reproduction of seismic records - перевод на русский
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reproduction of seismic records - перевод на русский

STUDY OF THE RESPONSE OF BUILDINGS/STRUCTURES TO EARTHQUAKES
Seismic design; Seismic performance; Seismic performance analysis
Найдено результатов: 51789
reproduction of seismic records      

нефтегазовая промышленность

воспроизведение сейсмических записей

seismic shock         
  • Earthquake wave paths
  • The scheme of motion for spheroidal <sub>0</sub>S<sub>2</sub> oscillation.Dashed lines give nodal (zero) lines. Arrows give the sense of motion.
  • The sense of motion for toroidal <sub>0</sub>T<sub>1</sub> oscillation for two moments of time.
  • The hypocenter/epicenter of an earthquake is calculated by using the seismic data of that earthquake from at least three different locations. The hypocenter/epicenter is found at the intersection of three circles centered on three observation stations, here shown in Japan, Australia and the United States. The radius of each circle is calculated from the difference in the arrival times of P- and S-waves at the corresponding station.
  • s2cid=4304379 }}</ref> The negligible ''S''-wave velocity in the outer core occurs because it is liquid, while in the solid inner core the ''S''-wave velocity is non-zero
  • Patterns of seismic wave travel through Earth’s mantle and core. S-waves can’t travel through the liquid outer core, so they leave a shadow on Earth’s far side. P-waves do travel through the core, but P-wave refraction bends seismic waves away from P-wave shadow zones.
SEISMIC, VOLCANIC, OR EXPLOSIVE ENERGY THAT TRAVELS THROUGH EARTH'S LAYERS
Seismic waves; Earth quake waves; Elastic p-wave; Elastic p wave; Elastic s wave; Elastic s-wave; Elastic P-Wave; Elastic S-Wave; Body wave (seismology); Seismic shock; Body-wave seismograms; Seismic velocity; Seismic Velocity; Seismic graph; Earthquake waves; Seismic energy; Seismic energy waves

нефтегазовая промышленность

сейсмический импульс

seismic waves         
  • Earthquake wave paths
  • The scheme of motion for spheroidal <sub>0</sub>S<sub>2</sub> oscillation.Dashed lines give nodal (zero) lines. Arrows give the sense of motion.
  • The sense of motion for toroidal <sub>0</sub>T<sub>1</sub> oscillation for two moments of time.
  • The hypocenter/epicenter of an earthquake is calculated by using the seismic data of that earthquake from at least three different locations. The hypocenter/epicenter is found at the intersection of three circles centered on three observation stations, here shown in Japan, Australia and the United States. The radius of each circle is calculated from the difference in the arrival times of P- and S-waves at the corresponding station.
  • s2cid=4304379 }}</ref> The negligible ''S''-wave velocity in the outer core occurs because it is liquid, while in the solid inner core the ''S''-wave velocity is non-zero
  • Patterns of seismic wave travel through Earth’s mantle and core. S-waves can’t travel through the liquid outer core, so they leave a shadow on Earth’s far side. P-waves do travel through the core, but P-wave refraction bends seismic waves away from P-wave shadow zones.
SEISMIC, VOLCANIC, OR EXPLOSIVE ENERGY THAT TRAVELS THROUGH EARTH'S LAYERS
Seismic waves; Earth quake waves; Elastic p-wave; Elastic p wave; Elastic s wave; Elastic s-wave; Elastic P-Wave; Elastic S-Wave; Body wave (seismology); Seismic shock; Body-wave seismograms; Seismic velocity; Seismic Velocity; Seismic graph; Earthquake waves; Seismic energy; Seismic energy waves

общая лексика

сейсмические волны

seismic design         

строительное дело

проектирование с учётом сейсмических воздействий

расчёт (зданий, сооружений) на сейсмические нагрузки (сейсмическое воздействие)

seismic wave         
  • Earthquake wave paths
  • The scheme of motion for spheroidal <sub>0</sub>S<sub>2</sub> oscillation.Dashed lines give nodal (zero) lines. Arrows give the sense of motion.
  • The sense of motion for toroidal <sub>0</sub>T<sub>1</sub> oscillation for two moments of time.
  • The hypocenter/epicenter of an earthquake is calculated by using the seismic data of that earthquake from at least three different locations. The hypocenter/epicenter is found at the intersection of three circles centered on three observation stations, here shown in Japan, Australia and the United States. The radius of each circle is calculated from the difference in the arrival times of P- and S-waves at the corresponding station.
  • s2cid=4304379 }}</ref> The negligible ''S''-wave velocity in the outer core occurs because it is liquid, while in the solid inner core the ''S''-wave velocity is non-zero
  • Patterns of seismic wave travel through Earth’s mantle and core. S-waves can’t travel through the liquid outer core, so they leave a shadow on Earth’s far side. P-waves do travel through the core, but P-wave refraction bends seismic waves away from P-wave shadow zones.
SEISMIC, VOLCANIC, OR EXPLOSIVE ENERGY THAT TRAVELS THROUGH EARTH'S LAYERS
Seismic waves; Earth quake waves; Elastic p-wave; Elastic p wave; Elastic s wave; Elastic s-wave; Elastic P-Wave; Elastic S-Wave; Body wave (seismology); Seismic shock; Body-wave seismograms; Seismic velocity; Seismic Velocity; Seismic graph; Earthquake waves; Seismic energy; Seismic energy waves

нефтегазовая промышленность

сейсмическая волна

seismic analysis         

нефтегазовая промышленность

сейсмический анализ

seismic design         
проектирование с учётом сейсмических воздействий; расчёт (зданий, сооружений) на сейсмические нагрузки (сейсмическое воздействие)
seismic energy         
  • Earthquake wave paths
  • The scheme of motion for spheroidal <sub>0</sub>S<sub>2</sub> oscillation.Dashed lines give nodal (zero) lines. Arrows give the sense of motion.
  • The sense of motion for toroidal <sub>0</sub>T<sub>1</sub> oscillation for two moments of time.
  • The hypocenter/epicenter of an earthquake is calculated by using the seismic data of that earthquake from at least three different locations. The hypocenter/epicenter is found at the intersection of three circles centered on three observation stations, here shown in Japan, Australia and the United States. The radius of each circle is calculated from the difference in the arrival times of P- and S-waves at the corresponding station.
  • s2cid=4304379 }}</ref> The negligible ''S''-wave velocity in the outer core occurs because it is liquid, while in the solid inner core the ''S''-wave velocity is non-zero
  • Patterns of seismic wave travel through Earth’s mantle and core. S-waves can’t travel through the liquid outer core, so they leave a shadow on Earth’s far side. P-waves do travel through the core, but P-wave refraction bends seismic waves away from P-wave shadow zones.
SEISMIC, VOLCANIC, OR EXPLOSIVE ENERGY THAT TRAVELS THROUGH EARTH'S LAYERS
Seismic waves; Earth quake waves; Elastic p-wave; Elastic p wave; Elastic s wave; Elastic s-wave; Elastic P-Wave; Elastic S-Wave; Body wave (seismology); Seismic shock; Body-wave seismograms; Seismic velocity; Seismic Velocity; Seismic graph; Earthquake waves; Seismic energy; Seismic energy waves

нефтегазовая промышленность

сейсмическая энергия, энергия сейсмических волн

Guinness Book of Records         
  • Guinness Museum in Hollywood
  • The North Beach ([[Nazaré, Portugal]]), listed on the Guinness World Records for the biggest waves ever surfed
  • archive-date=10 May 2013}}</ref>
  • access-date=12 January 2020}}</ref>
  • m}}, as verified by ''Guinness World Records''.
  • url-status=live}}</ref> Petrosino set record times for 250 ml, 500 ml and 1.5 litres as well, but Guinness accepted only the record for one litre. They later dropped all alcohol records from their compendium in 1991, then reinstated the records in 2008.
  • Indian Canadian]] film actor and producer and multiple-Guinness World Record holder who has broken over 50 world records set in several countries in attempts to benefit the underprivileged children around the world. Some world record attempts are more unusual than others: he is pictured here minutes away from breaking the [[ironing]] world record at 2 days, 7 hours and 5 minutes, at [[Shoppers World, Brampton]].
  • Japanese competitive eater [[Takeru Kobayashi]] with two Guinness World Record certificates
  • lc=y}}.
  • Ross]] at 107 [[Fleet Street]], London, in August 1955
REFERENCE BOOK LISTING WORLD RECORDS
Guinness Book of World Records; The Guinness Book of World Records; Guiness Book of World Records; Guiness Book of Records; Guinness Book Of World Records; Guinness Record Book; Guinness World Record; Guinness book of records; Guiness world record; Guiness book of records; Guinness Book of World records; The Guinness World Records; Guinness Book of Records; The Guinness World Record; Guinness Book; Guinness World Book of Records; Guiness World Records; Guiness book of world records; Guinness record; Guiness World Records 2006; Guinness world record; Guinness book of world record; Guinness Book Of Records; The Guinness Book Of Records; The Guinness Book of Records; World guiness records; Book of world records; Guinness world records; Features of Guinness World Records Books; List of Guinness World Records Books; Guiness record; Guinness Record; Guiness World Records Ltd.; Guiness World Record; Guiness book; Guinness World Records Gamer's Edition; Guinness world records gamers edition; Guinness world records, 2008; Guinness book; Guinness World Records Gamer's Edition, 2009; Gbowr; Craig Glenday; Guinness World Records Gamer's Edition, 2010; Guinness World Record Gamer's Edition, 2010; Guinness World Records Gamer's Edtion, 2010; Guinness Publishing; Guinness Records; Guiness records; Guinness Superlatives; Guinness book of World Records; Guinness World Records Limited; Impossible Vietnamese VG; The Guinness Book Of World Records; Guinness World Records (TV series); GUINNESS WORLD RECORDS; Guinness world records 2014; Guinness Books; Guinness Worlds Record; Guinness Worlds Records; Guinness World's Record; Guinness World's Records; Guiness Worlds Record; Guiness Worlds Records; Guiness World's Record; Guiness World's Records; The Guiness Book of Records; The Guinness Book of Worlds Records; The Guinness Book of World's Records; The Guiness Book of World Records; The Guiness Book of Worlds Records; The Guiness Book of World's Records; Guinness Book of Worlds Records; Guinness Book of World's Records; Guiness Book of Worlds Records; Guiness Book of World's Records; Guinness World Records Gamer’s Edition; Guinness World Records 2011 Gamers' Edition; Guinness World Record Gamer's Edtion, 2010; Guinness World Records 2016 Gamer's Edition; Guinness record holder; Guinness World Records Corporate; Guinness Book Records; GuinnessWorldRecords.com; Guinnessworldrecords.com; Guinness World Records, Ltd.; Guiness Records

[,gɪnɪs,bukəv'rekɔ:dz]

общая лексика

"Книга рекордов Гиннесса" (ежегодный справочник, издающийся компанией "Гиннесс" [Guinness]; содержит данные о рекордах в самых различных областях. Выходит с 1955)

public records         
RECORDS ORIGINATING WITH OR MAINTAINED BY A GOVERNMENT AND AVAILABLE FOR ACCESS BY THE PUBLIC
Public record; Record (administrative); Public Record; Local records; Town records; Administrative documents; Public records request; Public records requests
судебные протоколы

Определение

грип
ГРИП, ГРИПП, гриппа, ·муж. (·франц. grippe) (мед.). Инфекционная болезнь - катарральное воспаление дыхательных путей, сопровождаемое лихорадочным состоянием; то же, что инфлуэнца
.

Википедия

Seismic analysis

Seismic analysis is a subset of structural analysis and is the calculation of the response of a building (or nonbuilding) structure to earthquakes. It is part of the process of structural design, earthquake engineering or structural assessment and retrofit (see structural engineering) in regions where earthquakes are prevalent.

As seen in the figure, a building has the potential to 'wave' back and forth during an earthquake (or even a severe wind storm). This is called the 'fundamental mode', and is the lowest frequency of building response. Most buildings, however, have higher modes of response, which are uniquely activated during earthquakes. The figure just shows the second mode, but there are higher 'shimmy' (abnormal vibration) modes. Nevertheless, the first and second modes tend to cause the most damage in most cases.

The earliest provisions for seismic resistance were the requirement to design for a lateral force equal to a proportion of the building weight (applied at each floor level). This approach was adopted in the appendix of the 1927 Uniform Building Code (UBC), which was used on the west coast of the United States. It later became clear that the dynamic properties of the structure affected the loads generated during an earthquake. In the Los Angeles County Building Code of 1943 a provision to vary the load based on the number of floor levels was adopted (based on research carried out at Caltech in collaboration with Stanford University and the U.S. Coast and Geodetic Survey, which started in 1937). The concept of "response spectra" was developed in the 1930s, but it wasn't until 1952 that a joint committee of the San Francisco Section of the ASCE and the Structural Engineers Association of Northern California (SEAONC) proposed using the building period (the inverse of the frequency) to determine lateral forces.

The University of California, Berkeley was an early base for computer-based seismic analysis of structures, led by Professor Ray Clough (who coined the term finite element. Students included Ed Wilson, who went on to write the program SAP in 1970, an early "finite element analysis" program.

Earthquake engineering has developed a lot since the early days, and some of the more complex designs now use special earthquake protective elements either just in the foundation (base isolation) or distributed throughout the structure. Analyzing these types of structures requires specialized explicit finite element computer code, which divides time into very small slices and models the actual physics, much like common video games often have "physics engines". Very large and complex buildings can be modeled in this way (such as the Osaka International Convention Center).

Structural analysis methods can be divided into the following five categories.

Как переводится reproduction of seismic records на Русский язык