{"id":20736,"date":"2015-05-05T19:00:49","date_gmt":"2015-05-05T16:00:49","guid":{"rendered":"https:\/\/e-marineeducation.com\/tr\/?p=20736"},"modified":"2015-05-05T14:48:29","modified_gmt":"2015-05-05T11:48:29","slug":"gemilerin-denizdeki-alti-hareketi","status":"publish","type":"post","link":"https:\/\/e-marineeducation.com\/tr\/gemilerin-denizdeki-alti-hareketi\/","title":{"rendered":"Gemilerin Denizdeki Alt\u0131 Hareketi"},"content":{"rendered":"

\"GemilerinSu i\u00e7erisinde y\u00fczmekte olan bir gemi, makinesi \u00e7al\u0131\u015fm\u0131yor bile olsa daima hareket halinde olacakt\u0131r. Bunun sebebi ise ba\u015fl\u0131ca okyanus ak\u0131nt\u0131lar\u0131<\/em><\/span>, r\u00fczg\u00e2rlar <\/em><\/span>ve<\/em> medcezir<\/em> <\/span>ak\u0131nt\u0131lar\u0131d\u0131r. Dalgalar\u0131n olu\u015fumu, sin\u00fczoidal olmayan dalga modeli teorisi<\/em><\/span> ile (Trochoidal Theory) a\u00e7\u0131klanmaktad\u0131r.<\/p>\n\n\n\n
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\"Wind<\/p>\n\n\n\n
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Gemiler su i\u00e7erisinde makineleriyle yol al\u0131rlarken \u00e7e\u015fitli hareketler sergilerler. Gemi personelince genellikle ba\u015f-k\u0131\u00e7 ve yalpa hareketleri hissedilir. Fakat asl\u0131nda geminin yapmakta oldu\u011fu alt\u0131 hareket vard\u0131r. Bu hareketler: yalpalama<\/span><\/em> (rolling), ba\u015f-k\u0131\u00e7 vurma<\/em><\/span> (pitching), savrulma<\/span><\/em> (yawing), dal\u0131p-\u00e7\u0131kma<\/em><\/span> (heaving), ileri-geri \u00f6teleme<\/em> <\/span>(surging), yan \u00f6teleme<\/em><\/span> (swaying) olarak literat\u00fcrde kabul g\u00f6rm\u00fc\u015ft\u00fcr.<\/p>\n\n\n\n
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\u015eimdi bu hareketleri incelemeye ba\u015flayal\u0131m. \u00d6ncelikle geminin i\u00e7inden ge\u00e7mekte olan X, Y ve Z eksenlerini hayal etmeliyiz. L\u00fctfen a\u015fa\u011f\u0131daki g\u00f6rseli inceleyiniz.<\/p>\n\n\n\n
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\"Six<\/strong><\/p>\n\n\n\n
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1. Yalpalama (Rolling):<\/strong> Yalpalama, geminin X ekseni etraf\u0131nda yapm\u0131\u015f oldu\u011fu rotatif (d\u00f6ner) bir harekettir. Gemi, sakin su i\u00e7erisinde y\u00fczer vaziyetteyken geminin a\u011f\u0131rl\u0131k merkezi ve kald\u0131rma kuvveti merkezi d\u00fc\u015fey olarak \u00fcst \u00fcstedir. Bir dalga tepesinin geminin sancak taraf\u0131na vurmas\u0131 durumunda bu taraftaki sualt\u0131 hacmi artacakt\u0131r. Bu durumda da kald\u0131rma kuvvetinin merkezi veya di\u011fer bir de\u011fi\u015fle sualt\u0131 hacminin merkezi sanca\u011fa do\u011fru hareket edecektir. Sanca\u011fa hareket eden sualt\u0131 hacmi merkezi art\u0131k a\u011f\u0131rl\u0131k merkezi ile ayn\u0131 hizada olmad\u0131\u011f\u0131ndan dolay\u0131 arada kald\u0131ra\u00e7 olu\u015fur. Bu kald\u0131ra\u00e7 geminin iskeleye do\u011fru meyletmesine neden olur. Dalga tepesi iskele tarafa ge\u00e7ti\u011finde ise yukar\u0131da anlat\u0131lanlar\u0131n tam tersi ger\u00e7ekle\u015fir.<\/p>\n\n\n\n
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2. Ba\u015f-k\u0131\u00e7 vurma (Pitching):<\/strong> Ba\u015f-k\u0131\u00e7 vurma hareketi, geminin Y ekseni etraf\u0131nda yapm\u0131\u015f oldu\u011fu rotatif bir harekettir. Gemi sakin su i\u00e7erisinde y\u00fczer vaziyetteyken geminin a\u011f\u0131rl\u0131k merkezi ve kald\u0131rma kuvveti merkezi d\u00fc\u015fey olarak \u00fcst \u00fcstedir. Bir dalga tepesinin geminin ba\u015f taraf\u0131na vurmas\u0131 durumunda bu b\u00f6l\u00fcmdeki sualt\u0131 hacmi artacakt\u0131r. Bu durumda da kald\u0131rma kuvvetinin merkezi veya di\u011fer bir de\u011fi\u015fle sualt\u0131 hacminin merkezi ba\u015f tarafa do\u011fru hareket edecektir. Fakat gemi \u00fczerindeki a\u011f\u0131rl\u0131klar\u0131n de\u011fi\u015fmemesinden dolay\u0131 a\u011f\u0131rl\u0131k merkezinin yeri de\u011fi\u015fmez ve art\u0131k a\u011f\u0131rl\u0131k merkezi ile kald\u0131rma kuvveti ayn\u0131 hizada olamazlar ve dolay\u0131s\u0131yla arada kald\u0131ra\u00e7 olu\u015fur. Bu kald\u0131ra\u00e7 geminin k\u0131\u00e7a do\u011fru meyletmesine neden olur. Dalga tepesi geminin k\u0131\u00e7\u0131na do\u011fru ge\u00e7ti\u011finde yukar\u0131da anlat\u0131lanlar\u0131n tam tersi ger\u00e7ekle\u015fir.<\/p>\n\n\n\n
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3. Savrulma (Yawing):<\/strong> Savrulma hareketi, geminin Z ekseni etraf\u0131nda yapt\u0131\u011f\u0131 rotatif bir harekettir. Bir dalga tepesi gemiye sancak ba\u015f omuzluktan geldi\u011finde pruva iskele tarafa dalga istikametinde itilecektir. Sancak ba\u015f omuzlukta olu\u015fan bir dalga \u00e7ukuru ise geminin bordasal olarak sanca\u011fa do\u011fru kaymas\u0131na neden olacakt\u0131r. Dalga tepesinin iskele ba\u015f omuzluktan gelmesi durumunda da yukar\u0131da anlat\u0131lanlar\u0131n tam tersi olacakt\u0131r.<\/p>\n\n\n\n
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4. Dal\u0131p \u2013 \u00c7\u0131kma (Heaving):<\/strong> Dal\u0131p \u2013 \u00e7\u0131kma hareketi geminin Z ekseninde yapm\u0131\u015f oldu\u011fu do\u011frusal bir harekettir. Bu hareket sert havalarda g\u00f6zlemlenir. Geminin alt\u0131na b\u00fcy\u00fck dalgalar geldi\u011finde, t\u00fcm gemi b\u00fct\u00fcn olarak yukar\u0131ya kald\u0131r\u0131l\u0131r. Gemi alt\u0131na dalga \u00e7ukuru geldi\u011finde ise gemi b\u00fct\u00fcn olarak a\u015fa\u011f\u0131ya iner. Dalgalar oldu\u011fu m\u00fcddet\u00e7e gemi, do\u011frusal olarak Z eksenindeki sal\u0131n\u0131m\u0131na devam edecektir.<\/p>\n\n\n\n
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5. Boy \u00d6teleme (Surging):<\/strong> Boy \u00f6teleme hareketi geminin X ekseninde yapm\u0131\u015f oldu\u011fu do\u011frusal bir harekettir. Dalga tepesinin geminin ba\u015f\u0131ndan veya k\u0131\u00e7\u0131ndan gelmesi durumunda gemi dalgan y\u00f6n\u00fcnde bedensel olarak itilecektir. Benzer \u015fekilde geminin ba\u015f\u0131ndan veya k\u0131\u00e7\u0131ndan bir dalga \u00e7ukuru gelmesi durumunda da gemi bedensel olarak dalga \u00e7ukuruna \u00e7ekilecektir. Dalgalar oldu\u011fu m\u00fcddet\u00e7e gemi, do\u011frusal olarak X eksenindeki sal\u0131n\u0131m\u0131na devam edecektir.<\/p>\n\n\n\n
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6. Yan \u00d6teleme (Swaying):<\/strong> Yan \u00f6teleme hareketi geminin Y ekseninde yapm\u0131\u015f oldu\u011fu do\u011frusal harekettir. Sancak bordadan dalga tepesinin gelmesi durumunda gemi iskele tarafa dalga istikametinde itilecektir. Benzer \u015fekilde sancak tarafta dalga \u00e7ukuru olmas\u0131 durumunda gemi bu \u00e7ukura do\u011fru \u00e7ekilecektir. Dalga tepesinin iskele bordadan gelmesi durumunda da yukar\u0131da anlat\u0131lanlar\u0131n tam tersi olacakt\u0131r. Dalgalar oldu\u011fu m\u00fcddet\u00e7e gemi, do\u011frusal olarak Y eksenindeki sal\u0131n\u0131m\u0131na devam edecektir.<\/p>\n\n\n\n
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\"Ship
Geminin denizdeki alt\u0131 hareketi<\/figcaption><\/figure>\n

Bu yaz\u0131ya ilave etmek istedi\u011finiz bilgiler varsa l\u00fctfen bunlar\u0131 yorum k\u0131sm\u0131na yazarak bizimle payla\u015f\u0131n\u0131z.<\/p>\n\n\n\n
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De\u011finmemizi istedi\u011finiz di\u011fer konular i\u00e7in info@e-MarineEducation.com adresine mail atabilirsiniz.<\/p>\n\n\n\n
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Kaynak: <\/strong>hubpages.com<\/a>
\n<\/a><\/span>Terc\u00fcme: Cem K\u00fct\u00fcko\u011flu<\/a><\/span>
\n<\/a><\/span><\/strong>D\u00fczenleme: Orkut Akar<\/a><\/span><\/strong>
\n Ekleyen: Ay\u015fe K\u0131r\u0131c\u0131<\/a><\/span><\/strong><\/p>\n","protected":false},"excerpt":{"rendered":"

Su i\u00e7erisinde y\u00fczmekte olan bir gemi, makinesi \u00e7al\u0131\u015fm\u0131yor bile olsa daima hareket halinde olacakt\u0131r. Bunun sebebi ise ba\u015fl\u0131ca okyanus ak\u0131nt\u0131lar\u0131, r\u00fczg\u00e2rlar ve medcezir ak\u0131nt\u0131lar\u0131d\u0131r. Dalgalar\u0131n olu\u015fumu, sin\u00fczoidal olmayan dalga modeli teorisi ile (Trochoidal Theory) a\u00e7\u0131klanmaktad\u0131r. Gemiler su i\u00e7erisinde makineleriyle yol al\u0131rlarken \u00e7e\u015fitli hareketler sergilerler. Gemi personelince genellikle ba\u015f-k\u0131\u00e7 ve yalpa hareketleri hissedilir. Fakat asl\u0131nda geminin …<\/p>\n","protected":false},"author":3369,"featured_media":20741,"comment_status":"open","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"_bbp_topic_count":0,"_bbp_reply_count":0,"_bbp_total_topic_count":0,"_bbp_total_reply_count":0,"_bbp_voice_count":0,"_bbp_anonymous_reply_count":0,"_bbp_topic_count_hidden":0,"_bbp_reply_count_hidden":0,"_bbp_forum_subforum_count":0,"footnotes":""},"categories":[522],"tags":[3137,1315,3278,1003,3279,3280],"class_list":["post-20736","post","type-post","status-publish","format-standard","has-post-thumbnail","","category-ozel-yazilar","tag-ayse-kirici-eklemeleri","tag-cem-kutukoglu-tercumeleri","tag-gemilerin-denizdeki-alti-hareketi","tag-orkut-akar-duzenlemeleri","tag-sinuzoidal-olmayan-dalga-modeli-teorisi","tag-trochoidal-theory"],"acf":[],"yoast_head":"\nGemilerin Denizdeki Alt\u0131 Hareketi - e-MarineEducation.com<\/title>\n<meta name=\"description\" content=\"Gemilerin denizdeki alt\u0131 hareketini anlatan yaz\u0131d\u0131r\" \/>\n<meta name=\"robots\" content=\"index, follow, max-snippet:-1, max-image-preview:large, max-video-preview:-1\" \/>\n<link rel=\"canonical\" href=\"https:\/\/e-marineeducation.com\/tr\/gemilerin-denizdeki-alti-hareketi\/\" \/>\n<meta property=\"og:locale\" content=\"tr_TR\" \/>\n<meta property=\"og:type\" content=\"article\" \/>\n<meta property=\"og:title\" content=\"Gemilerin Denizdeki Alt\u0131 Hareketi - 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