urban development in hilly eco-system terrain … development in hilly ... measures for controlling...
TRANSCRIPT
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Urban Development in Hilly Terrain with Ecological
Management Practices(EMPs)
Prof. Arup Kumar Sarma
Civil Engineering Department
Indian Institute of Technology Guwahati
ECO-SYSTEM
Water
Soil
Vegetation
AirDwellers
All sorts of living being
Result of Imbalance in Nature
• Resulting from Natural Imbalance– Flood, Landslide, Avalanches, Tsunami …….
• Resulting from Man Made Imbalance– Flood due to failure of Dam and Dike,
– Human induced Landslide and Flood,
– Environmental pollution ……..
• Man-Made Imbalance is Highest in Urban Area
• In Hilly Urban Area Such Imbalances lead to Landslide
Ecological Disturbance of Guwahati
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Back
Landslide becomes more devastating when failure
occurs in a slope having soil and rock mass Landslide in Northeast
• Apart from geological causes, landslide Occurs in many cases due to land abuse
• In Guwahati, where landslide should not have occurred from the consideration of geological structure, devastating slide has taken place (Deka, 1991)
• High correlation (0.91) between number of
landslide and Population growth has been observed in the the Guwahati City (Sarma 1991)
• Landslide in the urban areas of NE India are generally rain triggered (Sarma 1994)
Year 1972 2000
Built up area in plains (Sq km) 38.7 126
Built up area in hills (Sq km) 4.8 40
Built up area in hills and plains
7 8
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9
Monthly Income
(% of Household)
Less than Rs 2000 12%
Rs 3000-Rs10000 68%
Rs10000-Rs 20000 18 %
Above Rs 20000 6%
% of Kutcha house 34%
% of Household without sanitary toilet 27%
% of Household without pipe water supply 79%
% of Household without access road 5%
Landslide prone zones Total : 93 nos
Very steep slope : 14 nos
Steep slope : 14 nos
Gentle slope : 29 nos
Socio-Economic survey in hilly areas of Guwahati
The socio economic condition of the people implies that
attention should be given for selecting efficient management
practices at least possible cost
Influence of Rainfall on Landslide
• Direct effect
– Saturation
– Weathering and saturation
– Seepage from a perched water table
– Erosion of surface soil
• Indirect Effect
– Washing out of finer fraction
– Unfavorable orientation of soil structure
– Weathering action of water
Vegetative Cover and Landslide• Removal of vegetative cover leads to
•Splash erosion
•Rill erosion
•Gully formation leading to instability
•Expansion of natural drainage line due to higher water yield
•Erosion of top soil leads to exposition of rock resulting in their
faster weathering.
•Thus the shear strength of soil and rock mass reduces
•Erosion of supporting soil may make a purse boulder unstable
• Failure of rock may lead to devastating slide
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Multiple slides of Kacharibasti, Guwahati, Assam, India
Failure of Oct’91
Failure in Jul’89
Rock
Rock
160 m
Soil
81 m
For analysis of such slope it is essential to consider
the effect of rock mass on the stability of soil phase
as well as effect of supporting soil mass on the
stability of rock phase.
Watershed Based LanduseManagement Practices Through Ecological Management Practices
Watershed is a Hydrological Unit such that precipitation falling
within the boundary of that unit moves to a single outlet.
What is an Watershed ?
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Watershed management Aims at:
Optimal utilization and development of Water
Soil
Vegetation and
Human being
Of the Watershed
Watershed Management can be regarded as any
form of environmentally sustainable and socially
acceptable management practice that facilitates
optimal utilization of land, water and vegetation
of the watershed for the benefit of the people
residing in the watershed.
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Effects of Vegetative Cover on Water Yield (Rational method)
Present
Maximum
outflow at
pilot watershed
(cumec)
Outflow if
bareland
and open
mix forest
area are
covered
by
vegetation(cumec)
Outflow if
all the
vegetation
cover is
removed
from the watershed
(cumec)
6.031 5.27 7.25
Effect of Deforestation (RUSLE)
Present
annual
sediment
yield in tons/yr
Annual
sediment
yield in
tons/yr if
bare land
and open
mix forest
area are
completely
covered by vegetation
Annual
sediment
yield in
tons/yr if
vegetation
cover is
removed
completely
from the watershed
20943.88 7903.27 289412.6
23
Experimental Watershed at IITG CampusExperimental Watershed at IITG Campus
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Undisturbed
Disturbed
Sediments in runoffWater yield increase by 54%
Sediment yield increase by 20%
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Ecological Management Practices
Eco friendly sustainable management practices that are used for maintaining and enhancing land uses in a natural way
Some EMPs that can be used in a hilly urban area :
• Grass land
• Forest land
• Covering rain impacted areas with pebble, vegetation or wood chips
• Detention drain and Retention pond
• Sediment trap
• Vegetated waterways
• Rainwater harvesting system
Measures for runoff and
sediment control
Measures for Controlling Water and Sediment Yield
GRASS LAND
Perforated Concrete BlockSLOPE STABILIZATION STRUCTURE
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PAVED
GROUND
WITH SPACE
FOR
RAINWATER
PERCOLATION
HADGE FOR ROAD SIDE PROTECTION
ROFTOP RAINWATER HARVESTING
FOREST LAND
31
Perforated paved bocks for
the approach road
Hedge for roadside
protection
32
Vegetative EMPs
Golden Glory
Grass
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Grass
Golden glory
As compared to Bare land
Grass was found 80% efficient and
Creepers and Herbs 60% efficient in
controlling surface erosion
An optimization model has been developed for determining Optimal EMP
DESIGN OF RAIN WATER HARVESTING
(RWH) SYSTEMS
�Two options for RWH are proposed and their Layout
and Designs are discussed
�Roof Top RWH(RTRWH)
• Rain water harvesting from roof top
�Flood Well RWH (FWRWH)
• Rain water infiltration through flood wells.
�may be used individually or in combination
depending on the hydrological needs for Flood
Peak Reduction
Summary of RWH Analysis (Contd.)
After solution
Parameters
Before
Solution Only
RTRWH
RTRWH +10
FW/ha
RTRWH +20
FW/ha
Water level in drains
(m)
1.78 1.62 1.44 1.29
Sediment in
drain (m)
0.5 0.5 0.18 0.18
Depth of outlet drain (m) 1.5 1.5 1.5 1.5
Flood with sediment
control(m)
0.78 0.62 0.11 0.00
% Reduction in
Maximum Runoff
Volume
- 12.2 21.54 30.87
% Peak Discharge
Reduction
- 12.20 12.70 22.9
% Flood Reduction in
Drains (without
Sediment Control)
- 20.5 43.6 62.8
% Flood Reduction in
drains (With Sediment
Control, Studyed by
Bracht and Sarma)
- 20.5 85 100
� Landslide /soil erosion and urban flood need to be considered as
two sides of a coin
�Identification of critical issues and bottlenecks
�Awareness programme to ensure public participation
�Development of a sustainable and comprehensive plan for
mitigating landslide and water related hazard
�Survey and base map preparation for the Pilot Project in
association with Govt. Departments/Organizations
�IIT and other educational organization can provide technical
backup to the Govt. departments/organizations for preparing
necessary DPR for the Pilot Project
�development of Ecological Management
Practices for controlling sediment and water yield
�hydrological analysis and design of structural components for
landslide prevention
� innovative design concepts for drainage system
General Solution Approach
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Expected Departmental Involvement for Finding Solutions
GDD
GMC GMDARevenue
ASTEC
Soil Conservation
Environment and Forests Water resources
UDD
PWDNational Highway
Authority
• Implementation of Master Plan proposals through detail planning schemes
• Enforcement of Building Byelaws
• Coordinate Development activities as per GMDA Act
GDD: GMC and GMDA
• Verification of land-status
• Identification of Govt. land
• Resettlement programmeRevenue
• Soil conservation by structural and non structural measures
Soil Conservation
• Afforestation programmes
• Identification of Reserve Forest areas/Forest Village
Environment and Forest
• Regional planning inputUDD
• Restoring natural streams and springsWater Resources
• Construction of retaining wall, roadside drain, catchwater drain etc based on hydrological study
Public Works Department
• Urban Mapping
Assam Science Technology and
Environment Council
• To revisit for designing drainage way along the National Highway
National Highway Authority
• Awareness programme
Local NGO/ Ward Committee (special
invitee) 40