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SSO及GEO典型太陽質子事件單粒子翻轉率估算

Evaluation of proton-induced upset rate on SSO and GEO for typical solar particle events

  • 摘要: 文章根據NOAA衛(wèi)星和GOES衛(wèi)星的測量數據,對太陽質子事件期間地球同步軌道(GEO)和太陽同步軌道(SSO)的質子輻射情況進行考察。采用Bendel雙參數模型對GEO和SSO由質子引起的器件單粒子翻轉率進行估算,并分析了影響翻轉率的因素。在器件敏感度一定的情況下,單粒子翻轉率與大于能量閾值的質子總通量以及質子能譜硬度呈正相關。SSO與GEO的質子輻射及單粒子翻轉預測對比研究結果表明:由太陽質子事件引起的SSO質子能譜比GEO的要“軟”。太陽質子事件對SSO衛(wèi)星的影響與對GEO衛(wèi)星的影響之間存在相關性。兩軌道上DRAM型的D424100V器件和SRAM型的HM6516器件的翻轉率比值接近,SSO翻轉率約為GEO的13%~22%,而雙極型93L422器件翻轉率比值則在26%~57%之間。通過對比SSO與GEO翻轉率的比值和兩軌道輻射程度的比值發(fā)現,不同的器件對能譜硬度的反應各異,原因是每種器件產生SEU的能量閾值不同。

     

    Abstract: The proton flux measurements during several significant solar proton events (SPEs) by the NOAA and GOES satellites are utilized to compare the proton radiation environments in SSO and GEO. Furthermore, the predictions of the proton-induced SEU in the SPEs are calculated by using the two-parameter Bendel model. Generally speaking, the proton-induced SEU has a positive correlation with the total proton flux and the spectrum hardness. The comparison between the proton radiations in SSO and GEO shows that the proton spectrum in SSO is ‘softer’ than that in GEO. For the low-energy protons, the flux in SSO is greater than that in GEO, while the flux in SSO is less than that in GEO for the higher energy protons. The ratio of the upset rates of D424100V (DRAM) and HM6516 (SRAM) in SSO to that in GEO is about 13% to 22%; and the ratio of the upset rate of 93L422 (bipolar) in SSO to that in GEO is about 26% to 57%. By comparing the proton-induced upset rates with the proton radiation in SSO and GEO, it is discovered that each type of the electronic components is sensitive to the protons with different energies.

     

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