A direct CO2 control system for ocean acidification experiments: testing effects on the coralline red algae Phymatolithon lusitanicum

Most ocean acidification (OA) experimental systems rely on pH as an indirect way to control CO2. However, accurate pH measurements are difficult to obtain and shifts in temperature and/or salinity alter the relationship between pH and pCO(2). Here we describe a system in which the target pCO(2) is c...

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Published in:PeerJ
Main Authors: Sordo, L., Santos, Rui, Reis, João, Shulika, Alona, Silva, João
Format: Article in Journal/Newspaper
Language:English
Published: 2016
Subjects:
Online Access:http://hdl.handle.net/10400.1/9287
https://doi.org/10.7717/peerj.2503
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spelling ftunivalgarve:oai:sapientia.ualg.pt:10400.1/9287 2023-05-15T17:50:38+02:00 A direct CO2 control system for ocean acidification experiments: testing effects on the coralline red algae Phymatolithon lusitanicum Sordo, L. Santos, Rui Reis, João Shulika, Alona Silva, João 2016-09 http://hdl.handle.net/10400.1/9287 https://doi.org/10.7717/peerj.2503 eng eng info:eu-repo/grantAgreement/FCT/3599-PPCDT/115789/PT info:eu-repo/grantAgreement/FCT/SFRH/SFRH%2FBD%2F76762%2F2011/PT WOS:000384148600007 2167-8359 http://hdl.handle.net/10400.1/9287 doi:10.7717/peerj.2503 openAccess article 2016 ftunivalgarve https://doi.org/10.7717/peerj.2503 2022-05-30T08:47:32Z Most ocean acidification (OA) experimental systems rely on pH as an indirect way to control CO2. However, accurate pH measurements are difficult to obtain and shifts in temperature and/or salinity alter the relationship between pH and pCO(2). Here we describe a system in which the target pCO(2) is controlled via direct analysis of pCO(2) in seawater. This direct type of control accommodates potential temperature and salinity shifts, as the target variable is directly measured instead of being estimated. Water in a header tank is permanently re-circulated through an air-water equilibrator. The equilibrated air is then routed to an infrared gas analyzer (IRGA) that measures pCO(2) and conveys this value to a Proportional-Integral-Derivative (PID) controller. The controller commands a solenoid valve that opens and closes the CO2 flush that is bubbled into the header tank. This low-cost control system allows the maintenance of stabilized levels of pCO(2) for extended periods of time ensuring accurate experimental conditions. This system was used to study the long term effect of OA on the coralline red algae Phymatolithon lusitanicum. We found that after 11 months of high CO2 exposure, photosynthesis increased with CO2 as opposed to respiration, which was positively affected by temperature. Results showed that this system is adequate to run long-term OA experiments and can be easily adapted to test other relevant variables simultaneously with CO2, such as temperature, irradiance and nutrients. Article in Journal/Newspaper Ocean acidification Universidade do Algarve: Sapienta PeerJ 4 e2503
institution Open Polar
collection Universidade do Algarve: Sapienta
op_collection_id ftunivalgarve
language English
description Most ocean acidification (OA) experimental systems rely on pH as an indirect way to control CO2. However, accurate pH measurements are difficult to obtain and shifts in temperature and/or salinity alter the relationship between pH and pCO(2). Here we describe a system in which the target pCO(2) is controlled via direct analysis of pCO(2) in seawater. This direct type of control accommodates potential temperature and salinity shifts, as the target variable is directly measured instead of being estimated. Water in a header tank is permanently re-circulated through an air-water equilibrator. The equilibrated air is then routed to an infrared gas analyzer (IRGA) that measures pCO(2) and conveys this value to a Proportional-Integral-Derivative (PID) controller. The controller commands a solenoid valve that opens and closes the CO2 flush that is bubbled into the header tank. This low-cost control system allows the maintenance of stabilized levels of pCO(2) for extended periods of time ensuring accurate experimental conditions. This system was used to study the long term effect of OA on the coralline red algae Phymatolithon lusitanicum. We found that after 11 months of high CO2 exposure, photosynthesis increased with CO2 as opposed to respiration, which was positively affected by temperature. Results showed that this system is adequate to run long-term OA experiments and can be easily adapted to test other relevant variables simultaneously with CO2, such as temperature, irradiance and nutrients.
format Article in Journal/Newspaper
author Sordo, L.
Santos, Rui
Reis, João
Shulika, Alona
Silva, João
spellingShingle Sordo, L.
Santos, Rui
Reis, João
Shulika, Alona
Silva, João
A direct CO2 control system for ocean acidification experiments: testing effects on the coralline red algae Phymatolithon lusitanicum
author_facet Sordo, L.
Santos, Rui
Reis, João
Shulika, Alona
Silva, João
author_sort Sordo, L.
title A direct CO2 control system for ocean acidification experiments: testing effects on the coralline red algae Phymatolithon lusitanicum
title_short A direct CO2 control system for ocean acidification experiments: testing effects on the coralline red algae Phymatolithon lusitanicum
title_full A direct CO2 control system for ocean acidification experiments: testing effects on the coralline red algae Phymatolithon lusitanicum
title_fullStr A direct CO2 control system for ocean acidification experiments: testing effects on the coralline red algae Phymatolithon lusitanicum
title_full_unstemmed A direct CO2 control system for ocean acidification experiments: testing effects on the coralline red algae Phymatolithon lusitanicum
title_sort direct co2 control system for ocean acidification experiments: testing effects on the coralline red algae phymatolithon lusitanicum
publishDate 2016
url http://hdl.handle.net/10400.1/9287
https://doi.org/10.7717/peerj.2503
genre Ocean acidification
genre_facet Ocean acidification
op_relation info:eu-repo/grantAgreement/FCT/3599-PPCDT/115789/PT
info:eu-repo/grantAgreement/FCT/SFRH/SFRH%2FBD%2F76762%2F2011/PT
WOS:000384148600007
2167-8359
http://hdl.handle.net/10400.1/9287
doi:10.7717/peerj.2503
op_rights openAccess
op_doi https://doi.org/10.7717/peerj.2503
container_title PeerJ
container_volume 4
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