Geology, Geological Engineering - Heaving in the Subgrade of Highways Constructed on the Mancos Shale

- Organization:
- The American Institute of Mining, Metallurgical, and Petroleum Engineers
- Pages:
- 18
- File Size:
- 1300 KB
- Publication Date:
- Jan 1, 1965
Abstract
Heaving in roads built on the Mancos Shale is a serious problem in east-central Utah. Heaves are expressed as local bumps, general rises and severe cracking of the pavement. The heaves usually occur in shale road cuts and generally show a seasonal cycle, which reaches a maximum development in the winter. The presence of certain salts, absorption of moisture and physical properties of the subgrade materials were considered, in Utah, to be the main factors in the heaving mechanism. Work done on similar problems elsewhere and studies conducted by the author indicate that the latter two factors are the most important. Results of this investigation indicate that heaving areas are associated with slaking shale or expansive clays, with and without salts present. Laboratory studies show that the initial moisture content of remolded samples and the desiccation history of un- disturbed samples have a major effect on swelling. Swell tests on compacted samples at various temperatures indicate that water has more influence on swell than temperature, except for samples containing sodium sulphate, which swelled with decreasing temperature. Chloride salts inhibited swelling. Tests on shale cores indicate that the stability of slaking shale can be preserved by maintaining its original moisture content. It is concluded that shales and expansive clays, when exposed in road cuts, become desiccated and are subject to expansion when moisture is subsequently available. The seasonal cycle of heaving may possibly be explained by the annual moisture excess and deficiency. To minimize the problem, freshly exposed shale should be kept wet, and the thickness of the subbase and base courses should be increased. The Utah State Department of Highways has been plagued for many years with a distressed condition that develops in roads constructed on the Mancos Shale. Locally these distressed areas are known as heaves, frost boils and alkali boils. These names refer to the surface expression, time of year
Citation
APA:
(1965) Geology, Geological Engineering - Heaving in the Subgrade of Highways Constructed on the Mancos ShaleMLA: Geology, Geological Engineering - Heaving in the Subgrade of Highways Constructed on the Mancos Shale. The American Institute of Mining, Metallurgical, and Petroleum Engineers, 1965.