
NSF Org: |
OCE Division Of Ocean Sciences |
Recipient: |
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Initial Amendment Date: | July 9, 2010 |
Latest Amendment Date: | February 5, 2016 |
Award Number: | 0964888 |
Award Instrument: | Standard Grant |
Program Manager: |
Kandace Binkley
kbinkley@nsf.gov (703)292-7577 OCE Division Of Ocean Sciences GEO Directorate for Geosciences |
Start Date: | July 15, 2010 |
End Date: | February 28, 2017 (Estimated) |
Total Intended Award Amount: | $1,165,324.00 |
Total Awarded Amount to Date: | $1,340,324.00 |
Funds Obligated to Date: |
FY 2013 = $75,000.00 FY 2015 = $100,000.00 |
History of Investigator: |
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Recipient Sponsored Research Office: |
1608 4TH ST STE 201 BERKELEY CA US 94710-1749 (510)643-3891 |
Sponsor Congressional District: |
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Primary Place of Performance: |
1608 4TH ST STE 201 BERKELEY CA US 94710-1749 |
Primary Place of
Performance Congressional District: |
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Unique Entity Identifier (UEI): |
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Parent UEI: |
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NSF Program(s): | OCEAN TECH & INTERDISC COORDIN |
Primary Program Source: |
01001314DB NSF RESEARCH & RELATED ACTIVIT 01001516DB NSF RESEARCH & RELATED ACTIVIT |
Program Reference Code(s): |
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Program Element Code(s): |
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Award Agency Code: | 4900 |
Fund Agency Code: | 4900 |
Assistance Listing Number(s): | 47.050 |
ABSTRACT
The PI's request funding to complete the development of Particulate Inorganic Carbon (PIC) sensors to create an integrated system for autonomous profiling of a suite of parameters that characterize the ocean's biological pump. The proposed system will measure PIC, Particulate Organic Carbon (POC) and a measure of the Carbon Flux Index (CFI) chlorophyll fluorescence, conductivity and temperature, and likely other parameters. This suite of sensors will characterize the ocean's biological pump, as well as its sensitivity to changing environmental conditions. It is being designed for over-the-side CTD packages as well as autonomous, neutrally buoyant floats and gliders.
The ocean's biotic carbon pump exports approximately 10 Pg C/year of particulate organic matter below 100 m. It is fueled by phytoplankton populations, which turn over completely on week time scales. The bio-carbon pump is thus fast and very dynamic, but is poorly observed by conventional means. The changes in its substantial carbon flows brought by effects of CO2 induced global ocean warming and ocean acidification, are not predictable. Better observations of key biological pump variables, including concentration variability of Particulate Inorganic Carbon and Particulate Organic Carbon (PIC and POC) will enable prediction of the evolving carbon cycle of the ocean. Knowledge of the PIC dynamics is fundamental to the understanding and prediction of carbon sedimentation and depth profiles of remineralization.
Broader Impacts:
The broader impacts of this work are clear in its fostering of a better understanding of the ocean carbon cycle. This is critical to track the role of the oceans in the fate of anthropogenic CO2. To be able to easily and autonomously measure profiles of PIC would provide a wealth of badly needed data for remarkably little cost, shiptime, and effort. It would also compliment the work currently being done to image the particles that exist in the deep sea. The PI instructs a large number of undergraduate and graduate students and will involve them in the results of these tests. The project involves an undergraduate assisting in laboratory testing and at sea field trials.
PUBLICATIONS PRODUCED AS A RESULT OF THIS RESEARCH
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PROJECT OUTCOMES REPORT
Disclaimer
This Project Outcomes Report for the General Public is displayed verbatim as submitted by the Principal Investigator (PI) for this award. Any opinions, findings, and conclusions or recommendations expressed in this Report are those of the PI and do not necessarily reflect the views of the National Science Foundation; NSF has not approved or endorsed its content.
The ocean's biological carbon pump plays a major role in the global carbon cycle. Particulate carbon pools in the ocean turnover on weekly time scales making it difficult to observe them from ships. Better observations of key biological pump variables, including the concentration variability of Particulate Inorganic Carbon and Particulate Organic Carbon (PIC and POC) will enable prediction of the evolving carbon cycle of the ocean.
UC Berkeley, WETLabs Inc., Scripps Instrument Development Group, and Lawrence Berkeley National Laboratory worked to transition an advanced low-power full ocean profiling prototype sensor for particulate inorganic carbon (PIC) to robust ‘commercial quality’ forms. The group also perfected methodology for optical sensing of POC using commercial transmissometers. Sensors were demonstrated by deployment on ship-lowered instrument packages and on autonomous ocean profiling floats.
The new PIC sensor operates by detecting birefringent calcium carbonate particles in a transmissometer beam. It does this using laser light, a polarizer aligned with the laser, a 25 cm water path and a polarizer aligned to block the laser light (Figure 1). When calcium carbonate particles are present in the water path of the instrument, the laser light is depolarized and photons pass to the detector.
Project members engaged in a series of short oceanographic expeditions from 2010-2013 to incrementally test candidate instrument designs. In 2012, a first design utilizing open cells was successful; In 2013, the project achieved a major mile stone... three new PIC sensors yielded identical profiles during profiling to 2000 meters (Figure 2). This led to the deployment of two of the PIC sensors on Berkeley's robotic ocean profiling Carbon Explorer floats in 2013 (Figure 3). For the first time, data on calcium carbonate particle concentrations in the ocean watercolumn were relayed via satellite in real time from the remote ocean by the Carbon Explorers as they yo-yoed from 1000 m depths to the surface and back on a daily basis. The project discovered long term issues during the 100 day long CE deployments. Sensors were refined and tested at sea to depths of 4000 m in August 2016.
The calibration of the sensors has been carried out to sea utilizing particle samples from filtering 1 liter seawater samples and from 1000 liter volumes of seawater processed by large volume in-situ filtration pumps. The process of calibration is ongoing; however we have been able to demonstrate that the primary signal seen by the sensor is proportional to calcium carbonate particle concentrration in the water.
There have been two journal articles and 9 meeting presentations of project results.
The project has laid the basis for the commercialization of the PIC sensor and its availability to the international oceanographic community. Transmissometer products marketed by WETLabs, Inc. improved in their stability as a direct result of this project. Protocols for improved optical sensor accuracy have been communicated to and used by the oceanographic community.
This project provided hands-on research experience in the laboratory and at sea for UC Berkeley undergraduates. Since project inception 28 UC Berkeley undergraduates have participated in 8 expeditions (13F; 15M - including 4 Hispanic Americans (1F/3M); 4 Asian Americans (2F/2M); and 2 with disabilities (1F/1M); 12 (6F/6M) have been accepted to graduate schools in oceanography, chemistry, environmental law and engineering.
In Feb. 2013, we began a collaboration with the San Francisco Exploratorium to improve public outreach in the area of the science of the ocean’s carbon cycle. As an example of this outreach, one of our undergraduates, Jessica Kendall-Bar, lead a public presentation in the Exploratium series: "Everything Matters: Tales of the Periodic Table: Calcium", March 16 2017.
Last Modified: 05/30/2017
Modified by: James K Bishop
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