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The ARGO-YBJ experiment in Tibet

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The ARGO-YBJ experiment in Tibet(  ) A.Aloisio( 1 ),C.Ba i( 2 ),K. Z. Bao( 3 ),F. Barone( 4 ),B. Bartoli( 5 ) P.Bernardini( 6 ), C.Bleve( 6 ), P.Bran hini( 2 ),S. Bussino( 2 ),E.Calloni( 5 ) P.Camarri( 7 ), B. Y.Cao( 8 ),R. Cardarelli( 7 ),M. Casolino( 7 ) S.Catalanotti( 5 ),A.Cavaliere( 7 ),S.Cavaliere( 5 ),F.Cesaroni( 6 ),M.Cha( 9 ) P.Creti( 6 ),G. Cusimano( 10 ), G.D'Al  i Staiti( 10 ), Danzengluobu( 11 ) V.D'Elia( 7 ),I.De Mitri( 6 ),B. D'EttorrePiazzoli( 5 ), M.DeVin enzi( 2 ) T.Di Girolamo( 5 ),G.Di S ias io( 5 ),Z.Y. Feng( 12 ),Y. Fu( 8 ),X. Y. Gao( 13 ) Q. X.Geng( 13 ),H.W. Guo( 11 ), H.H. He( 9 ),Q. Huang( 12 ),M.Ia ova i( 5 ) N.Iu i( 2 ),H. Y. Jai( 12 ), F. M.Kong( 8 ),H. H.Kuang( 9 ), Laba iren( 11 ) B. Li( 3 ),J. Y. Li( 8 ),B. Liberti( 7 ),G.Liguori( 14 ),Z. Q. Liu( 13 ),H. Lu( 9 ) X.H.Ma( 9 ),G.Man arella( 6 ),S.M.Mari( 2 ),G.Marsella( 6 ),D.Martello( 6 ) X.R. Meng( 11 ),L. Milano( 5 ),T. Mineo( 10 ), J. Mu( 13 ),L. Ni astro( 10 ) D. Orlando( 6 ),M.Panareo( 6 ),A.Paoloni( 7 ),Z. R.Peng( 9 ),P.Pistilli( 2 ) G.Raso( 10 ),B. Sa o( 10 ),L. Saggese( 5 ),R.Santoni o( 7 ),L.S arsi( 10 ) P.R. Shen( 9 ),C.Stanes u( 2 ), M.Storini( 2 ),L. R.Sun( 3 ),S. C.Sun( 3 ) A.Surdo( 6 ),Y.H.Tan( 9 ),P.Vallania( 15 )(  ),S.Vernetto( 15 ),C.R. Wang( 8 ) H.Wang( 9 ),H.Y. Wang( 9 ),Y. N. Wei( 3 ), Q. K. Yao( 3 ),G.C.Yu( 12 ) X.D. Yue( 3 ), A.F. Yuan( 11 ), H.M.Zhang( 9 ),J. L. Zhang( 9 ), N.J. Zhang( 8 ) T.J. Zhang( 13 ), X.Y. Zhang( 8 ), Zhaxisangzhu( 11 ),Zhaxi iren( 11 ) andQ. Q. Zhu( 9 ) ( 1

) INFNSezionediNapoliandUniversitadelSannio-Benevento, Italy

( 2

) INFNandDipartimento diFisi adell'Universita\RomaTre"-Roma,Italy

( 3

) Zhenghou University-Henan, China

( 4

) INFNSezionediNapoliandDipartimentodi S ienzeFarma euti hedell'Universita

Salerno, Italy

( 5

) INFNandDipartimento diFisi adell'Universita-Napoli,Italy

( 6

) INFNandDipartimento diFisi adell'Universita-Le e,Italy

( 7

) INFNandDipartimento diFisi adell'Universita\TorVergata" -Roma,Italy

( 8

) ShandongUniversity-Jinan,China

( 9

) IHEP -Beijing,China

( 10

) INFNSezione diCataniaandIstituto diFisi aCosmi aIFCAI/CNR-Palermo,Italy

( 11

) TibetUniversity-Lhasa,China

( 12

) SouthWestJiaotongUniversity-Chengdu,China

( 13

) YunnanUniversity-Kunming,China

( 14

) INFNSezione diPavia-Italy

( 15

) IstitutodiCosmogeo si adelCNRandINFN-Torino,Italy

(ri evutoil4Di embre2000;approvatoil12Febbraio2001)

( 

) Paper presented at the Cha altaya Meeting on Cosmi Ray Physi s, La Paz, Bolivia,

July23-27 ,2000.

(  

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1. {Introdu tion

Thestudyof radiation in theenergy range100GeV{20 TeVis mainlydevotedto

-astronomy,forbothpointanddi usesour es,andgamma-raybursts(GRBs)physi s.

Pointsour esaregala ti andextragala ti obje ts;di usesour esin lude theGala ti

Plane,mole ular loudsandSupernovaRemnants. Atthese energiesthepau ityofthe

uxeshampersthedete tionfromspa e;thehighestenergydete tedtillnowisfewtenth

ofGeVfrom theEGRETexperimentonboardtheCGROsatellite. Sin ethedete tion

oftheCrabNebulain1989bytheWhippleCollaboration[1℄,ground-based -astronomy

has olle tedbrilliantresultsbymeansof 

Cerenkovteles opes;uptonow5gala ti and

3 extragala ti obje ts have been dis overed in the TeV energy region. During these

years this te hnique has been well developed, rea hing a low energy threshold ( 300

GeV,andevenlessforsolarpowerfa ilitiesusedaslight olle tors)andahighsensitivity

forpoint sour es(.1/10 oftheCrab ux,the \standard andle"for TeVastronomy).

Thelimits are the low duty- y le ( 5%), sin e observations an be doneonly during

lear moonless nights, and the small eld of view (# < 4 Æ

). This means that only

one andidate, sele ted sour e at atime an be observed, with no dis overypotential

forunknownsour es. A large eldofviewisevenmore ru ial forGRBsdete tion,the

probabilityof o urren eof theseunpredi tableeventsby han ein the eld ofviewof

a 

Cerenkovteles opebeingnegligible(< 10 4

).

Adi erentapproa hhasbeendoneusingEASarrays,thatsample ontinuouslyand

withalarge eldofview( sr)thelateraldistributionofextensiveairshowers. But

due to thepoor or la king osmi rays ba kgroundreje tion, and to thehigher energy

threshold(E>10TeV),nohighlyreliabledete tionhasbeendonesofar; alowenergy

threshold, parti ularly for extragala ti sour es (AGNs and GRBs), is requireddue to

the -rayabsorptionintheintergala ti spa ebyintera tionwithstarlightphotons.

Fromthese onsiderationswe andedu ethene essityofadete torwithalarge eld

(3)

Fig. 1. {Comparison between the longitudinal development of -indu edshowers of primary

energy100GeV{1000TeVand theshowerre onstru tionthresholdfordi erentte hniquesat

variousheights.

theserequirements,imagingtheele tromagneti omponentofsmallairshowersathigh

altitudewith: highspa e-timeresolution,togetahighgranularitypi tureoftheshower;

full overage,to de rease theenergy threshold withoutlosing showerdetails and large

olle ting area to in rease the sensitivity and the energy range. The ombined e e t

of the full overageand high altitude lo ation on the threshold energy an be seenin

g.1, where the longitudinaldevelopmentof -indu edshowersof di erentenergies is

ompared with the typi al sensitivities of two di erent te hniques lo ated at di erent

altitudes. The threshold energy of a traditional sampling array operating at 2000 m

a.s.l. anbeloweredfrom50 TeV to1TeV usingafull overage arpet andto 

200GeVmovingfrom2000to4000m a.s.l.,withatotalgainfa toras highas250.

WiththesefeaturestheGeV(satellites)andTeV( 

Cerenkovteles opes)energyregions

anbebridgedandtheenergyrangebetween20GeVand300GeV,thatis,forthetime

being, ompletelyunexplored, an beatleastpartlya essed.

2. {The dete tor

The ARGO-YBJ dete tor [2℄ is lo ated in Tibet, China, at the Yangbajing High

Altitude Cosmi Ray Laboratory (30 Æ .11 N, 90 Æ .53 E, 4300 m a.s.l., 606 g/ m 2 ). It

onsistsofasinglelayerofResistivePlateChambers(RPCs)ofdimensions7874m 2

with full overage (a tivesurfa e  92%). Thearea surrounding the entral arpet is

partially( 20%)instrumentedwithRPCsupto11199m 2

,thetotala tivesurfa e

being6700m 2

. As hemati planofthedete torisshownin g.2.

TheRPCsperforman e,in termsoftemporalandspatialresolution, atareasonable

ost makes this devi e an optimum dete tor for large area overing. A layer of 0.5

(4)

Fig.2.{S hemati viewoftheARGO-YBJbuildinganddete tor.

onstru tion,triggeringand dataa quisition,thebasi modulebeinga\ luster". Ea h

luster hasasurfa eof44 m 2

and isbuilt by12RPCs; ea hRPC isread bymeans of

10\logi alpads"6056 m 2

, orrespondingto 8stripsORed. Onepad 0.34m 2

area

orresponds to one pixel, givingthegranularityof thedete tor for timing and parti le

densitymeasurements. Firedstrips oordinates anbere ordedtogiveabetterparti le

lo ation ifneeded. For ea h event thetrigger multipli ity (numberof red pads), the

oordinatesof redpads, theirtiming andthenumberof red strips( orrespondingto

thenumberofdete tedparti les)arere orded. Thetriggerthresholdissettoaminimum

numberof red pads; theexpe ted triggerrate forat least15 pads red (based onthe

measuredpadrateatYBJ400Hz)is 20KHz. Thehugeamountofdatathat has

to be olle ted,analyzed and re ordedrepresentsone of thegreatest hallenge forthis

experiment.

3. {Sensitivity to pointsour es and GRBs

Figure3showstheexpe tedsensitivityoftheARGO-YBJdete torfor1yearof

data-takingand5standarddeviationsstatisti alsigni an e, omparedwiththeCrabNebula

ux. It an beseenthat the expe ted sensitivity isabout1/10the Crab ux overthe

wholeenergyrange100GeV{20TeV.

Theexpe tedsensitivityofARGO-YBJtoGRBsisshownin g.4forSingleParti le

(SP)andLowMultipli ity(LM)te hniques. WithSingleParti lete hniquethe ounting

rateof the dete tor is re ordedat xed time intervals; aburst is dete tedif it givesa

ountingratesigni antlyhigherthantheba kground,withnoinformationonthearrival

dire tion. The Low Multipli ity te hnique onsists in the dete tion of very small air

showersthatareanalyzedandtheirarrivaldire tionisre onstru ted;asigni antex ess

(5)

Fig.3.{Minimum uxfrompointsour esdete tablebyARGO-YBJduring1yearofdatataking

and5s.d. statisti alsigni an e, omparedwiththeCrabNebula ux. Reportedsensitivities

ofotherexperimentsareonlyindi ative.

haveto bedone: apower-law -ray ux dN dE =KE phm 2 upto E max is assumed,

with spe tral slope = 2.0 (the average spe tral slope measured by EGRET in the

30MeV{10GeVregionbeing =1.950.25),timedurationt=1sandstatisti al

signi an e=4s.d.. Moreoveritis onvenienttoexpresstheGRBssensitivityinterms

ofF

min

, i.e. theminimumdete table uen eforaGRB emittingintheenergyrange1

GeV{E

max

withspe tralslope . In g.4the uen eoftheGRBsdete tedbyEGRETis

alsoreported,extrapolatingtheirspe trumupto100GeVwiththeirindividualspe tral

index. It anbeseenthat iftheirspe traextendat leastupto100GeV,mostofthem

ouldbedete tedbyARGO-YBJ.

4. {The ARGO-test atYangbajing

Thetest[5,6℄hasbeen arriedoutin theperiod February-May1998. FifteenRPCs

( orrespondingto about one luster prototype) havebeenput in operation, for atotal

area of 51 m 2

and an a tive area of 46.2 m 2

(91% overage). Di erent gas mixtures

have been tested to hoose the best working onditions due to the low atmospheri

pressure. Data have been olle ted with and without a 0.5 m lead onverter. The

time jitter distribution of pad signals is uniform for all pads with an average s.d. of

1.3 ns; the resulting intrinsi RPC time resolution is  1 ns. The angular resolution,

obtainedbydividingthepadarrayintotwoindependentsub-arrays( hess-boardmethod)

and omparing the twore onstru ted showerdire tions is

#  2

Æ

for eventswith pad

multipli ity100. Thee e t oftheleadlayerismoreimportantatlowmultipli ity,as

expe ted, loweringtheangular resolutionfrom 8 Æ

to5 Æ

forpad multipli ity 35.

Forthe naldete tor,duetoitslargerdimensions,theexpe tedangularresolutionis

(6)

Fig. 4.{Minimum uen efromGRBsobservablebyARGO-YBJas afun tion ofthe ut-o

energyEmax for Single Parti le (SP) and Low Multipli ity (LM) te hniques (see text). The

pointsaretheextrapolationupto100GeVof14EGRETspe tra.

The overall results of the test look well promising for future operation of the full

ARGO-YBJdete tor.

5. {Con lusions

TheARGO-YBJdete torhastheuniquepossibilitytobridgetheGeVandTeVenergy

regions,providingfull omplementarityto severalsatelliteprograms. For the rst time

a  50 m 2

RPCs arpet has been su essfully operated at high altitude, on rming

that RPCs an beused eÆ iently( 95%) to dete t airshowerswith ex ellent time

resolution(1ns).

Theresults of the analysis of data olle tedon-site on rm theeÆ ien y and time

resolutionassumedinthesensitivity omputationforthefulldete tor. Thebuildinghas

been nishedand theinstallationof theRPCsstarted in November2000. Data taking

willstartduring2001witha800m 2

arpet,addressedtoGRBsphysi s.

REFERENCES

[1℄ WeekesT.C.etal.,Astrophys.J.,342(1989) 379.

[2℄ Abbres iaM.etal.,Astroparti lePhysi swithARGO,(1996),andBa i C.etal.,The

ARGO-YBJProje t,(1998).Theseunpublisheddo uments anbedownloadedattheURL:

http://www1.na.infn.it/wsubnu l/ os m/ar go/a rgo.h tml.

[3℄ VernettoS.etal.,Pro .26thICRC(Salt LakeCity),vol.4(1999)p.28.

[4℄ VernettoS.,Astropart.Phys.,13(2000)75.

Figura

Fig. 1. { Comparison between the longitudinal development of 
-indu
ed showers of primary
Fig. 2. { S
hemati
 view of the ARGO-YBJ building and dete
tor.
Fig. 3. { Minimum 
ux from point sour
es dete
table by ARGO-YBJ during 1 year of data taking
Fig. 4. { Minimum 
uen
e from GRBs observable by ARGO-YBJ as a fun
tion of the 
ut-o

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