论文标题
在地下GD掺杂水探测器中,岩石岩石诱导的高能中子的测量
Measurement of Muon-induced High-energy Neutrons from Rock in an Underground Gd-doped Water Detector
论文作者
论文摘要
我们介绍了守望箱检测器中中性捕获率的测量,该捕获器的深度约为390米,在Kimballton Underground研究机构(KURF)中的水等效率(M.W.E.)。 WatchBoy由一个圆柱形2吨水靶组成,掺杂了0.1%Gadolinium,周围环绕着40吨不含水的水隐形盾。我们将结果与预期的相关中子捕获率进行了比较,该中子捕获的相关性中子因高能中子的外部出现在WatchBoy盾牌外部,这是由基于混合Fluka/Geant4的模拟预测的。模拟中使用的入射中子能量分布通过快速中子光谱仪,1.8吨的多重性和后坐力光谱仪(MARS)检测器在相同的深度测量。我们发现,测得的两个相关中子的检测率与模拟预测的检测率一致。该结果对火星使用的检测技术以及在三个不同深度测量的火星光谱中提供了更多信心。快速中子通量和频谱的确认很重要,因为它有助于验证用于预测不同上流膨胀的快速中子通量的缩放模型。
We present a measurement of the rate of correlated neutron captures in the WATCHBOY detector, deployed at a depth of approximately 390 meters water equivalent (m.w.e.) in the Kimballton Underground Research Facility (KURF). WATCHBOY consists of a cylindrical 2 ton water target doped with 0.1% gadolinium, surrounded by a 40 ton undoped water hermetic shield. We present a comparison of our results with the expected rate of correlated neutron captures arising from high-energy neutrons incident on the outside of the WATCHBOY shield, predicted by a hybrid FLUKA/GEANT4-based simulation. The incident neutron energy distribution used in the simulation was measured by a fast neutron spectrometer, the 1.8-ton Multiplicity and Recoil Spectrometer (MARS) detector, at the same depth. We find that the measured detection rate of two correlated neutrons is consistent with that predicted by simulation. The result lends additional confidence in the detection technique used by MARS, and therefore in the MARS spectra as measured at three different depths. Confirmation of the fast neutron flux and spectrum is important as it helps validate the scaling models used to predict the fast neutron fluxes at different overburdens.