Heavy fuel oil

Heavy fuel oil (HFO) is a category of fuel oils of a tar-like consistency. Also known as bunker fuel, or residual fuel oil, HFO is the result or remnant from the distillation and cracking process of petroleum. For this reason, HFO is contaminated with several different compounds including aromatics, sulfur, and nitrogen, making emissions upon combustion more polluting compared to other fuel oils.[1] HFO is predominantly used as a fuel source for marine vessel propulsion using marine diesel engines due to its relatively low cost compared to cleaner fuel sources such as distillates.[2][3] The use and carriage of HFO on-board vessels presents several environmental concerns, namely the risk of oil spill and the emission of toxic compounds and particulates including black carbon. Presently, the use of HFOs is banned as a fuel source for ships travelling in the Antarctic as part of the International Maritime Organization's (IMO) International Code for Ships Operating in Polar Waters (Polar Code).[4] For similar reasons, an HFO ban in Arctic waters is currently being considered.[5]

"Bunker oil" redirects here. For the Norwegian company, see Bunker Oil (company).
Tar-like consistency of heavy fuel oil

Heavy fuel oil characteristics

HFO consists of the remnants or residual of petroleum sources once the hydrocarbons of higher quality are extracted via processes such as thermal and catalytic cracking. Thus, HFO is also commonly referred to as residual fuel oil. The chemical composition of HFO is highly variable due to the fact that HFO is often mixed or blended with cleaner fuels; blending streams can include carbon numbers from C20 to greater than C50. HFOs are blended to achieve certain viscosity and flow characteristics for a given use. As a result of the wide compositional spectrum, HFO is defined by processing, physical and final use characteristics. Being the final remnant of the cracking process, HFO also contains mixtures of the following compounds to various degrees: "paraffins, cycloparaffins, aromatics, olefins, and asphaltenes as well as molecules containing sulfur, oxygen, nitrogen and/or organometals".[1] HFO is characterized by a maximum density of 1010 kg/m3 at 15°C, and a maximum viscosity of 700 mm2/s (cSt) at 50°C according to ISO 8217.[6]

Combustion and atmospheric reactions

Given HFO elevated sulfur contamination (maximum of 5% by mass),[6] the combustion reaction results in the formation of sulfur dioxide SO2 which will eventually lead to the formation of acid rain (sulfuric acid or H2SO4) in the atmosphere.

Example of formation of acid rain:

OH + SO2 → HOSO2

HOSO2 + O2 → HO2 + SO3

SO3 + H2O → H2SO4[7]

Resulting formation of nitric acid (HNO3) a component of acid rain:

H2O + N2 + NO2 → HNO3 + HNO2

3 HNO2 → HNO3 + 2 NO + H2O

4NO + 3 O2 + 2 H2O → 4HNO3

Heavy fuel oil use and shipping

Since the middle of the 19th century, HFO has been used primarily by the shipping industry due to its low cost compared with all other fuel oils, being up to 30% less expensive, as well as the historically lax regulatory requirements for emissions of nitrogen oxides (NOx) and sulfur dioxide (SO2) by the IMO.[2][3] For these two reasons, HFO is the single most widely used engine fuel oil on-board ships. Data available until 2007 for global consumption of HFO at the international marine sector reports total fuel oil usages of 200 million tonnes, with HFO consumption accounting for 174 million tonnes. Data available until 2011 for fuel oil sales to the international marine shipping sector reports 207.5 million tonnes total fuel oil sales with HFO accounting for 177.9 million tonnes.[8]

Marine vessels can use a variety of different fuels for the purpose of propulsion, which are divided into two broad categories: residual oils or distillates. In contrast to HFOs, distillates are the petroleum products created through refining crude oil and include diesel, kerosene, naphtha and gas. Residual oils are often combined to various degrees with distillates to achieve desired properties for operational and/or environmental performance. Table 1 lists commonly used categories of marine fuel oil and mixtures; all mixtures including the low sulfur marine fuel oil are still considered HFO.[3]

Table 1: Types of Marine HFO and Composition[3]
Category of Marine HFO Marine HFO Composition
Bunker C/Fuel oil No.6 residual oil
Intermediate Fuel Oil (IFO) 380 distillate combined with 98% residual oil
Intermediate Fuel Oil (IFO) 180 distillate combined with 88% residual oil
Low Sulfur Marine Fuel Oils (HFO derivative) distillate/residual oil blend (higher ratio of distillate)

Arctic environmental concerns
Wildlife suffering from a tanker oil spill. Tar-like HFO coats and persistently sticks to feathers.

The use and carriage of HFO in the Arctic is a commonplace marine industry practice. In 2015, over 200 ships entered Arctic waters carrying a total of 1.1 million tonnes of fuel with 57% of fuel consumed during Arctic voyages being HFO.[9] In the same year, trends in carriage of HFO were reported to be 830,000 tonnes, representing a significant growth from the reported 400,000 tonnes in 2012. A report in 2017 by Norwegian Type Approval body Det Norske Veritas (DNV GL) calculated the total fuel use of HFO by mass in the Arctic to be over 75% with larger vessels being the main consumers. In light of increased area traffic and given that the Arctic is considered to be a sensitive ecological area with a higher response intensity to climate change, the environmental risks posed by HFO present concern for environmentalists and governments in the area.[10] The two main environmental concerns for HFO in the Arctic are the risk of spill or accidental discharge and the emission of black carbon as a result of HFO consumption.[9][3]

Environmental impacts of heavy fuel oil spills

Due to its very high viscosity and elevated density, HFO released into the environment is a greater threat to flora and fauna compared to distillate or other residual fuels. In 2009, the Arctic Council identified the spill of oil in the Arctic as the greatest threat to the local marine environment. Being the remnant of the distillation and cracking processes, HFO is characterized by an elevated overall toxicity compared to all other fuels. Its viscosity prevents breakdown into the environment, a property exacerbated by the cold temperatures in the Arctic resulting in the formation of tar-lumps, and an increase in volume through emulsification. Its density, tendency to persist and emulsify can result in HFO polluting both the water column and seabed.[9]

Table 2: Marine HFO Spill Characteristics and Impacts[3]
Category of Marine HFO Immediate Spill Impact Environmental Impact Cleanup Characteristics
Bunker C/Fuel oil No.6 May emulsify, form into tar balls, remain buoyant or sink to the seabed. Tar-like consistency of HFO sticks to feathers and fur, results in short and long term impacts on marine flora and fauna (benthic, intertidal and shoreline species) Water recovery of spill is limited, cleanup consists mainly of shoreline and oiled substrate remediation.
Intermediate Fuel Oil (IFO) 380 Emulsifies up to 3x the original spill volume, may sink to seabed or remain buoyant. Skimmers are used to recover on-water spill until the oil emulsifies making its removal more difficult. Once coated to the surface, the oil is difficult to remove from substrate and sediment.
Intermediate Fuel Oil (IFO) 180
Low Sulfur Marine Fuel Oils (HFO derivative) No ground data to determine immediate spill impact. Laboratory tests suggest behavior similar to other HFO mixtures namely environmental persistence and emulsification. Limited information. Likely to have similar impacts as IFO with increased initial toxicity due to the higher distillate component causing immediate dispersal and evaporation. Limited information. Likely to have similar impacts to other HFO mixtures.

History of heavy fuel oil spill incidents since 2000

The following HFO specific spills have occurred since the year 2000. The information is organized according to year, ship name, amount released and the spill location:

  • 2011 Golden Traded (205 tons in Skagerrak)
  • 2011 Godafoss, Malaysia (200,000 gallons in Hvaler Islands)
  • 2009 Full City, Panama (6,300-9,500 gallons in Langesund)
  • 2004 Selendang Ayu, Malaysia (336,000 gallons in Unalaska Island - near Arctic)
  • 2003 Fu Shan Hai, China (1,680 tons in the Baltic Sea)
  • 2002 Prestige oil spill, Spain (17.8 million gallons in Atlantic Ocean)
  • 2001 Baltic Carrier, Marshall Islands (2350 tons in the Baltic Sea)
  • 2000 Janra, Germany (40 tons in the Sea of Åland)[11]

Environmental impacts of heavy fuel oil use

The combustion of HFO in ship engines results in the highest amount of black carbon emissions compared to all other fuels. The choice of marine fuel is the most important determinant of ship engine emission factors for black carbon. The second most important factor in the emission of black carbon is the ship load size, with emission factors of black carbon increasing up to six times given low engine loads.[12] Black carbon is the product of incomplete combustion and a component of soot and fine particulate matter (<2.5 μg). It has a short atmospheric lifetime of a few days to a week and is typically removed upon precipitation events.[13] Although there has been debate concerning the radiative forcing of black carbon, combinations of ground and satellite observations suggest a global solar absorption of 0.9W·m−2, making it the second most important climate forcer after CO2.[14][15] Black carbon affects the climate system by: decreasing the snow/ice albedo through dark soot deposits and increasing snowmelt timing,[16] reducing the planetary albedo through absorption of solar radiation reflected by the cloud systems, earth surface and atmosphere,[15] as well as directly decreasing cloud albedo with black carbon contamination of water and ice found therein.[15][13] The greatest increase in Arctic surface temperature per unit of black carbon emissions results from the decrease in snow/ice albedo which makes Arctic specific black carbon release more detrimental than emissions elsewhere.[17]

IMO and the Polar Code

The International Maritime Organization (IMO), a specialized arm of the United Nations, adopted into force on 1 January 2017 the International Code for Ships Operating in Polar Waters or Polar Code. The requirements of the Polar Code are mandatory under both the International Convention for the Prevention of Pollution from Ships (MARPOL) and the International Convention for the Safety of Life at Sea (SOLAS). The two broad categories covered by the Polar Code include safety and pollution prevention related to navigation in both Arctic and Antarctic polar waters.[4]

The carriage and use of HFO in the Arctic is discouraged by the Polar Code while being banned completely from the Antarctic under MARPOL Annex I regulation 43.[18] The ban of HFO use and carriage in the Antarctic precedes the adoption of the Polar Code. At its 60th session (26 March 2010), The Marine Environmental Protection Committee (MEPC) adopted Resolution 189(60) which went into effect in 2011 and prohibits fuels of the following characteristics:[19]

  1. crude oils having a density at 15°C higher than 900 kg/m3 ;
  2. oils, other than crude oils, having a density at 15°C higher than 900 kg/m3 or a kinematic viscosity at 50°C higher than 180 mm2 /s; or
  3. bitumen, tar and their emulsions.

IMO's Marine Environmental Protection Committee (MEPC) tasked the Pollution Prevention Response Sub-Committee (PPR) to enact a ban on the use and carriage of heavy fuel in Arctic waters at its 72nd and 73rd sessions. This task is also accompanied by a requirement to properly define HFO taking into account its current definition under MARPOL Annex I regulation 43.[18] The adoption of the ban is anticipated for 2021, with widespread implementation by 2023.[20]

Resistance to heavy fuel oil phase-out

The Clean Arctic Alliance was the first IMO delegate nonprofit organization to campaign against the use of HFO in Arctic waters. However, the phase-out and ban of HFO in the Arctic was formally proposed to MEPC by eight countries in 2018: Finland, Germany, Iceland, the Netherlands, New Zealand, Norway, Sweden and the United States. [9] [18] Although these member states continue to support the initiative, several countries have been vocal about their resistance to an HFO ban on such a short time scale. The Russian Federation has expressed concern for impacts to the maritime shipping industry and trade given the relatively low cost of HFO. Russia instead suggested the development and implementation of mitigation measures for the use and carriage of HFO in Arctic waters. Canada and Marshall Islands have presented similar arguments, highlighting the potential impacts on Arctic communities (namely remote indigenous populations) and economies.[5]

To appease concerns and resistance, at its 6th session in February 2019, the PPR sub-committee working group developed a "draft methodology for analyzing impacts" of HFO to be finalized at PPR's 7th session in 2020. The purpose of the methodology being to evaluate the ban according to its economic and social impacts on Arctic indigenous communities and other local communities, to measure anticipated benefits to local ecosystems, and potentially consider other factors that could be positively or negatively affected by the ban.[21]

References
  1. McKee, Richard; Reitman, Fred; Schreiner, Ceinwen; White, Russell; Charlap, Jeffrey; O'Neill, Thomas; Olavsky Goyak, Katy (2013). "The toxicological effects of heavy fuel oil category substances". International Journal of Toxicology. 33 (1 Suppl): 95–109. doi:10.1177/1091581813504230. PMID 24179029.
  2. Bengtsson, S.; Andersson, K.; Fridell, E. (13 May 2011). "A comparative life cycle assessment of marine fuels: liquefied natural gas and three other fossil fuels". Proceedings of the Institution of Mechanical Engineers, Part M: Journal of Engineering for the Maritime Environment. doi:10.1177/1475090211402136. S2CID 110498596.
  3. DeCola, Elise; Robertson, Tim (July 2018). "Phasing Out the Use and Carriage for Use of Heavy Fuel Oil in the Canadian Arctic: Impacts to Northern Communities" (PDF). Report to WWF Canada.
  4. "Polar Code". www.imo.org. Archived from the original on 10 April 2019. Retrieved 5 March 2019.
  5. MEPC 72 (2018). Report of the Marine Environment Protection Committee on its Seventy-Second Session.
  6. "HFO". powerplants.man-es.com. Retrieved 7 April 2019.
  7. "Petroleum - Chemistry - How Hydrocarbons Burn". www.petroleum.co.uk. Retrieved 8 April 2019.
  8. "Third IMO Greenhouse Gas Study 2014" (PDF). 2014. Archived from the original (PDF) on 19 October 2015. Retrieved 9 April 2019.
  9. Prior, Sian; Walsh, Dave (2 November 2018). "A Vision for a Heavy Fuel Oil-Free Arctic". Environment: Science and Policy for Sustainable Development. 60 (6): 4–11. doi:10.1080/00139157.2018.1517515. ISSN 0013-9157. S2CID 158679052.
  10. Willis, Kathy J.; Benz, David; Long, Peter R.; Macias-Fauria, Marc; Seddon, Alistair W. R. (2016). "Sensitivity of global terrestrial ecosystems to climate variability". Nature. 531 (7593): 229–232. Bibcode:2016Natur.531..229S. doi:10.1038/nature16986. hdl:1956/16712. ISSN 1476-4687. PMID 26886790. S2CID 205247770.
  11. PAME (2016). "HFO Project Phase III(a) Heavy Fuel Oil & Other Fuel Releases from Shipping in the Arctic and Near-Arctic" (PDF).
  12. Lack, D. A., & Corbett, J. J. (2012). Black carbon from ships: a review of the effects of ship speed, fuel quality and exhaust gas scrubbing. Atmospheric Chemistry and Physics, 12(9), 3985-4000.
  13. Bellouin, Nicolas; Booth, Ben (2015). "Climate change: Black carbon and atmospheric feedbacks". Nature. 519 (7542): 167–168. Bibcode:2015Natur.519..167B. doi:10.1038/519167a. ISSN 1476-4687. PMID 25762278.
  14. Gustafsson, Ö., & Ramanathan, V. (2016). Convergence on climate warming by black carbon aerosols. Proceedings of the National Academy of Sciences, 113(16), 4243–4245.
  15. Ramanathan, V., & Carmichael, G. (2008). Global and regional climate changes due to black carbon. Nature Geoscience, 1(4), 221.
  16. Flanner, Mark G.; Zender, Charles S.; Randerson, James T.; Rasch, Philip J. (2007). "Present-day climate forcing and response from black carbon in snow". Journal of Geophysical Research: Atmospheres. 112 (D11): D11202. Bibcode:2007JGRD..11211202F. doi:10.1029/2006JD008003. ISSN 2156-2202.
  17. Sand, M., Berntsen, T. K., Von Salzen, K., Flanner, M. G., Langner, J., & Victor, D. G. (2016). Response of Arctic temperature to changes in emissions of short-lived climate forcers. Nature Climate Change, 6(3), 286.
  18. "MEPC 73rd session". www.imo.org. Retrieved 4 April 2019.
  19. MEPC 60 (2010). Amendments to the Annex of the Protocol of 1978 Relating to the International Convention for the Prevention of Pollution from Ships, 1973. http://www.imo.org/blast/blastDataHelper.asp?data_id=28814&filename=189(60).pdf
  20. "IMO Moves to Ban HFO from Arctic Shipping | World Maritime News". worldmaritimenews.com. Retrieved 4 April 2019.
  21. "PPR 6th Session". www.imo.org. Retrieved 4 April 2019.

See also
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