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Autonomous buoy for seismic reflection data acquisition in the inaccessible parts of the Arctic Ocean Y. Kristoffersen, O. Meyer, Dept. Earth Science, Univ. of Bergen, Norway D. Peddie CMR Instrumentation, Bergen, Norway An autonomous buoy which collects seismic reflection data and transmits to shore in real time via the Iridium satellite system: - GPS triggers a shot every 50 meter; - records 8 sec. data and stores on disc; - detects water bottom in the data and extracts the subsequent 1 sec of data; - transmits to Bergen via Iridium as 2 kB short burst (SBM) messages. The challenge The concept A large area of the Arctic Ocean is not accessible to icebreakers and marine surveys using towed equipment. 4.6 kJ sparker & electronics battery solar panels Field tests Results Deployment on the ice north of Svalbard Test locations of the seismic buoy (thick red, green and black lines). - we have successfully developed an autonomous buoy for acquisition of single channel seismic reflection data from drifting sea ice in the Arctic Ocean and real-time data transmission to shore via Iridium. - we have two-way data communication where buoy operation, acquisition and data transmission parameters can be set from shore. - the buoy data show 400-700 meter seismic sub-bottom penetration using a 4.6 kJoule sparker source and recording with a single hydrophone. Remaining challenges - power supplied by batteries charged by solar panels and wind mill has proven insufficient for stable operation; - this problem will be remedied by use of a fuel cell (90 W) which runs on ethanol (~1.5 liter/day). Plans - deployment July-August 2010 on Yermak Plateau north of Svalbard (82º N); - delopyment in 2011 on the Lomonosov Ridge, central Arctic Ocean. seismic line from databuoy seismic line by research vessel Acknowledgement This research was funded as part of the Norwegian contribution to IPY.

Autonomous buoy for seismic reflection data acquisition in ... · - records 8 sec. data and stores on disc; - detects water bottom in the data and extracts the subsequent 1 sec of

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Page 1: Autonomous buoy for seismic reflection data acquisition in ... · - records 8 sec. data and stores on disc; - detects water bottom in the data and extracts the subsequent 1 sec of

Autonomous buoy for seismic reflection data acquisi tion in the inaccessible parts of the Arctic Ocean

Y. Kristoffersen, O. Meyer, Dept. Earth Science, Un iv. of Bergen, NorwayD. Peddie CMR Instrumentation, Bergen, Norway

An autonomous buoy which collects seismicreflection data and transmits to shore in real time via the Iridium satellite system:

- GPS triggers a shot every 50 meter;- records 8 sec. data and stores on disc;- detects water bottom in the data and

extracts the subsequent 1 sec of data;- transmits to Bergen via Iridium as 2 kB

short burst (SBM) messages.

The challenge

The concept

A large area of the Arctic Ocean is not accessible to icebreakers and marine surveys using towed equipment.

4.6 kJ sparker & electronics

battery

solar panels

Field testsResults

Deployment on the ice north of Svalbard Test locations of theseismic buoy (thick red, green and black lines).

- we have successfully developed an autonomous buoy for acquisition of single channel seismic reflection data from drifting sea ice in the Arctic Ocean and real-timedata transmission to shore via Iridium.

- we have two-way data communicationwhere buoy operation, acquisition and datatransmission parameters can be set fromshore.

- the buoy data show 400-700 meter seismicsub-bottom penetration using a 4.6 kJoulesparker source and recording with a singlehydrophone.

Remaining challenges- power supplied by batteries charged by

solar panels and wind mill has proveninsufficient for stable operation;

- this problem will be remedied by use of a fuel cell (90 W) which runs on ethanol(~1.5 liter/day).

Plans- deployment July-August 2010 on Yermak

Plateau north of Svalbard (82º N);

- delopyment in 2011 on the Lomonosov Ridge,central Arctic Ocean.

seismic line from databuoy

seismic line by research vessel

AcknowledgementThis research was funded as part of the Norwegian contribution to IPY.