Mending the gap - Landscape Conservation for the island of Aliabet, Shreeni Benjamin

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Mending the Gap Landscape Conservation for Alia-bet

Shreeni Benjamin


Grains of Island of Alia-bet

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Abstract Coastal management is one of the most important parameter to be considered in urban planning for a resilient future. In today’s time especially when we are on the brink of climate change, it becomes mandatory to look at the existing ecosystem services and it’s impact in a larger spectrum. The island of aliabet is a part of the river Narmada’s estuary which has formed connections with the mainland due to the depositions afflicted by the anthropogenic activities like the construction of the Sardar Sarovar dam. Once an ecologically rich and diverse chunk of land, Aliabet was a home to many wetland birds and animals. The present conditions and disturbances has replaced the existing physical conditions and habitats that has affected to the biodiversity in many ways. The imposed man-made conditions has left Aliabet to become a desert and a saline wasteland. This research study is an attempt to understand the drivers and services of the ecosystem of Aliabet in order to revive and strengthen its resources thereby regaining its position in the larger ecological chain.

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3

Abstract

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Process

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Global Impact

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Narmada Estuary

24

Inside Aliabet

42

Proposal

66

Ecosystem services

69

Acknowledgment

70

References Content

Contents

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process

The process began with asking intriguing questions, based on the prior years of formal training and education in the field of Architecture and Landscape to finally stumbling upon an area of interest that resonated with a promising prospect. After identifying the area of concern, a deep, cohesive research oscillated between the ‘foundings’ and the undiscovered areas; to formulate a method of venturing the project further. This process involved intense discussions with the tutor and several brain storming sessions with other faculties to identify the scope and the overlooked details and inquiries if any to formulate a basic structure of the project. Formulation of the basic structure led to the collection of the primary data which began with multiple engaging site visits and verbal surveys. The oral narratives from the site visits raised

additional questions to an already unanswered questionnaire made while initial research. But with further engagements with the locals, various secondary resources including the discourses with the tutor helped unfolding a precise narrative. And as a result the questions of research became pointed and specific. This aided in reducing the spectrum of solutions and its search. The importance of existing research paper and softwares like GIS became essential. As they helped to generate the current data. The clear research questions focussed on targeted cases of solution that bought good time for generating appealing representation drawings. With the help of relevant case studies and added skills from prior training the resolution came out naturally in time. Though as a designer the outcome can always be improved but for the given scope of time and scale, the resulted outcomes were accepted as part of this research.

Process

The following research is an outcome of a 4-month long Studio project carried out during the final semester of the ‘Master of Landscape Architecture’ program at CEPT University. The project was carried out under the guidance of professional and senior studio tutors, faculties and external reviewers.

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Global impact

East- African West Asia Flyway

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The location of the site globally falls under the rich and hot tropical waters of the world, which are full of nutrients and varied bio-diversity. The highlighted circle is the larger site area. There are nine flyways in the world, a flyway is a geographical region within which a single or a group of migratory species completes its annual cycle - breeding, moulting, staging and non-breeding.

https://www.feow.org/global-maps/major-habitat-types http://wgbis.ces.iisc.ernet.in/energy/water/paper/TR123/section6.htm


global impact Flight path coinciding the site

Region of Aliabet

Central Asian Flyway encompasses overlapping migration route over 30 countries. The Indian sub-continent is a host to 370 Avian varities, 310 species of them use wetlands as habitat. Some of the species include the endangered Indian Saru, Flamingos, Pelicans, Tibetan crane, European roller and Red-necked crane amongst many others.

Global impact

Central Asian Flyway

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Narmada Estuary History and Evolution Narmada, the oldest river system in India, originates from Amarkantak in Madhya Pradesh, flows east-west, and joins with the Gulf of Khambhat on the Arabian Sea. The river drains 45.64 km3 of annual run-off and a series of dams was proposed to hold some of its water resources for multipurpose use.

The banks of Narmada are steady and the course relentless. The Narmada is basically a sloping stream, in contrast to Ganges or Indus. It has no long, expansive flood fields reached out more than a great many hectares, as in the Indo Gangetic fields. Alia-bet in Gulf of Khambhat

Rift

Singhbhum protocontinental plate

Narmada-History and Evolution

Dharwar protocontinental plate

Figure . on the right: Upper course of river Narmada

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https://www.mapsofindia.com/maps

The Narmad rift valley was a result of the upliftment between the Protocontinental plates of Aravali, Dharwar and the Singhbhum fracturing along the Precambrian patterns.

Biswas (1987)

bay

a

mad Nar r rive

Kachchh Rift valley

Cam

Aravali protocontinental plate

ada Narm y valle

Rift

State of Gujarat, Alia-bet highlighted with the Rift valley system at the Gulf of Khambhat, which is a part of an active estuarine area and thus undergoes regular changes in terms of deposition and shifting.


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Narmada-History and Evolution


Narmada-river basin

GUJARAT

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MADHYAPRADESH

MAHARASHTRA GULF OF KHAMBHAT

Map . Narmada river basin

https://www.mapsofindia.com/maps/rivers/narmada.html


Network of Narmada The Narmada, additionally called the Rewa is a waterway in central west India and the fifth longest stream in the Indian subcontinent. It is the third longest waterway that streams completely inside India. It shapes the customary limit between North India and South India and streams westwards over

a length of 1312 km before depleting through the Gulf of Khambhat into the Arabian Sea, 30km west of Bharuch city of Gujarat. The Narmada bowl, trimmed among Vindhya and Satpura ranges stretches out over a zone of 98796 Sq.km and lying on the northern furthest point of the Deccan Plateau.

Narmada Basin Area : 98,796 sq. km Length: 1312 km Dams : 30 major dams, 135 medium dams and around 3000 minor dams

Narmada-river basin

AMARKANTAK

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Area of study : Estuary of river Narmada

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Gulf of Khambhat : Geomorphology

Ravines

Younger tidal flats

Map . Gulf of Khambhat

The configuration of the Landforms in the Gulf of Khambhat consists of the Older tidal flats, Younger tidal flats and Ravines. The island of alia-bet is part of a younger tidal. flat. The younger tidal flats are a recent addition which is formed by the deposits of the sea and river due to the upliftment of

the rift valley and some anthropogenic pressure. This area is a part of the active estuarine area and thus it will still undergo changes in terms of deposition and shifting. The rate of the river flow will remain slow and thus the formation of shoals and deposition will continue to happen.

https://www.mapsofindia.com/maps/rivers/narmada.html Biswas (1987)

Gulf of Khambhat: Geo-morphology

Older Tidal flats

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water sweet

Fluvio-marine Dynamics of Aliabet

er at tw

ee sw

Arabian sea

Narmada River, west of Bhadbhut, enters in the delta region, part into two distributaries. These distributaries circle Aliabet, comparing Gulf of Cambay. Along the two banks of the waterway, mudflats and swamps are framed. Following reasons will define this Deltaic part of Narmada, AliaBet is an estuary:

01. Before Sardar Sarovar Dam, Aliabet was an island and was surrounded by river water channels on all the sides

Narmada- Fluviomarine dynamics

• Most parts of Aliabet stays submerged in the water during the elevated tide and it gets completely submerged amidst the floods. • During elevated tide, water stretches out up to Broach and even past. • Marshes and mud-pads are framed on both the banks and the island.

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Alia-Bet has been developing in size quickly with time. Its upper segment is portrayed by broad swamps and mud pads shaped in a bungle design by tidal channels and creeks. Its central part does not experience numerous progressions as it is secured by the shrubs and grass. In any case, this gets submerged amidst the elevated tides and floods. It is seen that the development of Aliabet is toward the sea side as opposed to upstream. Different variables might be in charge of this toward the ocean development. The distributaries streaming at the edges of the island cut the bank of the island and store silt along its edge. In this manner, the island develops in size and the distributaries’ sizes don’t change. Narmada River can likewise be an explanation behind the development of land mass. Mudflats are found along both the banks of Narmada River. In the northern part, they stretch out toward the west of Bharbhut and in the south, they reach out from north of Gonpatpura to south-west of Ambheta.

Map 1. https://www.mapsofindia.com/maps/rivers/narmada.html Map 2. By author Map 3. Google Earth

02. Aliabet was part of an active and perennial estuary where the water was a part of a varying salinity throughout the year

sea

er wat

03. During Floods and high tides the sea water currents travels North and North-Eastern part of the Gulf of Khambhat


Saline Wasteland

04. After the floods, the water recedes back to the sea

leaving behind loads of sediment, which is then left for the river water to clean up during ebb.

07. The process leads to the shifting of the Mudflat towards the mainland to an extend that it completely fills up the river water channel on the other side of the island. Forming a landwise connection to the island.

sion

Ero

ion

sit

05. River water has now lost the pressure to flush out the sediments in to the sea leading to the sediment deposition

08. The East-West aligned island faces saline water to a larger extent which shifts the ecological plane and leaves the island devoid of its natural vegetation

n

sio

sion

Ero

Ero

ion

sit

po

De

06. More deposition leads to the formation of Sand bars and Shoals, also many submerged sediments emerges in the absence of adequate flushing

09. The present condition may increase the deposition of the island towards the sea

Narmada- Fluviomarine dynamics

po

De

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Impact of Sardar Sarovar Dam

Narmada- Sardar Sarovar Dam

Invincible Sardar Sarovar Dam

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The 458.3km long, 1,133 cumecs limit Narmada Main Canal in Gujarat is the biggest water system lined waterway on the planet. It further reaches out by 74 km in Rajasthan, and has 38 off-taking branch trenches being worked in stages. The construction of the river Narmada required clearance of more than 10,000 hectares of forest, Not only the forests but the displacement of the surviving tribes by the banks of river Narmada whose livelihood was the river itself. Artificially dammed Narmada, has lost more than 10,000 hectares forests which has resulted in to the deposition of silts on the riverbed, heading into blocking of the entire rift valley.

The dam also resulted in thinning out the river channel which impacted its adjoining river ecology and biodiversity. The flowrate of the river dropped drastically and it affected the overall level of the water which in turn raised the hidden islands and shoals in the estuary.The stable banks of Narmada due to the forests are now devoid of its steady agents, which opens them now to destruction through floods. Minus the forests this river is facing raging torrents in the rains and dried up water courses in the summer. One of the shoals has resulted in to a considerably huge island named Aliabet which conserves a diverse and rich ecosystem of the Estuary.


Evolution of Natural features 1995

2000

2005

2010

Mangrove

Aliabet : Satellite images

Vegetation

Hydrology

Erosion & Deposition

1985

Map 1. https://www.mapsofindia.com/maps/rivers/narmada.html Map 2. By author Map 3. Google Earth

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Aliabet : GIS maps Maps generated from the remote sensing tool indicates heavy loss of habitats over the period of years. The 1974 map shows an extensive spread of mangroves across the island. Over the period of years mangroves disappear drastically and salt pan and salt marsh which were absent before starts appearing. One of the reason for the loss of mangroves projected is also due to the communities living close by that used the mangroves for wood fire. And salt pan changed the land terrain to a larger extent inviting saline water inside the land changing its existing ecology.

Map . 1974

201 1

01

Aliabet ; GIS maps

1974

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20

Salt Marsh Geographic Information System.2019

Mudflats

Mangrove

Salt Pan


Map . 2001

Map . 2011

Scrubland

Creeks

Settlement

Depression

Aliabet ; GIS maps

Mudflat Mangroves Scrub Shoals Salt Marsh Salt Pan Creek Depression / Water logged area

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Gulf of khambhat

Bharuch

Bhadbhut

a ad

rm

Na

Gulf of khambhat

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Aliabet 238 sqkm2

Ankleshwar

r

e riv


Sardar sarovar dam

Lower Narmada trail of Sardar sarovar dam to the Gulf of Khambhat. Narmada River, west of Bhadbhut, enters in the delta region, part into two distributaries. These distributaries circle Aliabet, and merges in the Gulf of Khambhat. Along with the two banks of the waterway, mudflats and swamps are framed. The Sardar sarovar dam is situated approximately 110 km away from the estuary of river Narmada

Gulf of Khambhat

Scale of the population in towns and villages nearby

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inside aliabet

Inside Aliabet: Elevation and Tidal range

Natural features: Elevation and Tidal ranges

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Map . Contour map

0

2.5

5

10 km

2m 4m 6m 8m 10 m


Map . Spring Tides

The average of periodical tides that occurs twice a month is estimated between 3.5-4 m

The highest amplitude of tide 6m during flooding of the sea

Map . High high tides 0

2.5

5

10 km

Inside Aliabet: Elevation and Tidal range

Map . Neap Tides

The average of the regular tides that occurs everyday is estimated 1-1.2m

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inside aliabet Natural features: Vegetation

Inside Aliabet: Vegetation

Avicennia marina

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Cressa cretica

Suaeda nudiflora

Main mangrove species

Mangrove associate

Mangrove associate

It is 0.5 to 2m high; stem glabrous much branched; pneumatophores 3-10 cm long, narrowly pointed, straight, not branched or hooked. Leaves 6 x 2 cm, ellipticoblongcorriaceous, dark-green, shining above, yellowish papilliose beneath, acute or obtuse at apex.

Coastal ground cover and creeper

Coastal ground cover and creeper

Shrubby diffuse herb about a feet high arising from a woody perennial rootstock. Flowers are small, white or pink, nealy stalkless in upper leaf axils. Soft leaves but saline in nature

A diffused branched, woody, perennial under shrub, stem prostrate, much branched, smooth, yellowish.

High salinity Near the coast Not eaten as a fodder

High salinity Near the coast Not eaten as a fodder

High salinity Near the coast Not eaten as a fodder

Devi, Vandna & Pathak, Bhawana. (2016). Ecological studies of mangroves species in Gulf of Khambhat, Gujarat. Tropical Plant Research.


Sesuvium portulacastrum Mangrove associate Perennial coastal ground cover and creeper Leaves have fleshy blades that are oval or lance-shaped, very succulent, flat above and convex below. 1.5-2 cm long leaves

Salvadora persica

Porteresia coarctata

Evergreen shrub or a tree

Coastal grass

A diffused branched, woody, perennial under shrub, stem prostrate, much branched, smooth, yellowish.

It has narrow, tough blades and special glands that secrete excess salt, allowing it to withstand intense heat and daily exposure to salt water.

Soft leaves but saline in nature Brackish water

Saline to brackish waters Near the coast, Along the creeks, Depression and water logged areas Less prefered by the animals. Leafs are soft but salty

Near the coasts

Near the estuary and water logged areas as creeks only during the monsoon and the initial period of winter Reason for declination: Accumulation of sediment absence of brackish water

and

Inside Aliabet: Vegetation

High salinity

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inside aliabet Natural features: Biodiversity Residential birds

Black hair-crested drongo

Common crane

Pond grey heron

Reef Haron

Black headed gull

White Egret

Grey Shrike

The forest officials of Bharuch have spotted various birds on Aliya Bet. Some of them are also Migratory birds from the Northern part of the world: China, Siberia and Russia are said to visit Gulf of Khambhat and Aliya Bet. Around 20,000 flamingos visit Aliya Bet in a year. Thousands of waterfowls can be seen in the salt- pans of Aliabet from October to March. The forest officials of Bharuch have spotted various birds on Aliabet. Some of them are also Migratory birds from the Northern part of the world: China, Siberia and Russia are said to visit Gulf of Khambhat and Aliya Bet. Around 20,000 flamingos visit Aliya Bet in a year. Thousands of waterfowls can be seen in the salt-pans of Aliabet from October to March.

Inside Aliabet: Bio-diversity

Migratory birds

Red necked Flamingo

Brown pelican

European roller

Painted Stork

Common Sandpiper

White necked Kingfisher

Bar-tailed god-wit

Aquatic creatures

The Kharai was recognised as a separate breed in 2015 by the Indian Council of Agricultural Research (ICAR). These camels are unique. Because they have the special ability to survive on both, dry land and in the sea. They swim in seawater and feed on saline plants and mangroves. Presently there are about 600-650 camels. http://birdsofgujarat.co.in/checklist.php

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Hilsa

Catfish

Mudskipper

Giant freshwater prawn

gb, Sreekanth & Jaiswar, A & Zacharia, P U & Pazhayamadom, Deepak & Chakraborty, S. (2019). Effect of environment on spatiotemporal structuring of fish assemblages in a monsoon-influenced tropical estuary. Environmental Monitoring and Assessment.


Inhabitants Jhat-Maldhari Community

Aerial view, Settlement at higher elevation, Aliabet

With a total of 110 familes (appr. 450 people), the Jat maldhari familes are the only community residing in Aliabet. They came to aliabet 250 years back in search of pasture for their cattles and carried out a journey of coming back an forth from Kutch to Aliabet for camel trading and rearing. Decrease in the local grass “aal” has reduced the number of camels from 2000 to 600 at present.

Potable water bought from nearby towns

Temporary huts made from hay stacks and wooden posts.

Inside Aliabet: Inhabitants

Animal husbandry is the primary occupation, with a total estimate of 1800 buffaloes and goats in the entire community. Fodder plays an important role for thriving the community which is bought from the nearby farms and towns.

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Settlements in the vast plains of


Vegetation types in Aliabet

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Inside aliabet

Map . Land-use

0

2.5

5

10 km Mud flat Salt Marsh Scrubland Mangroves Depression Ponds Settlements Salt pan Connection

Inside Aliabet : Land Use

Land-use and Vegetation types

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2011 2001 1974

Salt-marsh flat

Salt Marsh

27.1 %

Aliabet: Land use Mudflats and Wetlands Coastal edge and Salt-marsh Creeks and Depressions Flat land and Scrub-land Dense forest

Mangrove Cressa cretica

Suaeda nudiflora

Reef Haron

Inside Aliabet : Salt Marsh flat

Aliabet: Typical section

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Prosopis cinnereria

Tenualosa ilisha

Sesuvium portulacastrum

Brown pelican

Features

Issues

Sediment filteration Breeding ground for migratory brids and aquatic creatures Surge barriers

Groundwater Salinisation Degraded coastal edge Diminishing ecological habitat

Avicennia marina

Painted Stork

0.5 %


2011 2001 1974

Creeks

Tidal creeks & Depression

2.4 %

Aliabet: Land use Mudflats and Wetland Coastal edge and Salt-marsh Creeks and Depressions Flat land and Scrub-land Dense forest

Depression Black headed gull

Prosopis cinnereria

Grey Shrike

Sesuvium portulacastrum

Common Sandpiper

Suaeda nudiflora

White Egret

Porteresia coarctata

7.0 %

Tenualosa ilisha

Features Habitat for Hilsa fish, Migratory birds Ground-water recharge

Aliabet: Typical section

Salinity ingress Filled up creeks Diminishing natural vegetation

Inside Aliabet : Tidal creeks & Depression

Issues

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2011 2001 1974

Wetland

Mudflats

22.4 %

Aliabet: Land use Mudflats and Wetlands Coastal edge and Salt-marsh Creeks and Depressions Flat land and Scrub-land Dense forest

Pond grey heron

White necked Kingfisher

Inside Aliabet : Wetland

Aliabet: Typical section

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Common crane

Black headed gull

Red necked Flamingo

Grey Shrike

White Egret

Sesuvium portulacastrum

Tenualosa ilisha

Porteresia coarctata

Giant prawn

Painted Stork

Features

Issues

Feeding grounds for Migratory birds, Kharai camels, underground aquatic organism Ground-water recharge

Ground salinisation Diminishing natural vegetation


2011 2001 1974

Scrub-land

Scrubland

18.1 %

Aliabet: Land use

Prosopis cinnereria

Black hair crested drongo

Aliabet: Typical section

Sesuvium portulacastrum

Bubalus bubalis

Capra aegagrus hircus (goat)

Features

Issues

Grazing grounds for Buffaloes and goats Habitat for animals and birds

Groundwater Salinisation Diminishing local vegetation

Inside Aiabet : Scrub land

Mudflats and Wetlands Coastal edge and Saltmarsh Creeks and Depressions Flat land and Scrub-land Dense forest

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2011 2001 1974

Dry deciduous forest

Dense forest

1.2 %

Aliabet: Land use Mudflats and Wetlands Coastal edge and Salt-marsh Creeks and Depressions Flat land and Scrub-land Dense forest

Ailanthus excelsa

Tamarindus indica

Pavo cristatus

Albizia lebbek

Black hair crested drongo

Sesuvium

Bubalus bubalis

Peltophorum pterocarpum

Capra aegagrus hircus (goat)

Features Highest elevated area Settlement area for the local tribe Habitat for animals and birds Issues Groundwater Salinisation

Inside Aliabet : Dry deciduous forest

Aliabet: Typical section

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Cressa cretica


Mangrove chain of connections

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Rainfall Temperature

Jan

Feb

Mar

Apr

May

27

30

33

35

36

0

0

0

0

0

Celsius

Windspeed

%

9.7

10.3

12.1

13.7

17.9

28

24

22

31

44

38

Presence of few migratory birds

Hilsa fish

Partially active wetlands

Inundation

Inside Aliabet : Annual events

Local grass

Migratory

m/s

Humidity

mm

https://www.worldweatheronline.com/lang/en-us/hansot-weather/gujarat/in.aspx

High Temperature Absence of birds and vegetation Dried up wetlands


Jun

34

Jul

29

Aug

Sep

Oct

Nov

28

30

33

31

26

62.5

7

0

0

1023

Dec

24.4

21.4

20.4

13.8

8.3

9.4

11

60

79

78

68

37

31

29

Water recedes back to sea

Flooding and Sedimentation

Active coastal wetland Recreational period for near by towns and villages High Fishing activities

Inside Aliabet : Annual events

Aliabet inundates

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Diminishing of the brackish water-zone

Inside Aliabet : Connections

Reduction in the Residentary and Migratory birds

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Reduction in the number of Kharai camels

Absence of fodder for the animals of the herding community


inside aliabet Aliabet Connections and Survival chain thousands of waterfowls can be seen in the salt- pans of Aliabet from October to March. The only residing community the “Jhat maldharis” (Animal herders) who thrive on fresh river water and there domestic animals like camels, buffalos and goats are suffering because of lack of fodder and potable water. Camels have now adapted to survive on both, dry land and in the sea. They swim in seawater and feed on saline plants and mangroves. Presently there are 600-650 left of them.

Inside Aliabet : Connections

Narmada estuary is famous for the Hilsa fish that breeds in the ocean water but travels back to the brackish water for the rest of year. Sedimentation and Salinity ingress has reduced the rare mix of various saline levels and temperature of the brackish water to a larger extent, damaging its dependent ecology like the Mangroves and the “Aal grass” Reduction in Hilsa fish and Aal grass has affected in the number of wetland birds. Various migratory birds from China, Siberia and Russia are said to visit Gulf of Khambhat and Alia Bet. Around 20,000 flamingos,

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Proposal Strategy for Damage control

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Replenishing mangroves using salt-tolerant species

Prevention of Coastal Erosion by providing a natural surge Barrier

Filtration of sediments at both the ends of land and water

02

conserve

Proposal : Strategy for Damage control

replenish

01

Nursing grounds for local and migratory fishes and crustaceans

Preventing Salinity ingress

By introducing barriers at the strategic locations leads to conservation of water and prevention of sea-water to flood and degrade the resources further


replenish

03

SALT

BRACKISH

FRESH

Cultivating fodder for the grazing animals

+ Cultivation of fodder strengthens the only residing tribal community and their livestock, increasing the ownership and responsibility towards the degrading island more.

Proposal : Strategy for Damage control

Conservation of fresh water can help re-generate the lost habitats of varying salinity and biodiversity.

04

flourish

Fresh water conservation

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Proposal 01

Proposal : 01 Replenishing of Mangrove swamps

Replenishing Mangroves

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Map . 01 Mangrove swamps followed by salt marsh Replenishing the belt of mangroves in the descending order of salt tolerant species from the sea-ward to land-ward side. This will restore the lost habitats for the migratory birds and the benthic organisms of the mudflats.

Figure . on the right: Coastal edge before and after restoration of mangroves


BEFORE

Degraded edge

Encrusted salt

Filled up creeks Vegetated creeks

Salt marsh

Halophytes

AFTER Nesting grounds

High

Medium

Low

Salt tolerance of Mangroves

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Proposal 02

Salinity - High tide - After construction of Embankments

Areas under embankment : Salinity level - Less

Proposal : 02 Preventing Salinity

Understanding Salinity with Embankments

Salinity - Spring tide - After construction of Embankments

Areas under embankment : Salinity level Extremely low to moderate

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Salinity - Neap tide - After construction of Embankments

Less Moderate Extremely

Areas under embankment : Salinity level Extremely low to null


Embankment-Details

Typical section after the construction of embankment

Platform Overflow drain E-concrete Boulders packed with sand

Embankment section

E-concrete is an ecofriendly material that allows the growth of oysters and corals on its surface along with moss and algae. This promotes the small fishes and shrimps make shelter around it.

Embankment wall after 1-2 monsoon season

Proposal : 02 Embankment Details

Impenetrable concrete foundation mattress

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Salinity after Embankments

More than 90% of the area is subjected to salinity ingress

Less Moderate Extremely

Proposal : 02 Preventing Salinity

Map . Existing Salinity gradation

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Map . Spring tides before embankments

Map . Spring tides after embankments

More then half of the land parcel gets submerged periodically.

Creating embankments above the height of the spring tides at strategic levels to prevent the saline water from entering inside the land.

Map . Spring tides after Embankments & Rainwater pools The rain-water can be then conserved in the areas of depressions which were earlier flooded by the sea water.


Achieved state of salinity after embankments helps promote native vegetation and inhabit local bio-diversity

Less

0

2.5 5

10 km

Moderate Extremely

Map . High tides Second level of embankment above the height of the high tides preventing the saline water to enter at all.

Map . High tides after Embankments Extent of the high tides floods the first level of embankments making the water brackish in nature.

Map . High tides after Embankments & Rain water pools Rain water conserved after monsoon in the areas dammed under the second level of embankments which percolates to improve the salinity of the land.

Proposal : 02 Preventing Salinity

Map . Achieved Salinity gradation after 3-4 seasons

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Proposal : 02 Preventing Salinity

The three waters of Aliabet

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SALT FRESH BRACKISH

Map . Retained water - After Monsoon By introducing barriers at strategic locations leads to rain-water conservation and prevention of sea-water to flood and degrade the resources further

0

2.5

5

10 km


Brackish water

2 - 2.5 m

Fresh water

2-2.5m

4 - 4.5 m

Summer Winter

1-1.5m

1 - 1.5 m

3-4.5m

3 - 3.5 m

Monsoon

3 - 3.2 m

1.5 - 2 m

51 Figure . Expanse of waterbodies during different seasons


SPECIES

HABITAT

Variety of inland and coastal waters including lakes, marshes, mangroves and tidal creeks

WATER

WATER

S,B,F

Little egret

Wet and Dry grasslands, saltmarshes and coastal lagoons

S,B,F

Common crane

Glossy ibis

Lakes, rivers, grasslands, swamps, and coastal marshes.

Variety of inland and coastal waters including lakes, marshes, mangroves and tidal creeks

S,B,F

S,B,F Grassland, Marsh edge

Black headed gull

S,B,F

Red naped ibis

Coastal estuaries, saltmarshes, mangroves, small trees and bushes

F

S,B,F

Grasslands with freshwater ponds Red-wattled lapwing

Reef Haron

Well-spaced shrubs or low trees

F

Grey Shrike

Brackish or saline lakes or estuarine lagoons

S,B

Oceans, Mangrove swamps

S

Wetland, Swamps, Marsh

S,B

Wetland, Swamps, Marsh

S,B,F

Red necked Flamingo

Freshwater and Salt water areas

Avi-faunal Habitat

HABITAT

Lakes, rivers, marshes, Saltpans, estuaries

S,B,F

Pond grey heron

S,B,F

White Egret

Brown pelican

Lakes, rivers, marshes, Salt-pans, estuaries

S,B,F

White necked Kingfisher

52

SPECIES

Painted Stork

Variety of inland and coastal waters including lakes,

S

marshes, mangroves Bar-tailed godwit

and tidal creeks

Black necked stork


SPECIES

HABITAT

Light hill forest, Open wooded country and cultivations

WATER

SPECIES

F

SPECIES

WATER

Lakes, rivers, marshes, Light to deciduous forest

S,B,F

F Indian peafowl

European roller

F

S,B,F

Dense forest, Woodland

Well-spaced shrubs or low trees

F Spotted owlet

Merops orientalis

F

Common myna

Light hill forest, Open wooded country and cultivations

Woodlands, light hill forests

Black kite

Wet and Dry grasslands, Well spaced shrubs or low trees

Dense forest, Woodland and Meadow

Coppersmith barbet

F

Wet and Dry grasslands, Well spaced shrubs or low trees

Well-spaced shrubs or low trees Black drongo

Anthus campestris

F

Grasslands with tall grasses

Crested lark

Coastal wetlands, and freshwater source during breeding

S,B,F Indian skimmer

Wetlands, Swamps

Saru crane

S,B

Greater flamback

F

Bllue hair-crested drongo

S,B,F Dense forest, Woodland

F

F

53 Coastal wetland, Marshes

Common Sandpiper

Avi-faunal Habitat

Jungle babbler

Wet and Dry grasslands, Well spaced shrubs or low trees

F


SALINE

Sesuvium portulacastrum

Inventory - Shrubs and grasses

Leptochloa fusca uninervia

54

BRACKISH

Salsola iberica

Haloxylon salicornicum

Paspalum vaginatum

Salicornia brachiata Salvadora persica

Salsola iberica

Atriplex halimus

Paspalum vaginatum

Suaeda nudiflora

Aeluropus lagopoides

Heleochloa setulosa

Porteresia coarctata

Limonium stocksii


BRACKISH

Cyperus conglomeratus

Sporobolus maderaspatanus

Halopyrum mucronatum

Salvadora persica

Juncus effusus

Terminalia arjuna

Typha angustata Echinocloa colonum

Cyperus iria

Tradescantia axillaries

Fimbristylis tenera

Syzygium cumin

Heliotropium supinum

Tamarindus indica

Inventory - Shrubs and grasses

Cressa cretica

FRESH

55


Proposal : 02 Progressed habitats

Progression of Wetland habitats

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Map . 02 Freshwater and Brackish water habitats

Figure . on Pg: 53 Wetland habitats generated for the birds and residentary grazers after the construction of embankments


After the construction of embankments

Embankments as platforms for the tourist

Water-retaining ponds during the winter

E-concrete

57


Proposal 03 Bio-saline Agriculture Bio-saline agriculture - Cultivation of the salt-loving grasses or Halophytes Salinity ingress like in the case of Aliabet is a very common rapidly growing problem in many parts of the world due to seawater intrusion into aquifers or reduced river-water flushing. So much so that some farmers prefer to abandon their saltdegraded lands as traditional crops fail. The problem poses challenges to national efforts to enhance food security and self-sufficiency through local production.

Proposal : 03 Bio-saline agriculture

Bio-saline agriculture is one of the successful remedies to rejuvenate the ground with nutrients and make food production.

58

Leptochloa fusca subsp uninervia

Paspalum vaginatum

Halophytes is a potential source of salt resistant genes for increasing the salt tolerance of conventional crop plants. It is a potential source of halotolerant bacteria with plant growth promoting potential. It adds to the protection of the coast. Serves as a food source for the grazers. And in addition also acts as s Phytoremediation tool (restoration of heavy metal-contaminated land) and a Phytodesalinization tool (revegetation and remediation of salt-affected land). The wood and fibers produced helps in balancing the carbon cycle and reducing global warming

Salsola iberica

Distichlis spicata

Etesami, H., & Beattie, G. A. (2018). Mining Halophytes for Plant Growth-Promoting Halotolerant Bacteria to Enhance the Salinity Tolerance of Non-halophytic Crops. Frontiers in microbiology, 9, 148. doi:10.3389/fmicb.2018.00148

Sporobolus virginicus


Map . 03 Grasslands preceded by wetland habitats

Map . 04 Woodlands

Proposal : Succession of Forests

Succession of forests

59


20 20km km

10 km 10 km

60 km 00km

10km km 10

20 km

Map . 05 Succession of Woodlands to Dense forests and addition of the farmlands to cultivate the fodder.


Mangrove swamps Salt Marsh Brackish wetlands Fresh water ponds Grasslands Woodland Dense forest Farming 30 km

Embankments

61


Proposal 03 Tourism

Settlements Freshwater harvesting ponds

Agriculture

Proposal : 03 Tourism

Map .

62

Tourist Trail

0

2.5

Close to 25% of the land can be opened to public for research and tourism. The chosen land parcel includes the residential area of the Jhat-maldhari trip, productive farm lands and various wetland habitats for bird watchers, in addition to a part of the mangrove swamps.

Figure . on Pg 59_Conservation pools close to the ‘Animal herders’ community

5

10 km


SUMMER

MONSOON

E-concrete

Catchment ponds

63


Proposal Mangrove swamps

Marsh land

Freshwater wetland

Percolation

Woodland

Percolation

Percolation

Low marsh High marsh Mangrove Swamps

20 - 30 YEARS

64

EXISTING

Brackish- Marsh land

Intertidal flat

Fresh water wetland


Dense forest

Settlements

Percolation

Dense forest Upland forest/ Terrestrial bird habitat

Freshwater ponds

Farming

Percolation

High marsh Fresh-water Wetland

Settlements Dry deciduous forests

Farming

Proposal : Strategic Section

Woodland

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ecosystem services Sanctuary for Biodiveristy

Breaks floods, storm surges, protecting the coastal edge

Sediment Filters

Healthy Environment Indicators

Mangroves sequests 2.5 x more carbon then any tropical forest

Ecosystem Services

Nursery for various species of fishes and other creatures

66

Mangroves can be sustainably harvested in the future for honey, fuel and timber

Enough fodder for the residentary and migratory biobiversity


Fishing

Promotes research

Wilderness is our last habitat too, connecting with it refreshes us

Access to potable water

Physical activites for improved health

Cultivation generates livelihood opportunites

aides to:

Climate change Inhabitant local tribe Tourists and Visitors

Sustainable rearing of animals in the presence of sufficent food and water

Bird watching for nature enthusiast

Bio-diversity

Ecosystem Services

Monitors pests and insects

67


“He has made everything beautiful in its time.” Ecclesiastes 3:11


Acknowledgment

Firstly, I want to express my deepest gratitude and humble thanks to my guide and Head of division, Dr. Prof. Deepa Maheshwari, without whom this postulation would have not been formed the way it has. She patiently guided me through the whole process of the project and helped me ammend my errors whenever.

This research would not be completed without a steady and consistent help from my dear ones Ashka Vyas, Keval Sakaria, Arpan Pansuria, Samarth Barot, Rutuja Ulhe, Tanvi Parab, Rainee Saparia, Dixit Narola, Lalnunmawia, Shruti Purohit, Vidisha Barwal, Swati Surampally, Saylee Shinde and Nikunj Pithwa.

I want to extend the earnest gratitude to Prof. Sandip Patil, Prof Divya Shah, Prof. Priyal Shah, and the tutors from my Internal classes Prof. Mansi Shah, Dr. Rajesh Shah, Heena Gajjar and Dipani Sutaria; thank you for the criticaI reviews and guidance. I want to thank the entire Class of 2017-19 to help and accompany me accomplish this course successfully.

At long last, exceptional acknowledgment goes out to my family, for their help, consolation, and tolerance amidst my quest for completing the degree program. The steady support and backing given by them helped me to continue pushing ahead.

D: 05. 01. 2020

Acknowledgment

Shreeni Benjamin

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References

Research papers: O. (2004). Wetland ecosystems and coastal habitat diversity in Gujarat, India (Rep.). Gujarat Ecology C Numerical Modelling of Tidal Circulation and Sediment Transport in the Gulf of Khambhat and Narmada Estuary, West Coast of India - P.C. Sinha, G.K. Jena, Indu Jain, A.D. Rao and Mohd Lokman Husain Mahapatra, Manik & Ramakrishnan, Ratheesh & S Rajawat, A. (2014). Monitoring long-term morphological changes of Narmada estuary using remote sensing and GIS techniques. 8. Babu N, Arjun. (2015). Tidal Analysis in Gulf of Khambhat (Cambay) off Gujarat Coast. Salvi, H., Das, L., Brahmbhatt, B., Vaghela, N., & Kamboj, R. D. (2017). Diversity of Halophytes in Gulf of Kachchh, Gujarat. International Journal of Life-Sciences Scientific Research, 3(3). doi:10.21276/ijlssr.2017.3.3.6 Mohan Narasimha Rao, Geddada. (2008). Mangrove population of Visakhapatnam and Sarada, Varaha estuarine complex.. Int. Jour. Plant sciences. 3. 686-687. Book: Unni, K. S. (1996). Ecology of river Narmada. New Delhi: A.P.H. Pub.\ Report:

References

Snapshot Feasibility of Alia Bet in Bharuch District _ GIDC – 2009

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Research Paper: Dhara O. Bhavsar, Yogesh.T. Jasrai and Himanshu. A. Pandya, Vijay Singh, Ajay Patel, and Manik H. Kalubarme (2014) Monitoring Mangrove Status using Remote Sensing and Geo-informatics in Piram Island, Gulf of Khambhat, Gujarat State, India, InternationalJournal of Scientific and Engineering Research Bhaumik, Utpal. (2017). A case study of the Narmada River system in India with particular reference to the impact of dams on its ecology and fisheries. Aquatic Ecosystem Health and Management. 20. 151-159. 10.1080/14634988.2017.1288529. Sedimentology of the Narmada alluvial fan, western India - L.S. Chamyal, A.S. Khadkikar, J.N. Malik, D.M. Maurya Mitra, Abhijit. (2015). Effect of salinity on nutritional value of saltmarsh grass (Porteresia coarctata) from Gangetic delta, northeast coast of India. Indian Journal of Geo-Marine Sciences.

References

Salinity rise in Indian mangroves – a looming danger for coastal biodiversity S. Sandilyan, K. Thiyagesan, R. Nagarajan and Jayshree Vencatesan Devi, Vandna & Pathak, Bhawana. (2016). Ecological studies of mangroves species in Gulf of Khambhat, Gujarat. Tropical Plant Research.

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