{"id":4839,"date":"2011-12-20T15:51:53","date_gmt":"2011-12-20T13:51:53","guid":{"rendered":"http:\/\/www.islamidavet.com\/kutuphane\/\/?p=4839"},"modified":"2011-12-20T15:51:53","modified_gmt":"2011-12-20T13:51:53","slug":"kutle-hareketleri","status":"publish","type":"post","link":"https:\/\/www.islamidavet.com\/kutuphane\/kutle-hareketleri\/","title":{"rendered":"K\u00fctle hareketleri"},"content":{"rendered":"<p>Tan\u0131m: Hi\u00e7bir ta\u015f\u0131y\u0131c\u0131 (r\u00fczg\u00e2r, su, buzul) etkisi olmaks\u0131z\u0131n yery\u00fcz\u00fcn\u00fcn a\u015fa\u011f\u0131ya do\u011fru hareket etmesi, \u015fekil ve yer de\u011fi\u015ftirmesidir.<\/p>\n<p> K\u00fctle hareketlerinin s\u0131n\u0131fland\u0131r\u0131lmas\u0131<\/p>\n<p> D\u00fc\u015fme (Fall)<br \/>\n Akma (Flow)<br \/>\n Yava\u015f Akma (Creep)<br \/>\n H\u0131zl\u0131 Akma<br \/>\n Devrilme (Topple)<br \/>\n Kayma (Slide)<br \/>\n D\u00fczlemsel Kayma<br \/>\n Dairesel Kayma (Heyelan, Landslide)<br \/>\n Yanal Yay\u0131lma (Spread)<\/p>\n<p>D\u00dc\u015eME (FALL)<\/p>\n<p> Tan\u0131m: D\u0131\u015f ve i\u00e7 fakt\u00f6rler etkisi ile kopan malzemenin a\u015fa\u011f\u0131ya do\u011fru hareket etmesidir.<\/p>\n<p> Sebepleri<br \/>\n Topuk oyulmalar\u0131<br \/>\n \u00c7atlak ve k\u0131r\u0131klardaki erime ve donma olaylar\u0131<br \/>\n Hidrostatik bas\u0131n\u00e7 sonucu geni\u015flemeyle yer\u00e7ekiminin ba\u011flay\u0131c\u0131 kuvvetlerinden daha b\u00fcy\u00fck hale gelmesidir.<br \/>\n D\u00fc\u015fme hareketi ba\u015flang\u0131c\u0131; dalgalar\u0131n etkisiyle meydana gelen topuk oyulmas\u0131<br \/>\n D\u00fc\u015fme hareketi; k\u0131r\u0131k ya da \u00e7atlaklardaki donma olaylar\u0131 ve yer\u00e7ekimi<\/p>\n<p>AKMA (FLOW)<\/p>\n<p> Tan\u0131m:Y\u00fczeyde kayalar\u0131n ayr\u0131\u015fmas\u0131 sonucu olu\u015fmu\u015f kumlu, killi zeminlerde, toprak ya da ta\u015f-toprak kar\u0131\u015f\u0131m\u0131ndan ibaret y\u00fczeysel \u00f6rt\u00fcde, su miktar\u0131n\u0131n artmas\u0131 sonucunda geli\u015fen harekettir.<\/p>\n<p> Belirtileri<br \/>\n A\u011fa\u00e7lar\u0131n g\u00f6vdelerinin e\u011filmesi<br \/>\n Yap\u0131lar\u0131n, duvarlar\u0131n ve telefon direklerinin d\u00fc\u015feyden ka\u00e7mas\u0131<br \/>\n Yol, \u00e7it ve duvar gibi yap\u0131lar\u0131n yer de\u011fi\u015ftirmesi<br \/>\n Tabaka u\u00e7lar\u0131n\u0131n d\u0131\u015far\u0131ya do\u011fru k\u0131vr\u0131lmas\u0131<br \/>\n Tabakalar\u0131n a\u015fa\u011f\u0131ya do\u011fru akmas\u0131<br \/>\n Topografya y\u00fczeyinin k\u00fc\u00e7\u00fck basamakl\u0131 bir yap\u0131 kazanmas\u0131<\/p>\n<p> 1. Yava\u015f Akma (Creep) <\/p>\n<p> Tan\u0131m:Yamac\u0131n ya da \u015fevin y\u00fczeysel k\u0131sm\u0131n\u0131n s\u00fcrekli ama \u00e7ok yava\u015f yer de\u011fi\u015ftirmesidir.<\/p>\n<p> Hareket h\u0131z\u0131 y\u0131lda 2\u20133 cm olabilir.<br \/>\n Bloktan, silt ve kile kadar her \u00e7aptaki malzemede g\u00f6r\u00fclebilir.<\/p>\n<p> Sebepleri<br \/>\n Yer\u00e7ekimi<br \/>\n Y\u00fczeydeki malzemenin \u0131slanmas\u0131-kurumas\u0131<br \/>\n Y\u00fczeydeki malzemenin \u0131slak olmas\u0131 halinde i\u00e7erdi\u011fi suyun donmas\u0131-erimesi<br \/>\n Yeralt\u0131 ve yer\u00fcst\u00fc sular\u0131n\u0131n etkisi<br \/>\n Bitki k\u00f6klerinin b\u00fcy\u00fcmesi<br \/>\n Oyucu hayvanlar\u0131netkisi<\/p>\n<p>2. H\u0131zl\u0131 Akma<\/p>\n<p> Tan\u0131m: Yava\u015f akman\u0131n olu\u015ftu\u011fu toprak, ta\u015f-toprak kar\u0131\u015f\u0131m\u0131 yada ayr\u0131\u015fma sonucu gev\u015femi\u015f bloklu k\u0131s\u0131mlar\u0131n alttaki k\u0131smen veya tamamen ge\u00e7irimsiz temel \u00fczerinde g\u00f6zle g\u00f6r\u00fclebilecek bir h\u0131zla yama\u00e7 a\u015fa\u011f\u0131 hareket etmeleridir.<\/p>\n<p>DEVR\u0130LME (TOPPLE)<\/p>\n<p> Tan\u0131m:Bu harekette e\u011fik y\u00fczey boyunca kayma s\u00f6z konusu de\u011fildir. Buradaki hareket bir d\u00f6nme hareketidir. D\u00f6nme blo\u011fun e\u011fim a\u00e7\u0131s\u0131ndaki kenar\u0131 boyunca olmaktad\u0131r.<\/p>\n<p> KAYMA (SL\u0130DE) <\/p>\n<p> Tan\u0131m: Toprak, ta\u015f veya bunlar\u0131n kar\u0131\u015f\u0131m\u0131ndan olu\u015fan malzemelerin yer\u00e7ekimi etkisiyle belirli bir y\u00fczey boyunca a\u015fa\u011f\u0131ya do\u011fru hissedilebilir bir \u015fekilde hareket etmesidir.<\/p>\n<p> Sebepleri<br \/>\n Yama\u00e7 topuklar\u0131nda yap\u0131lan kaz\u0131lar ve a\u015f\u0131nd\u0131rmalar<br \/>\n Yama\u00e7lara fazla ek y\u00fck konmas\u0131<br \/>\n Y\u00fczey ve yeralt\u0131 sular\u0131<br \/>\n Ayr\u0131\u015fma<br \/>\n Farkl\u0131 litolojide kaya ardalanmas\u0131<br \/>\n Yer\u00e7ekimi<\/p>\n<p>1.D\u00fczlemsel Kayma<\/p>\n<p> Tan\u0131m:Yerli kayalar\u0131n tabaka, \u00e7atlak, k\u0131r\u0131k ya da herhangi bir s\u00fcreksizlik y\u00fczeyi boyunca s\u0131n\u0131rl\u0131 bir \u015fekilde a\u015fa\u011f\u0131ya do\u011fru hareket etmesidir.<\/p>\n<p>2. Dairesel Kayma (Heyelan, Landslide)<\/p>\n<p> Tan\u0131maha \u00e7ok ayr\u0131k veya zay\u0131f \u00e7imentolu ya da \u00e7ok s\u0131k \u00e7atlakl\u0131 kayalarda g\u00f6r\u00fcl\u00fcr.<\/p>\n<p> \u00c7o\u011funlukla birbirine paralel birden fazla kayma y\u00fczeyi geli\u015febilir.<\/p>\n<p>YANAL YAYILMA (SPREAD)<\/p>\n<p> Tan\u0131m:Kohezyonlu zemin veya kaya k\u00fctlesinin alttaki yumu\u015fak tabaka i\u00e7ine k\u0131r\u0131larak batmas\u0131 sonucu uzamas\u0131d\u0131r.<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tan\u0131m: Hi\u00e7bir ta\u015f\u0131y\u0131c\u0131 (r\u00fczg\u00e2r, su, buzul) etkisi olmaks\u0131z\u0131n yery\u00fcz\u00fcn\u00fcn a\u015fa\u011f\u0131ya do\u011fru hareket etmesi, \u015fekil ve yer de\u011fi\u015ftirmesidir. K\u00fctle hareketlerinin s\u0131n\u0131fland\u0131r\u0131lmas\u0131 D\u00fc\u015fme (Fall) Akma (Flow) Yava\u015f Akma (Creep) H\u0131zl\u0131 Akma Devrilme (Topple) Kayma (Slide) D\u00fczlemsel Kayma Dairesel Kayma (Heyelan, Landslide) Yanal Yay\u0131lma (Spread) D\u00dc\u015eME (FALL) Tan\u0131m: D\u0131\u015f ve i\u00e7 fakt\u00f6rler etkisi ile kopan malzemenin a\u015fa\u011f\u0131ya do\u011fru &hellip;<\/p>\n","protected":false},"author":1,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[1403,1406],"tags":[3105,10399,3107,2752],"class_list":["post-4839","post","type-post","status-publish","format-standard","hentry","category-odevler","category-sosyal-bilgiler-odevleri","tag-heyelan","tag-kutle-hareketleri","tag-topografya","tag-yercekimi"],"_links":{"self":[{"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/posts\/4839","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/comments?post=4839"}],"version-history":[{"count":0,"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/posts\/4839\/revisions"}],"wp:attachment":[{"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/media?parent=4839"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/categories?post=4839"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/tags?post=4839"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}