News Release

New generation of micro sensors for monitoring ocean acidification

Peer-Reviewed Publication

National Oceanography Centre, UK

Microfluidic Chip

image: The image shows the microfluidic chip used in the pH micro sensor. Dimensions: 13 x 8 cm. view more 

Credit: National Oceanography Centre

The first step in developing a cost-effective micro sensor for long-term monitoring of ocean acidification has been achieved by a team of scientists and engineers.

The new technology, that will measure pH levels in seawater, was developed by engineers from the National Oceanography Centre, in close collaboration with oceanographers from University of Southampton Ocean and Earth Science, which is based at the centre.

The team successfully tested the new device aboard the old RRS Discovery, and presented their results recently in the scientific journal Anaytica Chimica Acta. In its current form it can be used for on-board analysis of seawater samples, but the ultimate aim is to further develop the design so that it can be deployed for long periods of time in the ocean, taking in situ measurements.

Ocean acidification is occurring as a consequence of rising levels of atmospheric carbon dioxide (CO2), which is absorbed by the oceans. When it dissolves in seawater, CO2 forms a mild acid, which is decreasing ocean pH globally and could impact marine ecosystems. "We need to monitor seawater pH to a high level of precision and accuracy, and over long periods of time, in order to detect changes in the carbon system," says Dr Victoire Rérolle, lead author and researcher with NOC's Sensors group.

As well as monitoring global change, the sensors can be used to measure more localised human impact. The micro sensors could be deployed to detect leakages from carbon capture and storage sites – whereby CO2 is artificially removed from the atmosphere and stored in subsea reservoirs – by measuring any proximal fluctuations in pH. The oil industry is also interested in this technology for monitoring seawater acidity around drilling sites.

The sensor works on the same principles as litmus paper that many people may have used in chemistry lessons at school, whereby the colour changes depending on the acidity of the solution.

"The microfluidic chip within the sensor has great advantages because it is robust, small, reasonably cheap to produce, and uses small amounts of reagents – which is really key for in situ deployment where it may be collecting data out at sea for long periods of time.

"The sensor uses a dye which changes colour with pH. The dye is added to the sample, then the colour is measured using an LED light source and a device called a 'spectrometer'. The microfluidic element simply describes the component needed to mix the seawater sample with the dye and the cell to measure the colour."

The next stage is to develop an in situ system that can be deployed on ocean observing platforms, as has been done with other sensors measuring different chemical properties of seawater. "Now that we know that the bench top system works, we can use the technology from other systems to create in situ pH micro sensors," says Dr Rérolle. "This is what we are working on now, in collaboration with oceanographers based at NOC.

"By working with both engineers and scientists, you benefit from the insights of the developers and the end-user, resulting in a fit-for-purpose end product built to high specification."

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The development work was funded by SENSEnet, an EU Framework 7 project for the development of aquatic sensors, and the research expedition aboard the old RRS Discovery – which was in service until 2012 – was funded by the UK Ocean Acidification Research Programme.

Collaborating institutes were the National Oceanography Centre, University of Southampton Ocean and Earth Science, the Norwegian Institute for Water Research, the Uni Bjerknes Centre Norway and the University of Bergen.

Notes for editors

1. Reference: Rérolle VM, Floquet CF, Harris AJ, Mowlem MC, BAnalyticaellerby RR, Achterberg EP (2013) Development of a colorimetric microfluidic pH sensor for autonomous seawater measurements Chimica Acta, 786:124-31. doi: 10.1016/j.aca.2013.05.008

2. The image shows the microfluidic chip used in the pH micro sensor. Dimensions: 13 x 8 cm. Credit: National Oceanography Centre.

3. The study formed a University of Southampton Ocean and Earth Science PhD project, undertaken by Dr Rérolle before joining NOC's Sensors group.

4. The National Oceanography Centre (NOC) is the UK's leading institution for integrated coastal and deep ocean research. NOC operates the Royal Research Ships James Cook and Discovery and develops technology for coastal and deep ocean research. Working with its partners NOC provides long-term marine science capability including: sustained ocean observing, mapping and surveying, data management and scientific advice.

NOC operates at two sites, Southampton and Liverpool, with the headquarters based in Southampton.

Among the resources that NOC provides on behalf of the UK are the British Oceanographic Data Centre (BODC), the Marine Autonomous and Robotic Systems (MARS) facility, the National Tide and Sea Level Facility (NTSLF), the Permanent Service for Mean Sea Level (PSMSL) and British Ocean Sediment Core Research Facility (BOSCORF).

The National Oceanography Centre is wholly owned by the Natural Environment Research Council (NERC).

http://www.noc.ac.uk

5. University of Southampton School of Ocean and Earth Science is based at the National Oceanography Centre, Southampton.

http://www.southampton.ac.uk/oes

Contact details

Catherine Beswick, Communications and Public Engagement, National Oceanography Centre, catherine.beswick@noc.ac.uk, +44 238 059 8490

The National Oceanography Centre has an ISDN-enabled radio broadcast studio.


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