| 书目名称 | Rock Anisotropy and the Theory of Stress Measurements |
| 编辑 | Bernard Amadei |
| 视频video | |
| 丛书名称 | Lecture Notes in Engineering |
| 图书封面 |  |
| 描述 | Any undisturbed rock mass is subject to natural stresses inclu ding gravitational stresses due to the mass of the overburden and possibly tectonic stresses due to the straining of the earth‘s crust and remanent stresses due to past tectonism. Knowledge of the in situ stress field must be integrated into any rock engineering design along with general rock mass characteristics such as de for mability, strength, permeability and time dependent behavior. For example, the choice of optimum orientation and shape of deep underground caverns or complex underground works will be controlled by the orientation and the magnitude of the in situ stress @ield if it is necessary to minimize stress concentration problems. Long term variation of the in situ stress field may also help to evaluate the potential hazard of earthquake occurences. The magnitude and orientation of the stress field ata point within a rock mass can be measured but there is no known method by which the state of stress at a point can be accurately determined by instruments located remotely. In general, measurements are made inside boreholes, on outcrops or on the internal surfaces of under ground cavities. Most of the measu |
| 出版日期 | Book 1983 |
| 关键词 | Anisotropie; Felsdynamik; Gestein; Spannungsmessung; Stress; Transformation; calculus; geometry |
| 版次 | 1 |
| doi | https://doi.org/10.1007/978-3-642-82040-3 |
| isbn_softcover | 978-3-540-12388-0 |
| isbn_ebook | 978-3-642-82040-3Series ISSN 0176-5035 |
| issn_series | 0176-5035 |
| copyright | Springer-Verlag Berlin Heidelberg 1983 |
发表于 2025-3-21 18:15:18
