assessing the climate trade-offs of gasoline direct ...€¦ · assessing the climate trade-offs of...
TRANSCRIPT
S1
Supporting Information:
Assessing the climate trade-offs of gasoline direct
injection engines
Naomi Zimmerman, †,*,x Jonathan M. Wang,† Cheol-Heon Jeong, † James S. Wallace, ‡ Greg J.
Evans†
†Department of Chemical Engineering and Applied Chemistry, University of Toronto, Toronto,
Ontario M5S3E5 Canada
‡ Department of Mechanical and Industrial Engineering, University of Toronto, Toronto, Ontario
M5S3G8 Canada
Corresponding author:
Dr. Naomi Zimmerman
Dept. of Chemical Engineering and Applied Chemistry
University of Toronto
200 College Street, Room 123, Toronto, Canada, M5S 3E5
xPresent Address
Dept. of Mechanical Engineering
Carnegie Mellon University
5000 Forbes Avenue, Pittsburgh, PA 15213
Tel. 412-268-2490
Fax: 416-978-8605
Email: [email protected]
12 pages, 3 tables, 2 figures
S2
S1: Inputs considered in development of black carbon (BC) emission scenarios
Table S1: Summary of emission factors considered in this study
Study MY Type Operation BC ER
(mg/mi) Notes
Bahreini et al.1
2010 PFI FTP-75 0.1
2010 PFI US06 0.1
2012 SG-GDI FTP-75 0.2
2012 SG-GDI US06 0.1
2012 WG-GDI FTP-75 1.1
2012 WG-GDI US06 0.2
Chan et al.2
2010 PFI FTP-75 0.3 22C
2010 PFI US06 0.2 22C
2013 PFI FTP-75 0.9 22C
2013 PFI US06 0.6 22C
2010 PFI FTP-75 14.5 -7C
2010 PFI US06 1.7 -7C
2013 PFI FTP-75 19.7 -7C
2010 PFI FTP-75 22.6 -18C
2010 PFI US06 0.9 -18C
2013 PFI FTP-75 33.1 -18C
2013 PFI US06 2.2 -18C
2011 WG-GDI FTP-75 8.0 22C
2011 WG-GDI US06 2.4 22C
2012 WG-GDI FTP-75 5.2 22C
2012 WG-GDI US06 4.5 22C
2011 WG-GDI FTP-75 19.0 -7C
2011 WG-GDI US06 1.4 -7C
2012 WG-GDI FTP-75 14.0 -7C
2011 WG-GDI FTP-75 33.9 -18C
2011 WG-GDI US06 4.2 -18C
2012 WG-GDI FTP-75 16.0 -18C
2012 WG-GDI US06 4.4 -18C
Forestieri et al.3
2001 PFI cold start +30min 60mph 0.0
2001 PFI cold start +30min 60mph 0.0
2008 PFI cold start +30min 60mph 0.1
2008 PFI cold start +30min 60mph 0.0
2011 WG-GDI cold start +30min 60mph 1.8
2011 WG-GDI cold start +30min 60mph 2.0
Kamboures et al.4
2009 PFI FTP-75 0.3
2009 PFI US06 0.3
2010 WG-GDI US06 1.2
Karavalakis et al.5
2007 PFI FTP-75 0.1 E10
2007 PFI UC 0.1 E10
2007 PFI FTP-75 0.4 E10
2007 PFI UC 0.2 E10
2012 PFI FTP-75 0.1 E10
2012 PFI UC 0.1 E10
2012 WG-GDI FTP-75 0.7 E10
2012 WG-GDI UC 0.7 E10
S3
2012 WG-GDI FTP-75 0.8 E10
2012 WG-GDI UC 0.6 E10
Short et al.6
2012 PFI UC 0.1 15% aromatic
2012 PFI UC 0.2 25% aromatic
2012 PFI UC 0.2 35% aromatic
2012 PFI UC 0.2 35% aromatic, high octane
2012 WG-GDI UC 0.7 15% aromatic
2012 WG-GDI UC 0.5 15% aromatic
2012 WG-GDI UC 0.3 15% aromatic
2012 WG-GDI UC 0.6 15% aromatic
2012 WG-GDI UC 0.6 15% aromatic
2012 WG-GDI UC 1.2 25% aromatic
2012 WG-GDI UC 1.1 25% aromatic
2012 WG-GDI UC 0.8 25% aromatic
2012 WG-GDI UC 1.7 25% aromatic
2012 WG-GDI UC 1.1 25% aromatic
2012 WG-GDI UC 2.0 35% aromatic
2012 WG-GDI UC 1.2 35% aromatic
2012 WG-GDI UC 1.2 35% aromatic
2012 WG-GDI UC 2.4 35% aromatic
2012 WG-GDI UC 1.6 35% aromatic
2012 WG-GDI UC 0.8 35% aromatic, high octane
2012 WG-GDI UC 1.1 35% aromatic, high octane
2012 WG-GDI UC 0.7 35% aromatic, high octane
2012 WG-GDI UC 2.1 35% aromatic, high octane
2012 WG-GDI UC 1.3 35% aromatic, high octane
Zimmerman et al.7
2012 WG-GDI 2600 rpm, 41 ft-lb 3.3
2012 WG-GDI 2600 rpm, 41 ft-lb 7.1
2013 WG-GDI Urban - Winter 2014 12.7 Real-world
2013 WG-GDI Urban - Spring 2014 7.0 Real-world
2013 WG-GDI Urban - Summer 2014 7.8 Real-world
2013 WG-GDI Urban - Winter 2015 9.6 Real-world
MY: model year
ER BC: emission rate black carbon
FTP-75: Federal Test Procedure 75
UC: Unified Cycle
PFI: Port Fuel Injection
WG-GDI: wall-guided GDI
SG-GDI: spray-guided GDI
S4
S2: Global Warming Potential (GWP) and Global Temperature Potential (GTP)
Here we introduce the equations for GWP and GTP as well as a discussion of the merits of the
GTP-based analysis when evaluating trade-offs between short- and long-lived species. A detailed
discussion is also available in the literature8–12.
The absolute global warming potential (AGWP) is defined in Shine et al.8:
𝐴𝐺𝑊𝑃𝑥(𝐻) = ∫ 𝐴𝑥 exp (−𝑡
𝛼𝑥) 𝑑𝑡 = 𝐴𝑥𝛼𝑥 [1 − exp (−
𝐻
𝛼𝑥)]
𝑡=𝐻
𝑡=0 (1)
Where AGWP, the absolute global warming potential, of species x at time horizon (H) is the time-
integrated radiative forcing from the pulse emission of a unit mass release. Here, α is the
adjustment time, which is similar to the lifetime of the species but accounts for the effects of
feedbacks from the pulse emission. Ax is the specific radiative forcing of the species (W m-2 kg-1).
GWP is made dimensionless by dividing by the AGWP of CO2 (note that calculating AGWPCO2
is slightly more complicated as CO2 does not decay exponentially).
The GWP is a simple metric that is relatively easy to calculate, and has been widely used by the
policymaking community and in reports by the Intergovernmental Panel on Climate Change
(IPCC). However, using the GWP to compare short-lived (e.g, black carbon) and long-lived (CO2)
species may lead to overestimations in the importance of a short-lived species when attempting to
calculate mean temperature changes at some target year in the future. This is due to the fact that
GWP is time-invariant, e.g., emissions occurring long before a target year are considered
equivalent to emissions at a time much closer to the target year. In reality, emissions of a short-
lived species long before a target year would contribute very little to the warming close to the
target year. To account for this, a new metric was introduced and discussed by Shine et al.8,9 which
they called the global temperature potential (GTP). The AGTP, absolute global temperature
potential of species x at time horizon H, is defined as:
S5
𝐴𝐺𝑇𝑃𝑥(𝐻) =𝐴𝑥
𝐶(𝜏−1−𝛼𝑥−1)
[exp (−𝐻
𝛼𝑥) − exp (−
𝐻
𝜏)] (2)
Where Ax and αx are as defined previously in the GWP, C is the heat capacity of the climate system
and τ is the time-scale of the climate response. Parameters C and τ are needed due to the inclusion
of a simple climate model within the metric (τ=C, where is a climate sensitivity parameter, see
Shine et al.8 for a detailed discussion). As with the GWP, the GTP is made dimensionless by
dividing by the AGTP of CO2 (note that calculating AGTPCO2 is also computed slightly
differently). Comparing equations (1) and (2), equation (2) is an end-point metric whereas equation
(1) is integrative. This metric is a function of both the time horizon and proximity to the target
time horizon, making it more relevant for comparisons of short and long-lived species.
Equation (2) is for a pulse emission of 1 kg at t=0; however, the GTP can also be used to estimate
the impact of a sustained change in emissions (equation 3). During the sustained emission period,
a constant emission of 1 kg/year from t=0 and t= H is assumed:
𝐴𝐺𝑇𝑃𝑥,𝑠𝑢𝑠𝑡𝑎𝑖𝑛𝑒𝑑(𝐻) =𝛼𝑥𝐴𝑥
𝐶{𝜏 [1 − exp (−
𝐻
𝜏)] −
1
𝜏−1−𝛼𝑥−1 [exp (−
𝐻
𝛼𝑥) − exp (−
𝐻
𝜏)]} (3)
Boucher and Reddy12, whose trade-off approach we apply as part of our analysis (see Section S5)
take a slightly different approach, defining the total emissions as equalling 1 kg across the
sustained emission period. Such an assumption allows for the sustained and pulse GTP metrics to
be more easily combined to assess a broader range of scenarios (e.g., modelling a scenario where
sustained emissions are only sustained to n=1,5,10 or 30 years, and evaluating time horizons longer
than the sustained emission period).
S6
S3: Inputs needed for all GWP calculations
Table S2: Climate trade-off inputs. Global warming potentials (GWPs) are from Bond et al.10 and the IPCC AR5
report. All black carbon (BC) and elemental carbon (EC) emission factors are from Table S1.
Input Value Unit
Carbon content of gasolinea 8887 g CO2 / gallon
Density of gasoline 755 g L-1
(2.86 kg gallon-1)
Density of ethanol 789 g L-1
20 year BC global warming potential
(uncertainty)b
3200 (270-6200) g CO2-e / g BC
100 year BC global warming potential
(uncertainty)b
900 (100-1700) g CO2-e / g BC
Scenario A: Mean ΔBCc 1.26 mg mile-1
Scenario B: Low ΔBC (25th percentile)c 0.18 mg mile-1
Scenario C: High ΔBC (75th percentile)c 3.36 mg mile-1
Scenario D: Extreme ΔBC (95th percentile)c 15.9 mg mile-1 aUnited States Environmental Protection Agency13 bBond et al.10 cScenarios developed from a Monte Carlo analysis (n=100,000).
S4: Sample Calculations
S4.1: Real-world fuel economy and black carbon trade-off:
1. Calculate the baseline CO2 emission factor of gasoline (CO2 content per mile) for a vehicle with a
fleet average fuel economy of 21.4 MPG, the 2014 in-use average14:
Baseline CO2 emissions =8887 g CO2
gallon fuel×
gallon
21.4 miles= 415.3
g CO2
mile
2. As an example, calculate CO2 emission factor for a GDI vehicle with a 5% fuel economy
improvement over the baseline case:
GDI fuel economy = 1.05 ∗ 21.4 = 22.47miles
gallon
GDI CO2 emissions =8887 g CO2
gallon fuel×
gallon
22.47 miles= 395.5
g CO2
mile
3. Calculate net change in CO2 by improving fuel economy:
CO2 savings = 395.5 g CO2
mile− 415.3
g CO2
mile= −19.8
g CO2
mile
4. Convert BC emission factors to g CO2-equivalent emission factors:
Example: Scenario C: ΔBC emission rate: 3.36 mg/mile
GWP: 20-year average (3200 g CO2-e / g BC)
3.36 mg BC
mile×
1 g BC
1000 mg BC×
3200 g CO2e
1 g BC= 10.7
g CO2e
mile
S7
5. Compare the CO2 savings to the CO2-eq BC emissions:
Net CO2 = 10.7 g CO2e
kg fuel− 19.8
g CO2
mile= −9.0
g CO2e
mile
In this example, a 5% increase in fuel economy with GDI negates the increase in BC emissions.
S4.2: Gasoline particulate filter and black carbon trade-off:
1. Calculate CO2-e savings by reducing BC using a GPF. For this example, assume a GPF BC removal
efficiency of 85% and an associated fuel penalty of 2%.
Example: Scenario C, BC emission factor: 3.36 mg/mile
GWP: 20 year average (3200 g CO2-e / g BC)
Removal efficiency = ηGPF = 85%
CO2e reduction = 𝜂𝐺𝑃𝐹 × ∆BC × GWPBC,20 yr
CO2e reduction = 0.85 × (3.36 mg BC
mile×
1 g BC
1000 mg BC×
3200 g CO2e
1 g BC) = 9.14
g CO2e
mile
2. Calculate extra CO2 from a 2% fuel penalty for a vehicle with a fuel economy of 27.4 MPG (Adj.
combined cycle fuel economy of average GDI vehicle in 2015 (see Table 2)13:
GDI CO2 emissions, no GPF =8887 g CO2
gallon fuel×
gallon
27.4 miles= 324.34
g CO2
mile
GDI fuel economy, with GPF (2% fuel penalty) = 0.98 ∗ 27.4 = 26.85miles
gallon
GDI CO2 emissions, with GPF =8887 g CO2
gallon fuel×
gallon
26.85 miles= 330.96
g CO2
mile
3. Calculate net change in CO2 from the fuel penalty:
CO2 fuel penalty = 330.96g CO2
mile− 324.34
g CO2
mile= +6.62
g CO2
mile
Burning more fuel per mile will also produce extra BC, 85% of which will be removed by the GPF. This
additional BC due to the GPF fuel penalty “CO2 fuel penaltyBC” can be accounted for as:
Baseline CO2,eqBC emissions =3.36 mg BC
mile×
1 g BC
1000 mg BC×
3200 g CO2e
1 g BC= 10.70
g CO2e
mile
CO2,eqBC emissions, 2% fuel penalty = 10.7 g CO2e
mile, no GPF×
27.4milesgallon
, no GPF
26.85milesgallon
, with GPF= 10.92
g CO2e
mile, with GPF
CO2 fuel penaltyBC = (1 − ηGPF) × [CO2 ,eq.BC(GPF) − CO2 ,eq.BC(no GPF)]
CO2 fuel penaltyBC = (1 − 0.85) × [10.92 g CO2e
mile− 10.7
g CO2e
mile] = +0.03
g CO2e
mile
Total CO2-equivalent from the fuel penalty:
CO2 fuel penalty total = 6.62 + 0.03 = 6.65g CO2e
mile
S8
4. Compare the CO2 increase from the fuel penalty to the reduction in BC emissions:
Net CO2 = 6.65g CO2eq.
mile− 9.14
g CO2e
mile= −2.5
g CO2e
mile
In this example, the reduction in BC from the GPF offsets the increase in CO2 from the fuel penalty.
S4.3: Black carbon and ethanol trade-off:
1. Calculate CO2 emission factor of pure ethanol (CO2 content per kg ethanol):
Wang et al.15 estimate from a lifecycle assessment that replacing gasoline with pure ethanol has a net
19% reduction in CO2-equivalent GHGs (incorporating CO2, CH4 and N2O) compared to gasoline.
In Zimmerman et al.7, the GDI vehicle had a highway fuel economy of 31 MPG:
CO2e gasoline =gallon
31 miles× 8887
g CO2
gallon= 286.7
g CO2
mile
CO2e ethanol = (1 − 0.19) ×gallon
31 miles× 8887
g CO2
gallon= 232.2
g CO2
mile
2. Calculate CO2 emission factor of E10 (10% ethanol v/v):
Consider 1 L of fuel:
0.1 L ethanol ×789 g ethanol
1 L ethanol= 78.9 g ethanol
0.9 L gasoline ×755 g ethanol
1 L ethanol= 679.5 g gasoline
On a mass basis, E10 (v/v) is equivalent to:
Ethanol content (m/m) =78.9 g ethanol
78.9 + 679.5= 0.104
For 1 kg of E10 (v/v) fuel, the CO2 emission factor is:
CO2e E10 = 0.104 × 232.2 g CO2
mile+ (1 − 0.104) × 286.7
g CO2
mile= 281.0
g CO2
mile
3. Calculate the net CO2 savings of burning 1 kg of E10 vs pure gasoline:
CO2 savings = 286.7g CO2
mile− 281.0
g CO2
mile= −5.7
g CO2e
mile
4. From Zimmerman et al.7, E10 in the laboratory measurements increased the EC (considered
equivalent to BC for this calculation) emission factor from 44 to 95 mg/kg fuel, calculate increase in
CO2-equivalent emissions (vehicle fuel economy 31 MPG):
For this example, use GWP: 20 year average (3200 g CO2-e / g BC)
CO2 from ∆BC = (95 − 44)mg BC
kg fuel×
1 g BC
1000 mg BC×
3200 g CO2e
1 g BC×
gallon
31 miles×
2.86 kg fuel
gallon= +15.0
g CO2e
mile
S9
5. Calculate the net impact of E10:
Net CO2 = 15.0g CO2e
mile− 5.7
g CO2e
mile= +9.3
g CO2e
mile
In this example, the increase in BC from the use of E10 is not offset by the greenhouse gas reductions of
E10 fuel (Figure S1). The results of this calculation for a 100-year time horizon are shown in Figure S1.
Figure S1: Climate trade-off analysis of increasing elemental carbon vs. decreasing life-cycle greenhouse gases with
E10 fuel vs. pure gasoline. The effect was assessed on a 20 year and 100 year time horizon. Error bars represent the
uncertainty bounds from uncertainty in the black carbon global warming potential (GWPs) in Bond et al.10 (Average
GWP = 3200 (20 year), 900 (100 year); Lower = 270 (20 year), 100 (100 year); Upper = 6200 (20 year), 1700 (100
year))
S5: Global Temperature Potential (GTP) analysis, sample calculation
Using the published curve for the GTP of BC with a 10 year sustained release12 (adapted below, Figure S2),
GTP values for BC at time horizons ranging from 1-40 years were compiled. Consider as an example:
Scenario C: increase in BC emissions of 3.36 mg/mile by replacing PFI engine with a 2015 GDI
engine with an average adjusted (combined cycle) fuel economy of 27.4 MPG
20-year time horizon: GTPnBC = 1.9 (see Figure S2, adapted from Boucher and Reddy12)
Calculate Xlimit (equation 2)
Xlimit(20) =1
GTPnBC(20)=
1
1.9= 0.526
30
20
10
0
-10
CO
2 g
-eq
. /
mile
20 year 100 year
Global Warming Potential (GWP) Time Horizon
S10
Now solve for ΔCO2 (equation 1)
X = GWPBC(T = 100)∆BC
∆CO2
∆CO2 =GWPBC(T = 100)∆BC
X=
900 ∗ 3.36 mg/mile
0.526= 5749
mg
mile
Knowing the CO2 emission factor of gasoline = 8887 g CO2 / gallon13, convert ∆CO2 from mg/mile to
∆gallons gasoline per mile:
∆ 5749 mg CO2
mile×
1g
1000 mg×
gallon
8887 g CO2
= ∆ 6.47x10−4gallon
mile
Re-arrange and solve for the critical fuel economy of the PFI vehicle:
∆CO2= 6.47x10−4
gallon
mile= (
1
MPGPFI
−1
MPGGDI
) = (1
MPGPFI
−1
27.4)
1
MPGPFI
= 0.037
MPGPFI = 26.9
Calculate the percentage fuel economy increase with GDI:
% increase =MPGGDI − MPGPFI
MPGPFI
x100 =27.4 − 26.9
26.9x100 = 1.7%
Therefore, on a 20-year time horizon for scenario C, a 1.7% improvement in fuel economy is needed to
offset the increase in BC emissions from the GDI vehicle.
Figure S2: GTP values for “normalized” BC (left) and the resulting critical value of X (right), adapted from Figures
4 and 6 in Boucher and Reddy12 (note, these figures were adapted from the Corrigendum for this article (see:
http://www.lmd.jussieu.fr/~obolmd/prod-ob1.htm)
S11
S6: Sample Fuel Composition – Summer 2015 Commercial Sample
Table S3 provides the results of a fuel analysis (analyzed by Alberta Innovates – Technology
Futures) of a summer grade commercial sample collected in 2015 from Toronto, Canada.
Table S3: Summary of fuel composition by group
Group Weight % Volume % Mol %
Aromatics 50.168 43.765 46.291
I-Paraffins 29.583 33.423 30.155
Naphthenes 3.424 3.414 3.598
Olefins 5.696 6.360 6.724
Paraffin 10.084 12.022 12.497
Oxygenates 0.027 0.026 0.057
Unidentified 1.017 0.988 0.678
Plus 0.000 0.000 0.000
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