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Statements

Subject Item
dbr:Asperity_(materials_science)
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애스패리티 アスペリティ Asperity (materials science)
rdfs:comment
애스패리티(영어: Asperity)는 판 경계의 접촉면 중 특히 마찰이 강한 부분을 뜻한다. 이 부분은 지진이 발생했을 때 특히 미끄럼 량이 커진다. 1981년에 가나모리 히로오가 제창했다. In materials science, asperity, defined as "unevenness of surface, roughness, ruggedness" (from the Latin asper—"rough"), has implications (for example) in physics and seismology. Smooth surfaces, even those polished to a mirror finish, are not truly smooth on a microscopic scale. They are rough, with sharp, rough or rugged projections, termed "asperities". Surface asperities exist across multiple scales, often in a self affine or fractal geometry. The fractal dimension of these structures has been correlated with the contact mechanics exhibited at an interface in terms of friction and contact stiffness. アスペリティ（英: asperity）は、地震学者の Thorne Lay と金森博雄が1980年に提唱した概念である。
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1122160860
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dbr:Normal_contact_stiffness dbr:Archard_equation dbr:Interface_(chemistry) dbr:Physics dbr:Burnishing_(metal) dbr:Materials_science dbr:Contact_mechanics dbr:Surface_roughness dbr:Wear dbr:Friction dbc:Materials_science dbc:Tribology dbr:Fractal dbr:Fractal_dimension dbr:Seismology n21:Asperities.svg dbc:Surfaces
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freebase:m.0b3pmw n11:4SvSC dbpedia-ja:アスペリティ dbpedia-ko:애스패리티 wikidata:Q4807910 yago-res:Asperity_(materials_science)
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In materials science, asperity, defined as "unevenness of surface, roughness, ruggedness" (from the Latin asper—"rough"), has implications (for example) in physics and seismology. Smooth surfaces, even those polished to a mirror finish, are not truly smooth on a microscopic scale. They are rough, with sharp, rough or rugged projections, termed "asperities". Surface asperities exist across multiple scales, often in a self affine or fractal geometry. The fractal dimension of these structures has been correlated with the contact mechanics exhibited at an interface in terms of friction and contact stiffness. When two macroscopically smooth surfaces come into contact, initially they only touch at a few of these asperity points. These cover only a very small portion of the surface area. Friction and wear originate at these points, and thus understanding their behavior becomes important when studying materials in contact. When the surfaces are subjected to a compressive load, the asperities deform through elastic and plastic modes, increasing the contact area between the two surfaces until the contact area is sufficient to support the load. The relationship between frictional interactions and asperity geometry is complex and poorly understood. It has been reported that an increased roughness may under certain circumstances result in weaker frictional interactions while smoother surfaces may in fact exhibit high levels of friction owing to high levels of true contact. The Archard equation provides a simplified model of asperity deformation when materials in contact are subject to a force. Due to the ubiquitous presence of deformable asperities in self affine hierarchical structures, the true contact area at an interface exhibits a linear relationship with the applied normal load. アスペリティ（英: asperity）は、地震学者の Thorne Lay と金森博雄が1980年に提唱した概念である。 애스패리티(영어: Asperity)는 판 경계의 접촉면 중 특히 마찰이 강한 부분을 뜻한다. 이 부분은 지진이 발생했을 때 특히 미끄럼 량이 커진다. 1981년에 가나모리 히로오가 제창했다.
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wikipedia-en:Asperity_(materials_science)?oldid=1122160860&ns=0
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3556
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wikipedia-en:Asperity_(materials_science)