{"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\/lv\/zemestrices-lielums\/","title":{"rendered":"Izpratne par zemestr\u012b\u010du lielumu un to ietekmi"},"content":{"rendered":"

Zemestr\u012bces ir pla\u0161i izplat\u012bta dabas par\u0101d\u012bba, kas regul\u0101ri notiek vis\u0101 pasaul\u0113. Saska\u0146\u0101 ar Amerikas Savienoto Valstu \u0122eolo\u0123isk\u0101s izp\u0113tes dienesta (USGS) datiem katru gadu notiek simtiem t\u016bksto\u0161u zemestr\u012b\u010du, no kur\u0101m liel\u0101k\u0101 da\u013ca ir p\u0101r\u0101k v\u0101jas, lai cilv\u0113ki t\u0101s paman\u012btu. <\/p>\n\n\n\n

Zemestr\u012b\u010du bie\u017eums iev\u0113rojami at\u0161\u0137iras atkar\u012bb\u0101 no to ra\u0161an\u0101s vietas. Da\u017e\u0101s viet\u0101s, piem\u0113ram, Kalifornij\u0101 un Jap\u0101n\u0101, zemestr\u012bces notiek regul\u0101ri, savuk\u0101rt cit\u0101s viet\u0101s, piem\u0113ram, Kalifornij\u0101 un Jap\u0101n\u0101, zemestr\u012bces var b\u016bt tikai epizodiskas.<\/p>\n\n\n\n

Ar\u012b S\u012brij\u0101 un Turcij\u0101 bie\u017ei notiek zemestr\u012bces. Turcija atrodas uz \u0100frikas un Eir\u0101zijas tektonisko pl\u0101t\u0146u robe\u017eas, savuk\u0101rt S\u012brija atrodas uz \u0100frikas un Ar\u0101bijas tektonisko pl\u0101t\u0146u robe\u017eas. <\/p>\n\n\n\n

T\u0101p\u0113c 2023. gada 6. febru\u0101r\u012b vi\u0146us piemekl\u0113ja briesm\u012bga zemestr\u012bce, kur\u0101 g\u0101ja boj\u0101 vair\u0101k nek\u0101 11 000 cilv\u0113ku un v\u0113l desmitiem t\u016bksto\u0161u tika ievainoti. Zemestr\u012bces stiprums sasniedza 7,8 magnit\u016bdas, kas tiek uzskat\u012bta par \u013coti lielu un potenci\u0101li posto\u0161u zemestr\u012bci. <\/p>\n\n\n\n

Kas ir zemestr\u012bces lielums?<\/h2>\n\n\n\n

Zemestr\u012bces lielums ir zemestr\u012bces lieluma vai stipruma r\u0101d\u012bt\u0101js, ko izmanto, lai atspogu\u013cotu zemestr\u012bces rad\u012bt\u0101s ener\u0123ijas daudzumu. Lielumu apr\u0113\u0137ina, izmantojot seismisko vi\u013c\u0146u lielumu un nov\u0113roto zemes kust\u012bbu daudzumu. <\/p>\n\n\n\n

Daudzus gadus tradicion\u0101l\u0101 zemestr\u012b\u010du lieluma m\u0113rvien\u012bba bija Rihtera skala, ko 1930. gados izveidoja \u010c\u0101rlzs Rihters, ta\u010du pa\u0161laik to ir aizst\u0101jusi Moment\u0101 re\u0123istr\u0113t\u0101 magnit\u016bdu skala. <\/p>\n\n\n\n

K\u0101 izm\u0113r\u012bt zemestr\u012bces lielumu? <\/h2>\n\n\n\n

Zemestr\u012bces lieluma m\u0113r\u012b\u0161anai ir daudz meto\u017eu, un katra metode sniedz at\u0161\u0137ir\u012bgu zemestr\u012bces lieluma nov\u0113rt\u0113jumu. T\u0101l\u0101k ir aprakst\u012btas visizplat\u012bt\u0101k\u0101s pieejas:<\/p>\n\n\n\n

Rihtera skala<\/h3>\n\n\n\n

Rihtera skalas lieluma m\u0113r\u012bjumu pamat\u0101 ir liel\u0101kais seismiskais vilnis, ko re\u0123istr\u0113 seismometrs, un t\u0101 sniedz vienu v\u0113rt\u012bbu, kas raksturo zemestr\u012bces kop\u0113jo lielumu. <\/p>\n\n\n\n

T\u0101 ir logaritmiska, kas noz\u012bm\u0113, ka neliels magnit\u016bdas pieaugums izraisa iev\u0113rojamu zemestr\u012bces lieluma pieaugumu. Piem\u0113ram, 7,0 magnit\u016bdas zemestr\u012bce ir desmit reizes liel\u0101ka nek\u0101 6,0 magnit\u016bdas zemestr\u012bce un simts reizes liel\u0101ka nek\u0101 5,0 magnit\u016bdas zemestr\u012bce.<\/p>\n\n\n\n

Zemestr\u012bces lielums p\u0113c Rihtera skalas ir no 0 l\u012bdz 9, un zem 2,0 parasti cilv\u0113ki nej\u016bt, bet zemestr\u012bces, kas ir liel\u0101kas par 8,0, tiek uzskat\u012btas par sp\u0113c\u012bg\u0101m zemestr\u012bc\u0113m, kas var izrais\u012bt pla\u0161us post\u012bjumus un katastrofas. <\/p>\n\n\n\n

Momenta lieluma skala<\/h3>\n\n\n\n

Momentmagnit\u016bdu skala tika ieviesta k\u0101 alternat\u012bva Rihtera skalai zemestr\u012b\u010du lieluma noteik\u0161anai. At\u0161\u0137ir\u012bb\u0101 no Rihtera magnit\u016bdu skalas Momentmagnit\u016bdu skala nov\u0113rt\u0113 zemestr\u012bces rad\u012bto kop\u0113jo ener\u0123iju. <\/p>\n\n\n\n

T\u0101 pamat\u0101 ir seismisk\u0101 momenta koncepcija, kas ir zemestr\u012bces lielums, kura pamat\u0101 ir sl\u012bd\u0113\u0161anas (kust\u012bbas) apjoms uz l\u016bzuma, sl\u012bdo\u0161\u0101 l\u016bzuma laukums un Zemes garozas st\u012bvums. Seismiskais moments tiek ieg\u016bts no seismisko vi\u013c\u0146u m\u0113r\u012bjumiem un tiek izmantots, lai nov\u0113rt\u0113tu zemestr\u012bces momenta lielumu.<\/p>\n\n\n\n

Moment magnit\u016bdu skala, t\u0101pat k\u0101 Rihtera magnit\u016bdu skala, ir logaritmiska, kas noz\u012bm\u0113, ka neliels magnit\u016bdu pieaugums ir l\u012bdzv\u0113rt\u012bgs milz\u012bgam zemestr\u012bces lieluma pieaugumam.<\/p>\n\n\n\n

Zemestr\u012b\u010du magnit\u016bdu skala sv\u0101rst\u0101s no -2,0 l\u012bdz 9,0, un t\u0101 ir visbie\u017e\u0101k izmantot\u0101 zemestr\u012b\u010du magnit\u016bdu skala, jo ar to zemestr\u012bces lielumu m\u0113ra daudz prec\u012bz\u0101k nek\u0101 ar Rihtera skalu, jo \u012bpa\u0161i lielu zemestr\u012b\u010du gad\u012bjum\u0101, kas notiek liel\u0101 dzi\u013cum\u0101.<\/p>\n\n\n\n

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Ilustr\u0101cija pieejama Mind the Graph<\/a><\/strong><\/em><\/figcaption><\/figure><\/div>\n\n\n
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<\/a>Merkalli skala<\/h3>\n\n\n\n

Merkalli skala ir zemestr\u012b\u010du stipruma skala, kas att\u0113lo zemestr\u012b\u010du ietekmi uz Zemes garozu, k\u0101 ar\u012b uz cilv\u0113kiem, \u0113k\u0101m un cit\u0101m konstrukcij\u0101m. Mercalli skalu bie\u017ei izmanto kop\u0101 ar Rihtera skalu vai Moment magnit\u016bdu skalu, ko izmanto, lai noteiktu zemestr\u012bces lielumu.<\/p>\n\n\n\n

Skalas pamat\u0101 ir romie\u0161u ciparu sist\u0113ma no I l\u012bdz XII, kur I apz\u012bm\u0113 v\u0101jus gr\u016bdienus, kurus cilv\u0113ki nej\u016bt, bet XII apz\u012bm\u0113 \u0101rk\u0101rt\u012bgi sp\u0113c\u012bgus gr\u016bdienus, kas izraisa pla\u0161us post\u012bjumus un post\u012bjumus. Taj\u0101 tiek \u0146emts v\u0113r\u0101 virsmas veids, uz kuras notiek zemestr\u012bce, skarto strukt\u016bru veids un nodar\u012bto post\u012bjumu apjoms.<\/p>\n\n\n\n

Mercalli skala un Momentmagnit\u016bdu skala jeb Rihtera skala kop\u0101 sniedz pla\u0161\u0101ku priek\u0161statu par zemestr\u012bci, ietverot gan t\u0101s lielumu, gan ietekmi. <\/p>\n\n\n\n

Piem\u0113ram, ja zemestr\u012bce ar liel\u0101ku momenta lielumu notiek maz\u0101k apdz\u012bvot\u0101 viet\u0101 vai ja zeme ir maz\u0101k jut\u012bga pret boj\u0101jumiem, t\u0101 var nenodar\u012bt tik lielus post\u012bjumus k\u0101 zemestr\u012bce ar maz\u0101ku momenta lielumu bl\u012bvi apdz\u012bvot\u0101 re\u0123ion\u0101 vai ja zeme ir \u013coti jut\u012bga pret boj\u0101jumiem, tad post\u012bjumi \u0161aj\u0101 situ\u0101cij\u0101 var b\u016bt liel\u0101ki. <\/p>\n\n\n\n

T\u0101p\u0113c abu skalu apvieno\u0161ana var b\u016bt vislab\u0101k\u0101 pieeja, jo Mercalli skala ir balst\u012bta uz to cilv\u0113ku nov\u0113rojumiem, kuri piedz\u012bvoja zemestr\u012bci un zi\u0146oja par redz\u0113to ietekmi.<\/p>\n\n\n\n

K\u0101 noteikt zemestr\u012bces epicentru?<\/h2>\n\n\n\n

Lai noteiktu zemestr\u012bces epicentru, seismologi izmanto metodi, kas paz\u012bstama k\u0101 triangul\u0101cija. <\/p>\n\n\n\n

Triangul\u0101cijas pamatideja ir t\u0101da, ka zemestr\u012bces rad\u012btie seismiskie vi\u013c\u0146i caur da\u017e\u0101diem materi\u0101liem p\u0101rvietojas ar at\u0161\u0137ir\u012bgu \u0101trumu un da\u017e\u0101dos laikos non\u0101k seismogr\u0101fiskaj\u0101s stacij\u0101s, kas atrodas da\u017e\u0101dos att\u0101lumos no epicentra. Seismologi var nov\u0113rt\u0113t epicentra atra\u0161an\u0101s vietu, izp\u0113tot seismisko vi\u013c\u0146u iera\u0161an\u0101s laiku vair\u0101k\u0101s seismogr\u0101fiskaj\u0101s viet\u0101s.<\/p>\n\n\n\n

Zemestr\u012bces intensit\u0101te<\/h2>\n\n\n\n
Magnit\u016bda<\/th>Intensit\u0101te<\/th>Ietekme<\/th>Zemestr\u012b\u010du vid\u0113jais bie\u017eums<\/th><\/tr><\/thead>
2,0 vai maz\u0101k<\/strong><\/td>Micro<\/td>Reti j\u016btams<\/td>Vair\u0101k nek\u0101 miljoni gad\u0101<\/td><\/tr>
2,0 l\u012bdz 2,9<\/strong><\/td>Maznoz\u012bm\u012bgs<\/td>Nedaudz j\u016btams<\/td>Vair\u0101k nek\u0101 viens miljons gad\u0101<\/td><\/tr>
3,0 l\u012bdz 3,9<\/strong><\/td>Vair\u0101k nek\u0101 neliels<\/td>Bie\u017ei j\u016btas<\/td>Vair\u0101k nek\u0101 simts t\u016bksto\u0161i gad\u0101<\/td><\/tr>
4,0 l\u012bdz 4,9<\/strong><\/td>Gaisma<\/td>Liel\u0101k\u0101 da\u013ca cilv\u0113ku j\u016bt<\/td>Vair\u0101k nek\u0101 desmit t\u016bksto\u0161i gad\u0101<\/td><\/tr>
5,0 l\u012bdz 5,9<\/strong><\/td>M\u0113rens<\/td>Var saboj\u0101t sliktas strukt\u016bras<\/td>Vair\u0101k nek\u0101 t\u016bkstotis gad\u0101<\/td><\/tr>
6,0 l\u012bdz 6,9<\/strong><\/td>Sp\u0113c\u012bgs<\/td>Nodara boj\u0101jumus vid\u0113ji labi uzb\u016bv\u0113t\u0101m konstrukcij\u0101m.<\/td>Vair\u0101k nek\u0101 simts gad\u0101<\/td><\/tr>
7,0 l\u012bdz 7,9<\/strong><\/td>Liel\u0101kais<\/td>Liel\u0101kajai da\u013cai \u0113ku nodara boj\u0101jumus<\/td>Desmit l\u012bdz divdesmit gad\u0101<\/td><\/tr>
8,0 l\u012bdz 8,9<\/strong><\/td>Lielisks<\/td>Liel\u0101ki boj\u0101jumi \u0113k\u0101m<\/td>Vienu reizi gad\u0101<\/td><\/tr>
9,0 vai vair\u0101k<\/strong><\/td>Liel\u0101kais<\/td>Var sabrukt visas \u0113kas<\/td>reizi desmit vai vair\u0101k gados<\/td><\/tr><\/tbody><\/table><\/figure>\n\n\n\n

M\u0113s specializ\u0113jamies grafiskos kopsavilkumos, zin\u0101tniskajos skait\u013cos, kurus ir izstr\u0101d\u0101ju\u0161i zin\u0101tnieki.<\/h2>\n\n\n\n

Grafiskie kopsavilkumi var pal\u012bdz\u0113t zin\u0101tniekiem atspogu\u013cot sare\u017e\u0123\u012btus j\u0113dzienus, uzsverot galvenos atkl\u0101jumus, palielinot p\u0113tniec\u012bbas atkl\u0101jam\u012bbu un veicinot starpdisciplin\u0101ru darbu. Zin\u0101tnieki var padar\u012bt savus p\u0113t\u012bjumus pieejam\u0101kus un saprotam\u0101kus, izmantojot grafiskos kopsavilkumus, kas var veicin\u0101t progresu zin\u0101tnes jom\u0101 vis\u0101s jom\u0101s. <\/p>\n\n\n\n

Ja jums ir nepiecie\u0161ams vienk\u0101r\u0161s r\u012bks grafisku kopsavilkumu \u0123ener\u0113\u0161anai, izmantojiet Mind The Graph - lietot\u0101jam draudz\u012bgu r\u012bku, kas \u013cauj ikvienam, pat cilv\u0113kam ar ierobe\u017eot\u0101m dizaina prasm\u0113m, rad\u012bt profesion\u0101las kvalit\u0101tes grafikas.<\/p>\n\n\n\n

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

Ir pien\u0101cis laiks izprast zemestr\u012b\u010du lielumu, visbie\u017e\u0101k izmantot\u0101s skalas un to, k\u0101 ar t\u0101m var prognoz\u0113t notikuma nopietn\u012bbu.<\/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\/lv\/wielkosc-trzesienia-ziemi\/\" \/>\n<meta property=\"og:locale\" content=\"lv_LV\" \/>\n<meta property=\"og:type\" content=\"article\" \/>\n<meta property=\"og:title\" 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