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A critical evaluation of predictive models for rooted soil strength with application to predicting the seismic deformation of rooted slopes
Authors
A Parr
A Stokes
+61 more
A Stokes
AGT Temgoua
AH Al-Defae
Andrew Carnaghan
Anthony Glyn Bengough
Anthony Leung
AR Ennos
AS Zaimoglu
B Abernethy
B Tobin
BB Docker
CC Fan
CR Mora
D Boldrin
DM Wood
E Comino
E Warren
FD Shields
GG Meyerhof
GJ Meijer
GJ Meijer
GJ Meijer
GN Karam
J Lysmer
JA Knappett
Jonathan Adam Knappett
JR Greenwood
JR Greenwood
KW Loades
L Waldron
LJ Waldron
LPH Van Beek
M Genet
M Schwarz
MD Bolton
MF Randolph
MF Randolph
N Pollen
P Foray
R Sonnenberg
R Sonnenberg
RE Thomas
RL Michalowski
Rui Zhao
SB Mickovski
SB Mickovski
SB Mickovski
T Chakraborty
T Liang
T Liang
T Liang
T Liang
T Liang
T Schanz
Teng Liang
TH Wu
TH Wu
V Kamchoom
X Zeng
Y Li
Z Mao
Publication date
1 January 2020
Publisher
'Springer Science and Business Media LLC'
Doi
Cite
Abstract
This paper presents a comparative study of three different classes of model for estimating the reinforcing effect of plant roots in soil, namely (i) fibre pull-out model, (ii) fibre break models (including Wu and Waldron’s Model (WWM) and the Fibre Bundle Model (FBM)) and (iii) beam bending or p-y models (specifically Beam on a Non-linear Winkler-Foundation (BNWF) models). Firstly, the prediction model of root reinforcement based on pull-out being the dominant mechanism for different potential slip plane depths was proposed. The resulting root reinforcement calculated were then compared with those derived from the other two types of models. The estimated rooted soil strength distributions were then incorporated within a fully dynamic, plane-strain continuum finite element model to assess the consequences of the selection of rooted soil strength model on the global seismic stability of a vegetated slope (assessed via accumulated slip during earthquake shaking). For the particular case considered in this paper (no roots were observed to have broken after shearing), root cohesion predicted by the pull-out model is much closer to that the BNWF model, but is largely over-predicted by the family of fibre break models. In terms of the effects on the stability of vegetated slopes, there exists a threshold value beyond which the position of the critical slip plane would bypass the rooted zones, rather than passing through them. Further increase of root cohesion beyond this value has minimal effect on the global slope behaviour. This implies that significantly over-predicted root cohesion from fibre break models when used to model roots with non-negligible bending stiffness may still provide a reasonable prediction of overall behaviour, so long as the critical failure mechanism is already bypassing the root-reinforced zones. © 2019, The Author(s)
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