Development of the channelized optical system II for in situ, high-frequency measurements of dissolved inorganic carbon in seawater

dc.contributor.author Ringham, Mallory C.
dc.contributor.author Wang, Zhaohui Aleck
dc.contributor.author Sonnichsen, Frederick
dc.contributor.author Lerner, Steven A.
dc.contributor.author McDonald, Glenn
dc.contributor.author Pfeifer, Jonathan A.
dc.date.accessioned 2024-10-10T17:57:52Z
dc.date.available 2024-10-10T17:57:52Z
dc.date.issued 2024-03-25
dc.description © The Author(s), 2024. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Ringham, M., Wang, Z., Sonnichsen, F., Lerner, S., McDonald, G., & Pfeifer, J. (2024). Development of the channelized optical system II for in situ, high-frequency measurements of dissolved inorganic carbon in seawater. ACS ES&T Water, 4(4), 1775–1785, https://doi.org/10.1021/acsestwater.3c00787.
dc.description.abstract This study describes the development of the CHANnelized Optical System II (CHANOS II), an autonomous, in situ sensor capable of measuring seawater dissolved inorganic carbon (DIC) at high frequency (up to ∼1 Hz). In this sensor, CO2 from acidified seawater is dynamically equilibrated with a pH-sensitive indicator dye encapsulated in gas-permeable Teflon AF 2400 tubing. The pH in the CO2 equilibrated indicator is measured spectrophotometrically and can be quantitatively correlated to the sample DIC. Ground-truthed field data demonstrate the sensor’s capabilities in both time-series measurements and surface mapping in two coastal sites across tidal cycles. CHANOS II achieved an accuracy and precision of ±5.9 and ±5.5 μmol kg–1. The mean difference between traditional bottle and sensor measurements was −3.7 ± 10.0 (1σ) μmol kg–1. The sensor can perform calibration in situ using Certified Reference Materials (CRMs) to ensure measurement quality. The coastal time-series measurements highlight high-frequency variability and episodic biogeochemical shifts that are difficult to capture by traditional methods. Surface DIC mapping shows multiple endmembers in an estuary and highlights fine-scale spatial variabilities of DIC. The development of CHANOS II demonstrates a significant technological advance in seawater CO2 system sensing, which enables high-resolution, subsurface time-series, and profiling deployments.
dc.description.sponsorship This work was supported by the National Science Foundation (OCE 1233654, OCE-BSF 1635388 and OCE 1841092), the National Oceanic and Atmospheric Administration (NOAA) the Ocean Exploration Research Program (NA18OAR0110352), the NOAA Massachusetts Institute of Technology Sea Grant (2017-R/RCM-51, subaward #5710004253), and Woods Hole Oceanographic Institution Ocean Ventures Funds and Grassle Fellowship Funds.
dc.identifier.citation Ringham, M., Wang, Z., Sonnichsen, F., Lerner, S., McDonald, G., & Pfeifer, J. (2024). Development of the channelized optical system II for in situ, high-frequency measurements of dissolved inorganic carbon in seawater. ACS ES&T Water, 4(4), 1775–1785.
dc.identifier.doi 10.1021/acsestwater.3c00787
dc.identifier.uri https://hdl.handle.net/1912/70748
dc.publisher American Chemical Society
dc.relation.uri https://doi.org/10.1021/acsestwater.3c00787
dc.rights Attribution 4.0 International
dc.rights.uri https://creativecommons.org/licenses/by-nc-nd/4.0/
dc.subject Dissolved inorganic carbon
dc.subject Carbon dioxide
dc.subject Sensor
dc.subject In situ
dc.subject Ocean acidification
dc.subject Carbonate system
dc.subject Carbon cycle
dc.title Development of the channelized optical system II for in situ, high-frequency measurements of dissolved inorganic carbon in seawater
dc.type Article
dspace.entity.type Publication
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