{"id":26914,"date":"2023-02-27T12:44:00","date_gmt":"2023-02-27T15:44:00","guid":{"rendered":"https:\/\/mindthegraph.com\/blog\/what-is-stargazing-copy\/"},"modified":"2023-02-28T18:06:09","modified_gmt":"2023-02-28T21:06:09","slug":"earthquake-magnitude","status":"publish","type":"post","link":"https:\/\/mindthegraph.com\/blog\/tr\/deprem-buyuklugu\/","title":{"rendered":"Deprem B\u00fcy\u00fckl\u00fcklerini ve Etkilerini Anlamak"},"content":{"rendered":"

Depremler d\u00fcnyan\u0131n her yerinde d\u00fczenli olarak meydana gelen yayg\u0131n bir do\u011fal olayd\u0131r. Amerika Birle\u015fik Devletleri Jeolojik Ara\u015ft\u0131rmalar Kurumu'na (USGS) g\u00f6re, her y\u0131l y\u00fcz binlerce deprem meydana gelmekte ve bunlar\u0131n \u00e7o\u011fu insanlar taraf\u0131ndan fark edilemeyecek kadar zay\u0131f olmaktad\u0131r. <\/p>\n\n\n\n

Depremlerin s\u0131kl\u0131\u011f\u0131, meydana geldikleri yere ba\u011fl\u0131 olarak \u00f6nemli \u00f6l\u00e7\u00fcde de\u011fi\u015fir. Aktif levha s\u0131n\u0131rlar\u0131 \u00fczerinde yer almalar\u0131 nedeniyle, Kaliforniya ve Japonya gibi baz\u0131 yerlerde d\u00fczenli depremler ya\u015fan\u0131rken, di\u011ferlerinde sadece ara s\u0131ra depremler g\u00f6r\u00fclebilir.<\/p>\n\n\n\n

Suriye ve T\u00fcrkiye de depreme yatk\u0131n \u00fclkelerdir. T\u00fcrkiye, Afrika ve Avrasya tektonik plakalar\u0131n\u0131n s\u0131n\u0131r\u0131nda yer al\u0131rken, Suriye Afrika ve Arap tektonik plakalar\u0131n\u0131n s\u0131n\u0131r\u0131nda yer almaktad\u0131r. <\/p>\n\n\n\n

Bu nedenle 6 \u015eubat 2023'te korkun\u00e7 bir depremle kar\u015f\u0131 kar\u015f\u0131ya kald\u0131lar ve bu deprem 11.000'den fazla insan\u0131n \u00f6l\u00fcm\u00fcne ve on binlerce insan\u0131n yaralanmas\u0131na neden oldu. Depremin b\u00fcy\u00fckl\u00fc\u011f\u00fc 7.8'e ula\u015ft\u0131 ki bu \u00e7ok b\u00fcy\u00fck ve potansiyel olarak y\u0131k\u0131c\u0131 bir deprem olarak kabul ediliyor. <\/p>\n\n\n\n

Deprem b\u00fcy\u00fckl\u00fc\u011f\u00fc nedir?<\/h2>\n\n\n\n

Bir depremin b\u00fcy\u00fckl\u00fc\u011f\u00fc, deprem taraf\u0131ndan \u00fcretilen enerji miktar\u0131n\u0131 temsil etmek i\u00e7in kullan\u0131lan boyutunun veya g\u00fcc\u00fcn\u00fcn bir \u00f6l\u00e7\u00fcs\u00fcd\u00fcr. B\u00fcy\u00fckl\u00fck, sismik dalgalar\u0131n b\u00fcy\u00fckl\u00fc\u011f\u00fc ve g\u00f6zlemlenen yer hareketi miktar\u0131 kullan\u0131larak hesaplan\u0131r. <\/p>\n\n\n\n

1930'larda Charles Richter taraf\u0131ndan olu\u015fturulan Richter \u00f6l\u00e7e\u011fi, uzun y\u0131llar boyunca geleneksel deprem b\u00fcy\u00fckl\u00fc\u011f\u00fc \u00f6l\u00e7\u00fct\u00fc olmu\u015ftur, ancak g\u00fcn\u00fcm\u00fczde Moment B\u00fcy\u00fckl\u00fck \u00d6l\u00e7e\u011fi esasen onun yerini alm\u0131\u015ft\u0131r. <\/p>\n\n\n\n

Depremin b\u00fcy\u00fckl\u00fc\u011f\u00fc nas\u0131l \u00f6l\u00e7\u00fcl\u00fcr? <\/h2>\n\n\n\n

Bir depremin b\u00fcy\u00fckl\u00fc\u011f\u00fcn\u00fc \u00f6l\u00e7mek i\u00e7in bir\u00e7ok y\u00f6ntem vard\u0131r ve her yakla\u015f\u0131m depremin b\u00fcy\u00fckl\u00fc\u011f\u00fc hakk\u0131nda farkl\u0131 bir tahmin sunar. A\u015fa\u011f\u0131da en yayg\u0131n yakla\u015f\u0131mlar yer almaktad\u0131r:<\/p>\n\n\n\n

Richter \u00d6l\u00e7e\u011fi<\/h3>\n\n\n\n

Richter b\u00fcy\u00fckl\u00fck \u00f6l\u00e7e\u011fi, bir sismometre taraf\u0131ndan kaydedilen en b\u00fcy\u00fck sismik dalgay\u0131 temel al\u0131r ve depremin genel b\u00fcy\u00fckl\u00fc\u011f\u00fcn\u00fc tan\u0131mlayan tek bir de\u011fer sunar. <\/p>\n\n\n\n

Logaritmiktir, bu da b\u00fcy\u00fckl\u00fckteki k\u00fc\u00e7\u00fck bir art\u0131\u015f\u0131n deprem boyutunda \u00f6nemli bir art\u0131\u015fa neden oldu\u011fu anlam\u0131na gelir. \u00d6rne\u011fin 7.0 b\u00fcy\u00fckl\u00fc\u011f\u00fcndeki bir deprem 6.0 b\u00fcy\u00fckl\u00fc\u011f\u00fcndeki bir depremden on kat, 5.0 b\u00fcy\u00fckl\u00fc\u011f\u00fcndeki bir depremden ise y\u00fcz kat daha b\u00fcy\u00fckt\u00fcr.<\/p>\n\n\n\n

Richter b\u00fcy\u00fckl\u00fck \u00f6l\u00e7e\u011fi 0 ila 9 aras\u0131nda de\u011fi\u015fmekte olup, 2.0'dan k\u00fc\u00e7\u00fck say\u0131lar genellikle insanlar taraf\u0131ndan hissedilmez ve 8.0'dan b\u00fcy\u00fck say\u0131lar b\u00fcy\u00fck hasar ve felakete neden olabilecek b\u00fcy\u00fck depremler olarak kabul edilir. <\/p>\n\n\n\n

Moment B\u00fcy\u00fckl\u00fck \u00d6l\u00e7e\u011fi<\/h3>\n\n\n\n

Moment B\u00fcy\u00fckl\u00fck \u00d6l\u00e7e\u011fi, bir depremin b\u00fcy\u00fckl\u00fc\u011f\u00fcn\u00fc belirlemek i\u00e7in Richter b\u00fcy\u00fckl\u00fck \u00f6l\u00e7e\u011fine alternatif olarak sunulmu\u015ftur. Moment B\u00fcy\u00fckl\u00fck \u00d6l\u00e7e\u011fi, Richter b\u00fcy\u00fckl\u00fck \u00f6l\u00e7e\u011finin aksine, bir deprem taraf\u0131ndan \u00fcretilen toplam enerjiyi tahmin eder. <\/p>\n\n\n\n

Fay \u00fczerindeki kayma (hareket) miktar\u0131na, kayan fay\u0131n alan\u0131na ve yer kabu\u011funun sertli\u011fine dayanan bir deprem b\u00fcy\u00fckl\u00fc\u011f\u00fc olan sismik moment kavram\u0131na dayanmaktad\u0131r. Sismik moment, sismik dalga \u00f6l\u00e7\u00fcmlerinden elde edilir ve depremin Moment B\u00fcy\u00fckl\u00fc\u011f\u00fcn\u00fc de\u011ferlendirmek i\u00e7in kullan\u0131l\u0131r.<\/p>\n\n\n\n

Moment B\u00fcy\u00fckl\u00fck \u00d6l\u00e7e\u011fi, Richter b\u00fcy\u00fckl\u00fck \u00f6l\u00e7e\u011fi gibi logaritmiktir, bu da b\u00fcy\u00fckl\u00fckteki k\u00fc\u00e7\u00fck bir art\u0131\u015f\u0131n deprem boyutunda b\u00fcy\u00fck bir art\u0131\u015fa e\u015fit oldu\u011fu anlam\u0131na gelir.<\/p>\n\n\n\n

Moment B\u00fcy\u00fckl\u00fck \u00d6l\u00e7e\u011fi -2.0 ile 9.0 aras\u0131nda de\u011fi\u015fir ve \u00f6zellikle \u00f6nemli derinliklerde meydana gelen b\u00fcy\u00fck depremler i\u00e7in depremin b\u00fcy\u00fckl\u00fc\u011f\u00fcn\u00fc Richter b\u00fcy\u00fckl\u00fck \u00f6l\u00e7e\u011finden daha do\u011fru bir \u015fekilde \u00f6l\u00e7t\u00fc\u011f\u00fc i\u00e7in en s\u0131k kullan\u0131lan deprem b\u00fcy\u00fckl\u00fc\u011f\u00fc \u00f6l\u00e7e\u011fidir.<\/p>\n\n\n\n

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\u0130ll\u00fcstrasyon mevcut Mind the Graph<\/a><\/strong><\/em><\/figcaption><\/figure><\/div>\n\n\n
<\/div>\n\n\n\n

<\/a>Mercalli \u00d6l\u00e7e\u011fi<\/h3>\n\n\n\n

Mercalli \u00d6l\u00e7e\u011fi, bir depremin yerkabu\u011funun yan\u0131 s\u0131ra bireyler, binalar ve di\u011fer yap\u0131lar \u00fczerindeki etkilerini g\u00f6steren bir deprem \u015fiddeti \u00f6l\u00e7e\u011fidir. Mercalli \u00d6l\u00e7e\u011fi s\u0131kl\u0131kla depremin b\u00fcy\u00fckl\u00fc\u011f\u00fcn\u00fc belirlemek i\u00e7in kullan\u0131lan Richter veya Moment B\u00fcy\u00fckl\u00fck \u00d6l\u00e7e\u011fi ile birlikte kullan\u0131l\u0131r.<\/p>\n\n\n\n

\u00d6l\u00e7ek, I'den XII'ye kadar bir Roma rakam sistemine dayanmaktad\u0131r; I, insanlar taraf\u0131ndan hissedilmeyen zay\u0131f sars\u0131nt\u0131lar\u0131, XII ise yayg\u0131n hasar ve y\u0131k\u0131ma neden olan a\u015f\u0131r\u0131 \u015fiddetli sars\u0131nt\u0131lar\u0131 g\u00f6stermektedir. Depremin meydana geldi\u011fi y\u00fczeyin t\u00fcr\u00fcn\u00fc, etkilenen yap\u0131lar\u0131n t\u00fcr\u00fcn\u00fc ve neden oldu\u011fu y\u0131k\u0131m miktar\u0131n\u0131 dikkate al\u0131r.<\/p>\n\n\n\n

Mercalli \u00d6l\u00e7e\u011fi ve Moment B\u00fcy\u00fckl\u00fck \u00d6l\u00e7e\u011fi veya Richter \u00f6l\u00e7e\u011fi bir araya getirildi\u011finde, bir depremin hem b\u00fcy\u00fckl\u00fc\u011f\u00fcn\u00fc hem de etkisini kapsayan daha genel bir anlay\u0131\u015f sunar. <\/p>\n\n\n\n

\u00d6rne\u011fin, daha y\u00fcksek Moment B\u00fcy\u00fckl\u00fc\u011f\u00fcne sahip bir deprem daha az n\u00fcfuslu bir yerde meydana gelirse veya zemin hasara kar\u015f\u0131 daha az duyarl\u0131 ise, y\u00fcksek n\u00fcfuslu bir b\u00f6lgede daha d\u00fc\u015f\u00fck Moment B\u00fcy\u00fckl\u00fc\u011f\u00fcne sahip bir deprem kadar hasar vermeyebilir veya zemin hasara kar\u015f\u0131 olduk\u00e7a duyarl\u0131ysa, bu durumda hasarlar daha b\u00fcy\u00fck olabilir. <\/p>\n\n\n\n

Bu nedenle iki \u00f6l\u00e7e\u011fi birle\u015ftirmek en iyi yakla\u015f\u0131m olabilir \u00e7\u00fcnk\u00fc Mercalli \u00d6l\u00e7e\u011fi depremi ya\u015fayan ve g\u00f6rd\u00fckleri etkileri rapor eden bireylerin g\u00f6zlemlerine dayanmaktad\u0131r.<\/p>\n\n\n\n

Depremin merkez \u00fcss\u00fc nas\u0131l bulunur?<\/h2>\n\n\n\n

Sismologlar, bir depremin merkez \u00fcss\u00fcn\u00fc belirlemek i\u00e7in \u00fc\u00e7genleme olarak bilinen bir teknik kullan\u0131rlar. <\/p>\n\n\n\n

Nirengi hesaplamas\u0131n\u0131n alt\u0131nda yatan fikir, bir depremden kaynaklanan sismik dalgalar\u0131n farkl\u0131 malzemelerden farkl\u0131 h\u0131zlarda ge\u00e7erek merkez \u00fcss\u00fcnden farkl\u0131 mesafelerde bulunan sismografik istasyonlara farkl\u0131 zamanlarda ula\u015fmas\u0131d\u0131r. Sismologlar, sismik dalgalar\u0131n \u00e7e\u015fitli sismografik konumlara var\u0131\u015f zamanlar\u0131n\u0131 inceleyerek merkez \u00fcss\u00fcn\u00fcn konumunu tahmin edebilirler.<\/p>\n\n\n\n

Deprem \u015eiddeti<\/h2>\n\n\n\n
B\u00fcy\u00fckl\u00fck<\/th>Yo\u011funluk<\/th>Etki<\/th>Depremlerin ortalama oran\u0131<\/th><\/tr><\/thead>
2.0 veya daha az<\/strong><\/td>Mikro<\/td>Nadiren hissedilir<\/td>Y\u0131lda milyonlar\u0131n \u00fczerinde<\/td><\/tr>
2.0 ila 2.9<\/strong><\/td>K\u00fc\u00e7\u00fck<\/td>Hafif\u00e7e hissedilir<\/td>Y\u0131lda bir milyondan fazla<\/td><\/tr>
3.0 ila 3.9<\/strong><\/td>K\u00fc\u00e7\u00fckten daha fazlas\u0131<\/td>S\u0131kl\u0131kla hissedilen<\/td>Y\u0131lda y\u00fcz binden fazla<\/td><\/tr>
4.0 ila 4.9<\/strong><\/td>I\u015f\u0131k<\/td>\u00c7o\u011fu insan taraf\u0131ndan hissedilir<\/td>Y\u0131lda on binden fazla<\/td><\/tr>
5.0 ila 5.9<\/strong><\/td>Orta d\u00fczeyde<\/td>Zay\u0131f yap\u0131lara zarar verebilir<\/td>Y\u0131lda binden fazla<\/td><\/tr>
6.0 ila 6.9<\/strong><\/td>G\u00fc\u00e7l\u00fc<\/td>Orta derecede iyi in\u015fa edilmi\u015f yap\u0131larda hasara neden olur<\/td>Y\u0131lda y\u00fcz\u00fcn \u00fczerinde<\/td><\/tr>
7.0 ila 7.9<\/strong><\/td>Binba\u015f\u0131<\/td>\u00c7o\u011fu binada hasara neden olur<\/td>Y\u0131lda on ila yirmi<\/td><\/tr>
8.0 ila 8.9<\/strong><\/td>Harika<\/td>Binalarda b\u00fcy\u00fck hasar<\/td>Her y\u0131l bir tane<\/td><\/tr>
9.0 veya daha fazla<\/strong><\/td>En b\u00fcy\u00fck<\/td>T\u00fcm binalar\u0131 \u00e7\u00f6kertebilir<\/td>Her on veya daha fazla y\u0131lda bir<\/td><\/tr><\/tbody><\/table><\/figure>\n\n\n\n

Grafik \u00f6zetler, bilim adamlar\u0131 taraf\u0131ndan k\u00fcrat\u00f6rl\u00fc\u011f\u00fc yap\u0131lan bilim fig\u00fcrleri konusunda uzman\u0131z<\/h2>\n\n\n\n

Grafik \u00f6zetler, bilim insanlar\u0131n\u0131n karma\u015f\u0131k kavramlar\u0131 aktarmas\u0131na, temel bulgular\u0131 vurgulamas\u0131na, ara\u015ft\u0131rman\u0131n ke\u015ffedilebilirli\u011fini art\u0131rmas\u0131na ve \u00e7ok disiplinli \u00e7al\u0131\u015fmay\u0131 te\u015fvik etmesine yard\u0131mc\u0131 olabilir. Bilim insanlar\u0131 grafik \u00f6zetler kullanarak \u00e7al\u0131\u015fmalar\u0131n\u0131 daha eri\u015filebilir ve anla\u015f\u0131l\u0131r hale getirebilir, bu da bilim alan\u0131nda genel olarak ilerlemeye yard\u0131mc\u0131 olabilir. <\/p>\n\n\n\n

Grafik \u00f6zetler olu\u015fturmak i\u00e7in basit bir araca ihtiyac\u0131n\u0131z varsa, kullan\u0131c\u0131 dostu olmas\u0131 ama\u00e7lanan ve s\u0131n\u0131rl\u0131 tasar\u0131m becerilerine sahip olanlar\u0131n bile profesyonel kalitede grafikler \u00fcretmesine olanak tan\u0131yan bir ara\u00e7 olan Mind The Graph'i kullan\u0131n.<\/p>\n\n\n\n

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<\/p>","protected":false},"excerpt":{"rendered":"

Depremin b\u00fcy\u00fckl\u00fc\u011f\u00fcn\u00fc, en s\u0131k kullan\u0131lan \u00f6l\u00e7ekleri ve bir olay\u0131n \u015fiddetini nas\u0131l tahmin edebileceklerini anlaman\u0131n zaman\u0131 geldi.<\/p>","protected":false},"author":28,"featured_media":26924,"comment_status":"closed","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":[],"categories":[959,28],"tags":[],"yoast_head":"\nUnderstanding Earthquake Magnitudes and Their Impact<\/title>\n<meta name=\"description\" content=\"It's time to understand the earthquake magnitude, the most often used scales, and how they might predict the severity of an event.\" \/>\n<meta name=\"robots\" content=\"index, follow, max-snippet:-1, max-image-preview:large, max-video-preview:-1\" \/>\n<link rel=\"canonical\" href=\"https:\/\/mindthegraph.com\/blog\/tr\/wielkosc-trzesienia-ziemi\/\" \/>\n<meta property=\"og:locale\" content=\"tr_TR\" \/>\n<meta property=\"og:type\" content=\"article\" \/>\n<meta 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