<metadata>
  <idinfo>
    <citation>
      <citeinfo>
        <origin>Melisa A. DiazByron J. AdamsKathleen A. WelchSue WelchAlia KhanDiane M. McKnightW. Berry Lyons</origin>
        <pubdate>2022-03-03</pubdate>
        <title>Major ion and nutrient concentrations of water-soluble salts leached from aeolian material, McMurdo Dry Valleys, Antarctica (2013-2016)</title>
        <!-- edition -->
        <geoform>tabular digitial data</geoform>
        <!-- serinfo -->
        <pubinfo>
          <pubplace>McMurdo Dry Valleys LTER</pubplace>
          <publish>McMurdo Dry Valleys LTER</publish>
        </pubinfo>
        <othercit>10.6073/pasta/6e55031fc79fa3cc6305ff318522b775</othercit>
        <onlink>https://mcm.lternet.edu/content/major-ion-and-nutrient-concentrations-water-soluble-salts-leached-aeolian-material-mcmurdo</onlink>
        <!--lworkcit -->
      </citeinfo>
      <descript>
        <abstract>To evaluate the role of Antarctic aeolian transport in surface chemistry homogenization, fifty-three samples of aeolian material from the McMurdo Dry Valleys region of Antarctica were collected and analyzed for water-soluble major ions and nutrients at a 1:5 sediment:water ratio. Samples were collected seasonally from&#160;Alatna Valley, Victoria Valley, Miers Valley, and Taylor Valley (Taylor Glacier, East Lake Bonney, F6 (Lake Fryxell), and Explorer’s Cove) at five heights (~5, 10, 20, 50, 100 cm) above the surface between 2013 and 2015. This data package is associated with Aeolian Material Transport and Its Role in Landscape Connectivity in the McMurdo Dry Valleys, Antarctica, published by Diaz et al. in 2018 (DOI:&#160;10.1029/2017JF004589).</abstract>
        <supplinf>Funding for this work was provided by the National Science Foundation for Long Term Ecological Research via grants #OPP-1115245 and #OPP-1637708.</supplinf>
      </descript>
      <timeperd>
        <timeinfo>
          <rngdates>
            <begdate>
              <caldate>2013-01-15</caldate>
            </begdate>
            <enddate>
              <caldate>2016-01-14</caldate>
            </enddate>
          </rngdates>
        </timeinfo>
        <current>ground condition</current>
      </timeperd>
      <status>
        <update>As needed</update>
      </status>
      <spdom>
        <descgeog>Big Spring Number Eight (BSNE) isokinetic wind aspirated sampler located 36 km from the coast in Alatna Valley. Location details provided by Melisa Diaz in March 2019.</descgeog>
        <bounding>
          <westbc>161.111020000000</westbc>
          <eastbc>161.111020000000</eastbc>
          <northbc>-76.900080000000</northbc>
          <southbc>-76.900080000000</southbc>
          <boundingalt>
            <altmin>950m</altmin>
            <altmax>950m</altmax>
            <altunits>meter</altunits>
          </boundingalt>
        </bounding>
      </spdom>
      <spdom>
        <descgeog>Big Spring Number Eight (BSNE) isokinetic wind aspirated sampler located 27 km from the coast near East Lake Bonney in Taylor Valley. Location details provided by Melisa Diaz in March 2019.</descgeog>
        <bounding>
          <westbc>162.562330000000</westbc>
          <eastbc>162.562330000000</eastbc>
          <northbc>-77.692630000000</northbc>
          <southbc>-77.692630000000</southbc>
          <boundingalt>
            <altmin>64m</altmin>
            <altmax>64m</altmax>
            <altunits>meter</altunits>
          </boundingalt>
        </bounding>
      </spdom>
      <spdom>
        <descgeog>Big Spring Number Eight (BSNE) isokinetic wind aspirated sampler located 3.5 km from the coast in the Explorer's Cove region of Taylor Valley. Location details provided by Melisa Diaz in March 2019.</descgeog>
        <bounding>
          <westbc>163.417520000000</westbc>
          <eastbc>163.417520000000</eastbc>
          <northbc>-77.588730000000</northbc>
          <southbc>-77.588730000000</southbc>
          <boundingalt>
            <altmin>24m</altmin>
            <altmax>24m</altmax>
            <altunits>meter</altunits>
          </boundingalt>
        </bounding>
      </spdom>
      <spdom>
        <descgeog>Big Spring Number Eight (BSNE) isokinetic wind aspirated sampler located 8.5 km from the coast near Lake Fryxell and the F6 camp in Taylor Valley. Location details provided by Melisa Diaz in March 2019.</descgeog>
        <bounding>
          <westbc>163.248700000000</westbc>
          <eastbc>163.248700000000</eastbc>
          <northbc>-77.608500000000</northbc>
          <southbc>-77.608500000000</southbc>
          <boundingalt>
            <altmin>19m</altmin>
            <altmax>19m</altmax>
            <altunits>meter</altunits>
          </boundingalt>
        </bounding>
      </spdom>
      <spdom>
        <descgeog>Big Spring Number Eight (BSNE) isokinetic wind aspirated sampler located 10.5 km from the coast in Miers Valley. Location details provided by Melisa Diaz in March 2019.</descgeog>
        <bounding>
          <westbc>163.794230000000</westbc>
          <eastbc>163.794230000000</eastbc>
          <northbc>-78.098050000000</northbc>
          <southbc>-78.098050000000</southbc>
          <boundingalt>
            <altmin>50m</altmin>
            <altmax>50m</altmax>
            <altunits>meter</altunits>
          </boundingalt>
        </bounding>
      </spdom>
      <spdom>
        <descgeog>Big Spring Number Eight (BSNE) isokinetic wind aspirated sampler located 38.5 km from the coast on Taylor Glacier in Taylor Valley. Location details provided by Melisa Diaz in March 2019.</descgeog>
        <bounding>
          <westbc>162.131350000000</westbc>
          <eastbc>162.131350000000</eastbc>
          <northbc>-77.740020000000</northbc>
          <southbc>-77.740020000000</southbc>
          <boundingalt>
            <altmin>334m</altmin>
            <altmax>334m</altmax>
            <altunits>meter</altunits>
          </boundingalt>
        </bounding>
      </spdom>
      <spdom>
        <descgeog>Big Spring Number Eight (BSNE) isokinetic wind aspirated sampler located 47 km from the coast in Victoria Valley. Location details provided by Melisa Diaz in March 2019.</descgeog>
        <bounding>
          <westbc>161.600620000000</westbc>
          <eastbc>161.600620000000</eastbc>
          <northbc>-77.330920000000</northbc>
          <southbc>-77.330920000000</southbc>
          <boundingalt>
            <altmin>450m</altmin>
            <altmax>450m</altmax>
            <altunits>meter</altunits>
          </boundingalt>
        </bounding>
      </spdom>
      <keywords>
        <themekt>LTER Core Areas</themekt>
        <themekey>inorganic nutrients</themekey>
      </keywords>
      <accconst>None</accconst>
      <ptcontact>
        <cntinfo>&lt;cntperp&gt; &lt;cntper&gt;McMurdo Dry Valleys LTER Information Manager&lt;/cntper&gt; &lt;/cntperp&gt; &lt;cntemail&gt;im@mcmlter.org&lt;/cntemail&gt;</cntinfo>
      </ptcontact>
      <datacred>Name: Stephen O. Opiyo Role: associated researcher Name: S. Craig Cary Role: associated researcher Name: Renée F. Brown Role: data manager</datacred>
      <dataqual>
        <logic>Not Applicable</logic>
        <complete>Not Applicable</complete>
        <lineage>
          <method>
            <methtype>Field and/or Lab Methods</methtype>
            <methdesc>Big Spring Number Eight (BSNE) isokinetic wind aspirated samplers were deployed at seven collection sites throughout the McMurdo Dry Valleys. These samplers passively collect 95% of airborne material that enters the collection box opening, regardless of wind velocity or direction. Though the aeolian material collection trays were initially set to standardized heights above the surface (5, 10, 20, 50, and 100 cm), strong winds generated variation in heights among the individual units. Therefore, relative elevation terms (bottom lower, bottom middle, bottom upper, middle, and top) are used in this work rather than absolute heights. Aeolian material from Alatna, Victoria, Taylor (Explorer's Cove, F6, East Lake Bonney, and Taylor Glacier), and Miers Valleys was collected seasonally in 2013 and 2014 and year-round for 2015. Fifty-three samples were obtained, with 38 samples containing more than 5 g. Samples were collected twice: once in November and again in January. November collections are termed “winter” (from 15 January to 31 October), while January collections are termed “summer” (from 1 November to 14 January). With samples with greater than 5 g of mass, 0.5 g of sample was leached with 2.5 ml of 18 Ω deionized (DI) water chilled to 3 °C. Samples with ~5 g of mass were leached using the entire mass of the sample. Sequential leaches of aeolian material were performed at a 1:5 sediment:DI water ratio.&#160;For the first leach, samples were agitated for 1 min by hand then set to rest at 3 °C for 30 min. After 30 min, the water from the first leach was extracted and filtered using a 0.45-μm Whatman® polypropylene syringe filter and stored in a clean Falcon™ tube at 3 °C in preparation for chemical analysis. The first two to three drops of leachate were discarded to minimize potential contamination from the filtration process. The second leach followed a similar procedure, but the extraction lasted for 24 hr. These two time steps were chosen to ideally simulate short pulses of water hydrating aeolian sediment in the McMurdo Dry Valleys to dissolve rapidly soluble solids (30 min) and long-term wetting (24 hr).&#160; Soluble reactive phosphorous (PO43-) and nitrate plus nitrite (NO3- + NO2-) analyzed on a Skalar San++ Automated Wet Chemistry Analyzer with an SA 1050 Random Access Auto-sampler. Cations were analyzed using a Dionex DX-120 ion chromatograph (IC) with an AS40 automated sampler and anions were analyzed using a Dionex ICS-2100 ion chromatograph and an AS-DV automated sampler.</methdesc>
          </method>
          <procstep>
            <procdesc>Big Spring Number Eight (BSNE) isokinetic wind aspirated samplers were deployed at seven collection sites throughout the McMurdo Dry Valleys. These samplers passively collect 95% of airborne material that enters the collection box opening, regardless of wind velocity or direction. Though the aeolian material collection trays were initially set to standardized heights above the surface (5, 10, 20, 50, and 100 cm), strong winds generated variation in heights among the individual units. Therefore, relative elevation terms (bottom lower, bottom middle, bottom upper, middle, and top) are used in this work rather than absolute heights.Aeolian material from Alatna, Victoria, Taylor (Explorer's Cove, F6, East Lake Bonney, and Taylor Glacier), and Miers Valleys was collected seasonally in 2013 and 2014 and year-round for 2015. Fifty-three samples were obtained, with 38 samples containing more than 5 g. Samples were collected twice: once in November and again in January. November collections are termed “winter” (from 15 January to 31 October), while January collections are termed “summer” (from 1 November to 14 January).With samples with greater than 5 g of mass, 0.5 g of sample was leached with 2.5 ml of 18 Ω deionized (DI) water chilled to 3 °C. Samples with ~5 g of mass were leached using the entire mass of the sample. Sequential leaches of aeolian material were performed at a 1:5 sediment:DI water ratio.&#160;For the first leach, samples were agitated for 1 min by hand then set to rest at 3 °C for 30 min. After 30 min, the water from the first leach was extracted and filtered using a 0.45-μm Whatman® polypropylene syringe filter and stored in a clean Falcon™ tube at 3 °C in preparation for chemical analysis. The first two to three drops of leachate were discarded to minimize potential contamination from the filtration process. The second leach followed a similar procedure, but the extraction lasted for 24 hr. These two time steps were chosen to ideally simulate short pulses of water hydrating aeolian sediment in the McMurdo Dry Valleys to dissolve rapidly soluble solids (30 min) and long-term wetting (24 hr).&#160;Soluble reactive phosphorous (PO43-) and nitrate plus nitrite (NO3- + NO2-) analyzed on a Skalar San++ Automated Wet Chemistry Analyzer with an SA 1050 Random Access Auto-sampler. Cations were analyzed using a Dionex DX-120 ion chromatograph (IC) with an AS40 automated sampler and anions were analyzed using a Dionex ICS-2100 ion chromatograph and an AS-DV automated sampler.</procdesc>
            <procdate>unknown</procdate>
          </procstep>
        </lineage>
      </dataqual>
      <eainfo>
        <detailed>
          <enttyp>
            <enttypl>AEOLIAN_CHEM</enttypl>
          </enttyp>
          <attr>
            <attrlabl>Dataset Code</attrlabl>
            <attrdef>Internal dataset code.</attrdef>
            <attrdefs>The data provider</attrdefs>
            <attrdomv>
              <udom>Internal dataset code.</udom>
            </attrdomv>
          </attr>
          <attr>
            <attrlabl>Site</attrlabl>
            <attrdef>Location where sample was collected.</attrdef>
            <attrdefs>The data provider</attrdefs>
            <attrdomv>
              <udom>Location where sample was collected.</udom>
            </attrdomv>
          </attr>
          <attr>
            <attrlabl>Relative sample height</attrlabl>
            <attrdef>Height above the ground where sample was collected. Relative terms (bottom lower, bottom middle, bottom upper, middle, top) loosely correspond with ~ 5, 10, 20, 50, 100 cm above the surface.</attrdef>
            <attrdefs>The data provider</attrdefs>
            <attrdomv>
              <udom>Height above the ground where sample was collected. Relative terms (bottom lower, bottom middle, bottom upper, middle, top) loosely correspond with ~ 5, 10, 20, 50, 100 cm above the surface.</udom>
            </attrdomv>
          </attr>
          <attr>
            <attrlabl>Sample height</attrlabl>
            <attrdef>Approximate sample height. The aeolian material collection trays were initially set to standardized heights above the surface (5, 10, 20, 50, and 100 cm). However, strong winds generated variation in heights among the individual units. Relative terms (bottom lower, bottom middle, bottom upper, middle, top) loosely correspond with ~ 5, 10, 20, 50, 100 cm above the surface.</attrdef>
            <attrdefs>The data provider</attrdefs>
            <attrdomv>
              <rdom>
                <attrunit>centimeter</attrunit>
              </rdom>
            </attrdomv>
          </attr>
          <attr>
            <attrlabl>Timeframe</attrlabl>
            <attrdef>Timeframe when sample was collected. November collections are termed “winter” (from 15 January to 31 October), while January collections are termed “summer” (from 1 November to 14 January).</attrdef>
            <attrdefs>The data provider</attrdefs>
            <attrdomv>
              <udom>Timeframe when sample was collected. November collections are termed “winter” (from 15 January to 31 October), while January collections are termed “summer” (from 1 November to 14 January).</udom>
            </attrdomv>
          </attr>
          <attr>
            <attrlabl>Leach time</attrlabl>
            <attrdef>The amount of time during which the sample was leached (30 min or 24 hour). Total represents the sum of the first (30 min) and second (24 hour) leach.</attrdef>
            <attrdefs>The data provider</attrdefs>
            <attrdomv>
              <udom>The amount of time during which the sample was leached (30 min or 24 hour). Total represents the sum of the first (30 min) and second (24 hour) leach.</udom>
            </attrdomv>
          </attr>
          <attr>
            <attrlabl>Fluoride</attrlabl>
            <attrdef>Fluoride (F-) concentration in the sample. Empty cells represent concentration levels below the instrument detection limit.</attrdef>
            <attrdefs>The data provider</attrdefs>
            <attrdomv>
              <rdom>
                <attrunit>micromolePerGram</attrunit>
              </rdom>
            </attrdomv>
          </attr>
          <attr>
            <attrlabl>Chloride</attrlabl>
            <attrdef>Chloride (Cl-) concentration in the sample. Empty cells represent concentration levels below the instrument detection limit.</attrdef>
            <attrdefs>The data provider</attrdefs>
            <attrdomv>
              <rdom>
                <attrunit>micromolePerGram</attrunit>
              </rdom>
            </attrdomv>
          </attr>
          <attr>
            <attrlabl>Bromide</attrlabl>
            <attrdef>Bromide (Br-) concentration in the sample. Empty cells represent concentration levels below the instrument detection limit.</attrdef>
            <attrdefs>The data provider</attrdefs>
            <attrdomv>
              <rdom>
                <attrunit>micromolePerGram</attrunit>
              </rdom>
            </attrdomv>
          </attr>
          <attr>
            <attrlabl>Sulfate</attrlabl>
            <attrdef>Sulfate (SO42-) concentration in the sample. Empty cells represent concentration levels below the instrument detection limit.</attrdef>
            <attrdefs>The data provider</attrdefs>
            <attrdomv>
              <rdom>
                <attrunit>micromolePerGram</attrunit>
              </rdom>
            </attrdomv>
          </attr>
          <attr>
            <attrlabl>Sodium</attrlabl>
            <attrdef>Sodium (Na+) concentration in the sample. Empty cells represent concentration levels below the instrument detection limit.</attrdef>
            <attrdefs>The data provider</attrdefs>
            <attrdomv>
              <rdom>
                <attrunit>micromolePerGram</attrunit>
              </rdom>
            </attrdomv>
          </attr>
          <attr>
            <attrlabl>Potassium</attrlabl>
            <attrdef>Potassium (K+) concentration in the sample. Empty cells represent concentration levels below the instrument detection limit.</attrdef>
            <attrdefs>The data provider</attrdefs>
            <attrdomv>
              <rdom>
                <attrunit>micromolePerGram</attrunit>
              </rdom>
            </attrdomv>
          </attr>
          <attr>
            <attrlabl>Magnesium</attrlabl>
            <attrdef>Magnesium (Mg2+) concentration in the sample. Empty cells represent concentration levels below the instrument detection limit.</attrdef>
            <attrdefs>The data provider</attrdefs>
            <attrdomv>
              <rdom>
                <attrunit>micromolePerGram</attrunit>
              </rdom>
            </attrdomv>
          </attr>
          <attr>
            <attrlabl>Calcium</attrlabl>
            <attrdef>Calcium (Ca2+) concentration in the sample. Empty cells represent concentration levels below the instrument detection limit.</attrdef>
            <attrdefs>The data provider</attrdefs>
            <attrdomv>
              <rdom>
                <attrunit>micromolePerGram</attrunit>
              </rdom>
            </attrdomv>
          </attr>
          <attr>
            <attrlabl>Nitrate</attrlabl>
            <attrdef>Nitrate (NO3- + NO2-) concentration in the sample. Empty cells represent concentration levels below the instrument detection limit.</attrdef>
            <attrdefs>The data provider</attrdefs>
            <attrdomv>
              <rdom>
                <attrunit>micromolePerGram</attrunit>
              </rdom>
            </attrdomv>
          </attr>
          <attr>
            <attrlabl>Soluble reactive phosphorus</attrlabl>
            <attrdef>Soluble reactive phosphorus (SO43-) concentration in the sample. Empty cells represent concentration levels below the instrument detection limit.</attrdef>
            <attrdefs>The data provider</attrdefs>
            <attrdomv>
              <rdom>
                <attrunit>micromolePerGram</attrunit>
              </rdom>
            </attrdomv>
          </attr>
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              <cntorg>McMurdo Dry Valleys LTER</cntorg>
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        <metd>2022-03-03</metd>
        <metrd>2022-03-03</metrd>
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