Vui lòng dùng định danh này để trích dẫn hoặc liên kết đến tài liệu này: http://thuvienso.vanlanguni.edu.vn/handle/Vanlang_TV/18836
Nhan đề: Effect of Garnet Characteristics on Abrasive Waterjet Cutting of Hard Granite Rock
Tác giả: Oh, Tae-Min
Joo, Gun-Wook
Cha, Yohan
Cho, Gye-Chun
Từ khoá: Velocity
Tensile strength
Minerals
Specific gravity
Garnets
Cutting parameters
Particle size distribution
Abrasive cutting
Particle size
Physical properties
Disintegration
Stone
Advanced manufacturing technologies
Mechanics
Abrasive erosion
Abrasives
Feed rate
Efficiency
Năm xuất bản: 2019
Nhà xuất bản: Hindawi Limited
Tóm tắt: Abrasive waterjet cutting technology has come back into use in the field of rock excavation (such as for tunneling) due to the need for precision construction with low vibration. Because the abrasive particles play an important role in efficient erosion during the cutting process, the abrasive characteristics strongly affect the rock cutting performance. In this study, rock cutting tests were performed with five different coarse (40 mesh) garnets to explore the effect of the abrasive feed rate, physical properties, and particle size distribution on rock cutting performance. In addition, garnet particle disintegration was investigated with garnet characteristics for the abrasive waterjet. The test results indicate that the particle size distribution, garnet purity, specific gravity, and hardness are the most important parameters for rock cutting performance. This study offers better understanding of coarse garnet performance and efficiency according to the garnet characteristics. This should provide assistance in selection of the garnet needed to achieve the desired performance for hard rock cutting.
Mô tả: "Hindawi Advances in Civil Engineering Volume 2019, Article ID 5732649, 12 pages https://doi.org/10.1155/2019/5732649"
Định danh: http://thuvienso.vanlanguni.edu.vn/handle/Vanlang_TV/18836
ISSN: 1687-8086
1687-8094 (eISSN)
Bộ sưu tập: Bài báo_lưu trữ

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BBKH1130_TCCN_Effect of Garnet Characteristics.pdf
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