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            <gco:CharacterString>Cite this dataset as: Zhou, M., Granger, J. (2022) Simulation of the volume-dependent changes in ẟ15N and ẟ18O for IAEA-NO3 and USGS-34 reference materials (Biological Nitrogen Isotope Fractionation project). Biological and Chemical Oceanography Data Management Office (BCO-DMO). (Version 1) Version Date 2021-12-01 [if applicable, indicate subset used]. doi:10.26008/1912/bco-dmo.865685.1 [access date]</gco:CharacterString>
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        <gco:CharacterString>Simulation of the volume-dependent changes in ẟ15N and ẟ18O for IAEA-NO3 and USGS-34 reference materials Dataset Description:  Methods and Sampling: &amp;lt;p&amp;gt;&amp;lt;strong&amp;gt;Sampling and analytical procedures:&amp;amp;nbsp;&amp;lt;/strong&amp;gt;&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt; &amp;lt;strong&amp;gt;Effects of sample volume and salinity on O atom exchange with water&amp;lt;/strong&amp;gt;&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;Given the potential influences on NO&amp;lt;sub&amp;gt;3&amp;lt;/sub&amp;gt;&amp;lt;sup&amp;gt;-&amp;lt;/sup&amp;gt; N and O isotope ratios, which include bacterial blanks, dissolved atmospheric N&amp;lt;sub&amp;gt;2&amp;lt;/sub&amp;gt;O, contaminant NO&amp;lt;sub&amp;gt;3&amp;lt;/sub&amp;gt;&amp;lt;sup&amp;gt;-&amp;lt;/sup&amp;gt; in reference materials, O atom exchange with water, and incomplete N&amp;lt;sub&amp;gt;2&amp;lt;/sub&amp;gt;O recovery and associated isotope fractionation, we attempt to reproduce the volume-dependent changes in ẟ&amp;lt;sup&amp;gt;15&amp;lt;/sup&amp;gt;N and ẟ&amp;lt;sup&amp;gt;18&amp;lt;/sup&amp;gt;O that we observed for IAEA-NO3 and USGS-34 reference materials.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;The observed ä&amp;lt;sup&amp;gt;15&amp;lt;/sup&amp;gt;N and ä&amp;lt;sup&amp;gt;18&amp;lt;/sup&amp;gt;O values of N&amp;lt;sub&amp;gt;2&amp;lt;/sub&amp;gt;O for IAEA-NO3 and USGS-34 samples were referenced to that expected for IAEA-NO3 vs. the N&amp;lt;sub&amp;gt;2&amp;lt;/sub&amp;gt;O reference tank. The expected IAEA-NO3 has a ä&amp;lt;sup&amp;gt;15&amp;lt;/sup&amp;gt;N of 0‰ vs. IAEA-NO3, and that expected for USGS-34 is -6.5‰ vs. IAEA-NO3. Being uncertain of the ä&amp;lt;sup&amp;gt;18&amp;lt;/sup&amp;gt;O of the industrial N&amp;lt;sub&amp;gt;2&amp;lt;/sub&amp;gt;O in the reference tank, we approximate the expected ä&amp;lt;sup&amp;gt;18&amp;lt;/sup&amp;gt;O value for IAEA-NO3 vs. N&amp;lt;sub&amp;gt;2&amp;lt;/sub&amp;gt;O&amp;lt;sub&amp;gt;ref&amp;lt;/sub&amp;gt; to be that observed for the highest N&amp;lt;sub&amp;gt;2&amp;lt;/sub&amp;gt;O yield (at lower aliquot volumes – which is admittedly already subject to blanks). Referenced to itself, the expected ä&amp;lt;sup&amp;gt;18&amp;lt;/sup&amp;gt;O of IAEA-NO3 is 0‰ (vs. IAEA-NO3), and that for USGS-34 is -52.2‰ (vs. IAEA-NO3).&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;We compare the simulated ä&amp;lt;sup&amp;gt;15&amp;lt;/sup&amp;gt;N and ä&amp;lt;sup&amp;gt;18&amp;lt;/sup&amp;gt;O values to the observed average of 3 trials in dataset “Incidence of volume effect.”&amp;lt;/p&amp;gt;</gco:CharacterString>
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        <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/award/856531.rdf" xlink:title="OCE-1554474" xlink:actuate="onRequest">Funding provided by NSF Division of Ocean Sciences (NSF OCE) Award Number: OCE-1554474 Award URL: https://www.nsf.gov/awardsearch/show-award?AWD_ID=1554474</gmx:Anchor>
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The nitrogen (N) cycle in the marine environment is controlled by biological processes. Unfortunately, quantifying these processes and assessing their effect on the N cycle is difficult by direct measurements because of large spatial and temporal differences. Isotopic composition measurements of N provide a means to constrain these processes indirectly; however, there is still a great deal to be understood about isotope fractionation of recycled nitrogen through biological processes, which has made interpretation of novel nitrogen isotope data difficult. A researcher from the University of Connecticut plans to determine the influence of biological consumption and production on the isotope fractionation in ammonium. By helping to understand the processes surrounding fractionation of recycled ammonium at the organism level, this research will create a basis for which future researchers can better interpret isotope composition data to infer nitrogen cycle dynamics. A graduate student, a postdoctoral fellow, and two or more undergraduate students will be involved in the research. The researcher plans to integrate science with community-engaged learning by developing an undergraduate field and laboratory course that will require the students to present their research to stakeholders in the community. There will be a manual created for this course that will be disseminated in open-access forums for teachers hoping to develop similar courses.&lt;/p&gt;
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&amp;lt;p&amp;gt; &amp;lt;strong&amp;gt;Effects of sample volume and salinity on O atom exchange with water&amp;lt;/strong&amp;gt;&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;Given the potential influences on NO&amp;lt;sub&amp;gt;3&amp;lt;/sub&amp;gt;&amp;lt;sup&amp;gt;-&amp;lt;/sup&amp;gt; N and O isotope ratios, which include bacterial blanks, dissolved atmospheric N&amp;lt;sub&amp;gt;2&amp;lt;/sub&amp;gt;O, contaminant NO&amp;lt;sub&amp;gt;3&amp;lt;/sub&amp;gt;&amp;lt;sup&amp;gt;-&amp;lt;/sup&amp;gt; in reference materials, O atom exchange with water, and incomplete N&amp;lt;sub&amp;gt;2&amp;lt;/sub&amp;gt;O recovery and associated isotope fractionation, we attempt to reproduce the volume-dependent changes in ẟ&amp;lt;sup&amp;gt;15&amp;lt;/sup&amp;gt;N and ẟ&amp;lt;sup&amp;gt;18&amp;lt;/sup&amp;gt;O that we observed for IAEA-NO3 and USGS-34 reference materials.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;The observed ä&amp;lt;sup&amp;gt;15&amp;lt;/sup&amp;gt;N and ä&amp;lt;sup&amp;gt;18&amp;lt;/sup&amp;gt;O values of N&amp;lt;sub&amp;gt;2&amp;lt;/sub&amp;gt;O for IAEA-NO3 and USGS-34 samples were referenced to that expected for IAEA-NO3 vs. the N&amp;lt;sub&amp;gt;2&amp;lt;/sub&amp;gt;O reference tank. The expected IAEA-NO3 has a ä&amp;lt;sup&amp;gt;15&amp;lt;/sup&amp;gt;N of 0‰ vs. IAEA-NO3, and that expected for USGS-34 is -6.5‰ vs. IAEA-NO3. Being uncertain of the ä&amp;lt;sup&amp;gt;18&amp;lt;/sup&amp;gt;O of the industrial N&amp;lt;sub&amp;gt;2&amp;lt;/sub&amp;gt;O in the reference tank, we approximate the expected ä&amp;lt;sup&amp;gt;18&amp;lt;/sup&amp;gt;O value for IAEA-NO3 vs. N&amp;lt;sub&amp;gt;2&amp;lt;/sub&amp;gt;O&amp;lt;sub&amp;gt;ref&amp;lt;/sub&amp;gt; to be that observed for the highest N&amp;lt;sub&amp;gt;2&amp;lt;/sub&amp;gt;O yield (at lower aliquot volumes – which is admittedly already subject to blanks). Referenced to itself, the expected ä&amp;lt;sup&amp;gt;18&amp;lt;/sup&amp;gt;O of IAEA-NO3 is 0‰ (vs. IAEA-NO3), and that for USGS-34 is -52.2‰ (vs. IAEA-NO3).&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;We compare the simulated ä&amp;lt;sup&amp;gt;15&amp;lt;/sup&amp;gt;N and ä&amp;lt;sup&amp;gt;18&amp;lt;/sup&amp;gt;O values to the observed average of 3 trials in dataset “Incidence of volume effect.”&amp;lt;/p&amp;gt;</gco:CharacterString>
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