什么是$Δm^2_{ee}$?
What is $Δm^2_{ee}$ ?
摘要:
目前的短基线反应堆实验,大亚湾和RENO(双中微子)已经测量(或能够测量)一个有效的$Δm^2$与大气振荡尺度为0.5 km/MeV的电子反中微子消失。在本文中,我比较和对比这样一个有效的$Δm^2$的不同定义,并认为,简单的,L/E独立的,定义由$Δm^2_{ee} \equiv \cos^2 θ_{12} Δm^2_{31}+ \sin^2 θ_{12} Δm^2_{32}$,即“的$ν_e$加权平均值的$Δm^2_{31}$和$Δm^2_{32}$”,是优于所有其他定义,是有用的短基线实验上述和未来的中基线实验JUNO和RENO 50。
英文摘要:
The current short baseline reactor experiments, Daya Bay and RENO (Double Chooz) have measured (or are capable of measuring) an effective $Δm^2$ associated with the atmospheric oscillation scale of 0.5 km/MeV in electron anti-neutrino disappearance. In this paper, I compare and contrast the different definitions of such an effective $Δm^2$ and argue that the simple, L/E independent, definition given by $Δm^2_{ee} \equiv \cos^2 θ_{12} Δm^2_{31}+ \sin^2 θ_{12} Δm^2_{32}$, i.e. "the $ν_e$ weighted average of $Δm^2_{31}$ and $Δm^2_{32}$," is superior to all other definitions and is useful for both short baseline experiments mentioned above and for the future medium baseline experiments JUNO and RENO 50.
机构、总结、中文摘要均由AI分析而来,可能存在错误,请以论文正文为准。