DI\u015e G\u00dc\u00c7LER VE ETK\u0130LER\u0130
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\n Faaliyetleri i\u00e7in gerekli olan enerjiyi G\u00fcne\u015f\u2019ten alan g\u00fc\u00e7lerdir. D\u0131\u015f g\u00fc\u00e7ler \u00e7e\u015fitli yollarla yerkabu\u011funu \u015fekillendirirler. D\u0131\u015f g\u00fc\u00e7ler, akarsular, r\u00fczgarlar, buzullar ve deniz suyunun hareketleridir.<\/p>\n
D\u0131\u015f g\u00fc\u00e7lerin etkisiyle yery\u00fcz\u00fcnde bir tak\u0131m olaylar ger\u00e7ekle\u015fir. Bu olaylar a\u015fa\u011f\u0131da s\u0131rlanm\u0131\u015ft\u0131r.<\/p>\n
Ta\u015flar\u0131n \u00e7\u00f6z\u00fclmesi
\n Toprak olu\u015fumu
\n Toprak kaymas\u0131 ve g\u00f6\u00e7me (heyelan)
\n Erozyon <\/p>\n
Ta\u015flar\u0131n \u00c7\u00f6z\u00fclmesi<\/p>\n
Yerkabu\u011funu olu\u015fturan ta\u015flar, iklimin ve canl\u0131lar\u0131n etkisiyle par\u00e7alan\u0131p, ufalan\u0131rlar. Ta\u015flar\u0131n \u00e7\u00f6z\u00fclmesinde ta\u015f\u0131n cinsi de etkili olmaktad\u0131r.<\/p>\n
Ta\u015flar\u0131n \u00e7\u00f6z\u00fclmesi fiziksel ve kimyasal yolla iki \u015fekilde ger\u00e7ekle\u015fir:<\/p>\n
Fiziksel (Mekanik) \u00c7\u00f6z\u00fclme
\n Kimyasal \u00c7\u00f6z\u00fclme <\/p>\n
UYARI: Kaya \u00e7atlaklar\u0131ndaki bitkilerin, k\u00f6klerini daha derinlere salmas\u0131 sonucunda kayalar par\u00e7alan\u0131r ve ufalan\u0131r. Bu t\u00fcr \u00e7\u00f6z\u00fclme, fiziksel \u00e7\u00f6z\u00fclmeyi art\u0131r\u0131c\u0131 etki yapar. Ayr\u0131ca bitki k\u00f6klerinden salg\u0131lanan \u00f6zsular ta\u015flarda kimyasal \u00e7\u00f6z\u00fclmeye neden olur.<\/p>\n
Fiziksel (Mekanik) \u00c7\u00f6z\u00fclme <\/p>\n
Ta\u015flar\u0131n fiziksel etkiler sonucunda k\u00fc\u00e7\u00fck par\u00e7alara ayr\u0131lmas\u0131na denir. Fiziksel \u00e7\u00f6z\u00fclme, ta\u015flar\u0131 olu\u015fturan minerallerin kimyasal yap\u0131s\u0131nda herhangi bir de\u011fi\u015fikli\u011fe neden olmaz.<\/p>\n
UYARI: Fiziksel (mekanik) \u00e7\u00f6z\u00fclme, kurak, yar\u0131 kurak ve so\u011fuk b\u00f6lgelerde belirgindir.<\/p>\n
Fiziksel (Mekanik) \u00e7\u00f6z\u00fclme \u00fc\u00e7 \u015fekilde olur:<\/p>\n
G\u00fcne\u015flenme yolu ile fiziksel \u00e7\u00f6z\u00fclme : Gece ile g\u00fcnd\u00fcz, yaz ile k\u0131\u015f aras\u0131ndaki s\u0131cakl\u0131k farklar\u0131n\u0131n fazla oldu\u011fu yar\u0131 kurak ve kurak b\u00f6lgelerde g\u00f6r\u00fcl\u00fcr. G\u00fcnd\u00fcz, g\u00fcne\u015flenme ve \u0131s\u0131nman\u0131n etkisiyle ta\u015flar\u0131 olu\u015fturan minerallerin etkisiyle ta\u015flar\u0131 olu\u015fturan minerallerin hacimleri geni\u015fler. Gece, s\u0131cakl\u0131k farklar\u0131n\u0131n fazla oldu\u011fu yar\u0131 kurak ve kurak b\u00f6lgelerde g\u00f6r\u00fcl\u00fcr. G\u00fcnd\u00fcz, g\u00fcne\u015flenme ve \u0131s\u0131nman\u0131n etkisiyle ta\u015flar\u0131 olu\u015fturan minerallerin hacimleri geni\u015fler. Gece, s\u0131cakl\u0131k d\u00fc\u015f\u00fcnce minerallerin hacimleri yeniden k\u00fc\u00e7\u00fcl\u00fcr. Bu hacim de\u011fi\u015fikli\u011fi ta\u015flar\u0131n par\u00e7alanmas\u0131na neden olur. <\/p>\n
Buz \u00e7atlamas\u0131 yolu ile fiziksel \u00e7\u00f6z\u00fclme : S\u0131cakl\u0131\u011f\u0131n \u00e7ok zaman donma noktas\u0131na yak\u0131n oldu\u011fu ve ya\u011f\u0131\u015f\u0131n yeter derecede oldu\u011fu y\u00fcksek da\u011flar ve y\u00fcksek enlemlerde g\u00f6r\u00fclen \u00e7\u00f6z\u00fclme \u015feklidir. Ya\u011f\u0131\u015flardan sonra ta\u015flar\u0131n delik, \u00e7atlak ve ince yar\u0131klar\u0131na sular dolar. S\u0131cakl\u0131k donma noktas\u0131na kadar d\u00fc\u015f\u00fcnce, ta\u015f\u0131n i\u00e7ine s\u0131zm\u0131\u015f olan sular donar. Donan suyun hacmi geni\u015fledi\u011fi i\u00e7in bas\u0131n\u00e7 etkisiyle ta\u015flar par\u00e7alan\u0131r ve \u00e7\u00f6z\u00fcl\u00fcr. <\/p>\n
Tuz \u00e7atlamas\u0131 yolu ile fiziksel \u00e7\u00f6z\u00fclme : Ta\u015flar\u0131n tuzlu sular\u0131 emmi\u015f bulundu\u011fu ve buharla\u015fman\u0131n \u00e7ok fazla oldu\u011fu \u00e7\u00f6l b\u00f6lgelerinde g\u00f6r\u00fcl\u00fcr. Kurak b\u00f6lgelerde buharla\u015fma ile k\u0131lcal ta\u015f \u00e7atlaklar\u0131ndan yery\u00fcz\u00fcne y\u00fckselen tuzlu sular, y\u00fczeye yakla\u015ft\u0131k\u00e7a suyunu yitirir. \u00c7atlaklar\u0131n kenar\u0131nda tuz billurla\u015fmas\u0131 olur. Gece nemli ge\u00e7erse, suyunu yitiren tuz billurlar\u0131 yeniden su al\u0131r ve hacmi geni\u015fler. Bas\u0131n\u00e7 etkisiyle ta\u015flar par\u00e7alan\u0131r ve \u00e7\u00f6z\u00fcl\u00fcr. <\/p>\n
Kimyasal \u00c7\u00f6z\u00fclme<\/p>\n
Kimyasal reaksiyonlar suya ihtiya\u00e7 duydu\u011funda ve s\u0131cakl\u0131k reaksiyonu h\u0131zland\u0131rd\u0131\u011f\u0131ndan, s\u0131cak ve nemli b\u00f6lgelerde yayg\u0131n olan \u00e7\u00f6z\u00fclme \u015feklidir. Kaya tuzu, kalker gibi ta\u015flar suda kolayca erirler. Ta\u015flar, kimyasal yolla par\u00e7alan\u0131p ufalan\u0131rken kimyasal bile\u015fimleri de de\u011fi\u015fir.<\/p>\n
UYARI: Kimyasal \u00e7\u00f6z\u00fclme, ekvatoral, okyanus ve muson iklim b\u00f6lgelerinde belirgindir.<\/p>\n
Toprak Olu\u015fumu <\/p>\n
Toprak, ta\u015flar\u0131n ve organik maddelerin ayr\u0131\u015fmas\u0131 ile olu\u015fan, i\u00e7inde belli oranda hava ve su bulunan, yerkabu\u011funun \u00fcst\u00fcn\u00fc ince bir tabaka halinde saran \u00f6rt\u00fcd\u00fcr . Topra\u011f\u0131n i\u00e7inde bulunan \u00e7e\u015fitli organizmalar topra\u011f\u0131n olu\u015fumuna yard\u0131m eder. Topra\u011f\u0131n \u00fcst\u00fcndeki organik maddece zengin b\u00f6l\u00fcme humus ad\u0131 verilir. Toprak olu\u015fumunu etkileyen etmenler :<\/p>\n
\u0130klim ko\u015fullar\u0131
\n Ana kayan\u0131n \u00f6zellikleri
\n Bitki \u00f6rt\u00fcs\u00fc
\n E\u011fim ko\u015fullar\u0131
\n Olu\u015fum S\u00fcresi\u2019dir <\/p>\n
UYARI: Mekanik \u00e7\u00f6z\u00fclmeyle toprak olu\u015fumu zordur. Kimyasal \u00e7\u00f6z\u00fclmede ise toprak olu\u015fumu daha kolayd\u0131r. \u00d6rne\u011fin \u00e7\u00f6llerde toprak olu\u015fumunun yava\u015f olmas\u0131 kimyasal \u00e7\u00f6z\u00fclmenin yetersiz olmas\u0131na ba\u011fl\u0131d\u0131<\/p>\n
Toprak Horizonlar\u0131 <\/p>\n
Yerkabu\u011fu \u00fcst\u00fcnde ince bir \u00f6rt\u00fc halinde bulunan toprak, \u00e7e\u015fitli katmanlardan olu\u015fur. Bu katmanlara horizon ad\u0131 verilir. Topra\u011f\u0131n d\u00f6rt temel horizonu vard\u0131r.<\/p>\n
A Horizonu : D\u0131\u015f etkilerle iyice ayr\u0131\u015fm\u0131\u015f, organik maddeler bak\u0131m\u0131ndan zengin, en \u00fcstteki katmand\u0131r. Tar\u0131msal etkinlikler, bu katman \u00fczerinde yap\u0131lmaktad\u0131r.<\/p>\n
B Horizonu : Suyun etkisiyle \u00fcst katmanda y\u0131kanan minerallerin biriktirdi\u011fi katmand\u0131r.<\/p>\n
C Horizonu : \u0130ri par\u00e7alardan olu\u015fan ve ana kayan\u0131n \u00fczerinde bulunan katmand\u0131r.<\/p>\n
D Horizonu : Fiziksel ve kimyasal \u00e7\u00f6z\u00fclmenin g\u00f6r\u00fclmedi\u011fi, ana kayadan olu\u015fan, en alt katmand\u0131r.<\/p>\n
Yer\u00e7ekimi : Heyelan\u0131 olu\u015fturan en \u00f6nemli etkendir. Yer\u00e7ekimi g\u00fcc\u00fc s\u00fcrt\u00fcnme g\u00fcc\u00fcnden fazla oldu\u011fu zaman yama\u00e7taki cisimler a\u015fa\u011f\u0131ya do\u011fru kayar.<\/p>\n
Yama\u00e7 Zeminin Yap\u0131s\u0131: Suyu emerek i\u00e7erisinde tutan ta\u015f ve topraklar kayganla\u015f\u0131r. \u00d6zellikle killi yap\u0131n\u0131n yayg\u0131n oldu\u011fu yama\u00e7larda kil suyu i\u00e7inde tuttu\u011fu i\u00e7in heyelan daha s\u0131k g\u00f6r\u00fcl\u00fcr. Kalker gibi suyu alt tabakalara ge\u00e7iren ta\u015flar\u0131n olu\u015fturdu\u011fu yama\u00e7larda ise heyelan ender g\u00f6r\u00fcl\u00fcr.<\/p>\n
E\u011fim : Yama\u00e7 e\u011fimi yer\u00e7ekiminin etkisini art\u0131r\u0131c\u0131 bir rol oynar. Bu nedenle dik yama\u00e7larda heyelan olas\u0131l\u0131\u011f\u0131 daha fazlad\u0131r. Ayr\u0131ca tabakalar yama\u00e7 e\u011fimine uyum sa\u011flam\u0131\u015fsa, yani paralelse yer kaymas\u0131 kolayla\u015f\u0131r. Yol, kanal, t\u00fcnel ve baraj yap\u0131mlar\u0131 s\u0131ras\u0131nda yama\u00e7 dengesinin bozulmas\u0131, volkanizma, deprem gibi etkenler de heyelana neden olur.<\/p>\n
Ya\u011f\u0131\u015f Ko\u015fullar\u0131 :<\/p>\n
Ya\u011fmur, kar sular\u0131 tabakalar aras\u0131na s\u0131zarak topra\u011f\u0131 kayganla\u015ft\u0131r\u0131r, topra\u011f\u0131 doygun hale getirir. B\u00f6ylece su ile doygun k\u00fctlelerin yama\u00e7 a\u015fa\u011f\u0131 kaymas\u0131 kolayla\u015f\u0131r. Heyelan genellikle ya\u011f\u0131\u015flardan sonra olu\u015fur. <\/p>\n
Heyelan\u0131n Etkileri ve Korunma Yollar\u0131<\/p>\n
Heyelan hemen her y\u0131l can ve mal kayb\u0131na yol a\u00e7maktad\u0131r. Ancak al\u0131nacak bir tak\u0131m \u00f6nlemlerle heyelan\u0131n etkileri azalt\u0131labilir. <\/p>\n
Heyelan\u0131n Etkileri <\/p>\n
\u0130nsan ve hayvan \u00f6l\u00fcmleri<\/p>\n
Tar\u0131msal hasar ve toprak kayb\u0131<\/p>\n
Bina hasarlar\u0131<\/p>\n
Ula\u015f\u0131m ve ta\u015f\u0131mac\u0131l\u0131\u011f\u0131n aksamas\u0131<\/p>\n
Heyelandan Korunma<\/p>\n
\u00d6ncelikle heyelan tehlikesi olan yerlerde setler yap\u0131lmal\u0131, yama\u00e7lar a\u011fa\u00e7land\u0131r\u0131lmal\u0131d\u0131r. Ayr\u0131ca yol, kanal, t\u00fcnel ve baraj yap\u0131mlar\u0131nda yamac\u0131n bozulmamas\u0131na \u00f6zen g\u00f6sterilmelidir.<\/p>\n
T\u00fcrkiye’de Heyalan <\/p>\n
T\u00fcrkiye\u2019de heyelan s\u0131k g\u00f6r\u00fclen, do\u011fal bir felakettir. T\u00fcrkiye\u2019de arazinin \u00e7ok engebeli olmas\u0131 toprak kaymalar\u0131n\u0131 kolayla\u015ft\u0131rmaktad\u0131r. B\u00f6lgeden b\u00f6lgeye farkl\u0131l\u0131k g\u00f6steren heyelanlar\u0131n en s\u0131k g\u00f6r\u00fcld\u00fc\u011f\u00fc b\u00f6lgemiz Karadeniz\u2019dir. B\u00f6lgede arazi e\u011fiminin fazla, ya\u011f\u0131\u015flar\u0131n bol ve killi yap\u0131n\u0131n yayg\u0131n olmas\u0131 heyelan\u0131n s\u0131k g\u00f6r\u00fclmesine neden olur. \u00dclkemizde ilkbahar aylar\u0131nda g\u00f6r\u00fclen kar erimeleri ve ya\u011f\u0131\u015flar heyelan olaylar\u0131n\u0131 art\u0131r\u0131r.<\/p>\n
Erozyon<\/p>\n
Toprak \u00f6rt\u00fcs\u00fcn\u00fcn, akarsular\u0131n, r\u00fczgarlar\u0131n ve buzullar\u0131n etkisiyle s\u00fcp\u00fcr\u00fclmesine erozyon denir. Yery\u00fcz\u00fcnde e\u011fim, toprak, su ve bitki \u00f6rt\u00fcs\u00fc aras\u0131nda do\u011fal bir denge bulunmaktad\u0131r. Bu dengenin bozulmas\u0131 erozyonu h\u0131zland\u0131r\u0131c\u0131 bir etki yapmaktad\u0131r. D\u0131\u015f etkenler ya da arazinin yanl\u0131\u015f kullan\u0131lmas\u0131 erozyona neden olmaktad\u0131r.<\/p>\n
UYARI: E\u011fim fazlal\u0131\u011f\u0131 ve c\u0131l\u0131z bitki \u00f6rt\u00fcs\u00fc erozyonu art\u0131ran en \u00f6nemli etkenlerdir. Bu nedenle kurak ve yar\u0131 kurak enlemlerde erozyon \u00f6nemli bir sorundur.<\/p>\n
D\u0131\u015f Etkenler <\/p>\n
Akarsu, r\u00fczgar gibi d\u0131\u015f g\u00fc\u00e7lerin yapm\u0131\u015f oldu\u011fu a\u015f\u0131nd\u0131rma sonucunda toprak \u00f6rt\u00fcs\u00fc s\u00fcp\u00fcr\u00fcl\u00fcr ve ba\u015fka yerlere ta\u015f\u0131n\u0131r. D\u0131\u015f g\u00fc\u00e7lerin etkisi bitki \u00f6rt\u00fcs\u00fcn\u00fcn bulunmad\u0131\u011f\u0131 ya da \u00e7ok c\u0131l\u0131z oldu\u011fu yerlerde daha belirgindir. Ayr\u0131ca e\u011fimin fazla oldu\u011fu yerlerde sular daha kolay ak\u0131\u015fa ge\u00e7erek toprak \u00f6rt\u00fcs\u00fcn\u00fcn s\u00fcp\u00fcr\u00fclmesini h\u0131zland\u0131r\u0131r.<\/p>\n
Arazinin Yanl\u0131\u015f Kullan\u0131lmas\u0131<\/p>\n
\u00d6zellikle yama\u00e7lardaki tarlalar\u0131n yama\u00e7 e\u011fimi y\u00f6n\u00fcnde s\u00fcr\u00fclmesi, e\u011fimli yerlerde tarla tar\u0131m\u0131n\u0131n yayg\u0131n olmas\u0131, arazinin teraslanmamas\u0131 erozyon h\u0131z\u0131n\u0131 art\u0131rmaktad\u0131r. <\/p>\n
Su Erozyonu<\/p>\n
Bitki \u00f6rt\u00fcs\u00fcn\u00fcn c\u0131l\u0131z ya da hi\u00e7 olmad\u0131\u011f\u0131 yerlerde topra\u011f\u0131n ve ana kayan\u0131n sularla yerinden kopart\u0131larak ta\u015f\u0131nmas\u0131na su erozyonu denir. K\u0131rg\u0131bay\u0131r ve peribacas\u0131 su erozyonu ile olu\u015fan \u00f6zel \u015fekillerdir.<\/p>\n
K\u0131rg\u0131bay\u0131r : Yar\u0131 kurak iklim b\u00f6lgelerinde sel yar\u0131nt\u0131lar\u0131yla dolu yama\u00e7lara k\u0131rg\u0131bay\u0131r (badlans) denir.<\/p>\n
Peribacas\u0131 : \u00d6zellikle volkan t\u00fcflerinin yayg\u0131n olarak bulundu\u011fu vadi ve platolar\u0131n yama\u00e7lar\u0131nda sel sular\u0131n\u0131n a\u015f\u0131nd\u0131rmas\u0131 ile olu\u015fan \u00f6zel yery\u00fcz\u00fc \u015fekillerine peribacas\u0131 denir. Baz\u0131 peribacalar\u0131n\u0131n \u00fczerinde \u015fapkaya benzer, a\u015f\u0131nmadan arta kalan sert volkanik ta\u015flar bulunur. Bunlar volkanik faaliyet s\u0131ras\u0131nda b\u00f6lgeye yay\u0131lm\u0131\u015f andezit ya da bazalt k\u00fctleridir. Peribacalar\u0131n\u0131n en g\u00fczel \u00f6rnekleri \u00fclkemizde Nev\u015fehir, \u00dcrg\u00fcp ve G\u00f6reme \u00e7evresinde g\u00f6r\u00fcl\u00fcr.<\/p>\n
R\u00fczgar Erozyonu<\/p>\n
Bitki \u00f6rt\u00fcs\u00fcn\u00fcn olmad\u0131\u011f\u0131 ya da c\u0131l\u0131z oldu\u011fu yerlerde topra\u011f\u0131n r\u00fczgarlarla yerinden kopart\u0131larak ta\u015f\u0131nmas\u0131na r\u00fczgar erozyonu denir.<\/p>\n
Erozyonun Etkileri ve Erozyondan Korunma Yollar\u0131<\/p>\n
Olu\u015fumu i\u00e7in milyonlarca y\u0131l ge\u00e7mesi gereken toprak \u00f6rt\u00fcs\u00fcn\u00fc yok eden ve her ge\u00e7en g\u00fcn etkilerini artt\u0131ran erozyon do\u011fal bir felakettir. Al\u0131nacak bir tak\u0131m \u00f6nlemlerle etkileri azalt\u0131labilir.<\/p>\n
Erozyonun Etkileri
\n Tar\u0131m topraklar\u0131n\u0131n azalmas\u0131, sellerin artmas\u0131, tar\u0131msal \u00fcretimin ve verimin azalmas\u0131, otlaklar\u0131n azalmas\u0131, hayvanc\u0131l\u0131\u011f\u0131n gerilemesi, \u00e7\u00f6lle\u015fmenin ba\u015flamas\u0131.<\/p>\n
Erozyondan Korunma Yollar\u0131 <\/p>\n
Var olan ormanlar ve meralar korunmal\u0131, \u00e7\u0131plak yerler a\u011fa\u00e7land\u0131r\u0131lmal\u0131, ormanl\u0131k alanlarda ke\u00e7i beslenmesi engellenmeli, yama\u00e7lardaki tarlalar, yama\u00e7 e\u011fimine dik s\u00fcr\u00fclmeli, meyve tar\u0131m\u0131 ve n\u00f6betle\u015fe ekim yayg\u0131nla\u015ft\u0131r\u0131lmal\u0131, orman i\u00e7i k\u00f6yl\u00fclerine yeni ge\u00e7im kaynaklar\u0131 sa\u011flanmal\u0131.<\/p>\n
T\u00fcrkiye’de Erozyon<\/p>\n
T\u00fcrkiye\u2019de arazi engebeli ve \u00e7ok e\u011fimli oldu\u011fu i\u00e7in toprak erozyonu \u00f6nemli bir sorundur. Baz\u0131 b\u00f6lgelerimiz d\u0131\u015f\u0131nda bitki \u00f6rt\u00fcs\u00fcn\u00fcn c\u0131l\u0131z olmas\u0131 da erozyonu art\u0131rmaktad\u0131r. Ayr\u0131ca n\u00fcfusun h\u0131zla artmas\u0131, tar\u0131m alanlar\u0131na olan gereksinimin artmas\u0131, ormanlar\u0131n tahrip edilmesine yol a\u00e7maktad\u0131r. Bunlara ba\u011fl\u0131 olarak hemen hemen t\u00fcm b\u00f6lgelerimizde toprak erozyon h\u0131z\u0131 y\u00fcksektir.<\/p>\n","protected":false},"excerpt":{"rendered":"
DI\u015e G\u00dc\u00c7LER VE ETK\u0130LER\u0130 l Faaliyetleri i\u00e7in gerekli olan enerjiyi G\u00fcne\u015f\u2019ten alan g\u00fc\u00e7lerdir. D\u0131\u015f g\u00fc\u00e7ler \u00e7e\u015fitli yollarla yerkabu\u011funu \u015fekillendirirler. D\u0131\u015f g\u00fc\u00e7ler, akarsular, r\u00fczgarlar, buzullar ve deniz suyunun hareketleridir. D\u0131\u015f g\u00fc\u00e7lerin etkisiyle yery\u00fcz\u00fcnde bir tak\u0131m olaylar ger\u00e7ekle\u015fir. Bu olaylar a\u015fa\u011f\u0131da s\u0131rlanm\u0131\u015ft\u0131r. Ta\u015flar\u0131n \u00e7\u00f6z\u00fclmesi Toprak olu\u015fumu Toprak kaymas\u0131 ve g\u00f6\u00e7me (heyelan) Erozyon Ta\u015flar\u0131n \u00c7\u00f6z\u00fclmesi Yerkabu\u011funu olu\u015fturan ta\u015flar, …<\/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":[3609,2926,3166,4155,3847,2730,3105,4160,4159,2925,3297,3287,4163,3106,3197,4162,4156,4158,4157,3293,3857,4161,3715,2752],"class_list":["post-1466","post","type-post","status-publish","format-standard","hentry","category-odevler","category-sosyal-bilgiler-odevleri","tag-akarsular","tag-bitki-ortusu","tag-buzullar","tag-dis-gucler-ve-etkileri","tag-erozyon","tag-gunes","tag-heyelan","tag-heyelandan-korunma","tag-heyelanin-etkileri-ve-korunma-yollari","tag-iklim","tag-kimyasal-cozulme","tag-kirgibayir","tag-peribacasi","tag-ruzgar-erozyonu","tag-ruzgarlar","tag-su-erozyonu","tag-taslarin-cozulmesi","tag-toprak-horizonlari","tag-toprak-kaymasi","tag-toprak-olusumu","tag-turkiyede-erozyon","tag-turkiyede-heyalan","tag-yagis","tag-yercekimi"],"_links":{"self":[{"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/posts\/1466","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=1466"}],"version-history":[{"count":0,"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/posts\/1466\/revisions"}],"wp:attachment":[{"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/media?parent=1466"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/categories?post=1466"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/tags?post=1466"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}