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Gonzalo Zambrano, PhD, PEng 
Research Associate 
University of Alberta 
Advanced Workshop for CO2 Storage 
August 26-17, 2014 
DF IPN ESIA Ticomán Auditorium 
SUPPORTED BY:
Monitoring Measuring and Verification (MMV) 
01 2003 
2006 
2009 
2012 
2015 
2018 
2021 
2024 
09 / 01 / 
2000 
2027 
2030 
01 / 01 / 2033 
01 / 01 / 2034 
End of EOR 
75 Pattern Reservoir Simulation from IEA Weyburn Monitoring and Storage Project – Law, ARC 
CO2 Global 
Mol. Fr. 
Numbers of Observation or Monitoring Wells? 
SUPPORTED BY:
3 
Capture Utilization Geological Storage 
CCUS 
O=C=O 
Risk Management 
Verification 
MMV 
Pre- operation 
Closure 
Post-closure 
Near 
Surface 
Above 
Container 
Container 
Domain 
R&D 
-EOR 
-Saline 
Aquifer 
Operation 
Field Studies
MMV – IPCC 2005
Previous Work - 2005 
MMV – CCS R&D 
CO2 Geological Storage – 
operational, verification, and 
environmental monitoring 
• Pembina Cardium CO2 
Monitoring Pilot Project
Other Field Studies 
6 
Weyburn 
IEA GHG Weyburn- 
Midale CO2 Storage 
and Monitoring Project 
Aquistore 
Shell Quest 
Otway Basin Pilot Project - OBPP 
Buttress 
Naylor-1
CSA Z741-12 (Future section of ISO for CCS) 
Table of Contents 
1 Scope 
2 Reference publications 
3 Definitions 
4 Management systems 
5 Site screening, selection, and 
characterization 
6 Risk management 
7 Well infrastructure development 
8 Monitoring and verification 
9 Closure
CSA Z741-12 (M&V) 
Monitoring — the measurement and surveillance activities necessary to 
provide an assurance of the integrity of CO2 storage. 
8.1 Purpose 
8.2 M&V program periods 
8.3 M&V program objectives 
8.4 M&V program design 
- procedures and practice 
- required specifications 
- recommended specifications 
- contingency monitoring
Intensity Uncertainty (%) 
Container 
Domain 
Above Container 
Domain 
Near Surface 
Domain 
Baseline 
Mode 
Operational 
Mode 
Environmental 
Mode 
Risk (%) 
Time (logarithmic) 
Monitoring 
MMV 
MMV 
MMV ?
Aquistore Project 
• Project Objectives: 
– Demonstrate CO2 storage 
in deep saline formation is 
a safe, workable solution 
to reduce greenhouse gas 
(GHG) emissions 
– Develop best methods & 
technologies to monitor 
GHG 
– Involve research 
institutions, policy makers, 
industry, and public
MMV Program 
Surface-based: 
– Regional 3D seismic survey 
• Baseline & time-lapse (?) 
• Geological characterization 
– Permanent seismic array 
• Baseline & time-lapse surveys 
– Electrical/electromagnetic 
– Gravity 
– Passive seismic 
– InSAR 
– GPS 
– Tiltmeters 
– Groundwater & Soil gas monitoring 
Well-based 
• Real-time P & T 
• Fluid sampling/tracers 
• Time-lapse logging 
• DAS/DTS 
• Heater cable 
• Cross-well seismic & VSP 
• Cross-well & surface-to-downhole 
electrical 
monitoring 
• Gravity 
• Passive seismic 
(1) plume/containment monitoring 
(2) public assurance 
(3) research objectives
Project Location: Williston Basin 
ALBERTA 
MANITOBA 
MONTANA 
WYOMING 
NORTH DAKOTA 
SOUTH DAKOTA 
EDMONTON 
SASKATOON 
WINNIPEG 
REGINA 
HELENA 
BISMARCK 
PIERRE 
CALGARY 
WILLISTON BASIN 
HUDSON 
BAY 
SASKATCHEWAN 
Estevan
Subsurface 
Model 
13 
Bearpaw Shale 
Colorado Shale 
Watrous “Red Beds” 
Prairie Evaporite Formation 
Till 
Mannville Group 
Midale Beds 
Bakken Formation 
Red River Formation 
Deadwood Formation 
Depth ~ 3.4 km 
Aquistore depth is equivalent to 
over 30 football fields end to end. 
Precambrian Basement
Phase 1: Demonstration & Evaluation 
• Site selection, permits, 
agreements, community 
engagement 
• Risk assessment, seismic 
surveys, monitoring 
programs 
• Evaluation/injection well 
• Observation/monitoring 
well 
• Water injection test
Phase 2: Commercial & Monitoring 
• On going monitoring and 
observation 
• On going community 
engagement 
• Pipeline tie-in CO2 from 
Boundary Dam Power 
Station 
• Word’s first commercial 
carbon capture technology 
in a coal plant and the sale 
of CO2 for EOR/storage
Project Management 
Aquistore 
PTRC 
Communications 
PTRC 
Research & 
Development 
PTRC 
Operations 
Schlumberger 
Carbon Services 
Management Committee 
•Petroleum Technology Research Centre 
•SaskPower 
•Schlumberger Carbon Services 
•Enbridge 
•SaskEnergy 
•Sask Ministry of Energy and Resources 
•Sask Ministry of Environment 
•Consumers Cooperative Refineries Ltd 
•Korea National Oil Corporation 
Science & Engineering 
Research Committee 
• Geological Survey of Canada 
• University of Alberta 
• University of Saskatchewan 
• Schlumberger Doll 
SaskPower 
Capture & Pipeline
Injection Well Design 
• Well depth 3396m to 
Deadwood in Estevan area 
• Surface 13-3/8” casing to 
~500m 
• Production 7-5/8” casing to 
~3300m 
• 7-5/8” production casing for 
operability with 4.5” tubing 
• Achieves evaluation and 
potential injection objectives 
• Coring, DST, Logging program
Well Evaluation Program 
• Coring 
– Multiple intervals of reservoir, caprock and 
seals 
• Logging – TD section 
– Gamma Ray / SP / Resistivity / Density / 
Neutron 
– Sonic Compressional and Dipole Shear 
– Nuclear Magnetic Resonance 
– Formation Elemental Analysis 
– MDT – formation pressure & samples 
– MDT – minifrac 
• Logging – Cased hole 
– Ultra sonic cement imager 
– Pulse Neutron Log (RST) 
– Spinner Log (Flow Profile)
Observation Well 
• 9-5/8” casing to ~620m 
• 4-1/2” casing to ~3400m 
• Fluid Recovery System 
• OPZ system - P/T Gauges 
Patent P1396PC00
Site Characterization: 3D Seismic 
• Size : 30 km2 
• Acquisition : UniQ 
• Acquired March 2012 
• Vibroseis source: 
– 2-100Hz sweep 
– 5 sec record length 
– 2ms sample rate 
– 288 m line interval, 36 m in-line 
– Recievers: 
• 288m line interval, 6m in-line 
– 2411 shots, 18100 geophones 
– Natural bin size: 3m x 18m 
– Full fold: 88 
– Offset range: 220m to 5388m 
CO2 Capture 
CO2 Injector
Seismic Interpretation – Time Data 
• Line 86815 
Prairie Evaporite 
Winnipegosis 
Ashern 
Winnipeg 
Winnipeg Sand 
Deadwood 
Precambrian 
W E
Isopach for Prairie Evaporite Formation 
C.I. = 10 m m
Interpretation Summary 
• Prairie Evaporite appears to be a continuous seal throughout the 3D 
volume. 
• No evidence of vertical faulting was observed that extended through the 
Devonian or deeper section. 
• A flexure is observed in the lower section that trends NNE. The flexure 
suggests the sediments are gently folded without clear evidence that the 
strata are ruptured or faulted. 
• Orientation of this feature (subparallel to minimum horizontal stress) 
minimizes likelihood of reactivation if it is a fault. 
• The reservoir (Deadwood/Winnipeg sands) varies little in thickness. 
• The injection well is located where Deadwood and Winnipeg sands may be 
marginally thicker.
Permanent Seismic Array 
• Active source and passive monitoring 
• 630 geophones over 6.25 km2 
• 20 m depth 
• Receiver lines 144m, in-line 72m 
• Baseline dynamite survey: 
• 260 shots, 1 kg at 15 m depth 
• Source lines 288m, in-line 144m
Permanent Seismic Array: 
Repeatability Test 
25 
Permanent Array 
Dynamite shots 
2.5 km
Baseline Gravity Survey 
• Accuracy of ≤ 3.5 μGal 
• A10 surveys are 
planned at locations 
adjacent to GPS sites 
(two times per year). 
A10-003
Surface Monitoring Site
28 
Surface Monitoring Sites 
InSAR GPS 
Tiltmeter
Scale 
5 mm/y 
Red: Uplift 
Blue: Subsidence 
GPS: Background Ground Deformation
Vertical Deformation Rate - InSAR data 
MSBAS methodology: Samsonov and d’Oreye, 2012
Tiltmeters/GPS 
1/4/2013 1/5/2013 1/6/2013 1/7/2013 1/8/2013 1/9/2013 1/10/2013 1/11/2013 
Tiltmeters 
GPS 
-312 
-314 
-316 
-318 
-320 
-322 
-324 
-326 
-54 
-55 
-56 
-57 
-58 
-59 
-60 
-61 
Tilt (uR) 
Tilt (uR) 
Date (D/M/Y) 
NW 
TL0 
6
Geophones vs Fibre Sensors 
40 mm 6 mm
Acoustic Fibre Recording (DAS)
Site Orientation for Surface Studies 
• Study area is west of 
SaskPower’s Boundary 
Dam Power Plant 
• Aquistore study area 
centered on the 
injection/observation 
well sites. 
• Mostly reclaimed mining 
areas from historic coal 
mining 
• Some wetlands, modified 
and natural grasslands
Site Design for Surface Studies 
• 49-site regular grid 
centered on the 
injection/observation 
wells (7 x 7=5 x 5 km) 
• 10-site irregular grid 
(targets of opportunity – 
e.g. ash piles) 
• 9-site background grid on 
PFRA land (not shown) 
• 12-sites slated for multi-depth 
probes
Soil Gas Measurement Approach 
• Soil gas probes installed at 1.0 meter depth at each location (2.0 m depth at 
multi-depth locations) 
• Probes leak-checked using helium prior to sampling; 
• Soil gas probes sampled for: He, H2, CO2, O2, N2, H2S, C1-C7+; 
• Also sampled for stable isotopes: δ13C of: CO2 and CH4, and δ2H of CH4; 
• Also sampled for radiocarbon, 14C of CO2.
Surface CO2 Flux Measurement Approach 
• Discrete measurements of surface CO2 flux, soil temperature and 
soil moisture for ~15 minutes (N = 5) at each location. 
• Extended measurements (~4 hrs) of surface CO2 flux at select 
locations (diurnal measurements in future). 
• Measurements linked back to long term grassland measurements 
(Fort Peck, Montana – long term ecological research station).
Continuous Measurements Approach 
• Continuous measurements (12-minute intervals) of in-situ soil gas 
CO2, and soil moisture (1.0 and 2.0 depths); 
• Soil temperature at 4 depths (0.1, 0.5, 1.0, 2.0 m) 
• Installed November 2012 at site I-07, site closest to the injection 
well.
Aquistore Project Risk Assessment 
• Risk Assessment Workshop 
Held in Aug ‘11 and July ‘13 
• SLB Carbon Services Risk 
Assessment 
– Top risks were identified 
– Identify features, events and 
processes (FEPs) which could 
lead to negative outcomes 
• Solicit expert opinion 
• Management 
– RACI Matrix Chart, Risk 
Response Plan
Monitored Decision Framework 
• Planned approach to decision making over time 
that draws on long-term field measurements for 
input, with planned analysis of the 
measurements and appropriate contingent 
actions 
• long-term monitoring requires integration with a 
“working hypothesis” of the storage mechanisms 
• monitoring results combined with their analysis 
or interpretation serve to support the hypotheses 
of storage processes or aid in improving our 
predictive capabilities
Monitored Decision Framework 
• Normal practice in subsurface waste disposal 
or oil and gas activities. 
• In geological storage of CO2 , there is the need 
(requirement?) to confirm the “science” of 
storage and to ensure adequate storage 
permanence. 
• These drivers demand monitoring programs 
that inform operating practices but provide 
value-added knowledge on the evolution of 
the CO2 storage processes.
Systematic Approach to Planning 
Monitoring Programs 
• Definition of project conditions 
• Prediction of mechanisms that control behavior 
• Identify the technical questions to be answered 
• Select parameters to be measured and their role 
in answering technical questions 
• Predict magnitude of change expected in 
parameters 
• Select instrumentation/monitoring approach 
• Instrument/monitoring locations
Purpose of Monitoring….. 
• To “truth” or validate the predictive capability of the 
simulators 
• To validate the physics of the storage process 
• To mitigate uncertainty associated with reservoir 
parameters 
• To identify and validate different categories of storage 
mechanisms in geological horizons 
• To correlate operational issues with aquifer and 
caprock response, trigger contingency plans and 
mitigation activities 
• To satisfy regulatory requirements.
CCS and MMV 
Know what you’re 
looking for ! 
Sometimes it really does 
make sense to just get 
started !

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Monitoring measuring and verification, Gonzalo Zambrano, University of Alberta

  • 1. Gonzalo Zambrano, PhD, PEng Research Associate University of Alberta Advanced Workshop for CO2 Storage August 26-17, 2014 DF IPN ESIA Ticomán Auditorium SUPPORTED BY:
  • 2. Monitoring Measuring and Verification (MMV) 01 2003 2006 2009 2012 2015 2018 2021 2024 09 / 01 / 2000 2027 2030 01 / 01 / 2033 01 / 01 / 2034 End of EOR 75 Pattern Reservoir Simulation from IEA Weyburn Monitoring and Storage Project – Law, ARC CO2 Global Mol. Fr. Numbers of Observation or Monitoring Wells? SUPPORTED BY:
  • 3. 3 Capture Utilization Geological Storage CCUS O=C=O Risk Management Verification MMV Pre- operation Closure Post-closure Near Surface Above Container Container Domain R&D -EOR -Saline Aquifer Operation Field Studies
  • 5. Previous Work - 2005 MMV – CCS R&D CO2 Geological Storage – operational, verification, and environmental monitoring • Pembina Cardium CO2 Monitoring Pilot Project
  • 6. Other Field Studies 6 Weyburn IEA GHG Weyburn- Midale CO2 Storage and Monitoring Project Aquistore Shell Quest Otway Basin Pilot Project - OBPP Buttress Naylor-1
  • 7. CSA Z741-12 (Future section of ISO for CCS) Table of Contents 1 Scope 2 Reference publications 3 Definitions 4 Management systems 5 Site screening, selection, and characterization 6 Risk management 7 Well infrastructure development 8 Monitoring and verification 9 Closure
  • 8. CSA Z741-12 (M&V) Monitoring — the measurement and surveillance activities necessary to provide an assurance of the integrity of CO2 storage. 8.1 Purpose 8.2 M&V program periods 8.3 M&V program objectives 8.4 M&V program design - procedures and practice - required specifications - recommended specifications - contingency monitoring
  • 9. Intensity Uncertainty (%) Container Domain Above Container Domain Near Surface Domain Baseline Mode Operational Mode Environmental Mode Risk (%) Time (logarithmic) Monitoring MMV MMV MMV ?
  • 10. Aquistore Project • Project Objectives: – Demonstrate CO2 storage in deep saline formation is a safe, workable solution to reduce greenhouse gas (GHG) emissions – Develop best methods & technologies to monitor GHG – Involve research institutions, policy makers, industry, and public
  • 11. MMV Program Surface-based: – Regional 3D seismic survey • Baseline & time-lapse (?) • Geological characterization – Permanent seismic array • Baseline & time-lapse surveys – Electrical/electromagnetic – Gravity – Passive seismic – InSAR – GPS – Tiltmeters – Groundwater & Soil gas monitoring Well-based • Real-time P & T • Fluid sampling/tracers • Time-lapse logging • DAS/DTS • Heater cable • Cross-well seismic & VSP • Cross-well & surface-to-downhole electrical monitoring • Gravity • Passive seismic (1) plume/containment monitoring (2) public assurance (3) research objectives
  • 12. Project Location: Williston Basin ALBERTA MANITOBA MONTANA WYOMING NORTH DAKOTA SOUTH DAKOTA EDMONTON SASKATOON WINNIPEG REGINA HELENA BISMARCK PIERRE CALGARY WILLISTON BASIN HUDSON BAY SASKATCHEWAN Estevan
  • 13. Subsurface Model 13 Bearpaw Shale Colorado Shale Watrous “Red Beds” Prairie Evaporite Formation Till Mannville Group Midale Beds Bakken Formation Red River Formation Deadwood Formation Depth ~ 3.4 km Aquistore depth is equivalent to over 30 football fields end to end. Precambrian Basement
  • 14. Phase 1: Demonstration & Evaluation • Site selection, permits, agreements, community engagement • Risk assessment, seismic surveys, monitoring programs • Evaluation/injection well • Observation/monitoring well • Water injection test
  • 15. Phase 2: Commercial & Monitoring • On going monitoring and observation • On going community engagement • Pipeline tie-in CO2 from Boundary Dam Power Station • Word’s first commercial carbon capture technology in a coal plant and the sale of CO2 for EOR/storage
  • 16. Project Management Aquistore PTRC Communications PTRC Research & Development PTRC Operations Schlumberger Carbon Services Management Committee •Petroleum Technology Research Centre •SaskPower •Schlumberger Carbon Services •Enbridge •SaskEnergy •Sask Ministry of Energy and Resources •Sask Ministry of Environment •Consumers Cooperative Refineries Ltd •Korea National Oil Corporation Science & Engineering Research Committee • Geological Survey of Canada • University of Alberta • University of Saskatchewan • Schlumberger Doll SaskPower Capture & Pipeline
  • 17. Injection Well Design • Well depth 3396m to Deadwood in Estevan area • Surface 13-3/8” casing to ~500m • Production 7-5/8” casing to ~3300m • 7-5/8” production casing for operability with 4.5” tubing • Achieves evaluation and potential injection objectives • Coring, DST, Logging program
  • 18. Well Evaluation Program • Coring – Multiple intervals of reservoir, caprock and seals • Logging – TD section – Gamma Ray / SP / Resistivity / Density / Neutron – Sonic Compressional and Dipole Shear – Nuclear Magnetic Resonance – Formation Elemental Analysis – MDT – formation pressure & samples – MDT – minifrac • Logging – Cased hole – Ultra sonic cement imager – Pulse Neutron Log (RST) – Spinner Log (Flow Profile)
  • 19. Observation Well • 9-5/8” casing to ~620m • 4-1/2” casing to ~3400m • Fluid Recovery System • OPZ system - P/T Gauges Patent P1396PC00
  • 20. Site Characterization: 3D Seismic • Size : 30 km2 • Acquisition : UniQ • Acquired March 2012 • Vibroseis source: – 2-100Hz sweep – 5 sec record length – 2ms sample rate – 288 m line interval, 36 m in-line – Recievers: • 288m line interval, 6m in-line – 2411 shots, 18100 geophones – Natural bin size: 3m x 18m – Full fold: 88 – Offset range: 220m to 5388m CO2 Capture CO2 Injector
  • 21. Seismic Interpretation – Time Data • Line 86815 Prairie Evaporite Winnipegosis Ashern Winnipeg Winnipeg Sand Deadwood Precambrian W E
  • 22. Isopach for Prairie Evaporite Formation C.I. = 10 m m
  • 23. Interpretation Summary • Prairie Evaporite appears to be a continuous seal throughout the 3D volume. • No evidence of vertical faulting was observed that extended through the Devonian or deeper section. • A flexure is observed in the lower section that trends NNE. The flexure suggests the sediments are gently folded without clear evidence that the strata are ruptured or faulted. • Orientation of this feature (subparallel to minimum horizontal stress) minimizes likelihood of reactivation if it is a fault. • The reservoir (Deadwood/Winnipeg sands) varies little in thickness. • The injection well is located where Deadwood and Winnipeg sands may be marginally thicker.
  • 24. Permanent Seismic Array • Active source and passive monitoring • 630 geophones over 6.25 km2 • 20 m depth • Receiver lines 144m, in-line 72m • Baseline dynamite survey: • 260 shots, 1 kg at 15 m depth • Source lines 288m, in-line 144m
  • 25. Permanent Seismic Array: Repeatability Test 25 Permanent Array Dynamite shots 2.5 km
  • 26. Baseline Gravity Survey • Accuracy of ≤ 3.5 μGal • A10 surveys are planned at locations adjacent to GPS sites (two times per year). A10-003
  • 28. 28 Surface Monitoring Sites InSAR GPS Tiltmeter
  • 29. Scale 5 mm/y Red: Uplift Blue: Subsidence GPS: Background Ground Deformation
  • 30. Vertical Deformation Rate - InSAR data MSBAS methodology: Samsonov and d’Oreye, 2012
  • 31. Tiltmeters/GPS 1/4/2013 1/5/2013 1/6/2013 1/7/2013 1/8/2013 1/9/2013 1/10/2013 1/11/2013 Tiltmeters GPS -312 -314 -316 -318 -320 -322 -324 -326 -54 -55 -56 -57 -58 -59 -60 -61 Tilt (uR) Tilt (uR) Date (D/M/Y) NW TL0 6
  • 32. Geophones vs Fibre Sensors 40 mm 6 mm
  • 34. Site Orientation for Surface Studies • Study area is west of SaskPower’s Boundary Dam Power Plant • Aquistore study area centered on the injection/observation well sites. • Mostly reclaimed mining areas from historic coal mining • Some wetlands, modified and natural grasslands
  • 35. Site Design for Surface Studies • 49-site regular grid centered on the injection/observation wells (7 x 7=5 x 5 km) • 10-site irregular grid (targets of opportunity – e.g. ash piles) • 9-site background grid on PFRA land (not shown) • 12-sites slated for multi-depth probes
  • 36. Soil Gas Measurement Approach • Soil gas probes installed at 1.0 meter depth at each location (2.0 m depth at multi-depth locations) • Probes leak-checked using helium prior to sampling; • Soil gas probes sampled for: He, H2, CO2, O2, N2, H2S, C1-C7+; • Also sampled for stable isotopes: δ13C of: CO2 and CH4, and δ2H of CH4; • Also sampled for radiocarbon, 14C of CO2.
  • 37. Surface CO2 Flux Measurement Approach • Discrete measurements of surface CO2 flux, soil temperature and soil moisture for ~15 minutes (N = 5) at each location. • Extended measurements (~4 hrs) of surface CO2 flux at select locations (diurnal measurements in future). • Measurements linked back to long term grassland measurements (Fort Peck, Montana – long term ecological research station).
  • 38. Continuous Measurements Approach • Continuous measurements (12-minute intervals) of in-situ soil gas CO2, and soil moisture (1.0 and 2.0 depths); • Soil temperature at 4 depths (0.1, 0.5, 1.0, 2.0 m) • Installed November 2012 at site I-07, site closest to the injection well.
  • 39. Aquistore Project Risk Assessment • Risk Assessment Workshop Held in Aug ‘11 and July ‘13 • SLB Carbon Services Risk Assessment – Top risks were identified – Identify features, events and processes (FEPs) which could lead to negative outcomes • Solicit expert opinion • Management – RACI Matrix Chart, Risk Response Plan
  • 40. Monitored Decision Framework • Planned approach to decision making over time that draws on long-term field measurements for input, with planned analysis of the measurements and appropriate contingent actions • long-term monitoring requires integration with a “working hypothesis” of the storage mechanisms • monitoring results combined with their analysis or interpretation serve to support the hypotheses of storage processes or aid in improving our predictive capabilities
  • 41. Monitored Decision Framework • Normal practice in subsurface waste disposal or oil and gas activities. • In geological storage of CO2 , there is the need (requirement?) to confirm the “science” of storage and to ensure adequate storage permanence. • These drivers demand monitoring programs that inform operating practices but provide value-added knowledge on the evolution of the CO2 storage processes.
  • 42. Systematic Approach to Planning Monitoring Programs • Definition of project conditions • Prediction of mechanisms that control behavior • Identify the technical questions to be answered • Select parameters to be measured and their role in answering technical questions • Predict magnitude of change expected in parameters • Select instrumentation/monitoring approach • Instrument/monitoring locations
  • 43. Purpose of Monitoring….. • To “truth” or validate the predictive capability of the simulators • To validate the physics of the storage process • To mitigate uncertainty associated with reservoir parameters • To identify and validate different categories of storage mechanisms in geological horizons • To correlate operational issues with aquifer and caprock response, trigger contingency plans and mitigation activities • To satisfy regulatory requirements.
  • 44. CCS and MMV Know what you’re looking for ! Sometimes it really does make sense to just get started !