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M. Velayudha DasInt. Journal of Engineering Research and Applications www.ijera.com 
ISSN : 2248-9622, Vol. 4, Issue 9( Version 6), September 2014, pp.167-173 
www.ijera.com 167|P a g e 
Spatial Analysis of Soil and Water Quality in Tsunami AffectedAreas of Nagapattinam District, Tamilnadu, India M. Velayudha Das1and Dr. S.Poongothai2 1. Assistant Professor2. Professor Department of Civil Engineering, Annamalai University,Annamalainagar– 608 002,Tamilnadu, India. ABSTRACT In India, the natural disasters, especially the Tsunami in 2004 having exposed our unpreparedness, variability, diverse scientific, engineering, financial and also social processes. Vedaranyamtalukof Nagapattinam coastal region of Tamilnadu, India,was severely affected by Tsunami-2004. Due to its unique geological nature and climate conditions, the quality of soil and water resources was subjected to natural and synthetic changes. The recent efforts of prawn culture and saltpan in these areas also affect the natural resources. This study has revealed the present scenario of soil and water resources by analyzing their chemical parameters in the Tsunami affected areas after ten years of Tsunami-2004. For this study, soil samples (less than 30cm depth from land surface) and groundwater samples (from existing hand/bore pumps) were collected in the study area. It was observed from the analysis that the pH of soil was improved well and EC was lowered significantly except few places. Regarding the available N, P, K of soil, N was low, P and Kwere low to medium range. Further thepH,DO, Turbidity, Hardness,Cl and Mgof groundwater were within the permissible limit;EC and TDS were slight to moderate range for irrigation and drinking.The SAR is within the maximum allowable limit which inferred that groundwater can be used for irrigation without any risk.Thisspatial-temporal variability of soil and water parameters were mapped in GIS environment (Surfer ver. 9) and compared with pretsunami-2004 as well as ground truth scenario. Keeping these results, the soil is suitable for agriculture production. The natural flash flood has helped to reduce contamination of soil and water due to Tsunami-2004. However,due to alkaline in nature the quality of groundwater is not fit for drinking in some places but suitable for irrigation. Among the affected villages, Vedaranyam village has worst quality. This study also recommends suitable management strategies for sustainable development. Keywords: Tsunami, water and soil parameters, spatial analysis, Surfer ver. 9 
I. INTRODUCTION 
Natural resources are the sources that are useful and essential to human being and all other living things. Soil and water are very vital for the advancement of civilization for a sustainable development. Groundwater is not static and its quality varies daily and seasonally.Tsunami is a harbour wave or tidal waves which affectdistant shores, originate from undersea or coastal seismic activity, landslides, and volcanic eruptions. Whatever the cause, seawater is displaced with a violent motion and swells up, ultimately surging over land with great destructive power. Due to an undersea earthquake (9.4 Richter scale) at the Indian ocean on December 26,2004 led to massive inflows of seawater (Tsunami-2004) which caused loss of life, injuries and devastatingdamage to natural sources, especially agricultural land's products, livelihoods and disrupt the governmental system of our country. Nagapattinamregion was one of the worst affected coastal belts ofTamilnadu state. 
Indian Agricultural Research Institute, New Delhi (2005) made spot investigation in some of the Tsunami affected areas of Nagapattinam and reported that due to poor drainage and sea water stood for a few days, the quality of soil and water was severely affected. The EC of soil and shallow ground water increased by about ten times and fifteen times respectively, and the degree of variations differed from place to place. Higher concentration of Calcium, Magnesium, Sodium, Chlorides, Sulphatesand Bicarbonate indicated that the soil turned saline. The EC varied from 3.9 to 46 ds/m compared with 0.5 ds/m for non-contaminated water, the pH was more than 8.5. The essential prerequisite for quality of water is to be safe for use to people and crops but should not damage it. The spatial analysis of water resources is essential to identify the areas most vulnerable to contamination for better decision– making. (Poongothai et al. 2008).The qualities of both surface and shallow ground water sources were observed to be unfit for irrigation and domestic purposes (Chandrasekaran et al. 2008).The groundwater increases its major ion concentration in 
RESEARCH ARTICLE OPEN ACCESS
M. Velayudha DasInt. Journal of Engineering Research and Applications www.ijera.com 
ISSN : 2248-9622, Vol. 4, Issue 9( Version 6), September 2014, pp.167-173 
www.ijera.com 168|P a g e 
the summer season in comparison to the post and premonsoon period, because of evaporation, precipitation and environment weathering (Ramkumaret al. 2010). Remediation of groundwater needs knowledge of the existing nature, magnitude, and sources of the various pollutions to assessing groundwater quality (Shankar et al. 2011). Rainfall is the most important cyclic phenomenon in tropical countries as it brings important changes in the hydrographic characteristics of the marine and estuarine environments (Ramalingam et al. 2012). 
The aim of this investigation is to analyse the present scenario of soil and water qualityandcreate spatial-temporal variability maps in the Tsunami- 2004 affected Vedaranyamtaluk of Nagapattinam district, Tamilnadu through the development of GIS software (Surfer ver.9). Also, suggestion ofsuitable management strategy is effort for sustainable development. 
II. STUDY AREA 
The study was conducted in Vedaranyamtaluk of Nagapattinam district, which situated in the east coast line of Tamilnadu state, India. Its location is at 79037’30”- 79051’30” E and 10016’00”- 10039’00”N. The geographical area of Vedaranyamtalukis 533.03 sq. km and the average annual rainfall was 1100mm. Geomorphologically, the study area consists of flood plains, delta plain and natural levees. The formation isa sedimentary terrain (Alluvium, Sandyclay and Beachsand).The hydrological soil types are Group A (30%), Group C (65%) and Group D (5 %,) andthe slope is -1%. The important crops are paddy and groundnut. The main sources of irrigation are bore well (81%), cannel (21%) and rain-fed tanks (31%). 
Fig. 1 Location map of study area with sample locations 
III. MATERIALS AND METHODS 
To analyse the spatial variability of soil and water sources, the primary data on 15 water samples (compressing surfacewater and bore water) and 10 surface soil samples (upto 20cm depth) were collected from affected and unaffected areas on December 2013 for measurement of specific chemical parameters of soil viz: pH, EC, N, P and K and of water viz: pH, EC, TDS, Turbidity, Salinity, DO, Hardness, Na, Cl, Ca, Mg and SAR were analysed at the Environmental laboratory, Annamalai University. The location of the sample acquisition 
points was recorded by using hand held Geo Positioning System (GPS). The results of soil and water quality parameters were inferred in the Excel spreadsheet for comparison with pretsunami-2004scenario (secondary data on soil and water quality 2000 -2012 collected from Government organization, Nagapattinam) and with crop tolerable limits by FAO for irrigation and BIS for domestic purposes.Various maps using GIS package (Surfer ver.9)were prepared to spatially locate the polluted area. (Fig.4&5) 
IV. RESULT AND DISCUSSION 
The findings are summarized in Table 1&2. Sample wise parameter variations are presented in Fig.2&3.
M. Velayudha DasInt. Journal of Engineering Research and Applications www.ijera.com 
ISSN : 2248-9622, Vol. 4, Issue 9( Version 6), September 2014, pp.167-173 
www.ijera.com 169|P a g e 
Table 1 Chemical Analysis of Soil samples on December 2013 
Sl.No. 
Sampling places 
pH 
EC ds/m 
Nitrogen (N)Kg/ha 
Phosphorus (P)Kg/ha 
Potassium (K)Kg/ha 
1. 
Pudupalli 
7.19 
0.493 
178 
22 
272 
2. 
Vettaikkaraniruppu 
6.82 
0.327 
112 
11 
119 
3. 
Kovilpattu 
7.44 
1.17 
159 
17 
214 
4. 
Naluvedapathi 
7.62 
0.631 
152 
21 
261 
5. 
Pushpavanam 
7.21 
0.520 
143 
19 
210 
6. 
Kollitheevu 
7.01 
0.432 
137 
24 
195 
7. 
Vedaranyam 
8.60 
1.250 
180 
28 
172 
8. 
Talainayar * 
7.25 
0.550 
380 
24 
240 
9. 
Marddur * 
7.30 
0.560 
420 
20 
230 
10. 
Tennadar * 
7.40 
0.350 
450 
22 
210 
FAO Permissible limit 
6.5 - 7.5 
< 2 
250 - 500 
20 - 50 
125 - 300 
*Unaffected area Table 2 Chemical Analysis of Water samples on December 2013 
SI. No. 
Sampling Places 
pH 
EC ds/m 
TDS mg/L 
TurbidityNTU 
DO mg/L 
Hardness mg/L 
Na mg/L 
Cl mg/L 
Salinity% 
Ca mg/L 
Mg mg/L 
SAR 
1. 
Pudupalli 
8.45 
3.495 
450 
1 
3.8 
210 
180 
186 
2 
28 
30 
5.63 
2. 
Vettaikkaraniruppu 
8.50 
2.725 
220 
3 
3.5 
175 
170 
165 
3 
30 
21 
5.82 
3. 
Kovilpattu 
8.60 
3.600 
1775 
2 
3.2 
140 
235 
1150 
3 
24 
17 
8.92 
4. 
Naluvedapathi 
8.25 
2.244 
760 
2 
3.6 
240 
160 
142 
2 
36 
29 
4.81 
5. 
Pushpavanam 
7.90 
1.094 
420 
3 
3.2 
210 
70 
410 
1 
24 
34 
2.16 
6. 
Kollitheevu 
8.20 
2.854 
190 
2 
3.5 
230 
110 
380 
1 
36 
29 
3.31 
7. 
Vedaranyam 
9.02 
13.500 
1387 
5 
2.4 
260 
870 
1210 
6 
38 
34 
24.71 
8. 
Talainayar* 
7.78 
0.927 
210 
1 
3.0 
105 
80 
20 
0 
12 
21 
3.22 
9. 
Marddur * 
7.60 
0.510 
165 
1 
3.4 
90 
65 
18 
0 
20 
16 
2.63 
10. 
Tennadar * 
7.98 
0.719 
180 
1 
2.8 
95 
70 
20 
0 
20 
17 
2.78 
BIS Permissible limit 
6.5 - 8.5 
< 3 
2000 
10 
6 
600 
200 
1000 
Nil 
200 
100 
< 26 
*Unaffected area 
Fig.2 Variability of pH and EC in soil samples 
0 
10 
20 
Soil pH 
2004 (Pre tsunami) 
2005 
2006 
2013 
0 
5 
10 
15 
20 
25 
Soil EC 
ds/m 
2004 (Pre tsunami) 
2005 
2006 
2013
M. Velayudha DasInt. Journal of Engineering Research and Applications www.ijera.com 
ISSN : 2248-9622, Vol. 4, Issue 9( Version 6), September 2014, pp.167-173 
www.ijera.com 170|P a g e 
Fig. 3 Variability of pH and EC in water samples 
0 
10 
20 
Water pH 
2004(Pre tsunami) 
2005 
2006 
2013 
0 
5 
10 
15 
20 
25 
30 
35 
Water EC 
ds/m 
2004(Pre tsanami) 
2005 
2006 
2013
M. Velayudha DasInt. Journal of Engineering Research and Applications www.ijera.com 
ISSN : 2248-9622, Vol. 4, Issue 9( Version 6), September 2014, pp.167-173 
www.ijera.com 171|P a g e 
Fig. 4Spatial variability of pH and EC in soil samples
M. Velayudha DasInt. Journal of Engineering Research and Applications www.ijera.com 
ISSN : 2248-9622, Vol. 4, Issue 9( Version 6), September 2014, pp.167-173 
www.ijera.com 172|P a g e 
Fig. 5Spatial variability of pH and EC in water samples 
4.1 Soil Quality With reference to pH values, there is a good improvement and within normal range of 6.5 to 7.5 except Naluvedapathi and Vedaranyam villages. The soil of these villages is clayey intexture whereas other affected villages are of sandy soil. There was a significant decrease of soil EC in comparison to values immediately after Tsunami-2004.This is due to the rainfall flushing of the surface salts that resulted in lowering of the EC of the surface soil. The soil samples where low in available N could be due to low amount of organic carbon in the soils, and most of the samples were low to medium in available P and K, which needs regular monitoring of fertility status.Depending on soil type, the gypsum of appropriate quantities can be applied before taking up agricultural activities. 4.2 Water Quality 
The pH is well within the norms in all the samples except Kovilpattu and Vedaranyam villages indicating study area water falls in alkaline nature. The EC influences crop and drinking purposes.The EC values for drinking purposes show poor category of >3 ds/m in Pudupalli, Kovilpattu and Vedaranyamvillages. In this study, the TDSvalues varied between 410 to7490 mg/L and are within the maximum permissible limit for drinking as per the BIS in all samples except Pudupalli, Kovilpattu and Vadaranyam villages.The highest concentration of TDS is likely due to mixing of groundwater with seawater. Turbidity is the cloudiness or haziness of water. No samples in the study area contain turbidity. DO, a vital parameter to know the status of the aquatic ecosystem, is within the norms (<6 mg/L) in all sample locations. Water hardness is determined by the concentration of multivalent cations in the water. Vedaranyamvillage has a higher concentration of hardness (840mg/L) which may cause health hazards.The high level of sodium inhibits soil permeability and gives a salty taste.Maximum concentration of Nahas been observed inthe Kovilpattu village (235mg/L) and Vedaranyam village (870 mg/L) due to seawater influence and study area near to saltpan deposits.Kovilpattu and Vedaranyamvillagesamplesrepresent maximum Cl concentration of 1150 and 1210 mg/L, which is more than BISfor drinking water, andbecome unsuitable for drinking purpose.Salinity is the saltiness content of water or soil. The salinity levels in the study area are varying between 0 to 6%.SAR is a measure of alkali/sodium hazard to crops. The SAR values ranged from 2.16 to 24.71are within the maximum allowable limit shows that groundwater can be used for irrigation without any risk. From the secondary sources and comparative study of pre and post Tsunami data, it was reported that the groundwater was fit for irrigation and drinking purposes before Tsunami-2004, but after Tsunami-2004 the quality of groundwater got deteriorated and needs conservation practices. 
V. CONCLUSION 
The study reveals that the surface soil samples qualities of Tsunami-2004 affected agricultural areas in Vedaranyamtaluk indicated faster improvement and are moderately suitable for agriculture production. But the qualities of groundwater were observed to beinhibited for irrigation and drinking purposes.Also, due to non-availability of good quality water in the study area, people are compelled to use water from bore/hand pumps. Groundwater in the study area is generally alkaline in nature, especiallyVedaranyamvillage which was worst affected.From questionnaire survey results show 43% respondents report a decreasing trend in the yield due to salinity land and low fertility. Moreover, to reclaim, both short-term and long-term strategyefforts should be made, such as adoption of improved crop varieties, water management practices, construction of drainage, drip and sprinkler irrigation system, renovation of defaulttanks and ponds and desilting of drainage channels and cannels. Micro level field data and mapping are required for sustainable development of natural resources of the study area.
M. Velayudha DasInt. Journal of Engineering Research and Applications www.ijera.com 
ISSN : 2248-9622, Vol. 4, Issue 9( Version 6), September 2014, pp.167-173 
www.ijera.com 173|P a g e 
REFERENCES 
[1.] Ayers R.S. (1985),“Water Quality Management for Agriculture”, FAO Irrigation and drainage paper. 
[2.] BIS (1983), “Standards for water for drinking and other purposes”, Bureau of Indian Standards Publication, New Delhi. 
[3.] Burroughs P.A. (1989) “Principle of Geological Information System for land Resources Assessment”, Clarendon Press, Oxford. 
[4.] ChandrasekaranH. and StalinM. (2008),“Variability of soil-water quality due to Tsunami-2004 in the coastal belt of Nagapattinam district,Tamilnadu”,Journal of Environmental Management,Vol.89(1), pp.63-72. 
[5.] Indian Agricultural Research Institute (IARI),(2005), “Effort of Tsunami on coastal crop husbandry in part of Nagapattinam district, Tamil Nadu”, Current science, Vol. 89. No.1, pp. 30-32. 
[6.] Norbert F. (2006), “Strategies to reduce the impact of salt on crop production: A case of the Tsunami-affected area of India”, Science Direct, Desalination 206, pp. 524-530. 
[7.] Palinivelu K. and NishraPriya M. (2006), “Water quality assessment in the Tsunami- affected coastal areas of Chennai”, Current Science, Vol. 91, No. 5, pp. 219-230. 
[8.] Poongothai S. and Ravisankar R. (2008),“A study on groundwater quality in Tsunami affected areas of Sirkazhi taluk, Nagapattinam district, Tamilnadu, India”, International Journal of Science of Tsunami Hazards,Vol.27(1),pp.48-55. 
[9.] Ramalingam M. and Subramanian A. (2012), “Seasonal variation of physical-chemical properties of Great Vedaranyam swamp, south-east coast of India”, African Journal of Environmental Science and Technology, Vol. 5(9), pp. 673-681. 
[10.] Ramkumar T. and Venkatramanan S. (2010), “Hydrogeochemical quality of groundwater in Vedaranyam Town, Tamilnadu, India”, Research Journal of Environmental and Earth Science, Vol. 2 (1), pp. 44-48. 
[11.] Rangalakshmi R. and Senthilkumar R. (2007), “Reclamation and status of Tsunami damaged soil in Nagapattinam district, Tamilnadu”, Current Science, Vol. 92, No. 9, pp. 1221-1223. 
[12.] Sankar K. and Aravindan S. (2011), “Spatial distribution of groundwater quality in Paravanar River Sub-basin, Cuddalore District, Tamilnadu”, International Journal of Geomatics and Geoscience, Vol. 1 (4), pp. 914-931. 
[13.] TRINet (2006), “Agriculturepost-Tsunami” TRINet Newsletter.

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Spatial Analysis of Soil and Water Quality in Tsunami AffectedAreas of Nagapattinam District, Tamilnadu, India

  • 1. M. Velayudha DasInt. Journal of Engineering Research and Applications www.ijera.com ISSN : 2248-9622, Vol. 4, Issue 9( Version 6), September 2014, pp.167-173 www.ijera.com 167|P a g e Spatial Analysis of Soil and Water Quality in Tsunami AffectedAreas of Nagapattinam District, Tamilnadu, India M. Velayudha Das1and Dr. S.Poongothai2 1. Assistant Professor2. Professor Department of Civil Engineering, Annamalai University,Annamalainagar– 608 002,Tamilnadu, India. ABSTRACT In India, the natural disasters, especially the Tsunami in 2004 having exposed our unpreparedness, variability, diverse scientific, engineering, financial and also social processes. Vedaranyamtalukof Nagapattinam coastal region of Tamilnadu, India,was severely affected by Tsunami-2004. Due to its unique geological nature and climate conditions, the quality of soil and water resources was subjected to natural and synthetic changes. The recent efforts of prawn culture and saltpan in these areas also affect the natural resources. This study has revealed the present scenario of soil and water resources by analyzing their chemical parameters in the Tsunami affected areas after ten years of Tsunami-2004. For this study, soil samples (less than 30cm depth from land surface) and groundwater samples (from existing hand/bore pumps) were collected in the study area. It was observed from the analysis that the pH of soil was improved well and EC was lowered significantly except few places. Regarding the available N, P, K of soil, N was low, P and Kwere low to medium range. Further thepH,DO, Turbidity, Hardness,Cl and Mgof groundwater were within the permissible limit;EC and TDS were slight to moderate range for irrigation and drinking.The SAR is within the maximum allowable limit which inferred that groundwater can be used for irrigation without any risk.Thisspatial-temporal variability of soil and water parameters were mapped in GIS environment (Surfer ver. 9) and compared with pretsunami-2004 as well as ground truth scenario. Keeping these results, the soil is suitable for agriculture production. The natural flash flood has helped to reduce contamination of soil and water due to Tsunami-2004. However,due to alkaline in nature the quality of groundwater is not fit for drinking in some places but suitable for irrigation. Among the affected villages, Vedaranyam village has worst quality. This study also recommends suitable management strategies for sustainable development. Keywords: Tsunami, water and soil parameters, spatial analysis, Surfer ver. 9 I. INTRODUCTION Natural resources are the sources that are useful and essential to human being and all other living things. Soil and water are very vital for the advancement of civilization for a sustainable development. Groundwater is not static and its quality varies daily and seasonally.Tsunami is a harbour wave or tidal waves which affectdistant shores, originate from undersea or coastal seismic activity, landslides, and volcanic eruptions. Whatever the cause, seawater is displaced with a violent motion and swells up, ultimately surging over land with great destructive power. Due to an undersea earthquake (9.4 Richter scale) at the Indian ocean on December 26,2004 led to massive inflows of seawater (Tsunami-2004) which caused loss of life, injuries and devastatingdamage to natural sources, especially agricultural land's products, livelihoods and disrupt the governmental system of our country. Nagapattinamregion was one of the worst affected coastal belts ofTamilnadu state. Indian Agricultural Research Institute, New Delhi (2005) made spot investigation in some of the Tsunami affected areas of Nagapattinam and reported that due to poor drainage and sea water stood for a few days, the quality of soil and water was severely affected. The EC of soil and shallow ground water increased by about ten times and fifteen times respectively, and the degree of variations differed from place to place. Higher concentration of Calcium, Magnesium, Sodium, Chlorides, Sulphatesand Bicarbonate indicated that the soil turned saline. The EC varied from 3.9 to 46 ds/m compared with 0.5 ds/m for non-contaminated water, the pH was more than 8.5. The essential prerequisite for quality of water is to be safe for use to people and crops but should not damage it. The spatial analysis of water resources is essential to identify the areas most vulnerable to contamination for better decision– making. (Poongothai et al. 2008).The qualities of both surface and shallow ground water sources were observed to be unfit for irrigation and domestic purposes (Chandrasekaran et al. 2008).The groundwater increases its major ion concentration in RESEARCH ARTICLE OPEN ACCESS
  • 2. M. Velayudha DasInt. Journal of Engineering Research and Applications www.ijera.com ISSN : 2248-9622, Vol. 4, Issue 9( Version 6), September 2014, pp.167-173 www.ijera.com 168|P a g e the summer season in comparison to the post and premonsoon period, because of evaporation, precipitation and environment weathering (Ramkumaret al. 2010). Remediation of groundwater needs knowledge of the existing nature, magnitude, and sources of the various pollutions to assessing groundwater quality (Shankar et al. 2011). Rainfall is the most important cyclic phenomenon in tropical countries as it brings important changes in the hydrographic characteristics of the marine and estuarine environments (Ramalingam et al. 2012). The aim of this investigation is to analyse the present scenario of soil and water qualityandcreate spatial-temporal variability maps in the Tsunami- 2004 affected Vedaranyamtaluk of Nagapattinam district, Tamilnadu through the development of GIS software (Surfer ver.9). Also, suggestion ofsuitable management strategy is effort for sustainable development. II. STUDY AREA The study was conducted in Vedaranyamtaluk of Nagapattinam district, which situated in the east coast line of Tamilnadu state, India. Its location is at 79037’30”- 79051’30” E and 10016’00”- 10039’00”N. The geographical area of Vedaranyamtalukis 533.03 sq. km and the average annual rainfall was 1100mm. Geomorphologically, the study area consists of flood plains, delta plain and natural levees. The formation isa sedimentary terrain (Alluvium, Sandyclay and Beachsand).The hydrological soil types are Group A (30%), Group C (65%) and Group D (5 %,) andthe slope is -1%. The important crops are paddy and groundnut. The main sources of irrigation are bore well (81%), cannel (21%) and rain-fed tanks (31%). Fig. 1 Location map of study area with sample locations III. MATERIALS AND METHODS To analyse the spatial variability of soil and water sources, the primary data on 15 water samples (compressing surfacewater and bore water) and 10 surface soil samples (upto 20cm depth) were collected from affected and unaffected areas on December 2013 for measurement of specific chemical parameters of soil viz: pH, EC, N, P and K and of water viz: pH, EC, TDS, Turbidity, Salinity, DO, Hardness, Na, Cl, Ca, Mg and SAR were analysed at the Environmental laboratory, Annamalai University. The location of the sample acquisition points was recorded by using hand held Geo Positioning System (GPS). The results of soil and water quality parameters were inferred in the Excel spreadsheet for comparison with pretsunami-2004scenario (secondary data on soil and water quality 2000 -2012 collected from Government organization, Nagapattinam) and with crop tolerable limits by FAO for irrigation and BIS for domestic purposes.Various maps using GIS package (Surfer ver.9)were prepared to spatially locate the polluted area. (Fig.4&5) IV. RESULT AND DISCUSSION The findings are summarized in Table 1&2. Sample wise parameter variations are presented in Fig.2&3.
  • 3. M. Velayudha DasInt. Journal of Engineering Research and Applications www.ijera.com ISSN : 2248-9622, Vol. 4, Issue 9( Version 6), September 2014, pp.167-173 www.ijera.com 169|P a g e Table 1 Chemical Analysis of Soil samples on December 2013 Sl.No. Sampling places pH EC ds/m Nitrogen (N)Kg/ha Phosphorus (P)Kg/ha Potassium (K)Kg/ha 1. Pudupalli 7.19 0.493 178 22 272 2. Vettaikkaraniruppu 6.82 0.327 112 11 119 3. Kovilpattu 7.44 1.17 159 17 214 4. Naluvedapathi 7.62 0.631 152 21 261 5. Pushpavanam 7.21 0.520 143 19 210 6. Kollitheevu 7.01 0.432 137 24 195 7. Vedaranyam 8.60 1.250 180 28 172 8. Talainayar * 7.25 0.550 380 24 240 9. Marddur * 7.30 0.560 420 20 230 10. Tennadar * 7.40 0.350 450 22 210 FAO Permissible limit 6.5 - 7.5 < 2 250 - 500 20 - 50 125 - 300 *Unaffected area Table 2 Chemical Analysis of Water samples on December 2013 SI. No. Sampling Places pH EC ds/m TDS mg/L TurbidityNTU DO mg/L Hardness mg/L Na mg/L Cl mg/L Salinity% Ca mg/L Mg mg/L SAR 1. Pudupalli 8.45 3.495 450 1 3.8 210 180 186 2 28 30 5.63 2. Vettaikkaraniruppu 8.50 2.725 220 3 3.5 175 170 165 3 30 21 5.82 3. Kovilpattu 8.60 3.600 1775 2 3.2 140 235 1150 3 24 17 8.92 4. Naluvedapathi 8.25 2.244 760 2 3.6 240 160 142 2 36 29 4.81 5. Pushpavanam 7.90 1.094 420 3 3.2 210 70 410 1 24 34 2.16 6. Kollitheevu 8.20 2.854 190 2 3.5 230 110 380 1 36 29 3.31 7. Vedaranyam 9.02 13.500 1387 5 2.4 260 870 1210 6 38 34 24.71 8. Talainayar* 7.78 0.927 210 1 3.0 105 80 20 0 12 21 3.22 9. Marddur * 7.60 0.510 165 1 3.4 90 65 18 0 20 16 2.63 10. Tennadar * 7.98 0.719 180 1 2.8 95 70 20 0 20 17 2.78 BIS Permissible limit 6.5 - 8.5 < 3 2000 10 6 600 200 1000 Nil 200 100 < 26 *Unaffected area Fig.2 Variability of pH and EC in soil samples 0 10 20 Soil pH 2004 (Pre tsunami) 2005 2006 2013 0 5 10 15 20 25 Soil EC ds/m 2004 (Pre tsunami) 2005 2006 2013
  • 4. M. Velayudha DasInt. Journal of Engineering Research and Applications www.ijera.com ISSN : 2248-9622, Vol. 4, Issue 9( Version 6), September 2014, pp.167-173 www.ijera.com 170|P a g e Fig. 3 Variability of pH and EC in water samples 0 10 20 Water pH 2004(Pre tsunami) 2005 2006 2013 0 5 10 15 20 25 30 35 Water EC ds/m 2004(Pre tsanami) 2005 2006 2013
  • 5. M. Velayudha DasInt. Journal of Engineering Research and Applications www.ijera.com ISSN : 2248-9622, Vol. 4, Issue 9( Version 6), September 2014, pp.167-173 www.ijera.com 171|P a g e Fig. 4Spatial variability of pH and EC in soil samples
  • 6. M. Velayudha DasInt. Journal of Engineering Research and Applications www.ijera.com ISSN : 2248-9622, Vol. 4, Issue 9( Version 6), September 2014, pp.167-173 www.ijera.com 172|P a g e Fig. 5Spatial variability of pH and EC in water samples 4.1 Soil Quality With reference to pH values, there is a good improvement and within normal range of 6.5 to 7.5 except Naluvedapathi and Vedaranyam villages. The soil of these villages is clayey intexture whereas other affected villages are of sandy soil. There was a significant decrease of soil EC in comparison to values immediately after Tsunami-2004.This is due to the rainfall flushing of the surface salts that resulted in lowering of the EC of the surface soil. The soil samples where low in available N could be due to low amount of organic carbon in the soils, and most of the samples were low to medium in available P and K, which needs regular monitoring of fertility status.Depending on soil type, the gypsum of appropriate quantities can be applied before taking up agricultural activities. 4.2 Water Quality The pH is well within the norms in all the samples except Kovilpattu and Vedaranyam villages indicating study area water falls in alkaline nature. The EC influences crop and drinking purposes.The EC values for drinking purposes show poor category of >3 ds/m in Pudupalli, Kovilpattu and Vedaranyamvillages. In this study, the TDSvalues varied between 410 to7490 mg/L and are within the maximum permissible limit for drinking as per the BIS in all samples except Pudupalli, Kovilpattu and Vadaranyam villages.The highest concentration of TDS is likely due to mixing of groundwater with seawater. Turbidity is the cloudiness or haziness of water. No samples in the study area contain turbidity. DO, a vital parameter to know the status of the aquatic ecosystem, is within the norms (<6 mg/L) in all sample locations. Water hardness is determined by the concentration of multivalent cations in the water. Vedaranyamvillage has a higher concentration of hardness (840mg/L) which may cause health hazards.The high level of sodium inhibits soil permeability and gives a salty taste.Maximum concentration of Nahas been observed inthe Kovilpattu village (235mg/L) and Vedaranyam village (870 mg/L) due to seawater influence and study area near to saltpan deposits.Kovilpattu and Vedaranyamvillagesamplesrepresent maximum Cl concentration of 1150 and 1210 mg/L, which is more than BISfor drinking water, andbecome unsuitable for drinking purpose.Salinity is the saltiness content of water or soil. The salinity levels in the study area are varying between 0 to 6%.SAR is a measure of alkali/sodium hazard to crops. The SAR values ranged from 2.16 to 24.71are within the maximum allowable limit shows that groundwater can be used for irrigation without any risk. From the secondary sources and comparative study of pre and post Tsunami data, it was reported that the groundwater was fit for irrigation and drinking purposes before Tsunami-2004, but after Tsunami-2004 the quality of groundwater got deteriorated and needs conservation practices. V. CONCLUSION The study reveals that the surface soil samples qualities of Tsunami-2004 affected agricultural areas in Vedaranyamtaluk indicated faster improvement and are moderately suitable for agriculture production. But the qualities of groundwater were observed to beinhibited for irrigation and drinking purposes.Also, due to non-availability of good quality water in the study area, people are compelled to use water from bore/hand pumps. Groundwater in the study area is generally alkaline in nature, especiallyVedaranyamvillage which was worst affected.From questionnaire survey results show 43% respondents report a decreasing trend in the yield due to salinity land and low fertility. Moreover, to reclaim, both short-term and long-term strategyefforts should be made, such as adoption of improved crop varieties, water management practices, construction of drainage, drip and sprinkler irrigation system, renovation of defaulttanks and ponds and desilting of drainage channels and cannels. Micro level field data and mapping are required for sustainable development of natural resources of the study area.
  • 7. M. Velayudha DasInt. Journal of Engineering Research and Applications www.ijera.com ISSN : 2248-9622, Vol. 4, Issue 9( Version 6), September 2014, pp.167-173 www.ijera.com 173|P a g e REFERENCES [1.] Ayers R.S. (1985),“Water Quality Management for Agriculture”, FAO Irrigation and drainage paper. [2.] BIS (1983), “Standards for water for drinking and other purposes”, Bureau of Indian Standards Publication, New Delhi. [3.] Burroughs P.A. (1989) “Principle of Geological Information System for land Resources Assessment”, Clarendon Press, Oxford. [4.] ChandrasekaranH. and StalinM. (2008),“Variability of soil-water quality due to Tsunami-2004 in the coastal belt of Nagapattinam district,Tamilnadu”,Journal of Environmental Management,Vol.89(1), pp.63-72. [5.] Indian Agricultural Research Institute (IARI),(2005), “Effort of Tsunami on coastal crop husbandry in part of Nagapattinam district, Tamil Nadu”, Current science, Vol. 89. No.1, pp. 30-32. [6.] Norbert F. (2006), “Strategies to reduce the impact of salt on crop production: A case of the Tsunami-affected area of India”, Science Direct, Desalination 206, pp. 524-530. [7.] Palinivelu K. and NishraPriya M. (2006), “Water quality assessment in the Tsunami- affected coastal areas of Chennai”, Current Science, Vol. 91, No. 5, pp. 219-230. [8.] Poongothai S. and Ravisankar R. (2008),“A study on groundwater quality in Tsunami affected areas of Sirkazhi taluk, Nagapattinam district, Tamilnadu, India”, International Journal of Science of Tsunami Hazards,Vol.27(1),pp.48-55. [9.] Ramalingam M. and Subramanian A. (2012), “Seasonal variation of physical-chemical properties of Great Vedaranyam swamp, south-east coast of India”, African Journal of Environmental Science and Technology, Vol. 5(9), pp. 673-681. [10.] Ramkumar T. and Venkatramanan S. (2010), “Hydrogeochemical quality of groundwater in Vedaranyam Town, Tamilnadu, India”, Research Journal of Environmental and Earth Science, Vol. 2 (1), pp. 44-48. [11.] Rangalakshmi R. and Senthilkumar R. (2007), “Reclamation and status of Tsunami damaged soil in Nagapattinam district, Tamilnadu”, Current Science, Vol. 92, No. 9, pp. 1221-1223. [12.] Sankar K. and Aravindan S. (2011), “Spatial distribution of groundwater quality in Paravanar River Sub-basin, Cuddalore District, Tamilnadu”, International Journal of Geomatics and Geoscience, Vol. 1 (4), pp. 914-931. [13.] TRINet (2006), “Agriculturepost-Tsunami” TRINet Newsletter.