<eml:eml xmlns:eml="eml://ecoinformatics.org/eml-2.1.0" xmlns:stmml="http://www.xml-cml.org/schema/stmml-1.1" xmlns:ds="eml://ecoinformatics.org/dataset-2.1.0" xmlns:xs="http://www.w3.org/2001/XMLSchema" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="eml://ecoinformatics.org/eml-2.1.0 http://nis.lternet.edu/schemas/EML/eml-2.1.0/eml.xsd" packageId="knb-lter-mcm.254.663" system="knb">
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  <dataset>
    <shortName>bdso</shortName>
    <title>Habitat Suitability - Soil Moisture</title>
    <creator>
      <individualName>
        <givenName>Diana</givenName>
        <surName>Wall</surName>
      </individualName>
      <address>
        <deliveryPoint>Johnson Hall 107</deliveryPoint>
        <city>Fort Collins</city>
        <administrativeArea>CO</administrativeArea>
        <postalCode>80523</postalCode>
        <country>US</country>
      </address>
      <electronicMailAddress>Diana.Wall@colostate.edu</electronicMailAddress>
      <onlineUrl>http://wp.natsci.colostate.edu/walllab/</onlineUrl>
      <userId directory="https://orcid.org">https://orcid.org/0000-0002-9466-5235</userId>
    </creator>
    <creator>
      <individualName>
        <givenName>Ross</givenName>
        <surName>Virginia</surName>
      </individualName>
      <address>
        <deliveryPoint>Hinman Box 6182</deliveryPoint>
        <city>Hanover</city>
        <administrativeArea>NH</administrativeArea>
        <postalCode>03755</postalCode>
        <country>US</country>
      </address>
      <phone phonetype="voice">(603) 646-0192</phone>
      <electronicMailAddress>ross.a.virginia@dartmouth.edu</electronicMailAddress>
      <onlineUrl>http://sites.dartmouth.edu/ravirginia/</onlineUrl>
      <userId directory="https://orcid.org">https://orcid.org/0000-0002-0890-0981</userId>
    </creator>
    <metadataProvider>
      <organizationName>McMurdo Dry Valleys LTER</organizationName>
      <onlineUrl>http://mcmlter.org/</onlineUrl>
    </metadataProvider>
    <associatedParty>
      <individualName>
        <givenName>Nicole</givenName>
        <surName>DeCrappeo</surName>
      </individualName>
      <address>
        <deliveryPoint>US Geological Survey</deliveryPoint>
        <city>Corvallis</city>
        <administrativeArea>OR</administrativeArea>
        <postalCode>97330</postalCode>
        <country>US</country>
      </address>
      <electronicMailAddress>ndecrappeo@usgs.gov</electronicMailAddress>
      <onlineUrl>http://fresc.usgs.gov/people/Profile.aspx?Emp_ID=476</onlineUrl>
      <role>lab crew</role>
    </associatedParty>
    <associatedParty>
      <individualName>
        <givenName>Inigo</givenName>
        <surName>San Gil</surName>
      </individualName>
      <address>
        <deliveryPoint>Department of Biology, MSC03 2020 University of New Mexico</deliveryPoint>
        <city>Albuquerque</city>
        <administrativeArea>NM</administrativeArea>
        <postalCode>87131</postalCode>
        <country>US</country>
      </address>
      <phone phonetype="voice">(505) 277-2625</phone>
      <phone phonetype="facsimile">(505) 277-2541</phone>
      <electronicMailAddress>isangil@lternet.edu</electronicMailAddress>
      <role>data manager</role>
    </associatedParty>
    <pubDate>2014-11-11</pubDate>
    <language>English</language>
    <abstract>
      <section>
        <para>
          <literalLayout>Investigation of the variation in soil biota and soil properties across the McMurdo Dry Valleys as part of the McMurdo Dry Valleys Long Term Ecological Research (LTER) project. The moisture content of soil samples which are collected for organism extraction and identification is determined. This study was carried out in the austral summer 1993/1994</literalLayout>
        </para>
      </section>
    </abstract>
    <keywordSet>
      <keyword>Antarctica</keyword>
      <keyword>LTER</keyword>
      <keyword>soil</keyword>
      <keyword>soil moisture</keyword>
      <keywordThesaurus>Station Keywords</keywordThesaurus>
    </keywordSet>
    <keywordSet>
      <keyword>population dynamics</keyword>
      <keywordThesaurus>LTER Core Areas</keywordThesaurus>
    </keywordSet>
    <intellectualRights>
      <section>
        <title>Data Policies</title>
        <para>
          <literalLayout>This data package is released under the Creative Commons Attribution 4.0 International License (CC BY 4.0; http://creativecommons.org/licenses/by/4.0/), which allows consumers (hereinafter referred to as “Data Users”) to freely reuse, redistribute, transform, or build on this work (even commercially) so long as appropriate credit is provided. Accordingly, Data Users are required to properly cite this data package in any publications or in the metadata of any derived products that result from its use (in whole or in part). A recommended citation is provided on the summary metadata page associated with this data package in the McMurdo Dry Valleys LTER Data Catalog (https://mcmlter.org/data), and a generic citation may be found on the summary metadata page in the repository where this data package was obtained. When these data contribute significantly to the contents of a publication, Data Users must also acknowledge that data were provided by the NSF-supported McMurdo Dry Valleys Long Term Ecological Research program (OPP-2224760). This data package has been released in the spirit of open scientific collaboration. Hence, Data Users are strongly encouraged to consider consultation, collaboration, and/or co-authorship (as appropriate) with the data package creator(s). Data Users should be aware these data may be actively used by others for ongoing research; thus, coordination may be necessary to prevent duplicate publication. Data Users should also recognize that misinterpretation of data may occur if they are used outside the context of the original study. Hence, Data Users are urged to contact the data package creator(s) if they have any questions regarding methodology or results. While substantial efforts are made to ensure the accuracy of this data package (with all its components), complete accuracy cannot be guaranteed. Periodic updates to this data package may occur, and it is the responsibility of Data Users to check for new versions. This data package is made available “as is” and comes with no warranty of accuracy or fitness for use. The creator(s) of this data package and the repository where these data were obtained shall not be liable for any damages resulting from misinterpretation, use, or misuse of these data. Finally, as a professional courtesy, we kindly request Data Users notify the primary contact referenced in the metadata when these data are used in the production of any derivative work or publication. Notification should include an explanation of how the data were used, along with a digital copy of the derived product(s). Thank you.</literalLayout>
        </para>
      </section>
    </intellectualRights>
    <distribution>
      <online>
        <url function="information">https://mcm.lternet.edu/content/habitat-suitability-soil-moisture</url>
      </online>
    </distribution>
    <coverage>
      <geographicCoverage>
        <geographicDescription>The Cape Royds Pond 1 is an ice free pond in the Ross IslandCode : CR1Area:&#160;1,792 Temperature:&#160;6.3 celsius&#160;</geographicDescription>
        <boundingCoordinates>
          <westBoundingCoordinate>166.163772583008</westBoundingCoordinate>
          <eastBoundingCoordinate>166.163772583008</eastBoundingCoordinate>
          <northBoundingCoordinate>-77.552818298340</northBoundingCoordinate>
          <southBoundingCoordinate>-77.552818298340</southBoundingCoordinate>
        </boundingCoordinates>
      </geographicCoverage>
      <geographicCoverage>
        <geographicDescription>The&#160;Labyrinth Pond 4 is located in the Wright Valley.&#160;Ice-covered, heavily shaded, lense-shaped.Code: LAB4Area:&#160;25,805Temperature: 2.6 celsius&#160;</geographicDescription>
        <boundingCoordinates>
          <westBoundingCoordinate>161.063613891602</westBoundingCoordinate>
          <eastBoundingCoordinate>161.063613891602</eastBoundingCoordinate>
          <northBoundingCoordinate>-77.560478210449</northBoundingCoordinate>
          <southBoundingCoordinate>-77.560478210449</southBoundingCoordinate>
        </boundingCoordinates>
      </geographicCoverage>
      <geographicCoverage>
        <geographicDescription>Lake Bonney occupies a glacially scoured bedrock basin in Taylor Valley. It is located at the head of the valley and is perennially ice-covered. The lake has two basins (lobes) connected by a narrow, shallow channel. There are no surface outflows; the only known water loss is through ice ablation (evaporation, sublimation and physical scouring). The lake is bordered to the north by the Asgard Range and to the south by the Kukri Hills. Mountain and cirque glaciers occupy hanging valleys between these peaks and supply meltwater intermittently to the lake during warmer periods in summer. The largest source of meltwater, however, is from the Taylor Glacier, which extends from the polar ice-cap and terminates in the western end of the west lobe of Lake Bonney. Valley: Taylor Distance to Sea : 25 Maximum Length (km): 7 Maximum Width (km): 0.9 Maximum Depth (m): 40 Surface Area (km^2): 4.3 Ice Thickness Average Surface (m): 2.8 - 4.5 Volume (m^3 * 10^6): 64.8</geographicDescription>
        <boundingCoordinates>
          <westBoundingCoordinate>162.371994018555</westBoundingCoordinate>
          <eastBoundingCoordinate>162.371994018555</eastBoundingCoordinate>
          <northBoundingCoordinate>-77.719100952148</northBoundingCoordinate>
          <southBoundingCoordinate>-77.719100952148</southBoundingCoordinate>
          <boundingAltitudes>
            <altitudeMinimum>57</altitudeMinimum>
            <altitudeMaximum>57</altitudeMaximum>
            <altitudeUnits>meter</altitudeUnits>
          </boundingAltitudes>
        </boundingCoordinates>
      </geographicCoverage>
      <geographicCoverage>
        <geographicDescription>Lake Brownworth is&#160;a meltwater lake west of&#160;Wright Lower Glacier&#160;at the east end of&#160;Wright Valley.&#160;It was named by the&#160;Advisory Committee on Antarctic Names&#160;for&#160;Frederick S. Brownworth Jr.,</geographicDescription>
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          <westBoundingCoordinate>162.718856811523</westBoundingCoordinate>
          <eastBoundingCoordinate>162.823226928711</eastBoundingCoordinate>
          <northBoundingCoordinate>-77.417655944824</northBoundingCoordinate>
          <southBoundingCoordinate>-77.442016601563</southBoundingCoordinate>
          <boundingAltitudes>
            <altitudeMinimum>5</altitudeMinimum>
            <altitudeMaximum>5</altitudeMaximum>
            <altitudeUnits>meter</altitudeUnits>
          </boundingAltitudes>
        </boundingCoordinates>
      </geographicCoverage>
      <geographicCoverage>
        <geographicDescription>Lake Vanda is located in the Wright Valley, adjacent to the Taylor Valley. It is fed primarily by the Onyx River, which has its origin at Lake Brownworth, and ultimately at the Lower Wright Glacier located ~27 km east of the lake. The lake has no outflow. Valley: Wright Distance to Sea : 47 Maximum Length (km): 8 Maximum Width (km): 2 Maximum Depth (m): 75 Surface Area (km^2): 5.2 Ice Thickness Average Surface (m): 2.8 - 4.2 Volume (m^3 * 10^6): 160</geographicDescription>
        <boundingCoordinates>
          <westBoundingCoordinate>161.391906738281</westBoundingCoordinate>
          <eastBoundingCoordinate>161.691970825195</eastBoundingCoordinate>
          <northBoundingCoordinate>-77.518882751465</northBoundingCoordinate>
          <southBoundingCoordinate>-77.542304992676</southBoundingCoordinate>
          <boundingAltitudes>
            <altitudeMinimum>143</altitudeMinimum>
            <altitudeMaximum>143</altitudeMaximum>
            <altitudeUnits>meter</altitudeUnits>
          </boundingAltitudes>
        </boundingCoordinates>
      </geographicCoverage>
      <geographicCoverage>
        <geographicDescription>The Lake Fryxell basin is formed by a moraine depression in a wider portion of the Taylor Valley. It has a number of moraine islands and shallower areas, as well as several relatively well developed deltas. The lake is fed by at least 10 meltwater streams with a total drainage catchment of 230 km2. The lake is dammed to the southwest by the Canada Glacier and is topographically closed. It is perennially ice covered; during summer months, an ice-free moat generally forms around much of the lake margin. Lake levels have risen ~2 m between 1971 and 1996. There are no surface outflows; the only known water loss is through ice ablation (evaporation, sublimation and physical scouring). Valley: Taylor Distance to Sea : 9 Maximum Length (km): 5.8 Maximum Width (km): 2.1 Maximum Depth (m): 20 Surface Area (km^2): 7.08 Ice Thickness Average Surface (m): 3.3 - 4.5 Volume (m^3 * 10^6): 25.2</geographicDescription>
        <boundingCoordinates>
          <westBoundingCoordinate>163.048782348633</westBoundingCoordinate>
          <eastBoundingCoordinate>163.259582519531</eastBoundingCoordinate>
          <northBoundingCoordinate>-77.597076416016</northBoundingCoordinate>
          <southBoundingCoordinate>-77.622711181641</southBoundingCoordinate>
          <boundingAltitudes>
            <altitudeMinimum>18</altitudeMinimum>
            <altitudeMaximum>18</altitudeMaximum>
            <altitudeUnits>meter</altitudeUnits>
          </boundingAltitudes>
        </boundingCoordinates>
      </geographicCoverage>
      <geographicCoverage>
        <geographicDescription>Lake Vida is a hypersaline lake in Victoria Valley, the northernmost of the large McMurdo Dry Valleys, on the continent of Antarctica. It is isolated under year-round ice cover, and is considerably more saline than seawater. Lake Vida is one of the largest lakes in the McMurdo Dry Valley region and is a closed-basin endorheic lake. The permanent surface ice on the lake is the thickest non-glacial ice on earth, reaching a depth of at least 21 metres or 69 ft. The ice at depth is saturated with brine that is seven times as saline as seawater. The high salinity allows the brine to remain liquid at an average yearly water temperature of 13 degrees Celsius or 9 farenheit. Hydrology: Lake Vida has at least three named inflows: Victoria River, Kite Stream, and Dune Creek. Victoria River passes through the Vida Basin into Victoria Valley, Victoria Land as ephemeral glacial meltwater from the Upper Victoria Glacier, draining from Victoria Upper Lake. Geology: In the vicinity of Lake Vida, a variety of geological features are noted, the most significant being glaciers, lakes, valleys, ridges, and summits. There are approximately 25 named glaciers within a 25 kilometres radius with the nearest being Upper Victoria Glacier, Packard Glacier, Clark Glacier, and Clio Glacier. Valley: Victoria</geographicDescription>
        <boundingCoordinates>
          <westBoundingCoordinate>161.930999755859</westBoundingCoordinate>
          <eastBoundingCoordinate>161.930999755859</eastBoundingCoordinate>
          <northBoundingCoordinate>-77.388298034668</northBoundingCoordinate>
          <southBoundingCoordinate>-77.388298034668</southBoundingCoordinate>
          <boundingAltitudes>
            <altitudeMinimum>349</altitudeMinimum>
            <altitudeMaximum>349</altitudeMaximum>
            <altitudeUnits>meter</altitudeUnits>
          </boundingAltitudes>
        </boundingCoordinates>
      </geographicCoverage>
      <geographicCoverage>
        <geographicDescription>Lake Hoare occupies a narrower portion of the Taylor Valley, dammed by the Canada Glacier. It would drain almost completely without this dam. There are a number of islands which may be related to an old terminal of Canada Glacier. The lake is fed primarily from direct runoff from the glacier, as well as meltwater streams. (Lake level rose ~1.5 m between 1972 and 1996). There are no surface outflows; the only known water loss is through ice ablation (evaporation, sublimation and physical scouring). Valley: Taylor Distance to Sea : 15 Maximum Length (km): 4.2 Maximum Width (km): 1 Maximum Depth (m): 34 Surface Area (km^2): 1.94 Ice Thickness Average Surface (m): 3.1 - 5.5 Volume (m^3 * 10^6): 17.5</geographicDescription>
        <boundingCoordinates>
          <westBoundingCoordinate>162.784423828125</westBoundingCoordinate>
          <eastBoundingCoordinate>162.935836791992</eastBoundingCoordinate>
          <northBoundingCoordinate>-77.623085021973</northBoundingCoordinate>
          <southBoundingCoordinate>-77.639259338379</southBoundingCoordinate>
          <boundingAltitudes>
            <altitudeMinimum>73</altitudeMinimum>
            <altitudeMaximum>73</altitudeMaximum>
            <altitudeUnits>meter</altitudeUnits>
          </boundingAltitudes>
        </boundingCoordinates>
      </geographicCoverage>
      <temporalCoverage>
        <rangeOfDates>
          <beginDate>
            <calendarDate>1993-01-01</calendarDate>
          </beginDate>
          <endDate>
            <calendarDate>1993-12-31</calendarDate>
          </endDate>
        </rangeOfDates>
      </temporalCoverage>
    </coverage>
    <maintenance>
      <description>
        <para>
          <literalLayout>This file was created by Mark St. John on 15 Oct 1998, using raw data from the Excel workbook '9394EGso.RAW'. The file format was suggested by the LTER data manager, to conform with the relational database structure. [AnP 19 Sept 1997]. The file name was changed to 9394bdso.dat on 17 Oct 01 by Nicole DeCrappeo. (ND17 Oct 01)</literalLayout>
        </para>
      </description>
    </maintenance>
    <contact>
      <organizationName>McMurdo Dry Valleys LTER</organizationName>
      <onlineUrl>http://mcmlter.org/</onlineUrl>
    </contact>
    <publisher>
      <organizationName>McMurdo Dry Valleys LTER</organizationName>
      <onlineUrl>http://mcmlter.org/</onlineUrl>
    </publisher>
    <pubPlace>McMurdo Dry Valleys LTER</pubPlace>
    <methods>
      <methodStep>
        <description>
          <section>
            <para>
              <literalLayout>&#160;General sampling sites representative of the dominant local environment were selected at each location. Nine grid points within a 1 m2 frame, oriented to the north, were sampled. Three equidistant samples were taken along the north side, through the middle and along the south side of the quadrat parallel to one another. These nine samples were labled "a" through "i" for each quadrat. &#160;Sampling bags were prepared with one sterile 'Whirlpak' bag and clean plastic scoop per sample. Samples were taken from within the 85 cm diameter circular area of each plot. The location of the sampling was recorded each year so that areas were not re-sampled. Using the plastic scoop, soil was collected to 10 cm depth. Very large rocks (&amp;gt;20 mm diameter) were excluded from the sample. The soil was shoveled into the 'Whirlpak' bag until three quarters full (about 1.5 kg soil). The soil was mixed well in the bag, then the bag was closed tightly, expelling as much air as possible. The soil samples were stored in a cooler for transportation. On return to the laboratory (within 8 hours of sampling), the soils were stored at -8C until further processing. &#160; In the laboratory, soil samples were handled in a laminar flow hood to prevent contamination. The Whirlpak bags of soil were mixed thoroughly prior to opening. A sub-sample of approximately 50g was removed and placed in a pre-weighed aluminum soil can, and weighed on a balance accurate to 0.01g. This sample was dried at 105C for 24 hours. The sample was removed, placed in a desiccator to cool down, and re-weighed. These data were used to calculate water content of the soil. &#160; Locations are: Adjacent to Lake Hoare, Cape Royds, Lake Fryxell, Lake Bonney, Lake Victoria, Lake Vida, Clark Glacier, Labyrinth, Lake Vanda and Lake Brownworth. Original data are stored in Room A208, &#160;Natural and Environmental Sciences Building, Colorado State University.</literalLayout>
            </para>
          </section>
        </description>
      </methodStep>
    </methods>
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      <entityName>bdso</entityName>
      <entityDescription>comma delimited file with the data for bdso</entityDescription>
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            <url>https://mcm.lternet.edu/sites/default/files/bdso.csv</url>
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      <attributeList>
        <attribute>
          <attributeName>LOCATION</attributeName>
          <attributeLabel>LOCATION</attributeLabel>
          <attributeDefinition>Name of area where measurement was made</attributeDefinition>
          <storageType>string</storageType>
          <measurementScale>
            <nominal>
              <nonNumericDomain>
                <textDomain>
                  <definition>Name of area where measurement was made</definition>
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        <attribute>
          <attributeName>DATE_TIME</attributeName>
          <attributeLabel>DATE_TIME</attributeLabel>
          <attributeDefinition>Date on which sample was gathered</attributeDefinition>
          <storageType>date</storageType>
          <measurementScale>
            <dateTime>
              <formatString>mm/dd/yyyy</formatString>
            </dateTime>
          </measurementScale>
        </attribute>
        <attribute>
          <attributeName>SAMPLE #</attributeName>
          <attributeLabel>SAMPLE #</attributeLabel>
          <attributeDefinition>Sample ID associated with transect, sampling location</attributeDefinition>
          <storageType>string</storageType>
          <measurementScale>
            <nominal>
              <nonNumericDomain>
                <textDomain>
                  <definition>Sample ID associated with transect, sampling location</definition>
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              </nonNumericDomain>
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        <attribute>
          <attributeName>SOIL WATER CONTENT (%)</attributeName>
          <attributeLabel>SOIL WATER CONTENT (%)</attributeLabel>
          <attributeDefinition>Percent water found in soil</attributeDefinition>
          <measurementScale>
            <ratio>
              <unit>
                <standardUnit>dimensionless</standardUnit>
              </unit>
              <precision>0.0001</precision>
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                <bounds>
                  <minimum exclusive="false">0</minimum>
                  <maximum exclusive="false">100</maximum>
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            <codeExplanation>None given</codeExplanation>
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        <attribute>
          <attributeName>COMMENTS</attributeName>
          <attributeLabel>COMMENTS</attributeLabel>
          <attributeDefinition>Helpful hints about the sample</attributeDefinition>
          <storageType>string</storageType>
          <measurementScale>
            <nominal>
              <nonNumericDomain>
                <textDomain>
                  <definition>Helpful hints about the sample</definition>
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        <attribute>
          <attributeName>FILE NAME</attributeName>
          <attributeLabel>FILE NAME</attributeLabel>
          <attributeDefinition>Name of file in which data was stored</attributeDefinition>
          <storageType>string</storageType>
          <measurementScale>
            <nominal>
              <nonNumericDomain>
                <textDomain>
                  <definition>Name of file in which data was stored</definition>
                </textDomain>
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