<?xml version='1.0' encoding='UTF-8'?>
<OAI-PMH xmlns="http://www.openarchives.org/OAI/2.0/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/ http://www.openarchives.org/OAI/2.0/OAI-PMH.xsd">
  <responseDate>2026-03-08T16:21:21Z</responseDate>
  <request identifier="oai:ir.kagoshima-u.ac.jp:00003755" verb="GetRecord" metadataPrefix="oai_dc">https://ir.kagoshima-u.ac.jp/oai</request>
  <GetRecord>
    <record>
      <header>
        <identifier>oai:ir.kagoshima-u.ac.jp:00003755</identifier>
        <datestamp>2026-03-05T00:32:27Z</datestamp>
        <setSpec>228:270:5647</setSpec>
        <setSpec>43:44</setSpec>
      </header>
      <metadata>
        <oai_dc:dc xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns="http://www.w3.org/2001/XMLSchema" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd">
          <dc:title>Features of Slope-Movements due to Heavy Rainfalls in the SHIRASU Region of Southern Kyushu</dc:title>
          <dc:creator>HARUYAMA, Motohisa</dc:creator>
          <dc:creator>19411</dc:creator>
          <dc:subject>610</dc:subject>
          <dc:subject>農学</dc:subject>
          <dc:subject>erosion</dc:subject>
          <dc:subject>landslide</dc:subject>
          <dc:subject>Shirasu</dc:subject>
          <dc:subject>site investigation</dc:subject>
          <dc:subject>specal soil</dc:subject>
          <dc:subject>volcamic soil</dc:subject>
          <dc:description>Baiu-fronts and typhoons passing through southern Kyushu and its adjacent area often bring about extraordinarily heavy rainfall, and, consequently, result dangerous floods and collapses of hill-slopes with Shirasu. Shirasu, which is widely distributed over souhern Kyushu, is very susceptible to water erosion and ready to collapse. This paper deals with the failure of hill-slope that occurs in the period of heavy rainfall. In this paper, the author classifies the failure of hill-slope into ten basic types according to the features of slope-movements and describes their causes for failures briefly. The hill-slopes with Shirasu are likely to be led to the most frequent collapses in the event of the rainfall exceeding about 300 mm during a spell of rain and in less than several hours after the time when the maximum hourly rainfall has occurred.</dc:description>
          <dc:description>departmental bulletin paper</dc:description>
          <dc:publisher>鹿児島大学</dc:publisher>
          <dc:publisher>Kagoshima University</dc:publisher>
          <dc:date>1974</dc:date>
          <dc:type>VoR</dc:type>
          <dc:format>application/pdf</dc:format>
          <dc:identifier>Memoirs of the Faculty of Agriculture, Kagoshima University</dc:identifier>
          <dc:identifier>10</dc:identifier>
          <dc:identifier>151</dc:identifier>
          <dc:identifier>163</dc:identifier>
          <dc:identifier>04530853</dc:identifier>
          <dc:identifier>AA00732376</dc:identifier>
          <dc:identifier>https://ir.kagoshima-u.ac.jp/record/3755/files/KJ00000010631.pdf</dc:identifier>
          <dc:identifier>http://hdl.handle.net/10232/00003747</dc:identifier>
          <dc:identifier>https://ir.kagoshima-u.ac.jp/records/3755</dc:identifier>
          <dc:language>eng</dc:language>
          <dc:rights>open access</dc:rights>
        </oai_dc:dc>
      </metadata>
    </record>
  </GetRecord>
</OAI-PMH>
