Under the microscope #13March 2nd, 2012 in Biology / Other
Matthew Kuo tells us how tiny worm faecal pellets affect how oil pipelines sit on the seabed.
Matthew Kuo: I have a research interest in the geotechnical behavior and biological origin of deep ocean clay crusts. These crusts are found in many areas that are of particular importance to offshore oil and gas developments, including the Gulf of Guinea, Gulf of Mexico and the Mediterranean Sea. I have discovered that sediments from these areas contain millions of tiny faecal pellets that have been produced by burrowing invertebrates (worms).
These pellets, whose abundance in the sediment may range from 30% to 60% by dry mass, are robust and much stronger than undigested material. Their presence and mechanical behavior can therefore explain the existence of the observed crusts. This video shows several pellets that have partially degraded over time adjacent to microfossils. I have discovered that when hot-oil pipelines are laid onto these pelletised sediments, the rough pipeline coatings cause the pellets to disintegrate. This in turn causes a reduction in friction between the pipeline and the seabed. I am therefore investigating how we can better understand this complicated soil-pipeline interaction. This research will help predict longer-term hot-oil pipeline behaviour, leading to safer and more economical designs.
The pellets shown in this image are about 50 micrometers in diameter. This is about the same diameter as a human hair.
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Provided by University of Cambridge
"Under the microscope #13." March 2nd, 2012. http://phys.org/news/2012-03-microscope.html