By Ljubomir Tanchev
Dams and Appurtenant Hydraulic constructions, now in its moment variation, offers a entire and whole assessment of all types of dams and appurtenant hydraulic constructions in the course of the world.
The reader is guided via various elements of dams and appurtenant hydraulic buildings in 35 chapters, that are subdivided in 5 themes:
I. Dams and appurtenant hydraulic constructions – General
II. Embankment dams
III. Concrete dams
IV. Hydromechanical apparatus and appurtenant hydraulic structures
V. Hydraulic schemes.
Subjects taken care of are basic questions, layout, development, surveillance, upkeep and reconstruction of assorted embankment and urban dams, hydromechanical gear, spillway buildings, backside shops, distinctive hydraulic buildings, composition of constructions in river hydraulic schemes, reservoirs, environmental results of river hydraulic schemes and reservoirs and environmental safeguard. specified consciousness is paid to complex tools of static and dynamic research of embankment dams.
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Extra info for Dams and Appurtenant Hydraulic Structures, 2nd edition
Dam builders, of course, have always been aware of this fact; however, the variety of features of the foundation, until not long ago, has dictated the experiences, together with some empirical rules, to be used mainly in the calculations of dams. The uppermost layer of the earth’s crust, which is interesting from the point of view of civil engineering, generally consists of three parts: the surface soil or topsoil, having a very limited depth and originating in the disintegration of organic matter.
Lipkovo 4. Gratche 5. Mladost 6. Globochica 7. Vodocha 8. Prilep 9. Tikvesh 10. Kalimanci 11. Shpilje 12. Ratevska 13. Turiya 14. Glaznja 15. Mantovo 16. Strezevo 17. Paljurci 18. Suvodol 19. Mavrovica 20. Podles 21. Ilovica 22. Kozyak 23. Loshana 24. Markova R. 25. Lisiche 26. Knezhevo 27. Saint Petka Treska Mavrovska Lipkovska Kochanska Otovica Crn Drim Vodocha Oreovechka Crna Reka Bregalnica Crn Drim Ratevska Turiya Lipkovska Lakavica Shemnica Luda Mara Suvodolska Mavrovica Vodnik Ilovichka Treska Loshana Markova R.
The degree of metamorphism is related to the conditions of temperature and pressure under which the new metamorphic rock has formed, and may be assessed by the appearance of certain new minerals. These index minerals, each of which indicates a particular temperature and pressure at the time it formed, are used to define the metamorphic grade of the rock in which they occur. Their presence and interpretation are conditional on the composition of the original parental rocks as well as on the grade of metamorphism.
Dams and Appurtenant Hydraulic Structures, 2nd edition by Ljubomir Tanchev