8/17/2019 Poster No 2 Kita
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Slippage
Causes :There are cracks on the surface
of the original
Eects :Land collapse and the moveup to exceed downslope
&accumulated at the foot of
the slope
Causes :Movement of soil awa! from "od!especiall! that are not
continuous#
Eg : fracture
Landslides
$actors :%# eathering actions that erode
slope distur" sta"ilit!#'# Stresses that lead to the
existence
of gravitational shear surface on theslope#
(# Climate change allow de"ris enterthe land#
SL)*E $+,L-.ES +T S., T)/0,LL+ .ES,1E/T+L+.E+ 2)M3+4
,ntroductionSlope5 means steep rugged steep hillsides # This
means the slope associated with the height of anea# The researchers
"elieve the higher of an area it will also increasingl! steep
slope# hereas 5ruins5
means o"6ects that have fallen the former "uilding and others
damaged de"ris#
+pplication%# *lanting grass or cover
crops'# *re cast cri" wall (# Construction of 2a"ion
wall
Location : *hase 7 Taman Sri 2om"ak Selangor#*ro"lem :
.ainfall record in the area of the slideindicate that heav!
rains on %8 %7 %9 and '% Ma! '%%"ased
on the Mala!sian Meteorological 1epartment#
CaseStud!
Slope $ailureMechanism
1uring periods of wet soil moisturecontent increased and at the
same time
decreasing the suction force suctionmatrix which will provide
additional shear
forces to the ground# ;eav! rain willweaken the shear strength
causing land
slide#
Conclusion
Solution
$ailure slope at Townvilla housing
area
Mohamad ,khwan "in Missnon+hmad +s!raf "in Sa
