"

10 Introducing Piston Coring

two men hanging over the side of a ship on the ocean setting up sampling equipment
Dick Edwards (top) and Maurice Ewing hoisting a piston corer off R/V Atlantis (circa 1949). © Woods Hole Oceanographic Institution, D. Fay. Used with permission.

 

Cores extracted from the sea are especially useful because, unlike land sediments, they are largely undisturbed. No one has unsettled them by digging or walking on them. By studying undisturbed ocean sediment, scientists obtain the clearest picture of specific time periods on Earth. The also learn more about Earth’s interacting systems so that they can predict patterns and forecast events in the future. Piston coring allows for the extraction of long, intact ocean sediment samples, making it an essential tool for scientific ocean drilling.

Piston Coring is similar to Coring an Apple

The piston corer is a long, heavy tube plunged into the seafloor to extract samples of soft sediment. Inside the tube, a piston creates suction, helping to retrieve undisturbed samples that can reach impressive lengths—over 27 meters (90 feet).  In 1947, Maurice Ewing, founder of the Lamont Geological Institute (now the Lamont-Doherty Earth Observatory), famously compared piston coring to coring an apple—simple yet highly effective. The key advantage lies in the piston, which helps draw up soft sediment that would otherwise be lost.

Piston Coring Improves Sample Collection

All corers share the same fundamental goal: extracting samples of seafloor sediment. Maurice Ewing also once compared corers to cookie cutters, with the size and shape of the “mud cookies” depending on the type of corer used. Traditional corers have  a long, weighted tube that relies on gravity to drive it into the seafloor. However, this free-falling method can disturb the sediment layers, compromising the quality of the sample. Cores with rotary blades can also disrupt sediment. The photo below contrasts the sediment retrieved by both methods. Note the fine undisturbed sediment from piston coring.

Dark sediment layers in two columns. The left one is bumpy and the right one is smooth with visible fine layers.
A comparison of disrupted sediment from rotary coring on the left and piston coring, on the right (Credit: Advanced Piston Corer. IODP).

In the late 1940s, Swedish oceanographer Börje Kullenberg refined this design by introducing an internal piston. As soon as the weighted coring tube makes contact with the sediment the piston mechanism activates.  The piston is held in place by a cable as the tube is forcefully driven into the sediment.  This difference in movement creates a vacuum effect inside the tube, which helps pull sediment in and reduces disturbance.

If you hve ever inserted a straw into a beverage, covered the top with your finger, and lifted it out with the liquid trapped inside, you can visualize how the piston corer works. The piston is like your thumb, covering the top of the tube to create the vacuum. Like a straw, the corer penetrates the seafloor and captures sediment within its hollow tube.

Unlike standard gravity corers, piston corers allow scientists to retrieve longer, more intact samples from soft seafloor materials, preserving a clearer record of Earth’s geological and environmental history. This diagram  and the animation below, show the steps in the piston coring method.

Piston Coring Sequence: 1) The piston corer is lowered from the ship on a cable. 2) The triggered weight corer hits the seafloor and
How Piston Coring Works: A view from the seafloor. The piston, shown in blue is stationary and the corer tu descends around it.  (Credit: Used with permission of Nichole Anest/Lamont-Dougherty Earth Observatory)

A black and white photo of a ship with sails in full view.
The Albatross, a Swedish research vessel first used the piston corer and was able to core farther into sediment than ever before (Credit: Wikimedia Commons). 

Piston Coring advances Paleoceanography

The  Kullenberg piston corer, now referred to as the piston corer was first used on a worldwide cruise of the Swedish research vessel Albatross from 1947 to 1948 (not to be confused with the United States’ steamer Albatross, mentioned in the last section). The sampling instruments previously used to retrieve sediments from the ocean floor had only managed to go down about two meters into the sediments, i.e. a few thousand years.  With the help of the piston corer, the Swedish researchers managed to retrieve sediment cores as long as 20 meters, which made for an additional two million years.

The long sediment cores collected during the Albatross expedition bolstered the field of paleoceanography—the study of Earth’s ocean history through the study of ocean sediments. Thanks to the markedly longer cores obtained with the piston corer scientists could trace past climate and oceanic changes in the thick sediment layers.  In fact, one of the discoveries from this expedition was that the last two million years have experienced more ice ages than previously thought. Paleoceanography has expanded into several specialized disciplines, including marine micropaleontology, physical paleoceanography, and palaeoclimatology.

Refinements to the original Kullenberg model led to the development of the advanced piston corer (APC), which became an essential device on JOIDES Resolution. The Drilling at Sea chapter provides further details on the APC and its significance.

References

University of Gothenburg, Department of Marine Sciences. (2023, April 21). The Swedish Albatross Expedition provided invaluable knowledge about the sea.

License

Icon for the Creative Commons Attribution-NonCommercial-ShareAlike 4.0 International License

Scientific Ocean Drilling: Exploration and Discovery through Time Copyright © 2024 by Laura Guertin; Elizabeth Doyle; and Tessa Peixoto is licensed under a Creative Commons Attribution-NonCommercial-ShareAlike 4.0 International License, except where otherwise noted.