Bathycache- The Truth is in the Ground

Example of a high-resolution side-scan sonar mosaic created from survey data collected by the GeoSwath sonar on the Gavia AUV.

Example of a high-resolution side-scan sonar mosaic created from survey data collected by the GeoSwath sonar on the Gavia AUV. The image results from the measurement of high-frequency (500 kHz) short bursts of sound waves that bounce off of the seabed and return to the sonar unit. Bright areas indicate high return energy associated with coral fragments or scattered rocks while dark patches represent shadow zones (areas where the sound was blocked) or patches of soft sand and/or mud that absorb more sound than rocks or corals. In this image the beach is towards the right and each grid cell is a 10 m x 10 m square. The total swath width (lateral distance from edge to edge) is 40 m and the line length from tip to tip is approximately 100 m. Click image for larger view and image credit.


Scientists look for patterns of the oxygen concentrations over the reef, which provides an indicator of the health and productivity of the coral system.

Despite what it looks like Chris is not trying to become an underwater plumber, rather he is getting quite a work out assisting Daniel in conducting oxygen profiles within the bottom boundary layer above the reef. This “Christmas Tree” device consists of PVC pipes; pipe is placed at a planned and measured elevation with narrow spacing towards the bottom and increased spacing moving upward following a logarithmic scale. Divers gently lay this device on the seafloor and use an oxygen sensor to gather a time-series of oxygen measurements at each elevation. Once the data is plotted, the scientists look for patterns of the oxygen concentrations over the reef, which provides an indicator of the health and productivity of the coral system. Click image for larger view and image credit.


January 17, 2008

Arthur Trembanis
Expedition Co-Principal Investigator
Assistant Professor, University of Delaware
AUV Operations and Marine Geologist

In addition to the shape of the seafloor, we also gather information from the AUVs about the nature of the composition of the bottom, e.g. whether it is sandy or coral covered. To do this, we use a technology called side-scan sonar resulting in images like that seen in the following image. This shows the intensity of the sound that bounces off the seafloor and back to the robots. Imagine what your living room would look like at night illuminated only by the light and shadow of a flashlight and you will begin to get a sense of what kinds of images side-scan sonar is providing. Light areas indicate hard acoustic returns such as what you would expect from a large brain coral while darker areas indicate shadow or zone with more subdued topography or possibly fine sand. Notice that I said rather ambiguously what might be causing the light and dark patches. The reason is that there are many combinations that can make similar patterns, and it is only through careful ground-truthing (that is taking close up visual or physical samples) that scientists are able to differentiate one bottom type from another. The task of ground-truthing is strenuous, repetitive, and thankless work but critical to habitat mapping such as we are doing here in Bonaire. Many students came to our aid recently to help us conduct sonar groundtruthing here at the science compound by swimming out to document various acoustic targets on the seafloor and noting the kind of bottom-type and marine organisms associated with the feature(s).

We have managed to conduct seafloor-mapping surveys in six separate locations acquiring many tens of square kilometers of seafloor mapping data in addition to water column data regarding the conditions within the water (salinity, temperature, oxygen levels, etc).

AUV operations especially on windy islands such as Bonaire are not without their challenges. Sometimes we have to call on various support equipment to help us locate the robots amidst the choppy surface waves. One such instrument we use is called and acoustic pinger and in the following image Bernard is demonstrating its use. The operator wears a set of headphones like you might use for listening to an MP3 player while the other end is composed of a hydrophone, essentially a microphone for picking up underwater sounds. By changing the orientation of the hydrophone “bell” the operator can get a sense of the direction from which the sound is coming from. The intensity, or loudness, of the sound is an indicator of the distance that the hydrophone is from the sound source. Each robot luckily has its very own distinctive sound pattern thus allowing us to tell each robot apart even if they are many hundreds of meters away underwater.

Bernard demonstrating the use of the acoustic pinger.

Bernard demonstrating the use of the acoustic pinger. Click image for larger view and image credit.


 

After a few showers, a brilliant rainbow emerges.

After a few showers, a brilliant rainbow emerges. Click image for larger view and image credit.


At the end of the day though the reward is to recover the robot and then enjoy a break in the clouds and showers to watch a brilliant rainbow emerge.

Next up
Jan 18- Exploring the Marine Reserve. 3 AUVs and a whole mess of divers make for lots of data collection. Unprecedented access to the marine reserve where diving of any kind has been off limits for as long as anyone can remember. First ever swath bathymetry, side-scan, and camera maps of the reserve.

 

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