Field Ready 14 C Isotopic Analyzer Bruno D.V. Marino PhD CEO & Founder [email protected] www.pem-carbon.com DOE/EPA Collaborative Review Tracking Geologically Sequestered CO 2 : Monitoring, Verification & Accounting (MVA), Simulation and Risk Assessment March 23 24, Pittsburgh, PA

Transcript of PLANETARY EMISSIONS MANAGEMENT INC. · PDF file1 Planetary Emissions Management, Inc....

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Planetary Emissions Management, Inc.111

PLANETARY EMISSIONS MANAGEMENT INC.

Near Surface Leakage Monitoring for the Verification & Accounting of Geologic Carbon Sequestration Using a Field

Ready 14C Isotopic Analyzer

Bruno D.V. Marino PhD

CEO & Founder

[email protected]

www.pem-carbon.com

DOE/EPA Collaborative Review –Tracking Geologically Sequestered CO2: Monitoring,

Verification & Accounting (MVA), Simulation and Risk Assessment

March 23 – 24, Pittsburgh, PA

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PEM Inc.

MVA focus, founded 2007

R&D isotopic field analyzers for biogenic CO2 (13C) and ff-CO2 (14C) fluxes over regional, national, international scales

Integration of local, regional & international carbon budgets in a standardized framework

FI based on data for trading, compliance & carbon management frameworks

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PROBLEM & APPROACH

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Problem MVA & FI

– Leakage of GCS ff-CO2 to atmosphere?

– Detect & locate, quantify, 1%, .01%, 0%?

– Differentiation of ff-CO2 from biogenic CO2?

– Data requirements for GCS credits?

Approach

– Multi-isotopic field analyzers (GMP)

• 14C as direct ff-CO2 signal (~2 per mil)

• 13C as ecosystem signal (<0.1 per mil)

– Deploy in natural CO2 vent geology/ecosystems

– Deploy in active GCS sites

– Verification process for GCS carbon credits

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PROJECT OVERVIEW

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PEM

PROJECT

MANAGEMENT

FIELD

SITES

MANUFACTURING

R&D

DATA

PRODUCTS

PEM

MODELGROUPS

PEM

LBNL

PEM

RUTGERS

CARBONEXCHANGES

GCSOPERATOR

KCP

TECH

PARTNERS

TECH

PARTNERS

J. Lewicki

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PEM FIELD 14C ANALYZER

~2 per mil precision/1ppm ff-CO2

– In situ analysis – no gas sample transport

– No gas concentration needed

– Limit of detection ~10-15 14/12C

– Simultaneous 13/12C, 14/12C analyses

– Flow through/batch mode

– Fast analytical time (< 1 Hz)

– Remote operation/query/diagnostics

– NOAA inter-comparison/global reference

– Cost factor (1,440+/day)

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EXPAND LEAK DETECTION SKILL

Link PEM GMP (13C,14C) with– Eddy covariance (micrometeorology)

– Soil atmosphere (ff-CO2 accumulation)*

– DIC groundwater (ff-CO2 accumulation)*

Baseline measurements– Differentiate natural diurnal/seasonal flux

– Vary device configurations (fixed/dynamic)

– GCS signal “on” , “off” field measurements

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VERTICAL DATA INTEGRATION

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PEM SYSTEM of SYSTEMSPEM Patent Pending

CLIENT DEFINED TEMPORAL/SPATIAL SCALES

INVENTORIES

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PEM ISOTOPIC LASERS

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Laser Resonances in CO2 are Isotope Dependent

LASER GAS FILL SAME AS ANALYTE

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PEM TECHNOLOGY: GMP 13C/14C

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Optogalvanic Effect

~ S=nILA C

8 Iterative maturation process

14C ICOGS 13C

~1.5 mCi

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STATUS: 13C, 14C ANALYZERS

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FIELD SITES: LBNL J. LEWICKI

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(Lewicki et al., 2008)

218 to 3500 g m-2 d-1

1 to > 10,000 g m-2 d-1

46 to 136 t d-1 (Gerlach et al., 2001)

Springerville-St Johns, AZ< 1 to 24 g m-2 d-1

(Allis et al., 2005)

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PEM GMP 13C/14C

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Biodiesel blends (diamonds) (Reddy et al., 2008); 13C values for natural gas, liquid fuels and coal (filled squares) (Widory 2006) 14C

assumed to be -1000 per mil; modern grasses 14C (solid bar) (Riley et al., 2008) 13C assumed to have average value for C3 grasses;

modern maize 14C (filled inverted triangle) (Hsueh et al., 2007) 13C assumed to have average value for C4 plants; modern air (oval)

(Levin et al., 2003) 13C value of -7.6 per mil for 1995 to 2000; open box representing range of modern C4 plants (O’Leary, 1988) 14C

assumed to be modern ; open box representing range of modern C3 plants (O’Leary, 1998) 14C assumed to be modern; solid box

representing 13 values for magmatic CO2 (Mary & Jambon, 1987) 14C assumed to be -1000 per mil; solid box representing 13C values

for marine carbonate derived CO2 (Ohomoto & Rye, 1979) 14C assumed to be -1000 per mil. Data for Mammoth Mountain given by

Farrar et al., 1995.

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GCS MVA

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