ROLE OF RAIN WATER HARVESTING IN ARTIFICIAL RECHARGE OF GROUND

Similar documents
Rainwater Management. Dr. Iftikhar Ahmad. College of Earth and. University of The Punjab Lahore

ASSESSMENT OF RAINWATER HARVESTING POTENTIAL FOR A PART OF CHANDIGARH

AGRAR. Augmenting Groundwater Resources by Artificial Recharge. ICARDA, Aleppo, Syria nd November 2006

INTERNATIONAL JOURNAL OF ENVIRONMENTAL SCIENCES Volume 1, No 7, Copyright 2010 All rights reserved Integrated Publishing Association

Rainwater Harvesting in Educational Institution and Residential Area: A Case Study of University of Asia Pacific in Dhaka

Urban Groundwater Scenario. M. S. Mohan Kumar. Department of Civil Engineering Indian Institute of Science Bangalore

Chapter 1 Introduction

ESTIMATION OF GROUND WATER RECHARGE FOR KHADAKWASLA REGION BY USING GIS SOFTWARE

Rainwater harvesting for Aquifer Storage and Recovery - Case Studies in Goa

Sixth Semester B. E. (R)/ First Semester B. E. (PTDP) Civil Engineering Examination

D.G.S.W. Pitakumbura Manager (Groundwater Studies) Groundwater Section NWS&DB. Groundwater recharge or deep drainage or

Kottayam, Kerala, India. Nattakam, Kerala, India

A CASE STUDY ON RAIN WATER HARVESTING TECHNOLOGIES FOR TRIBAL AREA OF MADHYA PRADESH, INDIA

Studies on Estimative Methods and their Role in Artificial Ground Water Recharge

Water Era in India. Rainwater harvesting systems. Rainwater harvesting. S.Vishwanath Twitter handle : zenrainman

Irrigation modeling in Prairie Ronde Township, Kalamazoo County. SW Michigan Water Resources Council meeting May 15, 2012

Urban Rainwater Harvesting Systems: Promises and Challenges

Impact Study of a check dam on Ground Water Recharge

RAINWATER HARVESTING FOR RECHARGING GROUNDWATER- A CASE STUDY FOR NURSING COLLEGE, T.M.U. MORADABAD

Materials and Methods

Global Water. Globally, 1.2 billion people live in areas with water supply.source:internationalwater

PROF. P.A. HANGARGEKAR Head of Department, Civil Engineering, S.T.B.C.E, Tuljapur (M.S.), India

Rainwater Harvesting Structures - A Case Study

Analyzing water resources in a monsoon-driven environment an example from the Indian Western Ghats

Lecture 9A: Drainage Basins

AN INTEGRATED FRAMEWORK FOR EFFECTIVE ADAPTATION TO CLIMATE CHANGE IMPACTS ON WATER RESOURCES

Effect Of Rainfall On Groundwater Level Fluctuations In Chapai Nawabgonj District

PERFORMANCE EVALUATION OF GROUNDWATER RECHARGE STRUCTURES: AN APPLICATION OF WATER BALANCE ANALYSIS,

WATER QUALITY SCENARIO OF URBAN POLLUTED LAKES A MODEL STUDY

Status, Quality and Management of Groundwater in India

DEPARTMENT OF GEOGRAPHY POST GRADUATE GOVT. COLLEGE FOR GIRLS.SECTOR-11 CHANDIGARH CLASS-B.A.II PAPER-A RESOURCES AND ENVIRONMENT: WORLD PATTERNS

Rainfall analysis is not only important for agricultural

Effectiveness of Artificial Recharge Structures in Enhancing Groundwater Storage: A Case Study

MAPPING AND MODELING OF GROUND WATER PATTERN USING GEO SPATIAL TECHNOLOGY

A COMPREHENSIVE REPORT ON GROUNDWATER QUALITY MONITORING AND MANAGEMENT BY USING GEOSPATIAL TECHNOLOGY - A MODEL STUDY

CHAPTER 7 GROUNDWATER FLOW MODELING

A comparative analysis of hydrologic responses to rainwater harvesting A case study

Issue paper: Aquifer Water Balance

A Case Study on Integrated Urban Water Modelling using Aquacycle NTUA, 2007

HYDROLOGY - BASIC CONCEPTS

Drying Up of Groundwater Wells and Sustainable Development Options for Preservation of Groundwater in Sri Lanka

GROUNDWATER Dr. DEEPAK KHARE GENERAL HYDROLOGY CYCLE FORMATIONS

Micro-Minor Methods of Rainwater Conservation and Groundwater Recharge

Hydrogeology 101 3/7/2011

Land Subsidence Management in Japanese Deltas

THINK GLOBAL & ACT LOCAL

Exploring the Possibilities At Prado Dam

Groundwater Balance Study in the High Barind, Bangladesh. A.H.M.Selim Reza 1, Quamrul Hasan Mazumder 1 and Mushfique Ahmed 1

Update on Cuyama Basin Groundwater Modeling

Managed Aquifer Recharge (MAR) Practical Techniques for the Caribbean

Adapting to Water Scarcity for Yemen s Vulnerable Communities. Dr. Mansour Haidera Dr. Abdulla Noaman Dr. Saif Ali Othman Dr.

PEACE RIVER MANASOTA REGIONAL WATER SUPPLY AUTHORITY BOARD OF DIRECTORS MEETING December 5, 2018 ROUTINE STATUS REPORTS ITEM 1

THE HYDROLOGICAL BEHAVIOR IN THE GREATER ZAB RIVER BASIN

Numerical Groundwater Model for the Kaweah Delta Water Conservation District

Welcome to the MWON Advanced Webinar Series

Modelling of hydrological processes for estimating impacts of man's interventions

ROOFTOP RAINWATER HARVESTING (RRWH) AT SPSV CAMPUS, VISNAGAR: GUJARAT - A CASE STUDY

General Groundwater Concepts

M.L. Kavvas, Z. Q. Chen, M. Anderson, L. Liang, N. Ohara Hydrologic Research Laboratory, Civil and Environmental Engineering, UC Davis

Flood Modelling and Water Harvesting Plan for Paravanar Basin

Regional Groundwater Flow Modeling of Yarkant Basin in West China

Effects of irrigation on groundwater recharge under deep buried depth condition

Groundwater 3/16/2010. GG22A: GEOSPHERE & HYDROSPHERE Hydrology

Information Request 11

Modelling the Effects of Climate Change on Hydroelectric Power in Dokan, Iraq

Assessment of the Groundwater Quantity Resulting from Artificial Recharge by Ponds at Ban Nong Na, Phitsanulok Province, Thailand

Water Management System A Case Study

RAINWATER HARVESTING FOR DOMESTIC CONSUMPTION IN BANGLADESH

Rainwater Harvesting

CHAPTER FIVE Runoff. Engineering Hydrology (ECIV 4323) Instructors: Dr. Yunes Mogheir Dr. Ramadan Al Khatib. Overland flow interflow

2-4 April 2019 Taets Art and Event Park, Amsterdam CLICK TO KNOW MORE

Artificial Groundwater Recharging In India

Agricultural Planning through Prediction of Rainfall Characteristics for Bilaspur Region of Chhattisgarh Plain in India

Wetland Water Balance Linking hydrogeological processes to ecological effect

WASA Quiz Review. Chapter 2

Estimation of Surface Runoff in the Man River Basin (MS)

Assessment of Ground Water Potential of Five Villages of Jasra Block of Allahabad District

Surface Runoff Estimation using Remote Sensing & GIS based Curve Number Method Ishtiyaq Ahmad, Dr. M. K. Verma

ARTIFICIAL RECHARGE PROJECT & AUGMENTATION OF SURFACE IRRIGATION IN THE COASTAL AREA OF VANUR TALUK, VILLUPURAM DISTRICT, TAMIL NADU, INDIA

Song Lake Water Budget

ENGINEERING HYDROLOGY

THE DATA COLLECTION AND COMPILATION PROCESSES

The Islamic University of Gaza- Civil Engineering Department Sanitary Engineering- ECIV 4325 L5. Storm water Management

East Maui Watershed Partnership Adapted from Utah State University and University of Wisconsin Ground Water Project Ages 7 th -Adult

SWIBANGLA. Managing Salt Water Impacts in Bangladesh. Marta Faneca Sanchez Gualbert Oude Essink Gijs Janssen Roelof Stuurman Yangxiao Zhou, UNESCO-IHE

ASSESMENT OF RAINWATER AND STORM WATER QUALITY IN BIDADI INDUSTRIAL AREA

Geotechnical Parameters Impact on Artificial Ground Water Recharging Technique for Urban Centers

Role of the State Engineer s Office

Groundwater Level and Movement

CHAPTER ONE : INTRODUCTION

Anshuman, Kapil Kumar Narula, Kamal Kumar Murari, Hrishikesh Mahadev, Poulomi Banerji

Overview of the Surface Hydrology of Hawai i Watersheds. Ali Fares Associate Professor of Hydrology NREM-CTAHR

Are Off-grid Solar PV Pumps a solution to Power Crisis in Agriculture Some reflections on the initiative of New State of Andhra Pradesh

M.L. Kavvas, Z. Q. Chen, M. Anderson, L. Liang, N. Ohara Hydrologic Research Laboratory, Civil and Environmental Engineering, UC Davis

Rashid Ali Khan, FAO (Ret.) Gurgaon, Haryana

ENGINEERING HYDROLOGY

MAPPING OF NATURAL RESOURCES AND DEVELOPING STRATEGY FOR WATER

4/3/2017. Water Accounting and Auditing for Irrigation and Drainage Systems. Changes in irrigation and drainage sector

Watershed Management and Rainwater Harvesting in Vishwaniketan Campus

The Impacts of Climate Change on Portland s Water Supply

Transcription:

International Journal of Civil Engineering and Technology (IJCIET) Volume 8, Issue 3, March 2017, pp. 991 998 Article ID: IJCIET_08_03_100 Available online at http://www.ia aeme.com/ijciet/issues.asp?jtype=ijciet&vtyp pe=8&itype=3 ISSN Print: 0976-6308 and ISSN Online: 0976-6316 IAEME Publication Scopus Indexed ROLE OF RAIN WATER HARVESTING IN ARTIFICIAL RECHARGE OF GROUND WATER Mohammad M J Associate professor, Department of Civil Engineering, SBIT Engineering College, Khammam, Telangana, India Ramyasree G, Swarooparani Ch, Krishnaveni T, Deepika P R, Sairam J Students, Department of Civil Engineering, SBIT Engineering College, Khammam, Telangana ABSTRACT This paper majorly focuses on role of rain water harvesting in artificial recharge of ground water in SBIT engineering college, Khammam, Telangana. Water is important for the survival of living organisms along with food, air etc. Ground water is the major source for domestic, industrial, agricultural, aquaculture etc. Ground water is a resource of immense value that is heavily used by people. The protection of ground water from contamination, however, has long been neglected. In recent years, the need for ground water protection and management has been recognized. Due to continuous pumping of ground water, the water table is decreasing rapidly and if this problem is not taken seriously, then the future generations has to face severe crisis of water. Rains are the main source of water and if this rainwater is harvested, scarcity of water can be eliminated. Rain water is bacteriologically pure, free from organic matter and soft in nature. So, rainwater is an ideal solution for water problems where there is inadequate water supply. Rainwater harvesting is a simple technique of collecting the rain water from either surface or rooftop of buildings, or both surface and rooftop and also can be used to rechargee the aquifers. Key words: Rainwater, Artificial recharge, Groundwater, aquifer, Recharge pits. Cite this Article: Mohammad M J, Ramyasree G, Swarooparani CH, Krishnaveni T, Deepika P R and Sairam J, Role of Rain Water Harvesting In Artificial Recharge of Ground Water, International Journal of Civil Engineering and Technology, 8(3), 2017, pp. 965-973. http://www.iaeme.com/ijci IET/issues.asp?JType=IJCIET&VType=8&ITy ype=3 http://www.iaeme.com/ijciet/index.asp 991 editor@iaeme.com

Role of Rain Water Harvesting In Artificial Recharge of Ground Water 1. INTRODUCTION Water is essential for the existence of all the living organisms. The demand for water is increasing due to so many reasons like increasing population, industrialization, urbanization, several climatic changes etc., To avoid that problem now a days we are adopting rainwater harvesting technique. Decreasing ground water is due to low water storage capacity, low infiltration, larger inter annual fluctuations of precipitation (due to monsoonal rains) and high evaporation demand. Rain water harvesting is used for collecting and storing runoff water resulting from rain in soil profile and reservoir both over surface/under surface [1]. Water is a most important renewable natural resource which plays an important role in the survival of living organisms [2]. Water is one of the most abundantly available substances in nature, covering more than 70% of the earth s surface. Water of the good quality is required for living organisms. At the same time growing populations, progressive industrialization and intensification of agriculture have led to increased pollution of water resources [3]. Rain water collected through rain water harvesting is utilized for recharging both open wells and bore wells [4]. Annually replenish able resources are assessed as 432 billion cubic meters (BCM). The basic need for increasing the groundwater recharging is the growing population which increased the demand of water resources. India s population has recently crossed the one billion mark, hence due to this increased population, our country is facing serious threat as there is a huge gap between the demand for water and the supply is getting widened day by day [5]. Although water is an important for survival of human being as much as food, air etc, but hardly any attention is paid for its economical use and conservation of this precious resource. Due to indiscriminate pumping of ground water, the water table is going down abnormally and if the problem is not given a serious look then the future generations may have to face severe crisis of water. Rains are the main source of water and if rain water is harvested the scarcity of water can be eliminated together [6]. So to overcome this problem, from our ancient days itself there are lot of widely developed techniques to harvest rainwater, which are simple, efficient and cost effective. A mix of ancient and modern techniques must be implemented to improve the water harvesting methods in our country. 1.1. Artificial recharge Artificial recharge is the planned, human activity of augmenting the amount of ground water available through works designed to increase the natural replenishment or percolation of surface waters in to the ground water aquifers, resulting in a corresponding increase in the amount of ground water [7]. 1.2. Artificial ground water recharge in India Artificial ground water recharge methods have been extensively used in the developed nations for several decades, their use in developing nations, like India has occurred only recently. Various techniques for artificial ground water recharge have been employed in the states of Maharashtra, Gujarat, Tamilnadu, and Kerala. Artificial Recharge has several potential advantages and disadvantages, The use of aquifers for storage and distribution of water and removal of contaminants by natural cleansing process that occurs as polluted rain and surface water in filtrate the soil and percolate down through the various geological formations, The main disadvantage is unless significant volumes of water are injected in an aquifer, ground water recharge may not be economically feasible [8]. http://www.iaeme.com/ijciet/index.asp 992 editor@iaeme.com

Mohammad M J, Ramyasree G, Swarooparani CH, Krishnaveni T, Deepika P R and Sairam J 2. MATERIALS AND METHODS 2.1. Study area Swarna Bharathi Institute of Science & Technology is an engineering college located in Khammam city, which is one of the major city located in the Indian state of Telangana. It is located about 193 Kilometers to the east of the state capital of Telangana (Hyderabad). The average elevation of Khammam city is about 107 meters (351.05 feet) and its geographical area is about 94.37 square kilometers. The city is situated in north latitude 16 45 to 18 35 and east longitude 79 47 to 81 47 (Figure-1, 2, 3). Figure 1 map of Study area of Khammam district. Figure 2 Google map of SBIT Engineering College, Khammam. Figure 3 Image of SBIT Engineering College, Khammam. http://www.iaeme.com/ijciet/index.asp 993 editor@iaeme.com

Role of Rain Water Harvesting In Artificial Recharge of Ground Water 2.2. Water Table Fluctuation in Khammam District Figure 4 Ground Water table Fluctuation of Khammam District. Water table fluctuation map is prepared by using action plan map of Khammam District which has been collected from Central ground water Board, Hyderabad. The maximum water level range is between 10-20m.bgl and minimum water level range is between 0-5 m.bgl. The water table fluctuation levels of Khammam district rising between 6-21.77m.bgl (Figure-4) [9]. The Khammam segment of the South Indian carton is in the Krishna and Godavari river basins. Physiographic ally, the area falls under the uplands category and it shows a dendraitic drainage pattern with a general flow toward the two major river courses. The Munneru River is a major source recharge for ground water in the Khammam area. [10]. 2.3. Ground water table With the reference of rainfall data shows effect on ground water table level (Table-1, Figure- 5) [11], in Khammam, in 2011 the water table level is available at 1.65 meters depth from the surface. It indicates that rainfall and ground water table levels are in proportional ratio. From the data available in the above tables like rainfall data and water level data and the runoff coefficient, we can estimate the total quantity of water that can be collected (in m³). Table 1(A) Groundwater level report from the year 2008-2016 (Khammam) Year Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec Average 2008 2.17 3.31 3.75 3.89 2.44 3.32 2.59 0.97 0.96 1.20 1.48 1.65 2.31 2009 1.93 2.33 2.47 2.92 3.70 4.21 4.93 4.70 4.83 4.25 4.63 5.11 3.83 2010 5.02-5.82 6.25 6.53 4.97 4.62 0.90 1.47 2.31 1.29 1.06 3.35 2011 1.37 1.75 1.34 2.18 5.48 2.00-1.52 1.21 1.61 1.98 2.39 1.65 2012 2.43 2.85 3.06 3.73 4.05 4.45 4.20 2.82 1.55 1.15 3.29 1.78 2.94 2013 3.57 2.62 3.01 3.78 3.91 3.86-0.45 1.52 0.45 0.74 0.85 2.06 2014 1.15 2.69 3.65 2.59 1.40 1.90 1.95 2.70 3.02 2.80 1.00 3.62 2.37 2015 3.80 4.05 4.45 5.02 4.50 2.90 2.65 1.50 1.38 2.38 2.25 2.56 3.12 2016 2.95 3.35 3.65 4.25 4.50 2.55 2.30 2.17 1.27 1.50 0.65 0.78 2.49 http://www.iaeme.com/ijciet/index.asp 994 editor@iaeme.com

Mohammad M J, Ramyasree G, Swarooparani CH, Krishnaveni T, Deepika P R and Sairam J Table 1(B) Groundwater level report Groundwater level (mtrs) Years 2020 2015 2010 2005 2000 1 2 3 4 5 6 7 8 9 Average 2.3 3.8 3.3 1.6 2.9 2.0 2.3 3.1 2.4 Year 200 200 201 201 201 201 201 201 201 Figure 5 Groundwater level report from the year 2008-2016 (Khammam) Figure 6 Identification Ground water prospects of Khammam District Table 2 Ground water prospects of Khammam District S.No Ground water prospects Zones Area in Km 2 1 Very good 511.45 2 Good 452.703 3 Good to Moderate 55458.89 4 Moderate 2301.82 5 Poor 6171.39 Khammam District ground water prospects are observed as very good as 511.45 Km 2, Good as 452.703 Km 2, Good at moderate 55458.89 Km 2, Moderate 2301.82 Km 2, poor as 6171.39 Km 2 in this Khammam Urban area containing of moderate levels shown in Figure 6, Table 2, [12]. 2.4. Groundwater Balance Equation Considering the various inflow and outflow components in a given study area, the ground water balance equation can be written as R r +R c + R i + R t + S i + I g = E t + T p + S e + O g + S Where, R r = recharge from rainfall; R c = recharge from canal seepage; R i = recharge from field irrigation; R t = recharge from tanks; http://www.iaeme.com/ijciet/index.asp 995 editor@iaeme.com

Role of Rain Water Harvesting In Artificial Recharge of Ground Water S i = influent seepage from rivers; I g = inflow from other basins; E t = evapotranspiration from groundwater; T p = draft from groundwater; S e = effluent seepage to rivers; O g = outflow to other basins; and S = change in groundwater storage. The groundwater balance equation therefore generally does not balance, even if all its components are computed by independent methods. The resultant discrepancy in groundwater balance is defined as a residual term in the balance equation, which includes the quantitative determination of various components as well as values of the components which have not been accounted in the equation [13]. 3. RECHARGE PITS Recharge pits are normally excavated pits, which are sufficiently deep to penetrate the low permeability layers overlying the unconfined aquifers. They are similar to recharge basin in principle, with the only difference begin that they are deeper and have restricted bottom area. In many such structures, most of the infiltration occurs laterally through the wall of the pit as in most layered sedimentary or alluvial material the lateral hydraulic conductivity is considerably higher that the vertical conductivity[14]. 3.1. Description of Soakpit Design The distance between SBIT main block to soak pit is 82.7m, and the distance between bore point and soak pit is 3.6m, so based on the catchment area of the SBIT main block we excavated soak pit up to 10m depth. Up to this depth we provided cement rings, each one of 4feet diameter and 1feet height. The total volume of the soak pit is 3.857 cubic meters, so that we can collect up to 415.737 Lt/day (figure-7). Figure 7 Constructed Recharge Soak pit, SBIT Campus http://www.iaeme.com/ijciet/index.asp 996 editor@iaeme.com

Mohammad M J, Ramyasree G, Swarooparani CH, Krishnaveni T, Deepika P R and Sairam J 4. CONCLUSION Ground water is immensely important to suffice human needs in both urban and rural areas of Developing nations [15]. Hence from the above analysis, we can conclude that the best way to artificially recharge the groundwater using low cost-effectiveness and sustainable method and also along with lowest level of contamination is Rainwater Harvesting. The Artifical Recharge of groundwater using Rainwater Harvesting System must be implemented in each and every city, town and Mandals in order to meet the increasing rate of over utilization of water. The groundwater conservation and artificial recharge structures must be constructed in watershed wise and this situation must be considered on war foot basis and by using scientific methods like GIS (Geographical Information System), the area where the necessity of artificial recharge structures are required must be identified and remedial measures must be taken immediately for meeting the future requirements and also to minimize the moderately high level requirement of water. Hence, the artificial recharge of ground water must be done in order to improve the depleted aquifers. The most-effective, easy and long-lasting method used to increase the ground water level is the Rainwater Harvesting. REFERENCES [1] R.K Sivvanappan, Rain water harvesting, Conservation and management strategies for urban and rural sectors, National seminar on rain water harvesting and water management 11-12 Nov. 2006, Nagpur. [2] M. J. Mohammad, P.V. Krishna. Analysis of water quality using Physico- Chemical parameters in paler reservoir of Khammam district, Telangana, India, Pharmanest, 5(6), 2014, 2515-2518. [3] M. J. Mohammad, P.V.Krishna. The Physico-chemical studies on water quality of Wyra reservoir, Khammam district, Telangana, India, Pharmanest, 5(6) 2014,2528-2531. [4] K.A. Patil & G.K. Patil, Rain water harvesting techniques, National seminar on rain water harvesting and water management 11-12 Nov. 2006, Nagpur. [5] M. B. Deshmukh, Rain water harvesting and Ground water Recharge, National seminar on rain water harvesting and water management 11-12 Nov. 2006, Nagpur. [6] Mohammad M J et, al., Rain water harvesting system for Domestic use in SBIT Engineering college, Khammam, Telangana, International Journal of Civil Engineering & Technology,8(2),2017,309-3015. [7] R Sakthivadivel, the ground water recharge movement in India, 2007, pp195-210, http://publications.iwmi.org/pdf/h040048.pdf. [8] AK Bhattacharya, Artificial ground water recharge with special reference to India, International journal of Recent research and applied Studies, 2010, 4(2), 214-221. [9] Sarala, Identification of ground water prospects in the Khammam district, Int. Journal of Applied Sciences and Engineering Research 2013, 2(2), 146-149. [10] M A Rasheed & M J Mohammad, Environmental Impact Assessment: A case study on Physico Chemical Analysis of Ground water Quality, International journal of Advanced Scientific Technologies in Engineering and Management Sciences, 2(3), 2015, 1-5. [11] M. J. Mohammad, et, al., design, Construction and Evaluation of Rain Water Harvesting System for SBIT Engineering College, Khammam, Telangana, International Journal of Civil Engineering & Technology, 2017,8(2), 274-281. [12] Mohammad et, al., Physico-Chemical Parameters Assessment of Ground Water In Urban Area of Khammam, Telangana. International Journal of Civil Engineering & Technology, 20117, 8(3), 232-243. http://www.iaeme.com/ijciet/index.asp 997 editor@iaeme.com

Role of Rain Water Harvesting In Artificial Recharge of Ground Water [13] C. P. Kumar, Ground water assessment methodology, National institute of Hydrology, Roorkee, Uttarakhand, pp 1-22, http://www.angelfire.com/nh/cpkumar/publication /Lgwa.pdf. [14] Dhiman S C, Central Ground water board, Rain water harvesting and artificial recharge, PP 1-160. http://mahenvis.nic.in/pdf/report/report_nrmc_water%20harvesting.pdf. [15] G Surekha et al., Ground water quality Mapping of East Godavari District, Andhrapradesh, India, Using Remote sensing and Geo statistics, International journal of Recent scientific Research, 2015, 6(4), 3602-3608. http://www.iaeme.com/ijciet/index.asp 998 editor@iaeme.com