Kayma tipi heyelanların farklı duyarlılık modellerinde kombinasyonu: Sakarya Havzası Yukarı Çığırı örneği
Heyelan duyarlılık haritaları heyelanın mekânsal tahmini için önem arz etmektedir. Bu nedenleheyelan duyarlılık modellerinin doğruluğu tehlike ve risk çalışmaları için temel oluşturmaktadır.Bir bölgede heyelanın tüm tipleri için tek bir model oluşturulması duyarlılığın başarısını etkilemektedir.Heyelanların her bir tipi, farklı mekanizma ve materyalde gerçekleştiği için heyelanıdenetleyen hazırlayıcı koşullar da değişmektedir. Bu yüzden duyarlılık modellerinin tek bir heyelantipine göre oluşturulması daha iyi sonuçlar vermektedir. Bu nedenle çalışmanın amacı, tekbir heyelan ana mekanizmasına bağlı moloz ve toprak kayması tipine göre duyarlılık haritalarınınnitel ve yarı nicel yaklaşımlarda nasıl sonuçlar verdiğini ortaya koymaktır. Bu amaç doğrultusundaSakarya havzasının yukarı çığırında bulunan çalışma alanı için, Varnes (1978) sınıflamasınagöre moloz ve toprak kayması tipindeki heyelanlar için Frekans Oran, Analitik Hiyerarşi Süreci,Ağırlıklandırılmış Çakıştırma, Modifiye AHP ve CBS Matris Model yaklaşımları ile duyarlılık modellerioluşturulmuştur. Model sonuçlarına bağlı duyarlılık oluşturulurken heyelanın yamacıntamamını etkileyeceğinden çalışma alanı yamaç ünitelerine bölünerek çalışılmıştır. Beş modelsonucuna göre ROC eğrisinin altında kalan sonuçlar 0,79 ile 0,92 arasında değişmektedir. Budurum modellerin çok iyi sonuçlar verdiğini ve çalışma sahasının heyelan duyarlılığı açısındaniyi temsil edildiğini göstermektedir. Sonuçlara göre heyelanın en yüksek ve en düşük olabileceğialanlar tüm modelde ortak alanlara karşılık gelmektedir. Çalışmada sonuç olarak ana heyelantipine göre oluşturulan modellerin yüksek sonuçlar verdiği ortaya çıkmıştır. Bu sonuçlar, tümmodelin tek bir modelde birleştirilmesinde kolaylık sağlamıştır. Böylece tüm modelden tek birmodel çıktısı elde eden çalışma, heyelan tehlike ve risk çalışmalarının iyileştirilmesine katkı sağlamaktadır.
Combination of slide-type landslides in different susceptibility: A case study of the Sakarya Basin Upstream
Landslide susceptibility maps are important for the spatial prediction of landslides. Therefore,the accuracy of landslide susceptibility models is the basis for hazard and risk studies.The creation of a single model for all types of landslides in a region affects the success ofsusceptibility. Since each type of landslide occurs in different mechanisms and materials, thelandslide controlling preparing conditions change. Creating susceptibility models according toa single landslide type gives better results. For this reason, it is the aim of the study to revealhow the susceptibility maps give results in qualitative and semi-quantitative approachesaccording to the type of a single landslide main mechanism which is debris and soil slide.For this purpose, susceptibility models were created for debris and soil type landslidesusing Frequency Ratio, Analytical Hierarchy Process, Weighted Overlay, Modified AnalyticalHierarchy Process and GIS Matrix Models according to Varnes (1978) classification in the studyarea located at the upstream of the Sakarya basin. While creating susceptibility depending onthe model results, the study area was divided into slope units, since a landslide would affectthe entire slope. According to the five model results, the results under the ROC change varybetween 0.79 and 0.92. This shows that the models give very good results and that the studyarea is well represented in terms of landslide susceptibility. According to the results, the areaswhere the landslide may be the highest and the lowest correspond to the common areas in allmodels. As a result of the study, it was revealed that the models created according to the mainlandslide type gave high results. These results made it easy to combine all models in a singlemodel. Thus, the study, which obtains a single model output from all models, contributes tothe improvement of landslide hazard and risk studies.
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