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DISTRICT SURVEY REPORT

OF TIRUNELVELI

PREFACE

In Compliance to the Notification Issued by the Ministry of Environment, Forest and Climate

change Dated 15.01.2016, the preparation of District survey report of minor minerals is in

accordance appendix 10 of the notification. It is also mentioned here that the procedure of

preparation of District Survey Report is as per notification guidelines. Every effort have been

made to cover mining locations, areas & overview of Mining activity in the district with all its

relevant features pertaining to geology & mineral wealth in replenishable and non-

replenishable areas. This report will be a model and guiding document which is a

compendium of available mineral resources, geographical set up, environmental and

ecological set up of the District and is based on data of various departments, published reports

and websites. The data may vary due to flood, heavy rains and other natural climates.

Therefore, it is recommended that Sub Divisional Level Committee may take into

consideration all its relevant aspects / data while scrutinizing and recommending the

application for EC to the concerned Authority.

SURVEY REPORT

OF

TIRUNELVELI DISTRICT

As per Gazette notification of 15th January 2016 of Ministry of Environment, Forest and

Climate Change a Survey shall be carried out by the District Environment Impact Assessment

Authority (DEIAA) with assistance of irrigation department, Drainage department, Forest

department, Mining department and Revenue department in the district for preparation of

District Survey Report as per the sustainable Miner mineral mining guidelines to ensure

identification of areas of aggradations or deposition where mining can be allowed; and

identification of areas of erosion and proximity to infrastructural structures and installations

where mining should be prohibited and calculation of annual rate of replenishment and

allowing time for replenishment after mining in that area.

Every effort have been made to cover mining locations, areas & overview of Mining activity

in the district with all its relevant features pertaining to geology & mineral wealth in

replenish-able and non-replenish-able of particular areas. The mineral potential is calculated

based on field investigation & geology of the catchment area. Also as per the site conditions

and locations, depth of minable mineral is defined. The area for removal of the mineral in a

particular area is decided depending on geo-morphology & other factors, it can be 10% to

40% of the area. Other constituents like clay soil and silt are excluded as waste while

calculating the mineral potential of particular mining area. This District Survey Report shall

form the basis for application for environment clearance, preparation of reports and

appraisal of projects. The report shall be updated once every five years.

1. INDRODUCTION:

Tirunelveli district is bounded by Virudhunagar district in the north, Thoothukudi

district in the east, in the south by Gulf of Mannar and by Kerala State in the west and

Kanniyakumari in the southwest. The District lies between 08º08'09’’N to 09º24'30’’N

Latitude, 77º08'30’’E to 77º58'30’’E Longitude and has an area extent of 6810 sq.km. There

are 19 Blocks, 425 Villages and 2579 Habitations in the District.

Fig.No.1: TIRUNELVELI DISTRICT AND TALUK MAP

2. PHYSICAL FEATURES & GEOGRAPHICAL AREA:

1. BRIEF DETAIL OF MADURAI DISTRICT

S.NO ITEMS STATISTICS

i)

GENERAL INFERMATION

a)Geographical area(S.q.km) 6823.08 (12.97%)

b) Administrative divisions

as on

31.03.2007

1. Number of Taluk 9

2. Number of Block 19

e)Number of villages 586

ii)

Population

(as on 2011Censes)

Total population

Total- 3,077,233

Male-1,520,912

Female-1,556,321

iii) Average annual rainfall (mm) 879.78

Geomorphology

1. Major physiographic

units

Papanasam Upper slopes, Kalakkadu upper slope.

Chittar plains, Thamarabarani plains &

Naguneri plains.

2. Major Drainage Thamarabarani, Nambiar, Chittar & Karamaniyar

iv)

Land use (Sq.km) during 2005-

06

1. Forest area

2. Net area sown

3. Cultivable waste

1208.01 Sq.km

1666.21 Sq.km

474.42 Sq.km

v) Major soil types Deep Red soil, Red Sandy soil, Black cotton Soil,

Saline Coastal Alluvium and River Alluvium.

vi)

Area under principal crops (as

on (2005-2006)

1. Paddy 86397Ha, 62%

2. Groundnut 2553Ha, 2%

3. Pulses 2193Ha, 2%

4. Sugarcane 4614, 3%

vii)

Irrigation by different sources

(2005-06)

Number

Area irrigated (Ha)

1. dug wells - 45376

2. Tube wells - 971

3. Tanks 22272 46980

4. Canals 285 175586

5. Net irrigated area 111132Ha

6. Gross irrigated area 139776Ha

NUMBERS OF GROUND WATER MONITORING WELLS OF CGWB (AS ON

31.03.2007)

1. No of dug wells 32

2. No of piezometers 24

viii) PREDOMINANT GEOLOGICAL Recent Alluvium, Granite Gneiss & Charnockites

FORMATIONS

ix) HYDROGEOLOGY

1. Major water bearing

formation

Alluvium, weathered Granite Gneiss &

Charnockites.

ii) Pre –Monsoon depth to

water level 1. o 13.35 m bgl

2. post- monsoon depth to

water level 1. o 07.97 m bgl

3. Long term water level trend

in 10 years

Rise (m/year) Fall (m/year)

Min:0.0021

Max:1.1284

Min:0.0169

Max:0.6893

xi)

GROUND WATER EXPORATION BY CGWB( AS ON 31-03-20070

1. Number of exploration

wells 25

1. II.Number of observation

wells 5

2. III.Number of piezometers

under Hydrology project. 25

iv.Depth range (m) 20.40 to 212.0 m bgl.

v. Discharge (lps) 1 to 4.50

vi. Storativity (S) 1.87 x 10-3 to 4.8 x 10-3

vii.Transmissivity ( m2/ day) 3 to 475

xii)

GROUND WATER QUALLITY

1. Presence of chemical

constituents more than

permissible limit

NO3, CL, & TDS

2. Type of water NaCl, & Mixed

xiii)

DYNAMIC GROUND WATER RESOURCES (as on 31.03.2004) in MCM

1. Annual Replenishable

ground water resources 897.49

2. Total Annual ground water

draft for all purposes. 465.69

3. Projected demand for

domestic and industrial uses

up to 2025

40.38

4. Stage of ground water

development 52%

1. ROAD TRANSPORT

Tirunelveli city is well-connected by roads. It is located on NH 7, 150 kilometers (93

mi) to the south of Madurai and 80 kilometers (50 mi) to the north of Kanyakumari. NH7A,

an extension of NH7, connects Tirunelveli with Tuticorin. The road infrastructure is being

expanded with an extensive 4 carriageway expansion and the NH7A stretch is almost in its

final stage.

2. RAILWAY TRANSPORT

The city is beautiful by a majestic looking structure with a high elevated faced is one

of the busiest and most important stations in Tamil Nadu. It is connected to major cities in all

four direction. Madurai to the North, Nagercoil to the south, Tenkasi to the West and

Tiruchendur to the East.

3.0 PHYSIOGRAPHY:

a) Topography and Drainage/River:

Tirunelveli district falls in Tamiraparani river basin, which is the main river of the distr

ict.The river has a large network of tributaries which includes the Peyar, Ullar, Karaiyar, Serv

alar, Pampar, Manimuthar,Varahanathi, Ramanathi, Jambunathi, Gadana nathi, Kallar, Karun

aiyar, Pachaiyar, Chittar, Gundar, Aintharuviar,Hanumanathi, Karuppanathi and Aluthakanni

ar draining the district. The river Tamiraparani originates from the hills in the west and enters

Thoothukudi District and finally confluences in Bay of Bengal.

The other two rivers draining the district are river Nambiar and Hanumanathi of Nangu

neri taluk in the south that are nothpart of the Tamiraparani river basin. The small part of the

district in the northern part falls in river Vaippar basin. Thamarabarani, Nambiar, Chittar and

Karamaniar are the important rivers draining the district. Amarabarani originating from

Papanasam flows thorough the district.The Nambiyar river originates in the eastern slopes of

the Western ghats near Nellikalmottai about 9.6 km west of Tirukkurugundi village at an

altitude of about 1060 m amsl At the foot of the hills, the river is divided into two arms. The

main arm is joined by Tamarabarani at the foothills. Chittar originatesnear Courtallam and

flows through Tenkasi and confluences with Tamarabarani. The hilly terrains have resulted in

number of falls in the district. There are three major falls in Manimuttar reservoir catchments

area and there are few falls in the Tamarabarani River also. A series of falls in Chittar River

in Courtallam comprising Five Falls, Honey Falls, Main falls and Old Courtallm Falls are

some of the important falls in the area. The drainage pattern in general is dendritic. In

addition, there are eight dams at the places as given below for irrigation and power eneration

purposes.

Papanasam, Servalar, Manimuttar, Gadana Nadhi, Ramanathi, karuppanadhi, Gundat

& Advainainar Koil.

4.0 CLIMATE AND RAINFALL DATA

1. Climate Conditions of Tirunelveli district:

The district, in general experiences tropical climate with minor changes. The normal

temperature varies between 24.4°C and 27.1°C at mean minimum, whereas the hottest climate

experiences from March to May with mercury reaching 38.5°C at the highest. The climate is

comparatively cool during the months from November to February. The average rainfall

during 2005-06 is 917.86mm and the number of rainy days varies from 98 to 110.

2. Humidity

The relative humidity, in general around the year is between 55 and 65% in most parts

of the district, except during the north-east monsoon season when it is over 65%. However,

the coastal areas will be comparatively more humid.

3. RAINFALL:

The average annual rainfall and the 5 years rainfall collected from IMD, Chennai is as

follows:

Actual Rainfall in mm Normal Rainfall in mm

2011 2012 2013 2014 2015

896.90 724.00 1348.50 1546.80 845.10

Senkottai, Sankarankoil and all along the coast and it decreases towards inland. The areas

around Ambasamudram, Tirunelveli and Kadayanallur receive minimum rainfall. The district

enjoys a Sub tropical climate. The period from May to June is generally hot and dry. The

weather is pleasant during the period from December to January. The relative humidity is on

an average between 79 and 84%. The mean minimum temperature is 22.9°C and means

maximum daily temperature is 33.5°C respectively.

1. GEOMORPHYLOGY AND SOIL TYPES

1. Geomorphology

Tirunelveli district is bordered by Western Ghats (Ridge and valley complex) in the

West. A major part of the district constitutes a plain terrain with a gentle slope toward East

and Southeast, except for the hilly terrain in the west. The general elevation of the area varies

from less than 10 to 1408 m (Tulukkaparai hill range). The prominent geomorphic units

identified in the district through interpretation of Satellite imagery are Structural Hill, Bazada

Zone, Valley Fill, Flood Plain, Pediment, Shallow buried pediment, Deep buried pediment

and Coastal Plain.

2. Soils type:

Soils in the area have been classified into

1. Deep Red soil

1. Red Sandy Soil.

2. Block Cotton Soil.

3. Saline Coastal Alluvium, and

4. River Alluvium.

Major parts of the area are covered by Deep Red soil and are found in Sivakasi,

Tenkasi, Senkottai and Sankarankoil blocks and it is suitable for cultivating coconut and

palmyrah trees. Red sandy soil also in reddish yellow in colour and are found in Nanguneri,

Ambasamudram, and Radhapuram blocks and it is suitable for cultivating groundnut, millets

and pulses etc.,

The soil condition of the district may be grouped into two main varieties namely red

loam soil and black soil. The black soil is of a higher value compared to the red loam soil and

the black soil of the Tamirabarani River Valley overlies a stiff yellow colour. The red loam

found in Tenkasi, Shenkottai, Sivagiri, and Radhapuram Taluks. The black soil is found in

Sankarankoil, Palayamkottai, and Tirunelveii Taluks. The other soils like lateritic, sandy

coastal alluvial soil and red-sand soil are not found much in the district. It is showed in Table

In the south-east coast of the soil is deep, loose and red loam surfaced by sand with its depth

varying from a few inches to 20 feet

The Block Cotton Soil is found in Tirunelveli, Palayankottai and Sankarankoil blocks,

and it is suitable for cultivating Paddy, Ragi and Cholam etc., The Saline Coastal Alluvium

are dark grey to deep brown in colour and spread over the Nanguneri and Radhapuram

blocks. The River alluvial soils occur along the river courses of Tamrabarani and Chittar river

covering in the blocks Tirunelveli and Palayankottai and it is suitable for cultivating

Groundnut, Chillies and Cumbu.

5. IRRIGATION: The nine-fold lands use classification for the district is given below. (2005-06)

The chief irrigation sources in the area are the tanks, reservoirs and followed by wells

and bore wells. The block wise and source wise net area irrigated in Ha is given below (2005-

06).

S.No Block

Net area irrigated by Total Net

Area

irrigated Canals Tanks

Tupe

/Bore

wells

Ordinary

wells

Other

sources

1. Manur 2453 2997 0 1856 0 7306

2. Palayamkottai 2314 3672 0 967 0 6953

3. Sankarankovil 0 2019 0 3276 0 5295

4. Kuruvikulam 0 943 0 3989 0 4932

5. Melaneelitha nallur 0 1264 49 2390 0 3703

6. Tenkasi 1178 2904 79 1032 2 5195

7. Kelapavoor 598 2891 0 1760 0 5249

8. Alagulam 0 775 0 3847 0 4622

9. Kadayanallur 503 3244 114 2567 0 6428

10. Senkottai 1052 1749 0 522 0 3323

11. Vasude vanallur 0 6311 0 6331 247 12889

12. Ambasamudram 2578 1253 8 329 0 4168

13. Kadayam 1700 1916 51 1517 0 5154

14. Cheranmadevi 2762 2492 25 1129 0 6408

15. Pappakudi 1486 1903 0 3204 0 6593

16. Nanguneri 16 4636 324 2668 0 7644

17. Kalakkadu 916 4161 6 2007 0 7090

18. Radhapuram 0 975 161 2685 0 3821

19. Valliyur 0 875 154 3300 0 4329

Total 17556 46980 917 45376 249 111132

6. STUDIES/ ACTIVITIES CARRIED OUT BY CGWB:

Central Ground Water Board carried out the Systematic hydrogeological surveys in

the district during the period between 1977-78, 1978–79 and 1989-90. Detailed

Geophysical investigations (Electrical Resistivity Surveys and Profiling) were carried out in

parts of Nanguneri, Sattankulam and Tiruchendur taluks in 1978. Reappraisal

hydrogeological surveys were conducted during the period of 1993 – 94. CGWB carried out

exploratory drilling in the coastal sedimentary tract of the area and six exploratory

boreholes were drilled down to the basements in depth ranging from 45 to 130m bgl.

Groundwater exploration was also taken up by CGWB in hard rock. In hard rock areas 12

bore holes were drilled down to a depth of 200m bgl.

CGWB is monitoring the groundwater regime for the changes in water level and

water quality through 32 dug wells and 24 piezometers. The monitoring of water levels are

carried out during May (Pre monsoon), August (Middle of south west monsoon),

November (post south west monsoon & initial stage of north east monsoon) & January

(Post North east monsoon) to study the impact of rainfall on groundwater regime. Water

samples are collected during May for determining the changes in chemical quality of

groundwater.

7. GROUND WATER SCENARIO:

1. Hydrogeology

The district is underlain by both porous and fissured formations. The important

aquifer systems in the district are constituted by i) Weathered and fractured hard rock

formations of Archaean age. ii) Porous sedimentary formations ranging in age from

Tertiary and Recent.

The porous formations are found as small patch in the southeastern part of the

district and include sandstones, Limestones, Laterite and Clays from Tertiary to

Quaternary. Isolated occurrence of calcareous sandstone and fossiliferous limestone are

seen in coastal area on the southeastern side. The fossiliferous limestone is found south

west of Kudankulam covering an area of 3 sq.km. Laterites are exposed as patches along

Radhapuram-Edakkadu, Vijayanarayanam-Kumarapuram, Ittamoli, Nanguneri and Uramozi

area. Beach sand occurs as a patch along the coast with a width varying from 50-250m in

Idindakarai-Ovari Belt. The river alluvium is found along the river courses and the thickness

of alluvium is restricted to 5-6m.

The exploration in sedimentary tract has revealed that the depth to basement occurs

at a depth of 120m bgl and granular zones are encountered between the depths of 20 to

92 m bgl. The yield of bore wells varies from 1-4.5 lps. The aquifer at the shallow depth is

under unconfined condition and aquifer at depth is under semi-confined to confined

condition. The shallow aquifer is developed through dug wells and deeper aquifer through

tube wells. The dug well can sustain a pumping of 4 to 6 hours while the tube wells can

sustain a pumping of 6-8 hours.

The water-bearing properties of crystalline formations, which lack primary porosity,

depend on the extent of development of secondary intergranular porosity. These aquifers

are highly heterogeneous in nature due to variation in lithology, texture and structural

features even within short distances. Ground water generally occurs under phreatic

conditions in the weathered mantle and under semi-confined conditions in the fissured

and fractured zones at deeper levels. The thickness of weathered zone in the district is in

the ranges up to 30m bgl.

The yield of large diameter wells in the district, tapping the weathered mantle of

crystalline rocks ranges from 50 to 250 lpm and are able to sustain pumping for 3 to 5

hours per day. The Specific capacity of large diameter wells tested in crystalline rocks

ranges from 25 to 300 lpm / m. of drawdown. The yield characteristics of wells vary

considerably depending on the topographic set-up, lithology and nature of weathering.

The groundwater exploration in the district down to a depth of 200m bgl has revealed

that in the western part of the district potential fractures are encountered beyond 100m

bgl while in the rest of the area, potential fractures are restricted to 100m bgl. The yield of

the wells varies from 1 to 3.6 lps. In general, the wells drilled by various State agencies

mainly for domestic purposes have yield in the range of 63 to 270 lpm. The depth to water

level in the district varied between 1.19 to 13.35 m bgl during premonsoon depth to water

level (May 2006) and varied between 0.18 to 7.97 m bgl during post monsoon depth to

water level (Jan 2007). The seasonal fluctuation shows a fall in water level, which ranges

from –0.12 to –2.14 m bgl, and rise in water level, which ranges from 0.33 to 11.24 m bgl.

The piezometric head varied between 1.72 to 13.65 m bgl (May 2006) during pre monsoon

and 0.47 to 13.25 m bgl during post monsoon.

Fig.No 2: GEOMORPHOLOGY OF THE TIRUNELVELI DISTRICT

2. Long Term Fluctuation:

The long-term water level fluctuation for the period 1998-2007 indicates both rise and

fall in different parts of the district. The rise in water level is in the range of 0.0021 to

1.1284 m/year, while the fall is the water level varies between 0.0169 and 0.6893 m/year.

3. Aquifer Parameters

Formation Yield of

wells (lps)

Transmisstivity

(m2/day)

Hydraulic

conductivity

(m/day)

Specific

Yield (%) Storability

Porous

Formation 1.0-4.5 50-250 20-65 3-6 1.98x10-4

Weathered

Rock <1-4.0 25-150 <1-15 1.5 -

Fractured

rock 1.0-3.6 25-250 <1.25 -

1.87x10-3 to

4.8x10-3

4. Ground Water Resources

The ground water resources have been computed jointly by Central Ground Water

Board and State Ground & Surface Water Resources and Development Centre (PWD, WRO

and Government of Tamil Nadu) as on 31st March 2004 and salient features of the

computations are furnished below.

5. Ground Water Quality

The chemical characteristics of ground water in the phreatic zone in Tirunelveli

District has been studied using the analytical data of ground water samples collected from

Network Hydrograph Stations of CGWB and for deeper aquifers from water samples

collected during exploration programme of CGWB.

Ground water quality of phreatic aquifers in Tirunelveli district, in general, is

colourless, odourless and slightly alkaline in nature. The specific electrical conductance of

ground water in phreatic zone (in Micro Seimens at 25oC) during May 2006 was in the range

of 510 to 9320 µS/cm. And major parts are having the electrical conductivity below

1500µS/cm. The quality of formation water in the fractured aquifer varies from place to place.

Electrical Conductivity varies form 487 (Kuruvikulam) to 3620 µS/cm(Taruvai) at 250 C and

Chloride content varies from 28 to 1049 mg/L. Electrical conductivity in major parts of the

district is less than 2000 µS/cm at 25C.

The quality of groundwater in porous formation shows variations with depth. The

exploration at Puttataruvai (near the boundary of Thoothukudi District) revealed the presence

of good quality water in the depth range of 24-32m while the saline water was noticed in the

depth range of 49-54 & 75-78m bgl. It is observed that the ground water is suitable for

drinking and domestic uses in respect of all constituents except few places are having higher

concentration of NO3 than the BIS permissible limit.

Fig.No:3 Ground Water Level of the Tirunelveli District

6. Water Conservation and Artificial Recharge:

CGWB had prepared a master plan to augment groundwater potential by

saturating the shallow aquifer taking into consideration the available unsaturated

space during post monsoon and available uncommitted surplus run off.

Subsequently, computations have been made for Drought Prone Area Programme

(DPAP) for over exploited and critical blocks in the districts warranting immediate

attention. Institute of Remote Sensing, Anna University had prepared block wise

maps demarcating potential zones for artificial recharge for the State of Tamil Nadu.

Subsequently, State Government agencies have constructed artificial recharge

structures with their own fund or with fund from Central Government, dovetailing

various government programmers.

Ministry of Water Resources, Government of India has initiated Dug Well

Recharge Scheme in the State. The scheme is being implemented by the Nodal

Department (SG &SWRDC, PWD, WRO and Government of Tamil Nadu) with the

technical guidance of CGWB. The subsidy of Rs4000/- for small and marginal

farmers and Rs2000/- for the other farmers is credited to the beneficiaries’ bank

account through NABARD. The scheme after implementation will prove to be

beneficial to the irrigation sector. The available uncommitted surplus run off has to

be recomputed, taking into consideration the quantum of recharge effected

through existing irrigation dug wells also. The existing structures and uncommitted

surplus flow should be considered for further planning of artificial recharge

programme. On the basis of experimental studies, it has been found that desilting

of existing tanks followed by percolation pond with recharge wells, recharge shafts

are economical.

There is considerable scope for implementation of roof – top rainwater

harvesting in the district. Recharge pits / Shafts / trenches of suitable design are

ideal structures for rainwater harvesting in such areas. Central Ground Water Board

is also providing free technical guidance for implementation of rooftop rainwater

harvesting schemes.

7. GROUNDWATER RELATED ISSUSE & PROBLEMS:

In view of the comparatively high level of ground water development in

Melneelithinallur, Valiyur, Sankarankoil & Radhapuram Blocks, these blocks may be

considered as vulnerable to water level depletion. Radhapuram Block being o the

coast, the high level of groundwater development may result in seawater intrusion

in

future if augmentation measures are not taken up.

8. GEOLOGY AND MINERAL RESOURCES:

In the coastal tract of Tuticorin and Tirunelveli Districts, a group of fine grained

limestone and gritty sandstone intercalated with pebble beds are found to overlie

the Archaean unconformably and below the recent formations. These are referred

to as Panamparai Sandstone and their fossil assemblage indicates Mio-Pliocene

age. The entire assemblage of Panamparai points to a mixture of continental and

marine derivation. Along the west coast of Kanyakumari District, a sequence of

sandstone and clay with thin lignite seams is recorded. These are correlated to

Warkhali beds of Mio-Pliocene age of south Kerala and are similar to Cuddalore

Formation.

Kankar and tuffaceous limestone occur in the southern part of Tuticorin District and

southeastern part of Coimbatore District. Kankar occurs as conspicuous high grounds along

the margin of black cotton soil. Beds of open textured loosely indurated, coarse calcareous

gritty sandstone and shell limestone are found in the coastal tracts of Tuticorin District. These

are mostly covered by red "Teri" sands. Similar calcareous gritty sandstone (Czc) is recorded

near Soyamali in Tirunelveli District beneath the kankar. It carries vertebrate fossils of

probable Pleistocene age.

The red sand or 'teri' as known locally occupies a great part of the coastal districts of

Ramanathapuram, Tuticorin and Tirunelveli. The 'teri' lies some distance away from the shore

and forms large barren wasteland of high mounds and ridges composed of piles of red dunes

with intervening depressions. The formation is made up mainly of red stained quartz with an

admixture of fine red clayey dust and fine grains of iron ore. The thickness of teri sand

increases from the coast the interior from about 1.5m to maximum 7.0 m. The sands are

composed of quartz, fragments of feldspar, magnetite and rare garnet. The alluvial soils vary

in colour and texture from light brown to dirty white and are composed of sand grains, clay

and silt. They are more sandy along River and stream courses but silty and clayey in the flood

plains.

Geological Formation Rock Type

Recent age - Topsoil- (2m Thick) Sandy clay, Alluvium soil

Tertiary age - Sandstone, Limestone

Archaean age - Gneiss, Granite,

Archaean complex - Granite, Pegmatite, Charnockite,

9. AREA NOTIFIED BY CGWA/SGWA:

Central Ground Water Authority has not notified any area in the district.

Government of Tamil Nadu vide G.O.No. 53 has restricted groundwater

development for irrigation in the over exploited blocks of Tamil Nadu. In Tirunelveli

district the over exploited blocks are as follows.

1. Melaneelitha nallur

2. Radhapuram

3.Sankarankovil

4. Valliyur

10. LAND USE/LAND COVER MAPPING USING SATELLITE DATA:

Tirunelveli district, about 79,668 (11.7%) hectares are wet lands well suited for

the cultivation of paddy and other crops which need adequate water supply, while

others are not useful for agricultural purposes. Nearly 3,58,151 (52.5%) hectares is

dry land with no irrigation facilities for agriculture, although soil condition is

moderate for growing crops, so that it mat be used to grow drought resistant plants

which offer firewood. A block of waste lands which about 39,274 (5.7%) hectares is

proclaimed to be not useful for growing crops, because of lack of enough water,

poor soil, and undesired topographic conditions. Approximately 57,676 (8.5%)

hectares is unassessed wasteland where soil condition is fair while water supply

scarcity prevails for several months, so that it is used for agriculture only when

rainfall is high. Yet, another 1, 22,055 (17.8%) hectares is occupied by forests which

are declared to be reserves as forest resources for lion- tailed monkeys, rich in

deciduous and evergreen plants. Poromboke - common lands, covers about 25,456

(3.8%) hectares, which may be used to create social forests although water is

scarce.

The output images of land use land cover and their analysis is presented. The land

use land cover images generated for the years 2005 and 2015 along with the future

predicted land use land cover image of the year 2025 are presented in the following

figure 4. Table 1 shows the statistical change analysis of the land use land cover

between the years 2005, 2015 and 2025. An overall change in the land use land

cover in all the three years is shown in figure 4. From the change analysis of the land

use land cover between 2005 and 2015 it is observed that there is an increase in

settlement, barren land and shrub land and a decrease in water body and

agriculture. The decreased land use land cover is mostly utilized for the settlement

based upon the increase in population density. A significant change has been

occurred between the years 2015 and 2025. It is observed that there is a greater

increase in the area of settlement. The barren land, shrub lands and the agricultural

areas are converted into settlement regions due to the increase in population

density and the soil conditions. Tirunelveli and palaymkottai taluk regions would

experience rapid urbanization as predicted in the final output land use land cover

image. This prediction would be an effective tool for urban planning and

environmental management plans.

Fig.No: 4 Land use land cover obtained for the different years

Fig. No: 5. Land use land cover (LULC) changes in different years

1. Forest

The total area of the forest in the district is 1, 22,055 hectares, of which 81,700

hectares are set apart as reserve of Kalakkadu-Mundanthurai. The entire forest of the district

stretches in the Western Ghats. As far as forest resources are concerned, about 600 species of

timber trees are grown in this district. The important of them are teak wood, rose wood, wild

jack, manjakadamba, ven teak, vengai, pillai maruthu, and karumaruthu. Cane and bamboo

are also grown in plenty. A number of industries utilising the above said woods have

developed in and around of Shenkottai and Tenkasi Taluks. The district has many lofty

mountains, low plains, rivers and sea-coasts which together provide unique geographical and

physical conditions suitable for the growth of tropical evergreen forests to thorny shrubs. The

forests in the district are technically classified as southern hill top, tropical evergreen forests,

west coast evergreen forests, southern moist mixed deciduous forests, ochlandra reed forests,

umbrella thorn forests, southern euphoria scurbs and southern thorn scurbs.

2. Agriculture

Factors like soil nature, climatic conditions, and irrigation facilities availed, and the

like determines the cropping pattern in the district. Tirunelveli district is predominantly an

agricultural district. The district has mainly two seasons namely Kar (the first crop season -

from June to September during south-west monsoon), and Pishanam (the second crop - from

November to February during north-east monsoon). However, most of the rain-fed areas in

the district are cultivated in both the seasons.

The district has fertile soils in scattered regions. Less fertile red loam soil is distributed

over most of the region. The network of the irrigation system makes full use of the water

resources. In the district there are number of crops having been cultivated. However, cropping

pattern of the district varies from Taluk to Taluk. Wet cultivation is, essentially paddy

cultivation obtains a major share of the gross cropped area. Under dry regions, diversified

crop patterns exist and no single crop claims a large share of the gross cropped area.

Cultivation which characterises these regions is also basically milled and cash crop

cultivations. Even in dry regions, wherever water is available, it is the paddy crop that sown

by the farmers. Paddy occupies however, the largest area of cultivation, followed by cotton.

Paddy is cultivated mainly in Tirunelveli, Palayamkottai, Tenkasi, Shenkottai,

Ambasamudram, and Nanguneri Taluks, through which the perennial river Tamirabarani

flows. Other crops grown in the district are Cumbu, Ragi, Pulses, Groundnut, Gingelly,

Banana, Chilli, Sugarcane, and Indigo. Most of the crops are on the ground for three or four

months, except chilli and cotton which take more than 5 months. Portions of Sankaran Kovil

Taluk have the rich, fertile black soil which is highly suitable for cotton cultivation.

3. Irrigation

Irrigation is the artificial application of water to soil for the purpose of crop cultivation.

As the timing and amount of rainfall are not adequate to meet the moisture requirement of

cultivation, irrigation is essential to raise crops and meet the need for food and fiber. In areas

where the rainfall is plentiful and well distributed over the year there will be year round

production. Indeed, rainfall in certain areas will be very scanty as well as uncertain. This is so

in Tirunelveli district.

The irrigation system in Tirunelveli district consists of rivers like Tamirabarani,

Manimuttaru, Pachaiyaru, Nambiyaru, and Chittaru which originating from Western Ghats

and running across the gentle slopes of the mid lands and confluence in Bay of Bengal. The

River Tamirabarani is the main source of irrigation which also provides drinking water

facilities to a number of places in the district, as well. Pabanasam, Manimuttar and Chervalar

are the major reservoirs in the district. Gadana Nathi, Ramanathi, Karuppanathi, Gundaru,

Adavi Nainar Koil, Vadakku Pachaiyaru, Kodumudiyaru, and Nambiyaru are the minor

reservoirs in the district. Besides these rivers and reservoirs the other different sources of

irrigation prevailing in the district are canal, tank and well. Of the total cropped 1, 61,976

hectares 38,080 hectares (23.5%) utilises such types of sources. The source-wise irrigation

distribution in Tirunelveli district during 2005-2006 is given in the Table.

4. Land Use Pattern

Of the total of 6, 82,300 hectares area in Tirunelveli district, about 79,668 (11.7%)

hectares are wet lands well suited for the cultivation of paddy and other crops which need

adequate water supply, while others are not useful for agricultural purposes. Nearly 3,58,151

(52.5%) hectares is dry land with no irrigation facilities for agriculture, although soil

condition is moderate for growing crops, so that it mat be used to grow drought resistant

plants which offer firewood. A block of waste lands which about 39,274 (5.7%) hectares is

proclaimed to be not useful for growing crops, because of lack of enough water, poor soil,

and undesired topographic conditions. Approximately 57,676 (8.5%) hectares is unassessed

wasteland where soil condition is fair while water supply scarcity prevails for several months,

so that it is used for agriculture only when rainfall is high. Yet, another 1, 22,055 (17.8%)

hectares is occupied by forests which are declared to be reserves as forest resources for

liontailed monkeys, rich in deciduous and evergreen plants. Poromboke - common lands,

covers about 25,456 (3.8%) hectares, which may be used to create social forests although

water is scarce.

8.0 RECOMMENDATION:

As the development of ground water has still in safe stage in many blocks of

this district, further development of ground water for creation of additional

irrigation potential has to be carried out with extreme caution.

Necessary measures for regulating the exploitation of ground water may be

implemented in the Over Exploited blocks of the district. Intensive monitoring of

ground water levels and water quality has to be taken up in the coastal areas of the

district to monitor the movement of fresh water – saline waterinterface.

Waste land development programme and micro irrigation system has to be

implemented for increasing the agricultural produces by way of more food and

income per drop of water in view of the limited water resources in the districts.

9.0 CONCLUSON:

In this work urban expansion of the rapidly growing regions Tirunelveli taluk

has been studied over the past 10 years (2005-2025) to predict the future urban

expansion in the year 2025. Satellite images from Land sat for the years 2005 and

2015 are used for this study. The total area of the study area is 6823 square

kilometers. Land use Land cover image are developed in ERDAS imagine and the

future land use land cover image was predicted using the CLUE-S due model. The

output result predict that there is a great increase in the growth of settlement due

to the conversion of barren land, shrub land and agriculture land areas in the year

2025. An accuracy of more than 80% was obtained in all stages. This rapid and

massive conversion of the agricultural and shrub land into settlement would lead to

serious environmental impacts unless proper environmental management plans

were implemented for the rapid urban area.