SubSeaFloor Observatories Installed To Run Dynamic Experiments
Sep 07, 2010
(News Release) VICTORIA – Scientists will study fluid flow, chemistry, and life off the BC coast. An international team of scientists has just returned from two months at sea near British Columbia, Canada, where they installed two observatories in the ocean floor to run innovative experiments at the bottom of the sea.
The Integrated Ocean Drilling Program (IODP) “Juan de Fuca Ridge-Flank Hydrogeology” Expedition left Victoria July 9 and returned Sept. 5. Using the scientific research vessel JOIDES Resolution, the team drilled boreholes nearly 530 metres deep (nearly 1,800 feet) into the ocean floor to install the observatories.
“The ocean crust is the largest aquifer on the planet. We know it’s made up of many sections, but we have no idea how these parts connect or how they interact with one another,” says co-chief scientist Dr. Andy Fisher of the University of California at Santa Cruz.
The observatories, known as “CORKs” (because they are used to seal boreholes), were installed 200 km (125 miles) west of Vancouver Island, Canada. Each CORK is packed with scientific instruments that collect samples and data at multiple depths to learn more about the water, pressures, temperatures, chemistry, and microbiology within the rocks and sediments of the ocean crust.
The CORKs are being used as part of a sampling and monitoring network to allow scientists to determine the properties of the ocean crust, and to better understand how water, heat, and chemicals are transported across vast distances below the bottom of the ocean.
The volume of salt water in the ocean crust is comparable to the volume of fresh water in Earth’s ice caps and glaciers—about 20-30 million cubic kilometres. For comparison, this is about 2,000 times greater than the global fresh water supply, and about a half million times greater than annual fresh water usage in the US.
Like fresh water on land, the salt water below the seafloor is in motion, moving rapidly from place to place. Until now, scientists have never been able to “tag” water in one place below the seafloor and determine where it flows. Experiments begun during the IODP Juan de Fuca Ridge-Flank Hydrogeology Expedition will provide the first direct evidence of active flow pathways and rates in the ocean crust.
Researchers used the boreholes to run experiments during the expedition. In one experiment, they injected benign tracers into the ocean floor to track the directions, rates, and patterns of fluid flow within the seafloor.
In another experiment, microbiologists placed chips of rocks and minerals in the CORKs to identify microorganisms living in the seafloor. “It’s like lowering an empty hotel into the borehole,” explains co-chief scientist Takeshi Tsuji of Kyoto University, Japan.
“When the chips are recovered in a few years, we will learn who moved in.” Scientists estimate that a large fraction of life on Earth thrives in the “subsurface biosphere.” Once identified, the microorganisms from the CORKs will be matched to pressure and temperature data to determine the physical conditions that are most favourable to life at different depths.
Fisher and his team will recover CORK samples and data and run additional experiments next summer and in later years. “Through monitoring and experiments with CORKS, we will learn how microorganisms may have developed on Earth, which offers insight into how life may develop on other planets. We’ll also learn how carbon is transported and might be stored within deep reservoirs,” he says.
Three educators, an engineering student, a computer graphics animator, and an artist from the US and France joined the expedition to develop tools to share the expedition’s goals with non-academic audiences. The team created written, photographic, audio and visual logs of expedition activities, participated in video conferences with museums and schools, and wrote classroom activities and experiments for students on shore.