Case Studies
Apr 13, 2018

Characteristics of Asphalt Pavement Damage in Degrading Permafrost Regions: Case Study of the Qinghai–Tibet Highway, China

Publication: Journal of Cold Regions Engineering
Volume 32, Issue 2

Abstract

In the context of climate warming, damage to road pavements and embankments in permafrost regions caused by thawing of underlying permafrost severely reduces the serviceability of roads. In this study, 10 types of asphalt pavement damage were measured every kilometer along the Qinghai–Tibet Highway (QTH), from Kunlun Mountain to Tonggula Mountain (approximately 440 km in permafrost regions). Based on observed data and embankment geometry along the QTH, and information about the characteristics of the permafrost, aspects of pavement deterioration are analyzed and discussed. The three most common forms of pavement damage in the permafrost regions are transverse cracking (TC), potholes, and longitudinal cracking (LC), observed in 87, 64, and 57% of the study section, respectively. About half of the damaged pavement was also affected by block cracking (BC) and alligator cracking (AC), in addition to LC and TC. Results also showed that pavement damage in the degrading permafrost regions was closely related to the underlying permafrost characteristics and embankment geometry. Damage from settlement and patching were more severe in sections with high ice content than low ice content. All the above forms of damage increase exponentially with higher underlying permafrost temperatures. Because of the significant thermal effects of sunlit/shaded slopes, BC, LC, and TC cracking is closely related to roadway orientation, with the most severe cracking damage observed in roads oriented approximately east to west (E–W). Also, more LC was seen in sections of greater embankment thickness, which exacerbates the sunlit/shaded thermal effect.

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Acknowledgments

This research was financially supported by the Natural Science Foundation of China (Grant Nos. 41630636 and 41401077) and the Foundation of State Key Laboratory of Frozen Soil Engineering (Grant No. SKLFSE-ZY-17). We thank the two anonymous reviewers for their insightful and constructive comments on this manuscript. We also thank the editor and the associate editor for their invaluable help on our manuscript.

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Go to Journal of Cold Regions Engineering
Journal of Cold Regions Engineering
Volume 32Issue 2June 2018

History

Received: Aug 29, 2016
Accepted: Dec 6, 2017
Published online: Apr 13, 2018
Published in print: Jun 1, 2018
Discussion open until: Sep 13, 2018

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Authors

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Mingtang Chai [email protected]
Ph.D. Candidate, State Key Laboratory of Frozen Soil Engineering, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000, China; Ph.D. Candidate, Univ. of Chinese Academy of Sciences, Beijing 100049, China. E-mail: [email protected]
Associate Professor, State Key Laboratory of Frozen Soil Engineering, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000, China (corresponding author). E-mail: [email protected]
Jianming Zhang [email protected]
Professor, State Key Laboratory of Frozen Soil Engineering, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000, China. E-mail: [email protected]
Professor, State Key Laboratory of Frozen Soil Engineering, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000, China. E-mail: [email protected]
Engineer, China Communication Construction Company, Highway Consultants Co. Ltd., Keji Rd. 63, Xi’an 710075, China. E-mail: [email protected]
Jianbing Chen [email protected]
Senior Engineer, China Communication Construction Company, Highway Consultants Co. Ltd., Keji Rd. 63, Xi’an 710075, China. E-mail: [email protected]

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