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            <gco:CharacterString>Cite this dataset as: Ho, D. T., Schlosser, P., Dobashi, R. (2024) SF6 and helium data from a tracer release experiment conducted June 2018 in the coastal Baltic Sea during FS Alkor cruise AL510. Biological and Chemical Oceanography Data Management Office (BCO-DMO). (Version 1) Version Date 2024-01-10 [if applicable, indicate subset used]. doi:10.26008/1912/bco-dmo.915772.1 [access date]</gco:CharacterString>
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        <gco:CharacterString>Baltic GasEx SF6 and He from tracer release experiment Dataset Description:  Methods and Sampling: &amp;lt;p&amp;gt;A tracer release experiment was conducted in the coastal Baltic Sea during&amp;amp;nbsp;cruise AL510 aboard the research vessel FS Alkor.&amp;amp;nbsp;On June 4th, 2018, we injected 3He and SF6 into the surface ocean (~5 m depth). After the injection, near the center of the SF6 patch, depth profiles of temperature and salinity were measured using a conductivity, temperature, and depth (CTD) sonde&amp;amp;nbsp;and water samples were collected in Niskin bottles.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;Discrete SF6 samples (and replicates) were drawn from the Niskin bottles using 550 ml glass bottles with ground-glass stoppers.&amp;amp;nbsp;For discrete&amp;amp;nbsp;3He samples, ~40 milliliters of seawater were collected in copper tubes mounted in aluminum channels and sealed at the ends with stainless steel clamps.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;SF6 samples were taken at the same stations and measured on board the FS Alkor. Concentration of SF6 was measured using a purge-and-trap SF6 analysis system designed following Law et al. (1994). In this system, SF6 was separated from other gases and measured with a gas chromatography electron capture detector (GC-ECD).&amp;lt;br /&amp;gt;
&amp;lt;br /&amp;gt;
3He&amp;amp;nbsp;samples were measured at the Lamont-Doherty Earth Observatory (LDEO) Noble Gas Laboratory.&amp;amp;nbsp; In the laboratory, 3He&amp;amp;nbsp;samples were extracted from the copper tubes using a vacuum extraction system (Ludin et al., 1998) and measured on a VG-5400 He isotope mass spectrometer. Precision is about 0.5 to 1% in δ3He&amp;amp;nbsp;for samples with high δ3He&amp;amp;nbsp;values (100% &amp;amp;lt; δ3He&amp;amp;nbsp;&amp;amp;lt; 1000%), and 0.2 to 0.5% for samples with lower δ3He&amp;amp;nbsp;values (-1.7% &amp;amp;lt; δ3He &amp;amp;lt; 100%).&amp;amp;nbsp;&amp;lt;/p&amp;gt;</gco:CharacterString>
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        <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/award/756792.rdf" xlink:title="OCE-1756807" xlink:actuate="onRequest">Funding provided by NSF Division of Ocean Sciences (NSF OCE) Award Number: OCE-1756807 Award URL: https://www.nsf.gov/awardsearch/show-award?AWD_ID=1756807</gmx:Anchor>
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&lt;p&gt;Gas exchange, the movement of gases between the atmosphere and the surface ocean (in both directions), is an important process to understand in global biogeochemistry. A particular area of interest is the rate of exchange of gases such as carbon dioxide and dimethyl sulfide, which play important roles in Earth's climate. Understanding and modeling air-sea exchange on a global scale requires understanding of how gas exchange rates vary in response to a number of factors such as temperature, wind speed, and the presence of surface chemical films (known as surfactants) in the ocean. Over the past 25 years, major advances have been made in understanding air-sea gas exchange in the open ocean, mainly due to improvements in methodology and a number of successful process studies. However, some important questions remain, such as what happens near coastal areas (including inland seas), and how surfactants affect gas exchange. The Baltic Sea Gas Exchange Experiment (Baltic GasEx) is a collaboration between scientists from the US and Germany designed to address these questions. Participants in Baltic GasEx will measure the air-sea gas exchange rates with different techniques in the Baltic Sea before and after the spring bloom, when concentrations and compositions of surfactants will be different. The expeditions will be conducted on a German ship (Alkor), with the ultimate goal of quantifying the relationship between wind speed and gas exchange in an inland sea, and understanding the impact of surfactants on air-sea gas exchange. The project will involve significant international collaboration, public education and outreach through both participating U.S. institutions, and substantial student training in partnership with the international collaborators.&lt;/p&gt;
&lt;p&gt;NSF funding will support helium-3 and sulfur hexafluoride measurements during Baltic GasEx to determine the gas exchange rate. German colleagues are independently funded to quantify surfactants with AC voltammetry, surface tension, and sum frequency generation; to determine chemical characteristics of the micro layer; and to estimate the gas exchange rate using eddy covariance flux measurements of CO2 and DMS. The proposed experiment is designed to address the question of whether open ocean wind speed/gas exchange parameterizations can be applied to inland seas like the Baltic. Also, the effect of surfactants on gas exchange has been studied extensively in the laboratory, but there is little direct field evidence for the effect of surfactants on gas exchange. The proposed experiment, with expeditions at times with both high and low surfactant concentrations, should shed new light on the effect of natural surfactants on gas exchange. Finally, some wind speed/gas exchange parameterizations proposed for the Baltic Sea appear to be higher than typical open ocean parameterizations. These are typically based on eddy covariance flux measurements of CO2. However, in open ocean experiments where both the helium-3/sulfur hexafluoride approach and eddy covariance of CO2 have been deployed, there seems to be a discrepancy between gas transfer velocities measured with the two techniques. This experiment should show whether a similar difference in gas transfer velocities measured via these two techniques also exists in the Baltic Sea.&lt;/p&gt;
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http://lod.bco-dmo.org/id/dataset-parameter/915827.rdf
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http://lod.bco-dmo.org/id/dataset-parameter/915829.rdf
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http://lod.bco-dmo.org/id/dataset-parameter/915831.rdf
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                <gco:CharacterString>&amp;lt;p&amp;gt;A tracer release experiment was conducted in the coastal Baltic Sea during&amp;amp;nbsp;cruise AL510 aboard the research vessel FS Alkor.&amp;amp;nbsp;On June 4th, 2018, we injected 3He and SF6 into the surface ocean (~5 m depth). After the injection, near the center of the SF6 patch, depth profiles of temperature and salinity were measured using a conductivity, temperature, and depth (CTD) sonde&amp;amp;nbsp;and water samples were collected in Niskin bottles.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;Discrete SF6 samples (and replicates) were drawn from the Niskin bottles using 550 ml glass bottles with ground-glass stoppers.&amp;amp;nbsp;For discrete&amp;amp;nbsp;3He samples, ~40 milliliters of seawater were collected in copper tubes mounted in aluminum channels and sealed at the ends with stainless steel clamps.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;SF6 samples were taken at the same stations and measured on board the FS Alkor. Concentration of SF6 was measured using a purge-and-trap SF6 analysis system designed following Law et al. (1994). In this system, SF6 was separated from other gases and measured with a gas chromatography electron capture detector (GC-ECD).&amp;lt;br /&amp;gt;
&amp;lt;br /&amp;gt;
3He&amp;amp;nbsp;samples were measured at the Lamont-Doherty Earth Observatory (LDEO) Noble Gas Laboratory.&amp;amp;nbsp; In the laboratory, 3He&amp;amp;nbsp;samples were extracted from the copper tubes using a vacuum extraction system (Ludin et al., 1998) and measured on a VG-5400 He isotope mass spectrometer. Precision is about 0.5 to 1% in δ3He&amp;amp;nbsp;for samples with high δ3He&amp;amp;nbsp;values (100% &amp;amp;lt; δ3He&amp;amp;nbsp;&amp;amp;lt; 1000%), and 0.2 to 0.5% for samples with lower δ3He&amp;amp;nbsp;values (-1.7% &amp;amp;lt; δ3He &amp;amp;lt; 100%).&amp;amp;nbsp;&amp;lt;/p&amp;gt;</gco:CharacterString>
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                <gco:CharacterString>&amp;lt;p&amp;gt;We calculated 3He excess from the measured 3He/4He ratio and 4He concentration.&amp;lt;br /&amp;gt;
3He excess is 3He in excess of solubility equilibrium calculated using the following equation:&amp;amp;nbsp;&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;[3He]exc = [4He]s (Rs − Ra) + [4He]eqRa(1 − a),&amp;amp;nbsp;&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;where:&amp;amp;nbsp;&amp;lt;/p&amp;gt;

&amp;lt;ul&amp;gt;
&amp;lt;li&amp;gt;[3He]exc is 3He in excess of solubility equilibrium&amp;lt;/li&amp;gt;
&amp;lt;li&amp;gt;[4He]s is the measured 4He concentration of the sample;&amp;lt;/li&amp;gt;
&amp;lt;li&amp;gt;[4He]eq is the atmospheric equilibrium concentration of 4He (Weiss, 1971);&amp;lt;/li&amp;gt;
&amp;lt;li&amp;gt;R&amp;lt;strong&amp;gt;s&amp;lt;/strong&amp;gt; is the measured 3He/4He ratio (ratio&amp;amp;nbsp;of &amp;lt;strong&amp;gt;s&amp;lt;/strong&amp;gt;ample);&amp;lt;/li&amp;gt;
&amp;lt;li&amp;gt;R&amp;lt;strong&amp;gt;a&amp;lt;/strong&amp;gt; is the 3He/4He&amp;amp;nbsp;ratio in the &amp;lt;strong&amp;gt;a&amp;lt;/strong&amp;gt;tmosphere (1.386 × 10^&amp;lt;sup&amp;gt;-6&amp;lt;/sup&amp;gt;&amp;amp;nbsp;(Clarke et al. 1976));&amp;lt;/li&amp;gt;
&amp;lt;li&amp;gt;From&amp;lt;em&amp;gt;&amp;amp;nbsp;(1 - a&amp;lt;/em&amp;gt;), a is the solubility isotope effect&amp;amp;nbsp; (0.983 (Benson and Krause, 1980)).&amp;lt;/li&amp;gt;
&amp;lt;/ul&amp;gt;

&amp;lt;p&amp;gt;&amp;amp;nbsp;&amp;lt;/p&amp;gt;</gco:CharacterString>
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                  <gco:CharacterString>* Imported data from source file &amp;quot;Baltic_Gas_Ex_1_20231113_with_SF6.txt&amp;quot; into the BCO-DMO data system.
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* Added column for station based on latitudes and longitudes</gco:CharacterString>
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This term applies to profiling CTDs. For fixed CTDs, see https://www.bco-dmo.org/instrument/869934. Community Standard Description: http://vocab.nerc.ac.uk/collection/L05/current/130/</gco:CharacterString>
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                          <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/affiliation/345.rdf" xlink:title="Affiliation" xlink:actuate="onRequest">GEOMAR Kiel</gmx:Anchor>
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          <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/platform/915499.rdf"
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      <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/platform/915499.rdf" xlink:title="FS Alkor" xlink:actuate="onRequest">vessel</gmx:Anchor>
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