Abstract:
All the landslides in Sri Lanka are triggered by excessive rainfall. Sloping grounds in Sri Lanka
are formed of; residual soils, rocks at different levels of weathering and colluvial soils. During
periods of dry weather, the groundwater table is low and prevailing matric suctions will ensure
stability. With rainwater infiltration, matric suction will be reduced or lost, and perched water
table conditions may occur developing instability.
Susceptibility to landslide in hilly terrain was assessed by National Building Research
Organization considering six terrain factors, and four levels of susceptibility were established.
The threshold rainfall values triggering failure in these four regions would be different. Hence,
they should be obtained by proper modelling of rainfall infiltration and the subsequent
reduction of safety factors. In the absence of such an analysis, threshold values based on
experience are currently used in issuing warnings. The process should be improved by
identifying site-specific threshold values.
In this research, initially, a parametric study was conducted by applying different rainfall
intensities for a typical high slope of uniform residual soil layer and a layer of residual soil
overlying a weathered rock using GeoStudio 2018. The threshold values were obtained under
different initial conditions (cohesion and matric suction). A strong correlation (R2 ~ 0.9)
between rainfall intensities and duration of instability was observed in all cases. Hence, if the
rainfall intensity of a particular event is known, the time taken for instability can be estimated.
It will be important to take remedial measures and make decisions on early warning more
reliable. Also, the identified dependence of threshold values on the initial conditions
highlighted the importance of establishing site-specific threshold values.
The study was then extended to three actual landslides: Pinnawala, Badulusirigama and
Ginigathhena. The rainfall records that triggered the landslide at Pinnawala were available.
Hence, the failure event was back analyzed using the subsoil conditions that were established
subsequently during the rectification stage. As Badulusirigama and Ginigathhena slopes were
recently rectified, the threshold intensities were studied separately for the situation before and
after the rectification. A clear indication of an increase in threshold rainfall values was
established. Hence, these slopes would be able to withstand intense rainfalls that may fall due
to climate changes. However, any records of the rainfall events that caused failure at the two
locations were not available for any back analysis.
The slopes with varied rectification techniques reveal that subsurface drains, which lower the
water table and partially desaturate the topsoil, more efficiently increase stability than surface
drains. The surface drains are only effective while raining to facilitate runoff before infiltration.
