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Quantum Leaps in CO 2 Detection Robert Byrne, Ph.D. USF chemical oceanographers are making quantum leaps in measuring carbon dioxide (CO 2 ) in the oceans and measuring the interactions of CO 2 between the water and the atmosphere. Such measurements are very important because of the rising amount of CO 2 absorbed by the world‘s oceans. This increase in CO 2 has a pro- found effect on all humanity in that these more acidic conditions are seriously threatening basic life forms - forms that are essential links in the ecological food chain. Our instruments allow determinations of the concentra- tions of biologically important nutrients and trace metals. They also allow determinations of important characteris- tics of the marine CO 2 system. Measurements with our systems allow descriptions of the potential for growth of organisms in seawater, the capacity of seawater for CO 2 uptake from the atmosphere and, in general, observations of human-induced perturbations of natural systems. All of our instruments can operate at depths up to 1,000 meters (soon to be expanded to 6,000 meters) - this capability is decidedly unique. We can deploy these instruments in a variety of ways; i.e., in-situ, on shipboard, buoys, autonomous underwater vehicles (AUVs), remotely-operated vehicles (ROVs), etc. Our in-situ instruments are designed to measure a very wide variety of chemicals in seawater. Each in-situ instrument measures a single type of chemi- cal. Our in-situ instruments are unique with respect to optical cell design. The light path in our optical cells is on the order of one to two meters. Other systems have path lengths that are shorter by one to two orders of magnitude. This lon- ger path length means we can observe concentrations that are at least ten times lower than can be observed with other systems. Our systems are versatile. Any single instrument can be used for a wide variety of types of chemical measure- ments. Our instruments can (uniquely) measure chemicals by observing either light attenuation, as described above, or fluorescence, in which case light of one color impinges on a sample, and re-emitted light (having a different color) is observed for quantification of concentrations.

QuantumLeapsinCO2 Detection RobertByrne,Ph.D. · 2005-12-07 · QuantumLeapsinCO2Detection RobertByrne,Ph.D. WhendeployedonshipboardourshipboardinstrumentationmeasuresmanyCO2 systemparameterssimultaneously.Forexample

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Page 1: QuantumLeapsinCO2 Detection RobertByrne,Ph.D. · 2005-12-07 · QuantumLeapsinCO2Detection RobertByrne,Ph.D. WhendeployedonshipboardourshipboardinstrumentationmeasuresmanyCO2 systemparameterssimultaneously.Forexample

Quantum Leaps in CO2 DetectionRobert Byrne, Ph.D.

USF chemical oceanographers are making quantum leaps in measuring carbondioxide (CO2) in the oceans and measuring the interactions of CO2 between the

water and the atmosphere. Such measurements are veryimportant because of the rising amount of CO2 absorbedby the world‘s oceans. This increase in CO2 has a pro-found effect on all humanity in that these more acidicconditions are seriously threatening basic life forms -forms that are essential links in the ecological food chain.

Our instruments allow determinations of the concentra-tions of biologically important nutrients and trace metals.They also allow determinations of important characteris-tics of the marine CO2 system. Measurements with our

systems allow descriptions of the potential for growth of organisms in seawater,the capacity of seawater for CO2 uptake from the atmosphere and, in general,observations of human-induced perturbations of natural systems. All of ourinstruments can operate at depths up to 1,000 meters (soon to be expanded to6,000 meters) - this capability is decidedly unique.

We can deploy these instruments in a variety of ways; i.e., in-situ, on shipboard,buoys, autonomous underwater vehicles (AUVs), remotely-operated vehicles(ROVs), etc. Our in-situ instruments are designed to measure a very wide varietyof chemicals in seawater. Each in-situ instrument measures a single type of chemi-cal. Our in-situ instruments are unique with respect to optical cell design. Thelight path in our optical cells is on the order of one to two meters. Other systemshave path lengths that are shorter by one to two orders of magnitude. This lon-ger path length means we can observe concentrations that are at least ten timeslower than can be observed with other systems. Our systems are versatile. Anysingle instrument can be used for a wide variety of types of chemical measure-ments. Our instruments can (uniquely) measure chemicals by observing eitherlight attenuation, as described above, or fluorescence, in which case light of onecolor impinges on a sample, and re-emitted light (having a different color) isobserved for quantification of concentrations.

Page 2: QuantumLeapsinCO2 Detection RobertByrne,Ph.D. · 2005-12-07 · QuantumLeapsinCO2Detection RobertByrne,Ph.D. WhendeployedonshipboardourshipboardinstrumentationmeasuresmanyCO2 systemparameterssimultaneously.Forexample

Quantum Leaps in CO2 DetectionRobert Byrne, Ph.D.

When deployed on shipboard our shipboard instrumentation measures many CO2system parameters simultaneously. For example, we have the unique capacity tosimultaneously measure pH (solution acidity), total dissolved inorganic carbon(DIC) and a parameter, called the CO2 fugacity, which depicts the tendency forCO2 to escape into the atmosphere. We also are able to measure the concentra-tion of CO2 in the atmosphere.

The capabilities provided by these instruments are much sought after for robustglobal observations of the response of the oceans to rising atmospheric CO2.