arXivDaily arXiv每日学术速递 周一至周五更新
北美退伍军人节(Veterans Day),12 日无更新
arXiv 2007.07371hep-exphysics.ins-det
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Borexino首次探测到来自CNO循环的太阳中微子

On first detection of solar neutrinos from CNO cycle with Borexino

L. B. Bezrukov, I. S. Karpikov, A. S. Kurlovich, A. K. Mezhokh, S. V. Silaeva, V. V. Sinev, V. P. Zavarzina

摘要:

Borexino合作报告了在Borexino探测器中首次测量太阳CNO- $ν$相互作用速率。这一结果与氢化地球模型预测的单个Borexino事件中$^{40}$ K地球反中微子相互作用的贡献是一致的。在地球质量的$1 ÷1.5$ \%范围内的地球中的钾丰度可以给出观察到的计数率的增强,其高于预期的CNO- $ν$计数率。地球的固有热通量必须在$200 ÷300$ TW的范围内,才能获得这种钾丰度。热通量的这一数值可以解释实时地转海洋学阵列项目观测到的海洋加热现象。我们认为氢化地球模型比硅酸盐地球模型更符合CNO- $ν$ Borexino结果。

英文摘要:

Borexino collaboration reported about first measurement of solar CNO-$ν$ interaction rate in Borexino detector. This result is consistent with Hydridic Earth model prediction about the contribution of $^{40}$K geo-antineutrino interactions in single Borexino events. The potassium abundance in the Earth in the range $1 ÷1.5$\% of the Earth mass could give the observed enhancement of counting rate above expected CNO-$ν$ counting rate. The Earth intrinsic heat flux must be in the range $200 ÷300$ TW for this potassium abundance. This value of the heat flux can explain the ocean heating observed by the project ARGO. We consider that Hydridic Earth model actually corresponds better to CNO-$ν$ Borexino results than Silicate Earth model.

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。

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