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Hydrological Model for Estimating Volume of Inflow into the Peppara Dam Reservoir Using GIS and SWAT
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Hydrological Model for Estimating Volume of Inflow into the Peppara Dam Reservoir Using GIS and SWAT
1.
International Research Journal
of Engineering and Technology (IRJET) e-ISSN: 2395-0056 Volume: 11 Issue: 01 | Jan 2024 www.irjet.net p-ISSN: 2395-0072 © 2024, IRJET | Impact Factor value: 8.226 | ISO 9001:2008 Certified Journal | Page 14 Hydrological Model for Estimating Volume of Inflow into the Peppara Dam Reservoir Using GIS and SWAT Midhila M1, Fathima Sherin T2 1Assistant Professor, Dept.of Civil Engineering, Vidya Academy of Science and Technology Technical Campus, Kerala, India 2Assistant Professor, Dept.of Civil Engineering, Vidya Academy of Science and Technology Technical Campus, Kerala, India ---------------------------------------------------------------------***--------------------------------------------------------------------- Abstract - This article presents an application of SWAT model to simulate and predict the volume of inflow into Peppara dam reservoir. The model was calibrated and validated using SWAT CUP (SWAT-Calibration Uncertainty Programs). The calibration was done from 2004 to 2013 and validation was performed from 2014 to 2018. The coefficient of determination (R2) and Nash Sutcliffe Efficiency (NSE) obtained were 0.77 and 0.69 respectively during calibration stage and 0.79 and 0.74 respectively during validation stage. Model showed good performance during calibration and validation stage. This rainfall runoffcan beusedforpredicting the volume of inflow into the reservoir for various rainfall events and it can help in planning the water distribution to TVM corporation. Key Words: Watershed model; GIS; SWAT: Peppara dam reservoir 1.INTRODUCTION Hydrological model is a simplification of real-world system, that helps in understanding, predicting and managingwater resources. Soil and Water Assessment Tool (SWAT) is one type of tool used for developing a hydrological model. Hydrological processes occur in watershed. The analysis of watershed is a fundamental step. Hydrological models are used to determine the stream flow over a long period. This model which produces historical current or natural stream flow records and is used to generate the future yields. Objective of this research is to develop a model for predicting volume of inflow into the Peppara dam reservoir. This model will help in planning the water distribution as well as for electricity generation planning in TVM corporation. The SWAT-CUP tool is a program that interfaces with Arc SWAT to perform calibration, validation and sensitivity analysis. 2. STUDY AREA The catchment area of Peppara dam reservoir is the study area. Peppara dam is located at Peppara around 55 km from Trivandrum City. Peppara dam is constructed across Karamana river. It is the main drinking water supply to Thiruvananthapuram district and sub urban areas. Peppara wild life sanctuary is one of the most beautiful wildlife sanctuary of kerala. Peppara dam reservoir located in latitude of 8.6228° N and longitude of 77.1379°E. Area ofthe reservoir is 5.82 sq.km Fig -1: Location map of Peppara
2.
International Research Journal
of Engineering and Technology (IRJET) e-ISSN: 2395-0056 Volume: 11 Issue: 01 | Jan 2024 www.irjet.net p-ISSN: 2395-0072 © 2024, IRJET | Impact Factor value: 8.226 | ISO 9001:2008 Certified Journal | Page 15 3. METHODOLOGY SWAT model was simulated by using Arc SWAT with help of DEM, Land use land cover map, soil map and meterological data from Nedumangadustation.SWATsimulationwasdone from 2004 to 2018. The reservoir waterlevel was collected from KWA (Kerala Water Authority) 4.MODEL EFFICIENCY The performance of the model was determined by statistical co- efficients. The calibration andthevalidationwerecarried out using the Coefficient of Determination (R^2), Nash– Sutcliffe Efficiency index (NSE) = (1) NSE=1-[ (2) where, = observation = simulated value Table-1 General performance rating R2 Very good Good Satisfactory Un Satisfactory >0.7 0.60< ≤ 0.70 0.50< ≤ 0.60 ≤0.50 NSE 0.75 <NSE <1.00 0.65 <NSE ≤0.75 0.5<NSE≤ 0.65 ≤0.50 5. CALIBRATION AND VALIDATION The SWAT-CUP tool is a program that interfaces with Arc SWAT to perform calibration, validation and sensitivity analysis. The method SUFI-2(Sequential UncertainityFitting Version 2) was selected. SUFI 2 provides good accuracy and has the ability to capture the observed data with small uncertainties. Calibration was done for 10 years (2004- 2013) along with sensitivity analysis that is same data set and parameters are used for both. The sensitivity analysis is so used to identify and rank the most responsive hydrological parameters that have significant impact on specific model output. Calibration and sensitivity analysis were carried out for 3 iterations each having 500 simulations. 18 parameters were used. In each of the simulations the values of parameters get updated in such a way that more data are bracketed inthe95PPU. Itcalculated at the 2.5% and 97.5% level of the output variables disallowing 5 % of the bad simulation. To evaluate the significance of the relative sensitivity t-stat and p- value were utilised. t- stat provides a measure of sensitivity. p- value determines the significance of sensitivity. The larger absolute t-stat signifies greater sensitivity.Closertozerothe p-value, the higher significance. Validation is the process of comparing the model and its behaviour to the real system and its behaviour. The purpose of validation is to check the accuracy and performance of the model basis on the past data for which we already have actuals. Validation was done from 2014 to 2018. Observed data is the Peppara dam reservoir inflow. The surface area of the reservoir was multiplied with reservoir water level difference to obtain volume of inflow into Peppara dam reservoir. Table- 2: Calibration Parameters Parameter code Parameter’s name R_CN2.mgt Initial SCS CNII value V_ALPHA_BF Base flow alpha factor V_GW_DELAY.gw Ground water delay time (days) V_GWQMN.gw Threshold water depth in Shallow aquifer for flow R_ESCO.hru Soil evaporationcompensationfactor R_EPCO.hru Plant uptake compensation factor R_CH_N2.rte Manning’s “n” value for the main channel R_CH_K2.rte Effective hydraulic conductivity in main channel (mm/hr) R_OV_N.hru Manning’s “n’’ value for the Overland flow R_REVAPMN.gw Threshold depth of water in Shallow aquifer for ‘revap’ R_GW_REVAP.gw Ground “revap’’ co efficient R_SURLAG.bsn Surface runoff lag time R_SOL_K.sol Saturated hydraulic conductivity R_SOL_BD Moist bulk density (Mg/m3) R_SOL_AWC.sol Available water capacity of the Soil layer R_ALPHA_BNK.rte Baseflow alpha factor for bank storage R_RCHRG_DP.gw Deep aquifer percolation factor R_SLSUBBSN.hru Average slope length
3.
International Research Journal
of Engineering and Technology (IRJET) e-ISSN: 2395-0056 Volume: 11 Issue: 01 | Jan 2024 www.irjet.net p-ISSN: 2395-0072 © 2024, IRJET | Impact Factor value: 8.226 | ISO 9001:2008 Certified Journal | Page 16 6. RESULT AND DISCUSSION Table-3: Parameter value obtained from calibration Parameter name Fitted value R_CN2.mgt 0.700500 V_ALPHA_BF.gw 0.459190 V_GW_DELAY.gw 93.449997 R_OV_N. hru 0.121 R_SOL_K.sol 93.699974 R_SOL_AWC.sol 0.76 R_SOL_BD.sol 1.580314 R_GW_REVAP.gw 0.021320 R_SLSUBBSN.hru 67.540001 R_SURLAG.bsn 1.302350 R_ESCO.hru 0.564086 R_REVAPMN.gw 55.000004 R_CH_K2.rte 95.275002 R_RCHRG_DP.gw 0.745000 R_EPCO.hru 0.975500 V_GWQMN.gw 0.767737 R_ALPHA_BNK.rte 0.558250 R_CH_N2.rte 0.297800 Fig -2: Monthly observed and simulated flow in calibration Fig -3: Monthly observed and simulated flow in validation Table- 4: Summary of the calibration and validation result Calibration (2004 -2013) Validation (2014- 2018) R2 0.77 (Very good) 0.79 (Very good) NSE 0.69 (Good) 0.74 (good) 7. CONCLUSIONS The Arc-SWAT model was developed to estimate reservoir volume of inflowperformedeffectivelyforPeppara reservoir catchment. During calibration of model the value of R2 and NSE obtained were 0.77and 0.69whichwerewithinthegood limits and the values for the sameobtainedduringvalidation were 0.79 and 0.74 which shows good performance of the model. 18 Parameters were used in this study. Curve number, Base flow alpha factor, Ground water delay time, Manning’s “n” value for the overland flow, Saturated hydraulic conductivity, Available water capacity of the soil layer and moist bulk density are the most sensitive parameters in the Peppara dam reservoir catchment. This rainfall runoff model can be used for predicting the volume of inflow into the reservoir for various rainfall events and it can help in planning the water distribution to TVM corporation. 8. REFERENCES [1]Arnold.J.G, Moriasi. D.N, Gassman. P.W,Abbaspour.K.C, White.M.J, Srinivasan.R, Santhi.C, Harmel.R.D, Van Griensven.A, Van Liew.M.W, Kannan.N, Jha.M.K (2012), SWAT:Model use, Calibration,Validation, AmericanSociety Agriculture and Biological Engineers,55(4),pp1491-1508 [2] Shimaa M. Ghoraba (2015), Hydrological modelingof the Simly dam watershed (Pakistan) using GIS and SWAT model, Journal of hydrology, 54, pp 583-594. [3]Bounhieng Vilaysanea, Kaoru Takaraa, Pingping Luob, Inthavy Akkharathc, Weili Duana (2015) Hydrological stream flow modelling for calibration and uncertainty analysis using SWAT model in the Xedone river basin, Lao PDR, Environmental sciences,28, pp 380-390 [4]Abbaspour.K.C,Rouholahnejad.E,Vaghefi.S, Srinivasan.R, Yang.H, Klove.B (2015), A Continental scale hydrologyand water quality model for Europe: Calibration and Uncertainit of a high resolution large scale SWAT model, Journal of Hydrology, 524, pp 733-752 [5]Milad Jajarmizadeh, Lariyah Mohd Sidek, Sobri Harun, Mohsen Salarpour (2017), Optimal calibration and uncertainity analysis of SWAT for an Arid Climate, Air Soil and water research, 10, pp 1-14
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International Research Journal
of Engineering and Technology (IRJET) e-ISSN: 2395-0056 Volume: 11 Issue: 01 | Jan 2024 www.irjet.net p-ISSN: 2395-0072 © 2024, IRJET | Impact Factor value: 8.226 | ISO 9001:2008 Certified Journal | Page 17 [6]Tejaswini.V, Sathian.K.K (2018), Calibration and validation of SWAT model for Kunthipuzha Basin using SUFI 2 Algorithm, International Journal of Current Microbiology and Applied Sciences, 7(1), pp 2162-2172 [7]Andriano Ansari, Tasuku Kato, Atiqotun Fitriah (2019), Simulating stream flow through the SWAT model in the Keduang sub watershed Wonogiri ,Indonesia, Agritech, 39(1), pp 60-69 [8]Thair Sharif Khayyan, Imzahim Abdulkareem Alwan , Ali Mohsen Hayder (2019), Hydrological model for Hemren dam reservoir catchment area at the middle river Diyala reach in Iraq using ArcSWAT model, Applied waterscience, 9(5), pp 1-15 [9]Gianluigi Busico, Nicolo Colombani, DavideFronzi,Marco Pellegrini, Alberto Tazioli, Micol Mastrocicco (2020), EvaluationSWATmodel performanceconsideringdifferent soil data input to quantify actual and future runoff susceptibility in a highly urbanized basin, Jounral of environmental management,266, 11062 [10]Sharlene L. Beharry, Ddonald Gabriels, Deyanira Lobo, Deanesh Ramsewak, Richard M. Clarke (2020), Use of the swat model for estimating reservoir volume in the upper navet watershed in Trinidad, SN Applied science, 3(2), pp 1-13 [12] Md Sharafat Chowdhury (2023),Modellinghydrological factors from DEM using GIS, MethodsX, Vol. 10, 102062 [11] http://www.2w2e.com accessed on 1.12.2022 @ 3.30 pm
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