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author Cabral, Alex
Yau, Yvonne Y Y
Reithmaier, Gloria Maria Susanne
Cotovicz Jr, Luiz C
Barreira, João
Brostöm, Göran
Viana, Bárbara
Fonseca, Alessandra
Santos, Isaac R
author_facet Cabral, Alex
Yau, Yvonne Y Y
Reithmaier, Gloria Maria Susanne
Cotovicz Jr, Luiz C
Barreira, João
Brostöm, Göran
Viana, Bárbara
Fonseca, Alessandra
Santos, Isaac R
collection Datos científicos de ciencias marinas y ambientales
contents Salinity, depth, current, temperature, oxygen, carbon dioxide (CO2), radon (222Rn), pH and chlorophyll hourly variation during a complete neap to spring tidal cycle in 2 mangrove creeks in Brazil: Paraty (23°18'06.2S 44°38'53.6W) and Florianópolis (27°38'55.6S 48°33'11.2W). Sea level and current velocities were measured every 2 minutes using a ADCP (Nortek ECO) deployed in the mouth of each tidal creek. Salinity and temperature (Solinst Levelogger 5), dissolved oxygen (PME miniDOT) and pH (Onset HOBO pH logger) probes were attached to the vessel at 0.5 m depth and set to record every minute. Chlorophyll was also recorded every minute using a YSI EXO2. A submergible water pump was installed from the vessel at 0.5 m depth to continuously transport (3 L min-1) surface mangrove creek water into a RAD AQUA DURRIDGE showerhead gas equilibrator. The headspace air was pumped to a Drierite® desiccant and then to an automated radon (222Rn) detector (RAD7, DURRIDGE) coupled with a CO2 trace gas analyzer (LI-COR 7810). The gas equilibrator and detectors were connected in series in a closed air loop . The 222Rn activities (measured each 30 min) and pCO2 (1 min frequency) in air were converted to dissolved in seawater using their partitioning and solubility coefficients. The time series data were integrated using moving averages every hour to allow comparison across the different variables and time scales.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_964171
institution PANGAEA
language en
publishDate 2024
publisher PANGAEA
record_format pangaea
spellingShingle Salinity, depth, current, temperature, dissolved oxygen, carbon dioxide, radon (222Rn), pH and chlorophyll hourly variation in two mangrove tidal creeks in Brazil: Paraty and Florianópolis
Cabral, Alex
Yau, Yvonne Y Y
Reithmaier, Gloria Maria Susanne
Cotovicz Jr, Luiz C
Barreira, João
Brostöm, Göran
Viana, Bárbara
Fonseca, Alessandra
Santos, Isaac R
Acoustic doppler current profiler (ADCP), Nortek, Eco; Brazil; Carbon dioxide; Carbon dioxide, partial pressure; Carbon dioxide saturation; chlorophyll; Chlorophyll total; CO2; Costeira; current; Current velocity, horizontal; DATE/TIME; DEPTH, water; Dissolved oxygen; ELEVATION; Event label; Florianópolis, Brazil; LATITUDE; LONGITUDE; Mamanguá; mangrove; MULT; Multiparameter probe, YSI Xylem Inc., EXO2; Multiple investigations; Oxygen; Oxygen logger, PME, miniDOT; Oxygen saturation; Paraty, Brazil; pH; pH logger, Onset, HOBO; radon; Radon-222; Radon detector, DURRIDGE, RAD7; Salinity; subtropical area; Temperate; Temperature, water; tidal cycle; Tides; Trace gas analyzer, LI-COR, LI-7810; Tropical; Water level datalogger, Solinst, Levelogger 5
Salinity, depth, current, temperature, oxygen, carbon dioxide (CO2), radon (222Rn), pH and chlorophyll hourly variation during a complete neap to spring tidal cycle in 2 mangrove creeks in Brazil: Paraty (23°18'06.2S 44°38'53.6W) and Florianópolis (27°38'55.6S 48°33'11.2W). Sea level and current velocities were measured every 2 minutes using a ADCP (Nortek ECO) deployed in the mouth of each tidal creek. Salinity and temperature (Solinst Levelogger 5), dissolved oxygen (PME miniDOT) and pH (Onset HOBO pH logger) probes were attached to the vessel at 0.5 m depth and set to record every minute. Chlorophyll was also recorded every minute using a YSI EXO2. A submergible water pump was installed from the vessel at 0.5 m depth to continuously transport (3 L min-1) surface mangrove creek water into a RAD AQUA DURRIDGE showerhead gas equilibrator. The headspace air was pumped to a Drierite® desiccant and then to an automated radon (222Rn) detector (RAD7, DURRIDGE) coupled with a CO2 trace gas analyzer (LI-COR 7810). The gas equilibrator and detectors were connected in series in a closed air loop . The 222Rn activities (measured each 30 min) and pCO2 (1 min frequency) in air were converted to dissolved in seawater using their partitioning and solubility coefficients. The time series data were integrated using moving averages every hour to allow comparison across the different variables and time scales.
title Salinity, depth, current, temperature, dissolved oxygen, carbon dioxide, radon (222Rn), pH and chlorophyll hourly variation in two mangrove tidal creeks in Brazil: Paraty and Florianópolis
topic Acoustic doppler current profiler (ADCP), Nortek, Eco; Brazil; Carbon dioxide; Carbon dioxide, partial pressure; Carbon dioxide saturation; chlorophyll; Chlorophyll total; CO2; Costeira; current; Current velocity, horizontal; DATE/TIME; DEPTH, water; Dissolved oxygen; ELEVATION; Event label; Florianópolis, Brazil; LATITUDE; LONGITUDE; Mamanguá; mangrove; MULT; Multiparameter probe, YSI Xylem Inc., EXO2; Multiple investigations; Oxygen; Oxygen logger, PME, miniDOT; Oxygen saturation; Paraty, Brazil; pH; pH logger, Onset, HOBO; radon; Radon-222; Radon detector, DURRIDGE, RAD7; Salinity; subtropical area; Temperate; Temperature, water; tidal cycle; Tides; Trace gas analyzer, LI-COR, LI-7810; Tropical; Water level datalogger, Solinst, Levelogger 5
url https://doi.org/10.1594/PANGAEA.964171