TAILIEUCHUNG - Geotechnical Earthquake Considerations

Geotechnical Earthquake Considerations . Introduction . Seismology . Measurement of Earthquakes Magnitude • Intensity • Time History • Elastic Response Spectra • Inelastic Response Spectra 33 . Strong Motion Attenuation and Duration Probabilistic Seismic Hazard Analysis Site Response Basic Concepts • Evidence for Local Site Effects • Methods of Analysis • Site Effects for Different Soil Conditions Earthquake-Induced Settlement Settlement of Dry Sands • Settlement of Saturated Sands Ground Failure Liquefaction • Liquefaction Susceptibility • Initiation of Liquefaction • Lateral Spreading • Gloal Instability • Retaining Structures Steven Kramer University of Washington. | Kramer S. Scawthorn C. Geotechnical Earthquake Considerations. Bridge Engineering Handbook. Ed. Wai-Fah Chen and Lian Duan Boca Raton CRC Press 2000 Section IV Seismic Design 2000 by CRC Press LLC . . . . Steven Kramer 339 University of Washington Charles Scawthorn EQE International 33 Geotechnical Earthquake Considerations Introduction Seismology Measurement of Earthquakes Magnitude Intensity Time History Elastic Response Spectra Inelastic Response Spectra Strong Motion Attenuation and Duration Probabilistic Seismic Hazard Analysis Site Response Basic Concepts Evidence for Local Site Effects Methods of Analysis Site Effects for Different Soil Conditions Earthquake-Induced Settlement Settlement of Dry Sands Settlement of Saturated Sands Ground Failure Liquefaction Liquefaction Susceptibility Initiation of Liquefaction Lateral Spreading Gloal Instability Retaining Structures Soil Improvement Densification Techniques Drainage Techniques Reinforcement Techniques Grouting Mixing Techniques Introduction Earthquakes are naturally occurring broad-banded vibratory ground motions that are due to a number of causes including tectonic ground motions volcanism landslides rockbursts and manmade explosions the most important of which are caused by the fracture and sliding of rock along tectonic faults within the Earth s crust. For most earthquakes shaking and ground failure are the dominant and most widespread agents of damage. Shaking near the actual earthquake rupture lasts only during the time when the fault ruptures a process which takes seconds or at most a few minutes. The seismic waves generated by the rupture propagate long after the movement on the fault has stopped however spanning the globe in about 20 min. Typically earthquake ground 2000 by CRC Press .

TỪ KHÓA LIÊN QUAN
TAILIEUCHUNG - Chia sẻ tài liệu không giới hạn
Địa chỉ : 444 Hoang Hoa Tham, Hanoi, Viet Nam
Website : tailieuchung.com
Email : tailieuchung20@gmail.com
Tailieuchung.com là thư viện tài liệu trực tuyến, nơi chia sẽ trao đổi hàng triệu tài liệu như luận văn đồ án, sách, giáo trình, đề thi.
Chúng tôi không chịu trách nhiệm liên quan đến các vấn đề bản quyền nội dung tài liệu được thành viên tự nguyện đăng tải lên, nếu phát hiện thấy tài liệu xấu hoặc tài liệu có bản quyền xin hãy email cho chúng tôi.
Đã phát hiện trình chặn quảng cáo AdBlock
Trang web này phụ thuộc vào doanh thu từ số lần hiển thị quảng cáo để tồn tại. Vui lòng tắt trình chặn quảng cáo của bạn hoặc tạm dừng tính năng chặn quảng cáo cho trang web này.