Improved wetting model for the prediction of topography and dimensionality of superomniphobic surfaces
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{
"revision": 8,
"id": "764",
"created": "2021-03-04T12:04:34.604182+00:00",
"metadata": {
"doi": "10.24435/materialscloud:z5-ec",
"status": "published",
"title": "Improved wetting model for the prediction of topography and dimensionality of superomniphobic surfaces",
"mcid": "2021.47",
"license_addendum": "",
"_files": [
{
"description": "A compressed tarball containing the following six directories: 1) executables_&_SourceCode, 2) input_files, 3) output_files, 4) visualization, 5) Instructions and 6) Example",
"key": "SuperOmniphobic.tgz",
"size": 824997,
"checksum": "md5:a7e0fa4f37276286bc0368fa908564f7"
}
],
"owner": 134,
"_oai": {
"id": "oai:materialscloud.org:764"
},
"keywords": [
"Swissuniversities",
"Wetting",
"Superomniphobic",
"Modelling",
"Hydrophobic"
],
"conceptrecid": "763",
"is_last": true,
"references": [
{
"type": "Journal reference",
"doi": "10.1088/2051-672X/ab9419",
"comment": "Paper in which the method is derived and described",
"citation": "N. Lempesis, A. Janka, O. Gnatiuk, S.J.L. van Eijndhoven, R.J. Koopmans, Surf. Topogr.: Metr. Prop. 8, 025021 (2020)"
}
],
"publication_date": "Mar 23, 2021, 17:01:50",
"license": "MIT License",
"id": "764",
"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 \u201cInput\u201d 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.",
"version": 1,
"contributors": [
{
"email": "nikolaos.lempesis@hefr.ch",
"affiliations": [
"College of Engineering and Architecture Fribourg HES-SO, Bd de P\u00e9rolles 80, Fribourg CH-1705, Switzerland",
"Plastics Innovation Competence Center, Passage du Cardinal 1, Fribourg CH-1700, Switzerland"
],
"familyname": "Lempesis",
"givennames": "Nikolaos"
},
{
"affiliations": [
"College of Engineering and Architecture Fribourg HES-SO, Bd de P\u00e9rolles 80, Fribourg CH-1705, Switzerland"
],
"familyname": "Janka",
"givennames": "Ale\u0161"
},
{
"affiliations": [
"Eindhoven University of Technology, Eindhoven 5600 MB, The Netherlands"
],
"familyname": "Gnatiuk",
"givennames": "Oksana"
},
{
"affiliations": [
"Eindhoven University of Technology, Eindhoven 5600 MB, The Netherlands"
],
"familyname": "van Eijndhoven",
"givennames": "Stef J.L."
},
{
"affiliations": [
"College of Engineering and Architecture Fribourg HES-SO, Bd de P\u00e9rolles 80, Fribourg CH-1705, Switzerland",
"Plastics Innovation Competence Center, Passage du Cardinal 1, Fribourg CH-1700, Switzerland"
],
"familyname": "Koopmans",
"givennames": "Rudolf J."
}
],
"edited_by": 100
},
"updated": "2021-03-23T16:01:51.057199+00:00"
}