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Preliminary Investigation of the Soil-Water Characteristics of Loess Soils in Canterbury, New Zealand

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IAEG/AEG Annual Meeting Proceedings, San Francisco, California, 2018—Volume 6

Abstract

Loess and loess-derived soils cover much of Canterbury, New Zealand. When dry, these deposits exhibit an undrained shear strength up to 200 kPa and are stable in vertical cut slopes. Small increases in moisture content (2–3%), particularly near the plastic limit, lead to weakening of the soil matrix and a large reduction in shear strength. This sensitivity to moisture contributes to the susceptibility of loess slopes to failure during rainfall events. Consequently the detail of the relationship between shear strength and moisture content is important to understand. Canterbury loess soils are typically situated above the water table and therefore behave as a partially saturated soil. As such, the shear strength is influenced by negative pore pressure and interparticle bonding. Historically, the relative contribution of these mechanisms to the overall soil strength of loess soils in Canterbury is not well understood. This paper outlines the methodology for investigating the soil-water characteristics of Canterbury loess soils. Preliminary observations of the soil-water characteristics are presented.

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Acknowledgements

Current research of Canterbury loess (Yates) is supported by Environment Canterbury and a University of Canterbury Ph.D. scholarship.

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Correspondence to K. Yates .

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Yates, K., Fenton, C. (2019). Preliminary Investigation of the Soil-Water Characteristics of Loess Soils in Canterbury, New Zealand. In: Shakoor, A., Cato, K. (eds) IAEG/AEG Annual Meeting Proceedings, San Francisco, California, 2018—Volume 6. Springer, Cham. https://doi.org/10.1007/978-3-319-93142-5_9

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