Fracture Peculiarities of Porous Alumina Metamaterial / M. V. Grigoriev, V. I. Kashirina, S. N. Kulkov

Уровень набора: (RuTPU)RU\TPU\network\4816, AIP Conference ProceedingsОсновной Автор-лицо: Grigoriev, M. V.Альтернативный автор-лицо: Kashirina, V. I.;Kulkov, S. N., specialist in the field of material science, Professor of Tomsk Polytechnic University, Doctor of physical and mathematical sciences, 1952-, Sergey NikolaevichКоллективный автор (вторичный): Национальный исследовательский Томский политехнический университет, Инженерная школа новых производственных технологий, Отделение материаловеденияЯзык: английский.Резюме или реферат: It has been studied alumina ceramics with multilevel porous structure consist of macro and micro pores, and porous channels separate of material blocks. Macro-pores were formed ultra-high molecular weight polyethylene and porous channels were formed due to zonal shrinkage during sintering of green body. The percentage ratio of these pore types are 15%, 30% and 55% for pore channels, fine and large pores, respectively. It has been shown that first cracks are formed almost from the beginning of deformations - approximately not more 30% of fracture strength and localized near blocks boundaries. It has been shown that a main fracture type under compression test is fractured of individual blocks without fracture of whole sample. This means that fracture scale level decrease from macroscopic to mesoscopic one..Примечания о наличии в документе библиографии/указателя: [References: 14 tit.].Аудитория: .Тематика: электронный ресурс | труды учёных ТПУ | разрушение | метаматериалы | керамика | пористые структуры | трещины | деформации Ресурсы он-лайн:Щелкните здесь для доступа в онлайн
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[References: 14 tit.]

It has been studied alumina ceramics with multilevel porous structure consist of macro and micro pores, and porous channels separate of material blocks. Macro-pores were formed ultra-high molecular weight polyethylene and porous channels were formed due to zonal shrinkage during sintering of green body. The percentage ratio of these pore types are 15%, 30% and 55% for pore channels, fine and large pores, respectively. It has been shown that first cracks are formed almost from the beginning of deformations - approximately not more 30% of fracture strength and localized near blocks boundaries. It has been shown that a main fracture type under compression test is fractured of individual blocks without fracture of whole sample. This means that fracture scale level decrease from macroscopic to mesoscopic one.

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