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Source of luminescence of water lower energy than the Cerenkov-light threshold during irradiation of carbon-ion

机译:碳离子辐照期间水的发光源的能量低于切伦科夫光阈值

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Although luminescence of water during irradiations of proton and carbon-ion lower energy than the Cerenkov-light threshold were found recently, the sources of the luminescence were not yet obvious. To estimate the sources of the luminescence, we measured the light spectrum of the luminescence of water during carbon-ion irradiations and estimated the sources of the luminescence. Using an ultraviolet (UV) light sensitive charge coupled device (CCD) camera, we measured the luminescence images of water during carbon-ion beam irradiations by changing optical filters, derived the light spectra of the luminescence of water and compared with the calculated results. The intensity of the measured light spectrum of the luminescence of water at the Bragg peak region was decreased as the wavelength of light proportional to ~λ~(-2.0) where λ is the wavelength of the light, indicating the source of the luminescence of water can be electromagnetic pulse produced by the dipole displacement inside the water molecules. In the shallow part of the water prior to the Bragg peak, where the Cerenkov-light is included, the spectrum showed steeper curve that is proportional to ~λ~(-2.6), which was similar to the calculated spectrum of Cerenkov-light including the refractive index changes of water with the wavelength of light. From these results, the luminescence of water is thought to be mainly come from electromagnetic pulse produced by the dipole displacement inside the water molecules.
机译:尽管最近发现质子和碳离子辐照期间水的发光低于切伦科夫光阈值,但发光的来源尚不明显。为了估算发光源,我们测量了碳离子辐照期间水的发光光谱,并估算了发光源。我们使用紫外线(UV)光敏电荷耦合器件(CCD)相机,通过更换滤光镜来测量碳离子束辐照期间水的发光图像,得出水的发光光谱,并将其与计算结果进行比较。随着光的波长与〜λ〜(-2.0)成比例,光在布拉格峰区域的测量光谱强度降低,其中λ是光的波长,表明水的发光源可以是水分子内部偶极子位移产生的电磁脉冲。在布拉格峰之前的浅水区(包括切伦科夫光),光谱显示出与〜λ〜(-2.6)成正比的陡峭曲线,与计算出的切伦科夫光光谱相似,包括水的折射率随光的波长而变化。根据这些结果,认为水的发光主要来自水分子内部的偶极位移所产生的电磁脉冲。

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