- 1、本文档共21页,可阅读全部内容。
- 2、原创力文档(book118)网站文档一经付费(服务费),不意味着购买了该文档的版权,仅供个人/单位学习、研究之用,不得用于商业用途,未经授权,严禁复制、发行、汇编、翻译或者网络传播等,侵权必究。
- 3、本站所有内容均由合作方或网友上传,本站不对文档的完整性、权威性及其观点立场正确性做任何保证或承诺!文档内容仅供研究参考,付费前请自行鉴别。如您付费,意味着您自己接受本站规则且自行承担风险,本站不退款、不进行额外附加服务;查看《如何避免下载的几个坑》。如果您已付费下载过本站文档,您可以点击 这里二次下载。
- 4、如文档侵犯商业秘密、侵犯著作权、侵犯人身权等,请点击“版权申诉”(推荐),也可以打举报电话:400-050-0827(电话支持时间:9:00-18:30)。
查看更多
energyspectrumofprimarycosmicraysintheenergyregion(21页)
The Cosmic Ray Spectrum at Ultrahigh Energies
M.I. Pravdin for Yakutsk Collaboration
Yu.G. Shafer Institute of Cosmophysical Research and Aeronomy, 31 Lenin Ave., 678980 Yakutsk, Russia
Estimation of EAS Energy by a Calorimetric Method
M.I. Pravdin for Yakutsk Collaboration
Yu.G. Shafer Institute of Cosmophysical Research and Aeronomy, 31 Lenin Ave., 678980 Yakutsk, Russia
A plan of the location of detector stations of the Yakutsk EAS Array
Station of Yakutsk EAS Array
The diagram of the trigger of the Yakutsk EAS array
Each trigger station has 2 scintillator detectors (Sdet=2 m2). The coincidences within a resolving time 2.0 - 2.2 μs is required. EAS is selected when an event is registered simultaneously by three neighboring stations forming a triangle. Resolving time in this case equals 40 μs
Red triangles - trigger-500 (now - 63 cells, SII=7.2 km2; up to 1992 - 19 cells SI =2.5 km2)
Blue ones - trigger-1000 (now - 24 cells, SII = 10.5 km2)
Green circle - 10 stations of the trigger-1000, working from 1973 up to 1990 (24 + 16=40 cells, SI = 17.3 км2)
Estimation of shower energy E0The calorimetric method
The relation between parameters S300 or S600 and primary particle energy E0 for EAS close to the vertical has been determined by the calorimetric method. For the average showers with different S300 or S600 E0 is estimated as the sum separate a components:
E0 = Ei + Eel + Eμ+ Eμi + Eν + Eh
Ei = k(( is the energy lost by a shower over the observation level. It is estimated by measurements of total Cerenkov light flux (, and k = 2.16(104 / (0.37 + 1.1((Xm /1000)
in the interval of light waves 300-800 nm, In view of mean atmospheric transmittance.
Eel = 2.2(106(Ns((N is the energy conveyed below the array level. It is estimated by the attenuation length (N of the number of charged particles Ns through the atmosphere depth;
E( = (((N( is the energy of the muon component. It is estima
您可能关注的文档
- earthmagneticfield-thefloridastateuniversityhigh(6页).doc
- earthquakefocalmechanisms-serc(6页).doc
- earthscience100-collegeofdupage-home(17页).doc
- earthscience110introductiontogeology(6页).doc
- earthsciencedataandinformationsystemproject,code423(30页).doc
- earthsciencelecturechapter3(12页).doc
- earthscience–quiz2(8页).doc
- earthscienceregents-tomsriverregionalschools(8页).doc
- earthscience-valleycentralschooldistrictoverview(10页).doc
- earthsystemsscience-fortlewiscollege(7页).doc
文档评论(0)