Tarball (oil)

Last updated
A tarball on a beach on the Galapagos Islands in 2001, from an oil spill from the tanker Jessica. Tarball.jpg
A tarball on a beach on the Galápagos Islands in 2001, from an oil spill from the tanker Jessica .
Tar balls from the Deepwater Horizon oil spill washed ashore on Okaloosa Island in Fort Walton Beach, Florida on June 16, 2010 16POilSpill.jpg
Tar balls from the Deepwater Horizon oil spill washed ashore on Okaloosa Island in Fort Walton Beach, Florida on June 16, 2010

A tarball is a blob of petroleum which has been weathered after floating in the ocean. Tarballs are an aquatic pollutant in most environments, although they can occur naturally and as such are not always associated with oil spills. [1] [2] [3]

Tarball concentration and features have been used to assess the extent of oil spills and their composition can also be used to identify their sources of origin. [4] [5] They are slowly decomposed by microorganisms such as Chromobacterium violaceum , Cladosporium resinae , Bacillus submarinus , Micrococcus varians , Pseudomonas aeruginosa , Candida marina , and Saccharomyces estuari . [1]

Tarballs may be dispersed over long distances by deep sea currents. [2] The density of tarballs depends on the solids picked up in the weathering process. [6] They can range in density with some being more dense than seawater, which, at 1.025 g/ml, is more dense than the density of fresh water. When the tarballs are less dense than seawater, they can travel over great distances.

They can also be contained like oil and picked up using a variety of methods. Containment booms can be used to isolate tarballs similar to methods used to isolate oil. [7] [8]

Related Research Articles

<span class="mw-page-title-main">Petroleum</span> Naturally occurring flammable liquid

Petroleum, also known as crude oil, or simply oil, is a naturally occurring yellowish-black liquid mixture of mainly hydrocarbons, and is found in geological formations. The name petroleum covers both naturally occurring unprocessed crude oil and petroleum products that consist of refined crude oil. A fossil fuel, petroleum is formed when large quantities of dead organisms, mostly zooplankton and algae, are buried underneath sedimentary rock and subjected to both prolonged heat and pressure.

<span class="mw-page-title-main">Oil spill</span> Release of petroleum into the environment

An oil spill is the release of a liquid petroleum hydrocarbon into the environment, especially the marine ecosystem, due to human activity, and is a form of pollution. The term is usually given to marine oil spills, where oil is released into the ocean or coastal waters, but spills may also occur on land. Oil spills may be due to releases of crude oil from tankers, offshore platforms, drilling rigs and wells, as well as spills of refined petroleum products and their by-products, heavier fuels used by large ships such as bunker fuel, or the spill of any oily refuse or waste oil.

<span class="mw-page-title-main">Tar pit</span> Asphalt pit or asphalt lake

Tar pits, sometimes referred to as asphalt pits, are large asphalt deposits. They form in the presence of oil, which is created when decayed organic matter is subjected to pressure underground. If this crude oil seeps upward via fractures, conduits, or porous sedimentary rock layers, it may pool up at the surface. The lighter components of the crude oil evaporate into the atmosphere, leaving behind a black, sticky asphalt. Tar pits are often excavated because they contain large fossil collections.

<span class="mw-page-title-main">Seawater</span> Water from a sea or an ocean

Seawater, or salt water, is water from a sea or ocean. On average, seawater in the world's oceans has a salinity of about 3.5%. This means that every kilogram of seawater has approximately 35 grams (1.2 oz) of dissolved salts. The average density at the surface is 1.025 kg/L. Seawater is denser than both fresh water and pure water because the dissolved salts increase the mass by a larger proportion than the volume. The freezing point of seawater decreases as salt concentration increases. At typical salinity, it freezes at about −2 °C (28 °F). The coldest seawater still in the liquid state ever recorded was found in 2010, in a stream under an Antarctic glacier: the measured temperature was −2.6 °C (27.3 °F). Seawater pH is typically limited to a range between 7.5 and 8.4. However, there is no universally accepted reference pH-scale for seawater and the difference between measurements based on different reference scales may be up to 0.14 units.

<span class="mw-page-title-main">Channel Islands (California)</span> Archipelago off the coast of southern California, US

The Channel Islands are an eight-island archipelago located within the Southern California Bight in the Pacific Ocean, off the coast of California. The four Northern Channel Islands are part of the Transverse Ranges geologic province, and the four Southern Channel Islands are part of the Peninsular Ranges province. Five of the islands are within the Channel Islands National Park, and the waters surrounding these islands make up Channel Islands National Marine Sanctuary. The Nature Conservancy was instrumental in establishing the Channel Islands National Marine Sanctuary. The islands were inhabited as early as 13,000 years ago, the earliest paleontological evidence of humans in North America. They are the easternmost islands in the Pacific Island group.

<span class="mw-page-title-main">Cold seep</span> Ocean floor area where hydrogen sulfide, methane and other hydrocarbon-rich fluid seepage occurs

A cold seep is an area of the ocean floor where hydrogen sulfide, methane and other hydrocarbon-rich fluid seepage occurs, often in the form of a brine pool. Cold does not mean that the temperature of the seepage is lower than that of the surrounding sea water. On the contrary, its temperature is often slightly higher. The "cold" is relative to the very warm conditions of a hydrothermal vent. Cold seeps constitute a biome supporting several endemic species.

<span class="mw-page-title-main">Bioremediation</span> Process used to treat contaminated media such as water and soil

Bioremediation broadly refers to any process wherein a biological system, living or dead, is employed for removing environmental pollutants from air, water, soil, flue gasses, industrial effluents etc., in natural or artificial settings. The natural ability of organisms to adsorb, accumulate, and degrade common and emerging pollutants has attracted the use of biological resources in treatment of contaminated environment. In comparison to conventional physicochemical treatment methods bioremediation may offer considerable advantages as it aims to be sustainable, eco-friendly, cheap, and scalable. Most bioremediation is inadvertent, involving native organisms. Research on bioremediation is heavily focused on stimulating the process by inoculation of a polluted site with organisms or supplying nutrients to promote the growth. In principle, bioremediation could be used to reduce the impact of byproducts created from anthropogenic activities, such as industrialization and agricultural processes. Bioremediation could prove less expensive and more sustainable than other remediation alternatives.

<span class="mw-page-title-main">Petroleum seep</span> Place where natural hydrocarbons escape

A petroleum seep is a place where natural liquid or gaseous hydrocarbons escape to the earth's atmosphere and surface, normally under low pressure or flow. Seeps generally occur above either terrestrial or offshore petroleum accumulation structures. The hydrocarbons may escape along geological layers, or across them through fractures and fissures in the rock, or directly from an outcrop of oil-bearing rock.

<i>Aegean Sea</i> tanker oil spill 1992 environmental disaster off the coast of Galicia, Spain

The Aegean Sea tanker oil spill was a spill that occurred on 3 December 1992 when the double-bottomed Greek-flagged oil tanker, Aegean Sea, en route to the Repsol refinery in A Coruña, Spain, suffered an accident off the Galician coast. The ship had successfully passed all required tests and revisions. The accident occurred during extreme weather conditions and affected the Galician coast resulting in ecosystem damage, as well as damage to the fishing and tourist industries in A Coruña. The captain and pilot were found to be criminally liable and the shipowner took on much of the monetary liability.

A dispersion is a system in which distributed particles of one material are dispersed in a continuous phase of another material. The two phases may be in the same or different states of matter.

<span class="mw-page-title-main">Brine pool</span> Large area of brine on the ocean basin

A brine pool, sometimes called an underwater lake, deepwater or brine lake, is a volume of brine collected in a seafloor depression. The pools are dense bodies of water that have a salinity that is three to eight times greater than the surrounding ocean. Brine pools are commonly found below polar sea ice and in the deep ocean. Those below sea ice form through a process called brine rejection. For deep-sea brine pools, salt is necessary to increase the salinity gradient. The salt can come from one of two processes: the dissolution of large salt deposits through salt tectonics or geothermally heated brine issued from tectonic spreading centers.

Green nails may be (1) due to a Pseudomonas aeruginosa infection causing a green nail syndrome or (2) the result of copper in tap water.

<span class="mw-page-title-main">Coal Oil Point seep field</span> Marine petroleum seep area near Goleta, California

The Coal Oil Point seep field (COP) in the Santa Barbara Channel offshore from Goleta, California, is a marine petroleum seep area of about three square kilometres, within the Offshore South Ellwood Oil Field and stretching from the coastline southward more than three kilometers (1.9 mi). Major seeps are located in water depths from 20 to 80 meters. The seep field is among the largest and best studied areas of active marine seepage in the world. These perennial and continuous oil and gas seeps have been active on the northern edge of the Santa Barbara Channel for at least 500,000 years. The combined seeps in the field release about 40 tons of methane per day and about 19 tons of reactive organic gas ; about twice the hydrocarbon air pollution released by all the cars and trucks in Santa Barbara County in 1990. The liquid petroleum produces a slick that is many kilometres long and when degraded by evaporation and weathering, produces tar balls which wash up on the beaches for miles around.

Marine mucilage, also referenced as sea snot or sea saliva, is thick, gelatinous organic matter found around the world's oceans, lately observed in the Mediterranean Sea.

<span class="mw-page-title-main">Boom (containment)</span> Temporary floating barrier used to contain an oil spill

A containment boom is a temporary floating barrier used to contain an oil spill. Booms are used to reduce the possibility of polluting shorelines and other resources, and to help make recovery easier. Booms help to concentrate oil in thicker surface layers so that skimmers, vacuums, or other collection methods can be used more effectively. They come in many shapes and sizes, with various levels of effectiveness in different types of water conditions.

Alcanivorax borkumensis is an alkane-degrading marine bacterium which naturally propagates and becomes predominant in crude-oil-containing seawater when nitrogen and phosphorus nutrients are supplemented.

Environmental impact of the <i>Deepwater Horizon</i> oil spill

The 2010 Deepwater Horizon oil spill in the Gulf of Mexico has been described as the worst environmental disaster in the United States, releasing about 4.9 million barrels of crude oil making it the largest marine oil spill. Both the spill and the cleanup efforts had effects on the environment.

Petroleum microbiology is a branch of microbiology that deals with the study of microorganisms that can metabolize or alter crude or refined petroleum products. These microorganisms, also called hydrocarbonoclastic microorganisms, can degrade hydrocarbons and, include a wide distribution of bacteria, methanogenic archaea, and some fungi. Not all hydrocarbonoclasic microbes depend on hydrocarbons to survive, but instead may use petroleum products as alternative carbon and energy sources. Interest in this field is growing due to the increasing use of bioremediation of oil spills.

Bioremediation of petroleum contaminated environments is a process in which the biological pathways within microorganisms or plants are used to degrade or sequester toxic hydrocarbons, heavy metals, and other volatile organic compounds found within fossil fuels. Oil spills happen frequently at varying degrees along with all aspects of the petroleum supply chain, presenting a complex array of issues for both environmental and public health. While traditional cleanup methods such as chemical or manual containment and removal often result in rapid results, bioremediation is less labor-intensive, expensive, and averts chemical or mechanical damage. The efficiency and effectiveness of bioremediation efforts are based on maintaining ideal conditions, such as pH, RED-OX potential, temperature, moisture, oxygen abundance, nutrient availability, soil composition, and pollutant structure, for the desired organism or biological pathway to facilitate reactions. Three main types of bioremediation used for petroleum spills include microbial remediation, phytoremediation, and mycoremediation. Bioremediation has been implemented in various notable oil spills including the 1989 Exxon Valdez incident where the application of fertilizer on affected shoreline increased rates of biodegradation.

Hydrocarbonoclastic bacteria are a heterogeneous group of prokaryotes which can degrade and utilize hydrocarbon compounds as source of carbon and energy. Despite being present in most of environments around the world, several of these specialized bacteria live in the sea and have been isolated from polluted seawater.

References

  1. 1 2 Itah, A. Y.; Essien, J. P. (October 2005). "Growth Profile and Hydrocarbonoclastic Potential of Microorganisms Isolated from Tarballs in the Bight of Bonny, Nigeria". World Journal of Microbiology and Biotechnology. 21 (6–7): 1317–1322. doi:10.1007/s11274-004-6694-z.
  2. 1 2 Hostettler, Frances D.; Rosenbauer, Robert J.; Lorenson, Thomas D.; Dougherty, Jennifer (June 2004). "Geochemical characterization of tarballs on beaches along the California coast. Part I: Shallow seepage impacting the Santa Barbara Channel Islands, Santa Cruz, Santa Rosa, and San Miguel". Organic Geochemistry. 35 (6): 725–746. doi:10.1016/j.orggeochem.2004.01.022. ISSN   0146-6380.
  3. Lorenson, T. D.; Hostettler, F. D.; Rosenbauer, R. J.; Peters, K. E.; Kvenvolden, K. A.; Dougherty, J. A.; Gutmacher, C. E.; Wong, F. L.; Normark, W. R. (2009). "Natural offshore seepage and related tarball accumulation on the California coastline; Santa Barbara Channel and the southern Santa Maria Basin; source identification and inventory". usgs.gov. US Geological Survey. Retrieved 2010-06-03.
  4. Knap, Anthony H.; Burns, Kathryn A.; Dawson, Rodger; Ehrhardt, Manfred; Palmork, Karsten H. (July 1986). "Dissolved/dispersed hydrocarbons, tarballs and the surface microlayer: Experiences from an IOC/UNEP Workshop in Bermuda, December 1984". Marine Pollution Bulletin. 17 (7): 313–319. doi:10.1016/0025-326X(86)90217-1.
  5. Wang, Zhendi; Fingas, Merv; Landriault, Michael; Sigouin, Lise; Castle, Bill; Hostetter, David; Zhang, Dachung; Spencer, Brad (1998). "Identification and Linkage of Tarballs from the Coasts of Vancouver Island and Northern California Using GC/MS and Isotopic Techniques". Journal of High Resolution Chromatography. 21 (7): 383–395. doi:10.1002/(SICI)1521-4168(19980701)21:7<383::AID-JHRC383>3.0.CO;2-3.
  6. Goodman, R. (April 2003). "Tar Balls: The End State". Spill Science & Technology Bulletin. 8 (2): 117–121. doi:10.1016/S1353-2561(03)00045-8.
  7. Fang, J.; Wong, K. V. (January 2006). "An Advanced VOF Algorithm for Oil Boom Design". International Journal of Modelling and Simulation. 26 (1): 36–44. doi:10.1080/02286203.2006.11442349.
  8. Fang, J.; Wong, K. V. (April 2003). "An Advanced VOF Algorithm for Oil Boom Design". International Journal of Modelling and Simulation. 8 (2): 117–121.

Further reading