A Comparative Analysis of Slope Height Using Simple Methods

Analysis of slope stability is crucial for the design of many engineering processes such as open pit mine and highway. Slope stability is generally evaluated by limit equilibrium and numerical analyses, and rock mass classification systems. The slope height is used as the input parameter in many of these methods. Advanced methods such as LiDAR and TLS are expensive and time consuming and they require professional use. Therefore, researchers generally need to use simple methods for the measurement of slope height because of their cheapness, rapidity and portability. In this study, height of the rock slopes was determined with tape line, laser meter, altimeter, clinometer and geological compass. Measurements were taken from steep (90̊) and inclined slopes (75̊). Further, various models were developed in the laboratory for understanding the mechanism of methods in inclined slopes (45̊–90̊). The findings of methods used compared with each other and the reliability of the methods was discussed. Strengths and weakness of the methods were highlighted. This study indicated that some factors (measurement distance, slope width, the inclination of the ground, rugged surface in toe of the slope, etc.) can negatively affect the estimations of slope height. 

Basit Yöntemlerle Şev Yüksekliğinin Karşılaştırmalı Analizi

Şev duraylılık analizi açık işletme ve karayolu gibi birçok mühendislik işlemlerinin tasarımı için çok önemlidir. Şev duraylılığı genellikle limit denge ve sayısal analizler ile kaya kütlesi sınıflama sistemleri kullanılarak değerlendirilmektedir. Şev yüksekliği bu yöntemlerin çoğunda girdi parametresi olarak kullanılmaktadır. LiDAR ve TLS gibi ileri yöntemler pahalı ve zaman alıcıdır ve profesyonel kullanım gerektirirler. Bu nedenle, araştırmacılar taşınabilirlikleri, ucuzlukları ve hızlılıkları nedeniyle genellikle şev yüksekliğinin belirlenmesinde basit yöntemlere ihtiyaç duyarlar. Bu çalışmada kaya şevlerinin yüksekliği şerit metre, altimetre, lazer metre, klinometre ve jeolog pusulası ile belirlenmiştir. Ölçümler dik (90̊)  ve eğimli şevlerden (75̊) alınmıştır. Ayrıca, eğimli şevlerde (45̊–90̊) yöntemlerin mekanizmasını anlamak için laboratuvarda çeşitli modeller geliştirilmiştir. Kullanılan yöntemlerin bulguları birbiriyle kıyaslanmış ve yöntemlerin güvenilirliği tartışılmıştır. Yöntemlerin güçlü ve zayıf yanları vurgulanmıştır. Bu çalışma bazı etkenlerin (ölçüm mesafesi, şev genişliği, zeminin eğimi, şev topuğu önünde engebeli yüzey, vb.) şev yüksekliği tahminlerini olumsuz etkilediğini göstermiştir. 

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