Abstract

The article is devoted to an extremely important topic of searching for a short-term warning of the entry of destructive vibrations in the territory of Ukraine by assessing in real-time conditions the characteristics of the seismic process — magnitude and localization parameters of the earthquake source, using the mathematical apparatus of neural network modeling. To solve the problem of estimating the parameters characterizing the zone of the excitation source and the geometry of the source-station system, the authors use the initial, least distorted P -sections of seismic signals, examining the postulate that by recording a seismic signal lasting several seconds after its entry, it is possible in real time it is sufficient to accurately predict the bypass of the expected signal (and, therefore, to estimate the magnitude) of the occurring earthquake. The simulation algorithm on networks of artificial neurons uses to determine the time, extremely dangerous from the point of view of seismic risk, the recording of earthquakes in the restricted zone of the sources of the Vrancea zone using the example of one seismic station “Odessa”. Magnitude prediction estimates are demonstrated on various components of earthquake records for time windows of various lengths. The authors also summarize the considered approach, extending it to the network of “Odessa”, “Skvira”, “Poltava” stations and those recorded on them, possibly dangerous later, seismic events at an epicentral distance of up to 12°. Estimates of the prediction of magnitude, depth of the source and the coordinates of the epicenter are demonstrated on the various components of earthquake records for time windows of various lengths. The proposed algorithms can be applied both in the automatic processing of seismic information and the seismic hazard prediction, which provides for direct operational intervention of seismological services in the seismic hazard assessment.

Highlights

  • Êëþ÷åâûå ñëîâà: íåéðîñåòåâîå ìîäåëèðîâàíèå, îöåíêà ïðåäñêàçàíèÿ, ñåéñìè÷åñêàÿ îïàñíîñòü, çåìëåòðÿñåíèÿ, ìàãíèòóäà, ïàðàìåòðû ëîêàëèçàöèè, ãëóáèíà èñòî÷íèêà, íà÷àëüíûå ó÷àñòêè ñèãíàëà, êðàòêîñðî÷íîå ïðåäóïðåæäåíèå, àëãîðèòì

  • â àëãîðèòìå èñïîëüçîâàíû çàïèñè çåìëåòðÿñåíèé Âðàí÷à â îãðàíè÷åííîé çîíå èñòî÷íèêîâ íà ïðèìåðå ñåéñìè÷åñêîé ñòàíöèè “Îäåññà”. Äàííûé ïîäõîä îáîáùåí äëÿ ñåòè ñòàíöèé “Îäåññà”

  • Îö3íêà ãëèáèíè ã3ïîöåíòðà 3 ìàãí3òóäè íàâ÷åíî¿ íåéðîííî¿ ìåðåæ3, çáóäæåíî¿ 39 âåêòîðàìè, ñôîðìîâàíèõ ç E-N-Z-êîìïîíåíòîþ çàïèñó çåìëåòðóñ3â ðåã3îíó ìîäåëþâàííÿ ìåðåæåþ ñåéñì3÷íèõ ñòàíö3é

Read more

Summary

Introduction

Êëþ÷åâûå ñëîâà: íåéðîñåòåâîå ìîäåëèðîâàíèå, îöåíêà ïðåäñêàçàíèÿ, ñåéñìè÷åñêàÿ îïàñíîñòü, çåìëåòðÿñåíèÿ, ìàãíèòóäà, ïàðàìåòðû ëîêàëèçàöèè, ãëóáèíà èñòî÷íèêà, íà÷àëüíûå ó÷àñòêè ñèãíàëà, êðàòêîñðî÷íîå ïðåäóïðåæäåíèå, àëãîðèòì. Íåéðîìåðåæåâå îö3íþâàííÿ ìàãí3òóäè 3 ïàðàìåòð3â ëîêàë3çàö3¿ çàðåoñòðîâàíèõ çåìëåòðóñ3â äæåðåëà Âðàí÷à çà äàíèìè ñåéñì3÷íî¿ ñòàíö3¿ “Îäåñà”. Îñîáëèâîñò3 ôóíêö3îíóâàííÿ íåéðîìåðåæåâî¿ ìîäåë3 ç ìåòîþ îö3íêè ìàãí3òóäè 3 ãëèáèíè ã3ïîöåíòðà äæåðåë çåìëåòðóñó, çàðåoñòðîâàíèõ ñåéñì3÷íîþ ñòàíö3oþ “Îäåñà” çà ïåð3îä 1997—2012 ðð., ðîçãëÿíóòî ðàí3øå [Ëàçàðåíêî, Ãåðàñèìåíêî, 2004, 2013].

Results
Conclusion
Full Text
Published version (Free)

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call