seismic risk map - перевод на русский
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seismic risk map - перевод на русский

STUDY OF THE RESPONSE OF BUILDINGS/STRUCTURES TO EARTHQUAKES
Seismic design; Seismic performance; Seismic performance analysis
Найдено результатов: 1455
seismic risk map      

строительное дело

карта сейсмических районов (страны)

seismic risk map      
карта сейсмических районов (страны)
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

risk aversion         
PREFERENCE AGAINST RISK, A COMMON HUMAN BEHAVIOR OF ATTEMPTING TO LOWER UNCERTAINTY AND AVOID RISK
Risk Aversion; Risk-aversion; Absolute risk aversion; Arrow-Pratt measure; Coefficient of absolute risk aversion; Coefficient of relative risk aversion; Decreasing absolute risk aversion; Increasing absolute risk aversion; Constant absolute risk aversion; Increasing relative risk aversion; Decreasing relative risk aversion; Constant Relative Risk Aversion; Risk averse; CARA utility; Risk tolerance; Risk tolerant; Risk-tolerant; Risk-averse; Log utility; Risk attitude; Co-efficient of absolute risk aversion; Risk Tolerance; Relative risk aversion; Risk aversion scale; Risk aversion (Economics); Risk aversion (economics)
неприятие риска

Определение

risk management
Risk management is the skill or job of deciding what the risks are in a particular situation and taking action to prevent or reduce them.
N-UNCOUNT

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 seismic risk map на Русский язык