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Original Articles

Investigation on disc cutter behaviors in cutting rocks of different strengths and reverse estimation of rock strengths from experimental cutting forces

ORCID Icon, , , , &
Pages 1-27 | Received 28 Oct 2017, Accepted 13 Aug 2018, Published online: 08 Nov 2018
 

Abstract

This paper investigates the disc cutter behaviors in full-scale linear cutting tests. The experimental results obtained from different rocks varying from relatively soft rock (σc=27.6 MPa) to extremely hard rock (σc=355.54 MPa) are compared to the results of the semi-theoretical prediction model (Rostami & Ozdemir, Citation1993; Rostami, Ozdemir, & Nilsen, Citation1996). Compared to the semi-theoretical results, higher experimental normal and rolling forces and lower experimental cutting coefficients and normalized resultant forces are obtained when cutting low strength rocks. Opposite results are found when cutting extremely hard rocks. An empirical disc cutter cutting force prediction model is suggested in which the input parameters are cutter diameter, cutter spacing, cutter penetration depth and rock uniaxial compressive strength. Furthermore, based on the semi-theoretical model and the new empirical model, reverse estimation of rock strengths from disc cutter cutting forces are undertaken. The results show that rock uniaxial compressive strength can be reliably evaluated from disc cutter cutting forces, but the estimation results for rock Brazilian tensile strength are not so good. This study is pertinent to the better understanding of the disc cutter behaviors in cutting rocks of different strengths and can improve the geological information acquisition and operation control during TBM tunneling.

Disclosure statement

No potential conflict of interest was reported by the authors.

Additional information

Funding

This work was supported by the National Key Basic Research Program of China [grant numbers 2014CB046904 and 2015CB058102]; China Postdoctoral Science Foundation Program [grant number 2017M622515]; National Funded Program for Graduate Students Studying Abroad of China Scholarship Council [grant number 201506270068 (to Miss Xiaoxuan Kong)]; and National Natural Science Foundation of China [grant numbers 41602326 and 41702254]. The authors are grateful for their continuous support, and also grateful to the authors’ colleagues for their valuable help to this research.

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