<?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>2026-05-17T16:09:41Z</responseDate>
  <request verb="GetRecord" identifier="oai:materialscloud.org:764" metadataPrefix="oai_dc">https://archive.materialscloud.org/oai2d</request>
  <GetRecord>
    <record>
      <header>
        <identifier>oai:materialscloud.org:764</identifier>
        <datestamp>2021-03-23T17:01:50Z</datestamp>
        <setSpec>openaire_data</setSpec>
        <setSpec>community-mcarchive</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/" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd">
          <dc:contributor>Lempesis, Nikolaos</dc:contributor>
          <dc:creator>Lempesis, Nikolaos</dc:creator>
          <dc:creator>Janka, Aleš</dc:creator>
          <dc:creator>Gnatiuk, Oksana</dc:creator>
          <dc:creator>van Eijndhoven, Stef J.L.</dc:creator>
          <dc:creator>Koopmans, Rudolf J.</dc:creator>
          <dc:date>2021-03-23</dc:date>
          <dc:description>This code calculates the contact angle formed between a sessile drop of an arbitrarily defined liquid and a rough surface based on our improved Cassie-Baxter wetting model (https://doi.org/10.1088/2051-672X/ab9419). The topography of the surface needs to be predefined into the input file and may be any of the types: a) 2D pillars, b) fibers, c) sinusoids, d) 3D pillars. Although, theoretically, our model can be applied to topographies with arbitrarily large multiplicity, here the code was devised such that it considers up to three-level topographies hierarchically placed on top of one another. In the "Input" directory, three input files are given for single, two-level and three-level topographies, respectively. In multilevel topographies, the above-mentioned topography types may be combined at will. So, for example, we may have a three-level topography with sinusoidal pulses as the coarser level, fibers as the middle-level and 2D pillars as the finest level. Similarly, two-level and single-level topographies are also possible. The definitions of the multiplicity level and topography types proceed in the input file.</dc:description>
          <dc:format>application/gzip</dc:format>
          <dc:format>text/markdown</dc:format>
          <dc:identifier>https://doi.org/10.24435/materialscloud:z5-ec</dc:identifier>
          <dc:identifier>oai:materialscloud.org:764</dc:identifier>
          <dc:identifier>mcid:2021.47</dc:identifier>
          <dc:language>eng</dc:language>
          <dc:publisher>Materials Cloud</dc:publisher>
          <dc:relation>https://doi.org/10.1088/2051-672X/ab9419</dc:relation>
          <dc:relation>https://archive.materialscloud.org/communities/mcarchive</dc:relation>
          <dc:relation>https://doi.org/10.24435/materialscloud:hf-qx</dc:relation>
          <dc:rights>info:eu-repo/semantics/openAccess</dc:rights>
          <dc:rights>MIT License</dc:rights>
          <dc:rights>https://opensource.org/licenses/MIT</dc:rights>
          <dc:subject>Swissuniversities</dc:subject>
          <dc:subject>Wetting</dc:subject>
          <dc:subject>Superomniphobic</dc:subject>
          <dc:subject>Modelling</dc:subject>
          <dc:subject>Hydrophobic</dc:subject>
          <dc:title>Improved wetting model for the prediction of topography and dimensionality of superomniphobic surfaces</dc:title>
          <dc:type>info:eu-repo/semantics/other</dc:type>
        </oai_dc:dc>
      </metadata>
    </record>
  </GetRecord>
</OAI-PMH>
