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Time distribution of neutron burst in thermal D/soiled system

机译：热D /土壤系统中中子爆发的时间分布

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The anomalous nuclear reaction from the thermal cycle experiment of metal-absorbed deuterium in pressurized deuterium has been studied by some investigators. The neutron burst signal from this kind of experiments using the high level neutron coincidence counter (HLNCC) device has been measured under the stringent temperature and humidity conditions in our lab last years. Most experiments have been conducted by us under DC-power condition, and some were carried out at deep-mine (500 m) location at Mentou Valley in Beijing. The results of these measurements show that the neutron burst signals have been observed with a good repeatability, one of which is shown in fig. 1. To clarify the nature of this phenomenon, we modified our device into a system formeasuring time distribution of the signal to measure the die-away time of the neutron burst in HLNCC in 1992. During the 3-month measurement, the information about anomalous nuclear reaction of metal (Ti)-absorbed deuterium in pressurized deuterium gashas been obtained, which shows that they are some real neutron pulse signals originating from the anomalous nuclear reaction in thermal cycling of D/Ti system.
机译：一些研究人员已经研究了加压氘中金属吸收氘的热循环实验中的异常核反应。去年，在我们实验室严格的温度和湿度条件下，使用高能中子符合计数器（HLNCC）装置进行的此类实验产生的中子爆裂信号已被测量。我们进行的大多数实验都是在直流电源条件下进行的，其中一些实验是在北京门头谷深矿（500 m）位置进行的。这些测量的结果表明已经观察到中子猝发信号具有良好的可重复性，图1示出了其中之一。 1.为了弄清这种现象的性质，我们将设备修改为用于测量信号时间分布的系统，以测量1992年HLNCC中子爆发的消失时间。在3个月的测量中，有关异常的信息获得了加压氘气中金属（Ti）吸收氘的核反应，表明它们是一些真实的中子脉冲信号，源于D / Ti系统热循环中的异常核反应。

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