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      <src>https://theses.otagogeology.org.nz/files/original/28db17dcb13a6db08100f7213335789b.pdf</src>
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          <element elementId="50">
            <name>Title</name>
            <description>A name given to the resource</description>
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              <elementText elementTextId="1">
                <text>Geology theses</text>
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    <name>OU Geology thesis</name>
    <description>Thesis or dissertation completed by University of Otago Geology students</description>
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      <element elementId="52">
        <name>Author last name</name>
        <description>Last name of the Author</description>
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          <elementText elementTextId="34843">
            <text>Dewdney</text>
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      <element elementId="53">
        <name>Project type</name>
        <description>Is it an MSc, PhD, BSc(Hons) or PGDipSci?</description>
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          <elementText elementTextId="34846">
            <text>BSc(Hons)</text>
          </elementText>
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      <element elementId="54">
        <name>Advisers</name>
        <description>Who supervised/advised this student</description>
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          <elementText elementTextId="34848">
            <text>Landis, C.A.</text>
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      <element elementId="55">
        <name>Abstract</name>
        <description>The Abstract for this thesis</description>
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          <elementText elementTextId="34849">
            <text>Comparisons are made between analyses of the 3.5 phi fraction of floating and shore sand samples from an estuarine tidal channel in Blueskin Bay. A suite of minerals, common to both floating and shore sand, with a density greater than quartz and feldspar (density &gt; 2. 769) is identified Relative. ·concentrations of the mineral suite are found to vary between all samples, and, an anomalous zone of ~0. 7ha with a relatively high concentration of the mineral suite is identified on the channel margin. The flotation process is found to preferentially select for the minerals with a density greater than quartz and foldspar. The relationship between grain angularity, surface wetability and ease of flotation is assessed. Grain angularity is indicated as an important parameter in the preferential flotation of the mineral suite. Transport of sand by flotation appears to be a one-way process and may be contributing to the relatively high concentrations of the mineral suite in the anomalous zone. The relationship between channel morphology, sea breeze/tidal dependence and floating sand deposition is discussed. It is estimated that 14 tonnes of sand per year are transported by flotation towards the head ofthe estuary.</text>
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      <element elementId="59">
        <name>Department</name>
        <description>The department where the student is studying primarily.</description>
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            <text>Geology</text>
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      <element elementId="61">
        <name>Named locality</name>
        <description>Named locality describing the field area location.</description>
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            <text>Blueskin Bay</text>
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            <text>Otago</text>
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      <element elementId="60">
        <name>Thesis description</name>
        <description>Number of pages, maps, CDs, etc.</description>
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            <text>vii, 50 p. : ill. (some col.), maps ; 30 cm.</text>
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      <name>Dublin Core</name>
      <description>The Dublin Core metadata element set is common to all Omeka records, including items, files, and collections. For more information see, http://dublincore.org/documents/dces/.</description>
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        <element elementId="43">
          <name>Identifier</name>
          <description>An unambiguous reference to the resource within a given context</description>
          <elementTextContainer>
            <elementText elementTextId="34842">
              <text>2001Dewdney</text>
            </elementText>
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        <element elementId="39">
          <name>Creator</name>
          <description>An entity primarily responsible for making the resource</description>
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            <elementText elementTextId="34844">
              <text>Dewdney, Rob (Robert C.)</text>
            </elementText>
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        </element>
        <element elementId="40">
          <name>Date</name>
          <description>A point or period of time associated with an event in the lifecycle of the resource</description>
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            <elementText elementTextId="34845">
              <text>2001</text>
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        <element elementId="50">
          <name>Title</name>
          <description>A name given to the resource</description>
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            <elementText elementTextId="34847">
              <text>Floating sand in Blueskin Bay estuary</text>
            </elementText>
          </elementTextContainer>
        </element>
        <element elementId="49">
          <name>Subject</name>
          <description>The topic of the resource</description>
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            <elementText elementTextId="34853">
              <text>Sedimentology</text>
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            <elementText elementTextId="34854">
              <text>Marine geology</text>
            </elementText>
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    <tag tagId="966">
      <name>floating sand</name>
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