Stability Slopes Underground Excavations (41 results)

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Taschenbuch. Condition: Neu. Stability of Slopes and Underground Excavations | Proceedings of Indian Geotechnical Conference 2020 Volume 3 | C. N. V. Satyanarayana Reddy (u. a.) | Taschenbuch | Lecture Notes in Civil Engineering | x | Englisch | 2022 | Springer | EAN 9789811656033 | Verantwortliche Person für die EU: Springer Ve…rlag GmbH, Tiergartenstr. 17, 69121 Heidelberg, juergen[dot]hartmann[at]springer[dot]com | Anbieter: preigu.

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Buch. Condition: Neu. Druck auf Anfrage Neuware - Printed after ordering - This book comprises select proceedings of the Indian Geotechnical Conference 2020 (IGC2020) focusing on recent developments in the field of transportation geotechnics, scour and erosion, offshore geotechnics, and environmental geotechnology. The contents…are useful to academicians, researchers, practitioners and policymakers to understand and tackle the challenges in an efficient manner and to adopt appropriate sustainable geotechnical engineering solutions.

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Stability of Slopes and Underground Excavations: Proceedings of Indian Geotechnical Conference 2020 Volume 3: 185 (Lecture Notes in Civil Engineering)
Satyanarayana Reddy, C. N. V. (Editor)/ Muthukkumaran, K. (Editor)/ Vaidya, Ravikiran (Editor)
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Taschenbuch. Condition: Neu. Druck auf Anfrage Neuware - Printed after ordering - Die folgenden Ausfiihrungen behandeln die Absehatzung der Seitendruek ziffer A fiir den Orange-Fish-Tunnel in Siidafrika. 3 Der Tunnel solI eine Wassermenge von 50 m /see vom Verwoerd-Stausee des Orange-River in das Gebiet des grofSen Fish-River br…ingen, urn dieses zu bewassern. Die Gesamtlange des Tunnels betragt etwa 85 km, der Ausbruehsdureh messer 6 m. Der Orange-Fish-Tunnel dureh6rtert eine im geologischen Sinne ruhige Landschaft. Er liegt im Karroo-Becken, welches von Sedimenten, vorwiegend Sandsteinen, Sehluffsteinen und Steinmergeln gefii11t ist. Die Ablagerungen sind dureh einen haufigen Weehsel dieser Gesteins arten sowohl in horizontaler wie in vertikaler Erstreckung gekennzeiehnet und werden von Dolerit-Intrusionen durehadert. Der Tunnel wird von mehreren Orten zugleieh vorgetrieben. Yom Ein lafSbauwerk aus, von sieben Zugangssehaehten und vom AuslafSbauwerk aus. Es war vorgesehen, den Tunnel mit einem rasehen Vortrieb aufzufahren. Ober weite Strecken (etwa 85 %) des Tunnels war eine geringfiigige, provi sorische Sicherung durch Anker sowie eine endgiiltige Betonauskleidung von etwa 23 em Dicke vorgesehen (diese fiir die ganze Tunnellange). Beim Tunnelvortrieb sind jedoeh unerwartete Sehwierigkeiten aufgetre ten, und auch in der betonierten endgiiltigen Auskleidung stellten sich Risse ein, die nicht erwartet worden waren. 2. Abschatzung der Seitendruckziffer aus der Geologischen Vorgeschichte Yom Kenntnisstand des Untertagebaues zum Zeitpunkt der Projektierung des Orange-Fish-Tunnel ausgehend ist zu sagen, dafS in etwa mit A-Werten im Bereich von 0,25 bis 1,2 zu rechnen war.

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Taschenbuch. Condition: Neu. Druck auf Anfrage Neuware - Printed after ordering - Bei der Durchfiihrung der Bauarbeiten fiir den Ausbruch des Hauptstrangs 2 der Zuleitungen Ost des Pumpspeicherwerks Hongrin-Uman ,3 ergaben sich in ihrem AusmaJ3 nicht vorhergesehene Schwierigkeiten. Dieser Stollen miindet prak tisch am Ende des S…taues (hochster Stauspiegel 1255,00 m) auf Kote 1250,00 m, im Tal des Hongrinbaches Paquier-Clavel in das Speicherbecken. Es handelt sich urn 2 einen Freispiegelstollen iiblicher Form, Querschnitt 5 bis 8 m , Langsgefalle 3 %0. Aus der Gesamtanordnung des Stollensystems ergab sich die Notwendigkeit, den Hauptstrang durch das Massif des Mont d'Or zu fiihren (Abb. 1 und 2). Der ,N BASSIN O 'CCUMUlAlION HONGRIN /~ Fain. ,00 0 500 1000' ~ .,f ''j';';;!;iil!~!I~I!;lilt~~:/:~ ::::::::: : ''~~~A''' Abb. 1. Chaine du Mont-d'Or - Lageplan der Zuleitungen Ost (nach J. Nor be r t, Geologe, Lausanne) Dichter Fels: 1 Tonschiefer mit Kalksandstein; 2 Anhydrit und Gips. Durchlassiger Fels: 3 zermalmte Rauhwacke; 4 stark zerkliifteter Dolomit und Dolomitenkalk; 5 zerkliifteter Kalkstein Chaine du Mont d'Or - Plan of galleries, East adduction Non water-bearing rock: 1 Clayey schist with sandy-limestone; 2 Anhydrite and gypsum. Water-bearing rock: 3 'Cornieules' (crushed yellow honeycomb dolomite); 4 Dolomitic limestone and badly fractured dolomite; 5 Fissured limestone Chaine du Mont d'Or - Situation des adductions Est Roches etanches: 1 Schiste argileux it niveaux greso-calcaires (flysch); 2 Anhydrite et gypse.

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Condition: New. Dieser Artikel ist ein Print on Demand Artikel und wird nach Ihrer Bestellung fuer Sie gedruckt. This book comprises select proceedings of the Indian Geotechnical Conference 2020 (IGC2020) focusing on recent developments in the field of transportation geotechnics, scour and erosion, offshore geotechnics, and envi…ronmental geotechnology. The contents.

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