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Cohesion and Internal Friction Angle Estimated from Brazilian Tensile Strength and Unconfined Compressive Strength of Volcanic Rocks in Jeju Island

제주도 화산암의 압열인장강도와 일축압축강도로부터 추정된 점착력과 내부마찰각

  • Moon, Kyoungtae (Dept. of Civil Eng., Jeju National Univ.) ;
  • Yang, Soon-Bo (Port and Airport Research Institute, National Institute of Maritime, Port and Aviation Technology)
  • 문경태 (제주대학교 토목공학과) ;
  • 양순보 (일본 국립연구개발법인 해상.항만.항공기술연구소 항만공항기술연구소)
  • Received : 2019.12.07
  • Accepted : 2020.02.24
  • Published : 2020.02.29

Abstract

With respect to the tensile strength of volcanic rocks in Jeju Island, a comparative study was conducted using the existing research results and the test results performed in this study. In addition, the characteristics and effectiveness of the cohesion and internal friction angle estimated from the Brazilian tensile strength and unconfined compressive strength of Jeju volcanic rocks were investigated. As results, the Brazilian tensile strength of Jeju volcanic rocks was closely related to absorption, and decreased exponentially as the absorption increased. It was confirmed that the internal friction angle was closely related to the ratio of unconfined compressive strength to Brazilian tensile strength (σc / σt), and increased logarithmically as the ratio of σc / σt increased. In addition, the ratios of σc / σt of Jeju volcanic rocks were in the range of 5~20 depending on the magnitude of internal friction angle. In the case of cohesion, it was closely related to the absorption and Brazilian tensile strength. The cohesion exponentially decreased as the absorption increased, such as the relation between the Brazilian tensile strength and absorption. It was confirmed that there was a linear relation between the cohesion and Brazilian tensile strength.

본 연구에서는, 제주도 화산암의 인장강도와 관련하여, 기존의 연구결과 및 본 연구에서 수행된 시험결과에 대한 종합적인 비교·분석을 수행하였으며, 제주도 화산암의 압열인장강도와 일축압축강도로부터 추정된 점착력과 내부 마찰각의 특성 및 그 유효성을 각각 살펴보았다. 제주도 화산암의 압열인장강도는 흡수율과 밀접한 관계에 있었으며, 흡수율이 증가함에 따라 지수 함수적으로 급격하게 감소하는 특성을 갖고 있었다. 내부 마찰각은 압열인장도강도에 대한 일축압축강도의 비(σc / σt)와 밀접한 관계에 있었으며, 강도비 σc / σt가 증가함에 따라 내부 마찰각은 로그 함수적으로 증가하는 특성을 갖고 있었다. 그리고 제주도 화산암의 강도비 σc / σt는 내부 마찰각의 크기에 따라 약 5~20 사이의 값을 나타내고 있었다. 한편, 점착력(c)의 경우, 흡수율 및 압열인장강도와 밀접한 관계에 있음을 확인할 수 있었다. 점착력과 흡수율 사이에는 압열인장강도와 흡수율의 관계와 같이 지수 함수적인 관계에 있으며, 점착력과 압열인장강도 사이에는 선형관계에 있음을 확인할 수 있었다. 그리고 일축압축강도와 압열인장강도로부터 추정된 내부 마찰각과 점착력은 각각 삼축압축강도로부터 추정된 내부 마찰각과 점착력에 비해 약 13% 과소평가 그리고 약 24% 정도 과대평가되는 경향을 보였다.

Keywords

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