DETECTING THE DIRECTION OF SEISMIC WAVE USING REAL TIME OPERATING SYSTEM

A natural geological occurrence known as a seismic earthquake occurs when the tectonic plates of Earth shift, shattering or cracking rock.Sometimes the shock wave is sensed as a vibration as it strikes the ground.The rock mass experiences changes in tension while being mined.These occur as a result of both the formation of cavities and our continued deep mining.Below and surrounding the mine, the rock stresses are re-distributed in novel ways.As a result, the strains may rise to the point where a seismic event takes place.Earthquakes, volcanic eruptions, explosions, landslides, avalanches, and surging rivers are examples of seismic events.All seismic occurrences, or vibrations in the earth that transport energy in the form of waves, produce seismic waves.Seismologists use accelerometers, hydrophones, geophones, and seismometers to examine seismic waves.In this study, the design of a sensor system and methods for real-time seismic wave direction detection are presented.Our method differs from the usual method mainly because to its limited aperture, ambiguity in orientation, and susceptibility to noise.In a given amount of time, we can determine the precise direction by putting our real-time operating system method into practice.An essential component of this application is the RTOS, which guarantees efficient task scheduling, prompt data processing, and system dependability.One of the projects contributing to the enhancement of sophisticated earthquake warning systems (EEWS) by HSE protocol that can result in timely response and disaster mitigation is this one.The reviews focuses on real-time monitoring of earthquakes, which can help emergency responders and disaster management teams respond quickly and effectively.From this review, it has the ability to contribute to the development of early warning systems for earthquakes, which can help save lives and reduce damage to infrastructure.