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期中考试提纲(Midtermexaminationoutline)
A:anelectronicpaymentcardthathassomeoral1ofthe
functionsofconsumption,transfer,settlement,accesstocash,
credit,etc.
B,hastheadvantagesofcreditcardscansetdeposits,
withdrawals,consumptionandsettlement,thequeryasawhole,
canreducetheuseofcash,simplifythecollectionprocedures,
convenientshopping,enhanceconsumersafety,bring
conveniencetothecardholder.
C,inwhichabankcreditcardisacreditcardissuedbya
commercialbanktoawellplacedcustomer.
(2)cheque:
Isthepaymentvoucherdeposit,thedrawerisentrustedtobanks
andotherfinancialinstitutionstoseetheticketto
unconditionallypayacertainsumofmoneytothepayeeor
bearer.Chequesaremainlydividedintotwokinds:transfer
checkandcashcheck.
(two)foreignexchangeandexchangerates:
1,foreignexchange:foreignexchangeisexpressedinforeign
currency,usedforinternationalsettlementmeansofpayment.
2,theexchangerate,alsoknownastheexchangerate,isthe
exchangeratebetweenthetwocurrencies.
Standardofjudgingtheexchangerateriseandfall:if100
unitscanbeconvertedintoforeignexchangemorerenminbi,
foreignexchangeraterise,foreigncurrencyappreciation,RMB
exchangeratedecline,thedevaluationoftheRMB;ontheother
hand,viceversa.
3,theimpactofexchangeratechangesontheeconomy:(analysis
oftheprosandconsofcurrencyappreciationanddepreciation)
(1)thecurrencyappreciation,meanthecurrencyamountless,
foreignexchangeeffectsare:Areducedexportsandincreased
importsofforeigninvestment;Bcostincrease;Cleadsto
decliningdomesticproduction,increasedunemployment;D
devaluationoftheirforeignexchangereserves,butis
conducivetorepaythedebt;Eisconducivetotheenterprises
togoout
(2)thedevaluationofthecurrency,foreignexchangecurrency
meansthesamemoreeffectsare:Aincreaseinexportsand
reduceimportsofforeigninvestment;Bcostreduction;Cto
enhancetheinternationalcompetitivenessofdomesticproducts,
domesticconsumptionofDisrelativelycheap,foreigntourists
increased.
4,keepthecurrencystablemeaningandsignificance:tokeep
theoverallpricelevelstableinternalandforeignRMB
exchangeratestability,thestabilityofpeople,slives,the
rapidandhealthydevelopmentofnationaleconomy,the
developmentoftheworld'sfinancialandeconomicstability,
hasimportantsignificance.
Three,establishacorrectviewofmoney
1,fromtheemergenceofview:moneyistheproductoflong-term
developmentofcommodityexchange;
2,fromtheessentialpointofview,moneyisafixedcommodity
thatactsasageneralequivalent;
Fromthefunctionpointofview,moneyhastwobasicfunctions,
namely,thevalueyardstickandthecirculationmethod;
Fromtheimportanceof:inacertainsense,moneyisasymbol
ofwealth,intheprimarystageofsocialism,therestillexists
therelationshipbetweengoodsandcurrency,production,
distribution,exchange,consumptionandothereconomic
activitiescannotdowithoutmoney.
Thesecondlessonischangeableprices
I.factorsaffectingprices
Pricesaredeterminedbyvalueandareinfluencedbysupplyand
demandandothereffects(thatis,pricesareformedbythe
market)
(I)supplyanddemandaffectprices
1.,supplyanddemandaffectprices
(1)causedbypricechangesanddifferencesinclimate,time,
region,production,andevenreligiousbeliefs,customsand
otherculturalfactorsalsoinfluence(indirectfactors);(2)
theeffectsofthesefactorsonthepriceofthegoodsisby
changingtherelationshipbetweensupplyanddemand(direct
factors)toachieve
2.howdoessupplyanddemandaffectprices?
Supplyexceedsdemandandpricesrise.Buyershavetoaccept
higherpricestomeettheirownneeds,theemergenceofthings
todilutethe“phenomenon,whichisthe“seller'smarket."”,
(atypeofmarketinwhichsellersplayaleadingrole;sellers
areinafavorablepositioninmarkettransactions);
Supplyexceedsdemandandpricesdecrease.Thesellerhasto
dealwiththeirsurplusinventoryatalowerprice,andthe
phenomenonof“howvaluableisthegoods“isthebuyer'smarket”
(thatis,atypeofmarketinwhichbuyersplayadominantrole.
Buyersareinafavorablepositioninmarkettransactions)
(two)valuedeterminesprice
1.therelationshipbetweenpriceandvalue
Priceisdeterminedbyvalue,valueisthebasisofprice,price
isthemonetaryperformanceofvalue(otherconditionsremain
unchanged,thegreaterthevalue,thehighertheprice.)
2.theamountofcommodityvalueisdeterminedbythesocially
necessarylabortime
3.laborproductivityanditsrelationtothequantityof
commodityvalue
Thevalueofunitgoodsisinverselyproportionaltosocial
laborproductivity;individuallaborproductivityis
proportionaltothetotalamountofcommodityvalue
4.,thebasiccontentofthelawofvalueandformsofexpression
(1):thebasiccontentofthecommodityvalueisdecidedbythe
socialnecessarylabortimeintheproductionofthecommodity,
thecommodityexchangeinvaluebasedimplementationof
equivalentexchange;(Note:thevalueoflawisabasiclawof
commodityeconomy,commodityeconomyisthelawofvalue)
(2)formofexpression:thepriceisinfluencedbytherelation
ofsupplyanddemand,fluctuatesaroundthevalue
Thepricefluctuatingaroundthevaluewhyisaformoflawof
value(i.e.,whydidnotviolatethelawofvalue,theprinciple
ofequalexchange?Whypricefluctuationsonthevalueofthe
lawofvalueisnotnegative)?
Thepriceandthesupplyanddemandofmutualinfluenceand
mutualrestrictioncausedbypricefluctuations,thepricemay
notriseindefinitely,itcannotbeunlimitedtofall,always
onthebasisofvaluefluctuatesaroundvalue.Fromasingle
exchangeprocess,oftendonotmatchthepriceandvalue,but
fromarelativelylongtime,theaveragepriceofgoodsorthe
valueofthegoodsarevisible,pricefluctuationsonthevalue
ofthelawofvalueisnotnegative,butthemanifestationof
thelawofvalue,andistheonlypossibleform,theaverage
numberofequivalentexchangeexistsincommodityexchangein
manytimes
Two,theimpactofpricechanges
(1)theimpactofpricechangesonpeople'slives
1,pricechangescancausechangesindemand(generally
speaking,otherconditionsremainunchanged)
(1)whenthepriceofacommoditygoesup,peoplebuyitless
(2)whenthepriceofacommodityfalls,peoplebuyitmore
2.Thedemandfordifferentgoodsvariesinresponsetoprice
changes
(1)pricechangeshavelittleinfluenceonthenecessitiesof
life
(2)pricechangeshaveagreatinfluenceonthedemandfor
high-gradedurablegoods
3,theimpactofpricechangesondemand
(1)inthetwoalternativecommodities,acommodityprice
increases,consumerswillreducethedemandforthecommodity,
andwillincreasethedemandforitssubstitutes;andvice
versa.
(2)inacomplementarycommodity,thepriceofacommodityrises,
andtheconsumerwillreducethedemandforthatcommodity,
whilereducingthedemandforitscomplementarygoods;vice
versa.
(nounexplanation:thealternativeisthatiftwocommodities
arethesameorsimilarfunction,canmeetthesameneedsof
consumers,thesetwokindsofgoodsaresubstitutes;
complementarygoodsaretwokindsofgoodsmustbecombined
togetherinordertomeetthepeoplesomeneeds,thesetwo
commoditiesarecomplementarygoods.)
(two)influenceonproductionandmanagement:
1,adjustthescaleofproduction2,improvelaborproductivity
3,andpromoteenterprisestoproducemarketablehigh-quality
products
Third,colorfulconsumption
1,thefactorsaffectingconsumption(themainfactors
affectingconsumption:income,pricesoveralllevel)
Theresidents;incomeisthemainfactoraffectingconsumer
incomeisthebasisandpremiseofconsumption;
Aandotherconditionsremainunchanged,andthemore
disposableincomepeoplehave(thecurrentincome),thegreater
theamountofconsumptionofgoodsandservices.Therefore,in
ordertoimprovethelivingstandardoftheresidents,wemust
maintainsteadyeconomicgrowthandincreasetheincomeofthe
residents.
Bgenerallyspeaking,thehighertheexpectedfuturerevenue
(futureincome),thegreaterthelikelihoodofanticipated
expenditure.
C,thesocialincomegapiscloselyrelatedtotheoveralllevel
ofsocialconsumption.People'sincomegapistoolarge,the
overallconsumptionlevelwillbereduced;onthecontrary,the
incomegapwillreducetheoverallconsumptionlevel.
Thepricelevelisthemainfactoraffectingconsumerprices:
Generallyspeaking,peoplewillreducetheconsumptionofgoods;
pricesfalling,purchasingpowerisgenerallyimproved,will
increasetheconsumptionofgoods.
2,thetypeofconsumption
(1)accordingtodifferentconsumptionobjects,theycanbe
dividedintotangiblegoodsconsumptionandlaborservice
consumption
(2)accordingtothetransactionsindifferentwayscanbe
dividedinto:twomoneygoodsconsumption,consumerloans,
consumerleasing
(3)accordingtothepurposesofconsumption,theyare
subsistencematerialsconsumption,developmentdata
consumptionandenjoymentofmaterialconsumption
Unit1earthintheuniverse
I.Thebasicformsoftheearthmotion:revolutionandrotation
Revolvearoundthecenterofthesun,saxis
ThedirectionfromwesttoEast(NorthPolelookingoverthe
counterclockwise)fromwesttoEast(seeabovetheArctic
counterclockwise,theAntarcticopposite)
Siderealday(23:56,4seconds)oftheyearofaperiodicstar
(365days,6minutes,9minutes,10seconds)
Theaverageangularvelocityoflo/perihelion(earlyJanuary)
(earlyJuly)fastfastaphelionaroundequalto150perhour
(exceptthepoles)
Theaveragespeedofthelineis30km/h,decreasingfromthe
equatortothepoles,theequatoris1670KM\hours,andthe
polesare0
Therelationbetweentherotationoftheearthandrevolution:
(1)theobliquityangle:theequatorialplaneandtheplaneof
theecliptic.It's23o26now
(2)thedirectmotionofthesunbetweentheTropicofcancer
Two:thegeographicalsignificanceoftherotationoftheearth
(1)diurnalalternation;
(2)localtime
(3)objectsmovinghorizontallyalongthesurfaceoftheearth
tendtoshifttotherightinthenorthernhemisphereandto
theleftinthesouthernhemisphere
Three:thegeographicalsignificanceoftherevolutionofthe
earth
(1)thelengthofdayandnightandthechangeofsolaraltitude
atnoon
Changesinthelengthofdayandnight
Insummer,thenorthernhemisphere,
Thelongerthenorth,thelongertheday
Thesuninthehemisphere,northoftheArcticCircleappear
lightphenomenonthehemispherethatdaylong,theequatorial
annualwinter,shortdayandlongnight,thedaytheshorter
northwardequinox,thespringequinoxglobalnorthofthe
ArcticCircleappeardarkequinoxphenomenonofthesouthern
hemisphereandthenorthernhemisphere:onthecontrary
Changeofsolaraltitudeatnoon
Springandautumndays:fromtheequatortothenorth-south
direction,fromthedirectpointofthesuntothenorthand
South
Withthechangeoflatitude,thesummersolsticedatedecreases
from23o26toNanddecreasestothenorthandSouth
Wintersolstice:loweredby23o26StothenorthandSouth
23o26,N,reachesthemaximumonthesummersolsticenorthof
thedirectpoint
Astheseasonchanges,thegreaterthe23o26,S,thegreater
themaximumonthewintersolstice
TherearetwodirecthitsbetweentheTropicofcancerevery
year
Four:illuminationinterpretation
(1)judgethenorthandsouthpoles,usuallyusedforthetop
view,andjudgeasfollows:fromthepointofviewoftheearth's
northpole,therotationoftheearthiscounterclockwise,
clockwisefromthesouthpole;orthedirectionoftheincrease
ofthelongitudeoftheeastlongitude
ThedirectionofthebalTsrotation
(2)determinethesolarterm,dateandsunpointlatitude
Twilightring(orapoleoverandwarp,coincidence)Sunpoint
istheequator,isthespringequinox;twilightlineandcircle
tangenttotheArcticCircle,if
Apolarphenomenonforthenorthernhemispheresummersolstice,
thesunisat23o26,“iftheArcticCircleisthepolarnight
phenomenonforthenorthernhemispherewintersolstice,thesun
is23o26south”
(3)determinetheplaceinthelightofthesun,wherethewarp
is12midday,themiddlepartofthemeridiansurroundedby
twilightlinefor12points,themorninglineandthe
intersectionpointforequatoriallongitude
6point,1ineandtheintersection.With18points,according
toevery150,thetimedifferenceof1hours,everylois4
minutes,thetwofirstcalculatethelongitudedifference
(ipsilateralcontralateralsubtraction,addition),andthen
convertedintotime,accordingtotheprincipleofreduction
ofEastWest,calculatethelocaltime
(4)judgethelengthofdayandnight,andseekthelengthof
day(night)ofaplace,thatis,thelengthoftheday(night)
arconthelatitudecoiloftheearth,andthatthelengthcan
alsobecalculatedbythelongitudeofthecrossingoftheday
(night)arc
(5)todeterminetheheightofthesunatnoonforthefirst
cornerareaandthesunpointlatitudedifference,ifthedemand
andsunpointinthesamehemisphere,thetwolatitude
difference,ifthedemandandthesunarenotinthesame
hemisphere,thetwolatitudesandtwolatitudeby90o-the
differenceisthesolutiontotheheightofthesunatnoon
Five:twilight1inewithwarpandweft
(1)accordingtotheterminatorlineandweftintersected
judgment
Theterminatorlinethroughthenorthandsouthpolescanbe
judgedonthisdayinMarch21storSeptember23rdafter
TheterminatorlineandtangentpoleofNorthandsouth,north
oftheArcticCirclefortheday,candeterminethedaybefore
June22nd,thenorthernhemispheresummersolstice,the
northernhemispheresummer,southernhemispherewinter
TheterminatorlineandtangentpoleofNorthandsouth,north
oftheArcticCircleforthenight,candeterminethedaybefore
December22nd,thenorthernhemisphereisthewintersolstice,
thenorthernhemispherewinter,thesouthernhemispherein
summer
(2)accordingtotheterminatorlineandmeridianintersection
relationjudgmentdaysarelongandthenightsarelong
Calculatethelengthofthedayorthelengthofthenight,for
thelongday,intherangeofthehemisphere,calculatethe
locationofthelatitudeoftheground,fromthemorningline
andweftcoilintersectiontotheintersectionofthefaintline
andtheweftcoil,thespanoflongitudedividedby15,that
is,theland
Ifthedayislong,ifonlyhalfofthehemisphereispainted
onthemap,itshouldbenotedthatthedifferencebetweenthe
longitudeofthedayinthedaytimeand2dividedby15isthe
lengthoftheday
Seven:area,localtimecalculation
Thefirststepistoseekthelongitudedifferencebetweenthe
twoplaces
Thesecondstep:tofindthetimedifference,eachlongitude
differenceof4minutestocount
Thethirdstep:thendeterminethedirectionoftheEastand
West,EastandWest,anduseless.Ifthetimeisgreaterthan
24hours,thenminus24,plus1days,ifthetimeisnegative,
thenadd24hours,minus1ofthedate
Day.
Secondunitatmosphere
I.compositionandverticalstratificationoftheatmosphere
1)thecompositionoftheloweratmosphere:drycleanair
(nitrogen,thebasiccomponentoftheorganism,oxygen,the
basicsubstanceoflifesustainingactivities,carbondioxide,
thebasicrawmaterialofphotosynthesis,ozoneabsorptionof
thesun
Ultravioletray"theumbrellaoflifeonearth"),watervapor
andsolidimpurities(thenecessaryconditionsforChengYun
tocauserain)
2)verticalstratificationoftheatmosphere(Textbook29,page
2.1)
Theinfluenceofhightemperatureandatmosphericmotionon
humanactivities
2000-3000kmofionosphereintheupperatmospherereflects
radiowaves
Stratospheric50-55kmrisewithaltitude,advection,ozone
absorption,ultravioletwarming,andconduciveto
high-altitudeflight
Thelowlatitude:17-18km,10-12km,Zhongwei:latitude:8-9
kmwithincreasingaltitudeanddecreasingconvectionweather
phenomenoniscomplicated,mostcloselyrelatedtohumanbeings
Two:atmosphericthermalaction
(1)theweakeningeffectofsolarradiation
Absorption:selective,watervaporandcarbondioxideabsorb
infraredrays,ozoneabsorbsultravioletlightandabsorbsless
forvisiblelight
Reflection:withoutselectivity,thethickertheclouds,the
strongerthereflex.Duringthecloudysummermonths,the
temperatureisnotveryhigh
Scattering:selective,shortwavelengthvioletlight
scattering,soclearskyisblue
(2)theinsulationeffectontheground
Theatmosphericabsorptionofthelongwaveradiationofthe
ground,whiletrappingtheheatandincreasingthetemperature,
becausetheabsorptioncapacityoftheatmosphereforsolar
shortwaveradiationisrelativelypoor,buttheabsorptionof
thelongwaveradiationonthegroundisstrong,sotheground
radiation
Mostareabsorbedbytheatmosphere
Theatmosphericreverseradiationisakindofatmospheric
radiation,whichisdirectedtowardthegroundandcompensates
fortheheatoftheground
Two:atmosphericthermalconditions
Thethermalactionoftheatmosphere
1)thermodynamiccirculation:aircirculationcausedbyuneven
groundtemperatureisoneofthesimplestformsofatmospheric
motion.
Itcanbeseenfromthefigure,nearthegroundtothedirection
oflowpressureisobar(down)bending,highpressuredirection
totheisobars(up)raised
2)horizontalmovementoftheatmosphere-wind
Impact:theisobarmoreintensiveplace,thenthehigherthe
wind(Figure2.10,2.11,2.12)
Intheroleofasinglehorizontalpressuregradientforceunder
theverticaldirection:isobar,pointingtolowpressure
TheCoriolisforceonthehorizontalpressuregradientforce
andunderthewinddirectionandparalleltotheisobars
Intheroleofthreeforces:thewinddirectionandtheisobars
formanincludedangle,alwaystowardthelowerpressurebyhigh
pressuredirection.
Three:GlobalAtmosphericCirculation
1)threecirclesofcirculation(Textbook37,2.14)
Theformationofthesevenzonesandsixwindpressureonthe
surfaceoftheearth,windzonewithsunpointmovingnorthand
Southandthenorthandthesouth,inthenorthernhemisphere,
thesummertothenorth,thelocationofthenorthtotheSouth;
inwinter,a
SetasideSouth(Figure2.15)
Theinfluenceoflandseadistributiononatmospheric
circulation
(3)monsooncirculation(Figure2.18)
RegionEastAsia,SouthAsia,SoutheastAsia
Climatetype,temperatemonsoonclimate,subtropicalmonsoon
climate,tropicalmonsoonclimate
Thedifferenceoflandseathermalpropertiesofsea-land
thermodynamicproperties,theseasonalmovementofatmospheric
pressureandwind
Winddirection;winternorthwestwind(Asiancontinent);
northeastwind(mainlandAsia)
Thesummerwind(Pacificsouthwestwind)(Indiaocean)
First,thepoliticalsystemofXia,ShangandWesternZhou
Dynasty
1,thecontentofthepoliticalsystemofXiaandShang
dynasties:
Central:
The1generationofShanrangsystemwithhereditary
preparation;
2participateinthedecision-makingphase,QingShi,
responsibleforsacrificeanddivinationandrecordingevents,
buZhu,Dynastyhistory,inchargeofthemilitarydivision.
Where:HouBo?
InfluenceofXiaandShangpoliticalsystem:earlypolitical
systemofXiaandShang,hasadirectimpactontheWesternZhou
Dynastypatriarchalandfeudalsystem.
2,theWesternZhouDynastyenfeoffs:
The1wasavassalstateofthedutyofguardingtheterritory,
afteroperation,paytribute,piIgrimageduty
2influence:
Positiveinfluence:strengthenedthereignoftheemperorof
Zhoutothelocal;formedthestarsoftheZhouDynasty
Thepoliticalstructureofthemonth
Negativeinfluence:theweaknessofkingshipinthelater
periodofWesternZhouDynasty,thedisputesinthesummer,the
springandAutumnperiodandtheWarringStatesPeriod
Results:3inthelateWesternZhouDynastyfeudalsystemwas
damaged;thelateWarringStatesperiodZhouroyalpowerlost
packet
3.ThelegalsystemoftheWesternZhoudynasty:
1content:withthepaternalkinshiprelationshiptomaintain
thepoliticallevel,theconsolidationofnationalpolitical
system.
The2characteristic:theeldestsonsuccessionsystem
3,influence:toensurethemonopolyandprivilegedstatusof
thearistocracy,tohelpthestabilityandunitywithinthe
rulinggroup.
Thesecondlessonistheformationofthecentralizedsystem
ofQinDynasty
1,theformationofthecentralizedsystem:
Features:onebeingthesupremeimperialpower;hereditary
throne;
Evaluation:theestablishmentofthecentralizedsystemof
feudaldespotism.Formtheformofcentralverticalmanagement,
andbureaucraticpoliticsisanimportantsymbolof
aristocraticpolitics.
2,thebasiccharacteristicsofcentralizedpower:high
concentrationofpower
3,theroleandinfluenceofcentralizedsystem:
Positiveeffect:
1,strengthenQin'sstrength,expandtheterritorythroughwar,
formthefirstunifiedmulti-ethnicfeudalcountryinChinese
historyandbecometheworldpoweratthattime.
2,enabletheQinDynastytoimplementallkindsofmeasures
toconsolidateandunifythecountry.
3,thebasicstructureofthefeudalsocialandpoliticalsystem
inChinaoverthepasttwothousandyearshasbeenlaidoutfor
thefeudaldynastiesofthepastdynasties,andhasbeen
constantlystrengthenedandperfected.
Negativeeffect:relyingontheemperor,sautocraticauthority
tostrengthentheoppressionofthepeople,resultinginrapid
intensificationofclasscontradictions.
Thethirdlesson:theevolutionofthepoliticalsystemfrom
Hantoyuan
1,theevolutionofthecentralpoliticalsystem:
HanDynasty,HanDynasty,Qinsystem
Changethecentralset(threephase,yushidaf
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