Upper Cretaceous - lower Tertiary lithostratigraphic relationships of three cores from Alberta, Saskatchewan, and Manitoba, Canada

Braman, Dennis R.; Sweet, Arthur R.; Lerbekmo, J. F.

doi:10.1139/e97-108

Cited by 11 publications

(1 citation statement)

References 35 publications

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“…The existence of quartz indicated the sedimentary origin of the investigated till [55]. Likewise, calcite at 34.4 • and dolomite at 36.3 • in the sample are related to deposition of calcareous compounds from seawater [56]. Furthermore, various types of feldspars (K-feldspar at 25.8 • and plagioclase at 27.7 • and 32.7 • ) are related to the deposition of volcanic debris in the Cretaceous period and subsequent weathering during the Quaternary period.…”

Section: Soil and Pore Water Compositionsmentioning

confidence: 99%

Effect of Composition on Engineering Behavior of Clay Tills

Paranthaman

Azam

2021

Geosciences

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Glacial geology, marine environment, and arid climate govern the composition of clay tills. The main purpose of this work is to develop a clear understanding of the engineering behavior of compacted clay till under soil suction and applied stress. The results indicate moderate water adsorption due to the presence of clay minerals (26% corrensite, 10% illite, and 8% kaolinite) with Ca2+ as the dominant cation and a flocculated fabric in a slightly basic (pH = 7.5) pore water. The water retention curve comprised four transition points that are associated with capillary water drainage from large pores (air entry value of 2 kPa and residual suction value of 20 kPa) and small pores (air entry value of 700 kPa and residual suction value of 5 × 104 kPa). Beyond the last value, vapor flow is dominant and removes the adsorbed water by evaporation. The ratio of soil volume change to water volume change best described the s-shaped shrinkage path that also comprised four stages, namely: from most large pores with low volume change; from remaining large and most small pores along with almost equal volume change; from some small pores with low volume change; and from the rest of the small pores with no volume change. Likewise, the s-shaped swelling potential curve comprised three stages and correlated well with bimodal hydraulic conductivity curve, that is, slow initial swelling (unsaturated hydraulic conductivity around 10−14 m/s) due to expansion of peripheral clay in lumps; high primary swelling (unsaturated hydraulic conductivity of up to 10−11 m/s) due to thickened double layer of most colloids; and slow secondary swelling (albeit unsaturated hydraulic conductivity around 10−10 m/s) due to expansion of remaining particles. Soil compression (compression index of 0.164) was due to a gradual reduction in number of large pores, whereas rebound (swelling index of 0.047) was due to water adsorption on clay with part of the deformations recovered. Finally, the consolidation rate was related to saturated hydraulic conductivity, which varied by three orders of magnitude.

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Section: Soil and Pore Water Compositionsmentioning

confidence: 99%