Nanocracks at Destruction of Nepheline

IF 0.9 4区 地球科学 Q4 GEOCHEMISTRY & GEOPHYSICS
V. I. Vettegren, A. V. Ponomarev, R. I. Mamalimov, I. P. Shcherbakov
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Abstract

Fracture process in crystals begin from the formation of tiny (“primary”) cracks. Larger cracks are formed when these primary cracks unite. To register primary cracks that appear on the surface of a nepheline crystal during the destruction by diamond microcrystals, the fractoluminescence method is used. The fractoluminescence spectrum consists of three bands: 1.4, 1.68, and 1.98 eV. The 1.98-eV band corresponds to excited free radicals ≡Si–O, 1.68 eV corresponds to excited Fe3+• ions, and the 1.4-eV band appears when empty traps are filled with electrons from the conduction band. These radicals, ions, and traps appear during the fracture of nepheline lattice cells and are located on the surface of “primary” cracks. The time dependences of the fractoluminescence signals are sets of separate signals with a duration of about 86 ns. The interval between the signals varies from 0.1 to 1 μs. The nepheline crystal has a hexagonal system and six systems of dislocation slip planes. At the intersection of these planes, six barriers are formed, which prevent the movement of dislocations. The breaking of each barrier causes the appearance of a primary crack and the formation of a peak in the fractoluminescence signal. When six barriers are broken, clusters are formed from the same number of primary cracks. Therefore, fractoluminescence signals contain six maxima. First, the largest crack appears. Its dimensions range from approximately 9 to 17 nm. The growth time of such crack is about 16 ns. The remaining (smaller) cracks have sizes 1.7 to 3.0 times smaller. The size distribution of cracks follows a power law with an exponent equal to 6.

Abstract Image

奈弗林毁灭中的纳米裂纹
晶体的断裂过程始于微小(“原生”)裂纹的形成。当这些原始裂缝结合在一起时,就会形成更大的裂缝。为了记录在钻石微晶破坏过程中霞石晶体表面出现的原生裂纹,采用了断裂发光方法。分形发光光谱由1.4、1.68和1.98 eV三个波段组成。1.98 eV波段对应于激发的自由基≡Si-O•,1.68 eV对应于激发的Fe3+•离子,而1.4 eV波段则出现在空阱被来自导带的电子填充时。这些自由基、离子和陷阱出现在霞石晶格细胞断裂的过程中,并位于“初级”裂纹的表面。断裂发光信号的时间依赖性是一组持续时间约为86 ns的独立信号。信号之间的间隔为0.1 ~ 1 μs。霞石晶体具有一个六边形体系和六个位错滑移面体系。在这些平面的交叉处,形成了六个屏障,以防止位错的移动。每一个障壁的破裂都会导致原始裂纹的出现,并在断裂发光信号中形成一个峰。当六个屏障被打破时,由相同数量的主裂缝形成簇。因此,断裂发光信号包含六个最大值。首先,出现最大的裂缝。它的尺寸范围从大约9到17纳米。裂纹的扩展时间约为16ns。剩下的(较小的)裂缝的尺寸是原来的1.7到3.0倍。裂纹的尺寸分布遵循指数为6的幂律。
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来源期刊
Izvestiya, Physics of the Solid Earth
Izvestiya, Physics of the Solid Earth 地学-地球化学与地球物理
CiteScore
1.60
自引率
30.00%
发文量
60
审稿时长
6-12 weeks
期刊介绍: Izvestiya, Physics of the Solid Earth is an international peer reviewed journal that publishes results of original theoretical and experimental research in relevant areas of the physics of the Earth''s interior and applied geophysics. The journal welcomes manuscripts from all countries in the English or Russian language.
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