The influence of the structure of a nanocrystalline solid (sandstone) on the dynamics of microcrack accumulation on friction
- 作者: Vettegren’ V.I.1, Ponomarev A.V.2, Shcherbakov I.P.1, Mamalimov R.I.1
-
隶属关系:
- Ioffe Institute
- Schmidt Institute of Physics of the Earth
- 期: 卷 59, 编号 8 (2017)
- 页面: 1580-1583
- 栏目: Mechanical Properties, Physics of Strength, and Plasticity
- URL: https://bakhtiniada.ru/1063-7834/article/view/200718
- DOI: https://doi.org/10.1134/S1063783417080315
- ID: 200718
如何引用文章
详细
On friction of a heterogeneous material: sandstone, flashes of triboluminescence are observed. Triboluminescence arises on the relaxation of excitation of free radicals ≡Si–O–. These radicals form on disruptions of Si–O–Si bonds and are located at microcrack edges. Microcracks form at the boundaries of feldspar and quartz microcrystals. Their sizes range from ~0.4 to ~7 μm. The microcrack formation on friction leads to the spalling of feldspar and quartz microcrystals from a sample.
作者简介
V. Vettegren’
Ioffe Institute
编辑信件的主要联系方式.
Email: Victor.Vettegren@mail.ioffe.ru
俄罗斯联邦, St. Petersburg, 194021
A. Ponomarev
Schmidt Institute of Physics of the Earth
Email: Victor.Vettegren@mail.ioffe.ru
俄罗斯联邦, Moscow, 123242
I. Shcherbakov
Ioffe Institute
Email: Victor.Vettegren@mail.ioffe.ru
俄罗斯联邦, St. Petersburg, 194021
R. Mamalimov
Ioffe Institute
Email: Victor.Vettegren@mail.ioffe.ru
俄罗斯联邦, St. Petersburg, 194021
补充文件
