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Energy Geoscience

Discharge water temperature assessment of thermal power plantusing remote sensing techniques

作     者:Priyom Roy Ivaturi N.Rao Tapas Ranjan Martha K.Vinod Kumar 

作者机构:Geosciences GroupNational Remote Sensing CentreISROHyderabadIndia Environment&SustainabilityCoastal Gujarat Power LimitedMundraGujaratInd 

出 版 物:《Energy Geoscience》 (能源地球科学(英文))

年 卷 期:2022年第3卷第2期

页      面:172-181页

核心收录:

学科分类:07[理学] 0707[理学-海洋科学] 

基  金:National Remote Sensing Centre  NRSC 

主  题:Discharge water Thermal power plant Ambient temperature Landsat 8 Seawater pollution 

摘      要:Thermal power plants are generally constructed near to sea coast to meet their requirement of coolingwater. The warm water discharge from the thermal power plant is one of the major environmentalconcerns in view of the thermal pollution in the sea water. The temperature limit for the warm waterdischarge from the thermal power plant has to be monitored and controlled. Coastal Gujarat PowerLimited (CGPL) operates (24×7) at an “once-through system based sea water circulation for powergeneration. The used sea water is then discharged into the sea through an outlet channel. As per environmental norms, the discharge water temperature needs to be maintained below the stipulated “deltarise (+7 ℃) with respect to ambient sea surface temperature at the inlet. We demonstrate the applicability of thermal remote sensing data in understanding the seasonal and temporal variations of thetemperature difference between the discharge water and the ambient sea water. We used thermal banddata from Landsat-8 satellite imagery to map water surface temperature and create temperature profilesalong the intake and outflow channels (till the sea), to understand the variation of temperature andestimate the “DT between intake point and various observation points along the outflow. This analysiswas carried out for all 11 months (except June) of the year 2018 to correlate temperature variations withseasonal changes. Tidal conditions during the time of data acquisition were also considered to accountfor the effect of tides on DT. The result shows that the average temperature rise between intake andoutflow are maintained at ~3 ℃ across all the months of 2018, with minor variations in the months ofJuly and August. Further, average temperature drop from outflow to cooling channel (before diaphragm)is seen to be ~2 ℃ across all the months with similar seasonal fluctuations.

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