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太阳能空气吸热器及其在太阳能热发电中的应用
SolarairreceiveranditsapplicationinCSPOutlineIntroductionSolarAirReceiverLiteraturereviewTheR&DofSolarairreceiverinChinaThermalcycletestPressuredropInterfacialheattransferExperimentalStudyofaReceiverAmacroscopicmodelConclusion/OutlookAirConcentratedSolarRadiationTsTfTOutlineIntroductionSolarAirReceiverLiteraturereviewTheR&DofSolarairreceiverinChinaThermalcycletestPressuredropInterfacialheattransferExperimentalStudyofaReceiverAmacroscopicmodelConclusion/OutlookAirConcentratedSolarRadiationTsTfTBPIEANBSCReleasedateJun2010Jul2010Feb2010China21.99
22.52
21.32USA21.82
21.70
21.76①
Difference0.78%3.78%-2.02%①TheaverageofIEAandBP’sdata.②Unit:100milliontonsofoilequivalentTable1energyuseofChina&USA
1.IntroductionNo.1energyconsumingcountry!?Solution:SolarenergySolarenergy:PVorCSP?PVCSPEnergyStorageNoteconomicallyviable6-12hpossibleCombinationwithconventionalpowerplantsnoyesDailyEnergypatternMaximumpoweraroundmiddayMaximumpowercanbeextendedtothenightComplexityLimitedamountofdifferentpieces,electricityonlyLargeamountofpieces,electricityandhydraulicsConstructionQuickandFlexible.Componentsreadilyavailable.Gridconnectioncanoccurinseveralsteps.Longandcomplexconstruction.Purchaseofcomponentssometimestakes2yearsOperationRemoteoperation,littlemaintenances.TechnicalStaffneededontheplantforoperationandmaintenanceWaterusagenoDependontheturbineandthecoolingmethod
Table2ComparisonofPVandCSP②Notmuchdifference:Arearequirement,InvestmentcostsandElectricityProductioncosts.②Lecoufle,D.SolarPACES2009:Berlin,Germany.OutlineIntroductionSolarAirReceiverLiteraturereviewTheR&DofSolarairreceiverinChinaThermalcycletestPressuredropInterfacialheattransferExperimentalStudyofaReceiverAmacroscopicmodelConclusion/OutlookAirConcentratedSolarRadiationTsTfTNREL,ETH,DLR,CNRS,WIS……2.1LiteraturereviewProjectYearPowerAbsorberMaterialOutlettemperatureEfficiencySulzerBros.Ltd1987200KWmetallicwirepack550°C65~70%PHOEBUS-TSA1987~2.5MWWiremeshes700°CSulzerBros.Ltd1989Stainlesssteelwiremesh600°C75~85%SandiaNationalLaboratories1990Ceramicfoam700°C60~75%REFOS-SOLGATE1997350KWCeramicfoam800°C75%Solair2000~SiC-honeycombs1000°CJülichTower20081.5MWSiC-honeycombs680°C85%Table3Theairreceiverprototypesintheworld
OutlineIntroductionSolarAirReceiverLiteraturereviewTheR&DofSolarairreceiverinChinaThermalcycletestPressuredropInterfacialheattransferExperimentalStudyofaReceiverAmacroscopicmodelConclusion/OutlookAirConcentratedSolarRadiationTsTfTConcentratedsolarradiationε~0.7-0.85d~1mmT、P、V……Developamodel:Topredictthepressure,temperatureandvelocitydistributionintheabsorber2.2TheR&DofSolarairreceiverinChinaOurworksWorkThermalcycleConvectiveheattransferPressuredropExperimentCFDExperiment&CFDMethodThemaintools:SolarFurnace(Odeillo,France),FLUENTPredictiveModelObjectiveSolarairreceiverExperimentOpticalpropertiesAnti-oxidizationThermo-mechanicalproperties2types:
with/withoutanti-oxidizationcoating2
Tmax:
1250℃,1350℃2.2.1ThermalcycletestWithanti-oxidizationcoatingWithoutanti-oxidizationcoatingThermalcycletimeAbsorptivity“Absorptivity”VS“Thermalcycletime”Result:absorptivity1250℃Withoutanti-oxidizationcoating1350℃With/Withoutanti-oxidizationcoatingResult:SEMTherearemanycorrelationsinliterature:Ergun(1949),DuPlessis(1994),Macdonald(1999),Moreira,2004……Darcylaw:(Re<10)ModifiedDarcylaw:(Re>10)Testrig:2.2.2PressuredropTheproposedmodelComparisonwith:experimentalresultAndothercorrelationsParametricstudy:d,ε,uTsTfThermalNon-equilibrium1.Solarirradianceonsolidsurface(radiationtoheat)Air△T2.Convectiveheattransfer(heatfromsolidtofluid)Ofcourse:2equationsmodelSolarFlux2.2.3InterfacialheattransferInterfacialheattransfercoefficient:Parametricstudy:d,ε,uResultanddiscussionW/(m2K)W/(m2K)W/(m2K)Alltherelationshipsarenon-linear!空气Objective:Thetemperaturedistributionoftheabsorber,anditsinfluencingfactorsThethermalefficiencyofthereceiveranditsinfluencingfactorsPorosity:0.7,0.8Meancellsize:1~2mmThick:25mm,50mm2.2.4ExperimentalStudyofaReceiverTestrigTemperature:frontsurfaceTemperaturehistory6Result:overallefficiencymomentumLTE
LNTEEnergyThreemethods:a、LTE:Rosseland
modelb、LTNE:Rosseland
modelc、LTNE:P1
modelContinuity2.2.5AmacroscopicmodelcouplefluidsolidClosuremodelEffectiveconductivitytensorPorescaleLocalscaleorREVvolueaveragingSolvingtomacroscopicscale:fictivezoneAvg:microscopicscale:dispersedzoneGoverningequationsLTE/LTNERosseland/P1Non-uniformheatfluxUniformheatfluxModelcomparisonOutlineIntroductionSolarAirReceiverLiteraturereviewTheR&DofSolarairreceiverinChinaThermalcycletestPressuredropInterfacialheattransferExperimentalStudyofaReceiverAmacroscopicmodelConclusi
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