Exploring the Interaction of Cosmic Rays with Water by Using an Old-Style Detector and Rossi’s Method

Marco Arcani, D. Liguori, Andrea Grana
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Abstract

Cosmic ray air showers are a phenomenon that can be observed on Earth when high-energy particles from outer space collide with the Earth’s atmosphere. These energetic particles in space are called primary cosmic rays and consist mainly of protons (about 89%), along with nuclei of helium (10%) and heavier nuclei (1%). Particles resulting from interactions in the atmosphere are called secondary cosmic rays. The composition of air showers in the atmosphere can include several high-energy particles such as mesons, electrons, muons, photons, and others, depending on the energy and type of the primary cosmic ray. Other than air, primary cosmic rays can also produce showers of particles when they interact with any type of matter; for instance, particle showers are also produced within the soil of planets without an atmosphere. In the same way, secondary cosmic particles can start showers of tertiary particles in any substance. In the 1930s, Bruno Rossi conducted an experiment to measure the energy loss of secondary cosmic rays passing through thin metal sheets. Surprisingly, he observed that as the thickness of the metal sheets increased, the number of particles emerging from the metal also increased. However, by adding more metal sheets, the number of particles eventually decreased. This was consistent with the expectation that cosmic rays were interacting with the atoms in the metals and losing energy to produce multiple secondary particles. In this paper, we describe a new–old approach for measuring particle showers in water using a cosmic ray telescope and Rossi’s method. Our instrument consists of four Geiger–Müller tubes (GMT) arranged to detect muons and particle showers. GMT sensors are highly sensitive devices capable of detecting electrons and gamma rays with energies ranging from a few tens of keV up to several tens of MeV. Since Rossi studied the effects caused by cosmic rays as they pass through metals, we wondered if the same process could also happen in water. We present results from a series of experiments conducted with this instrument, demonstrating its ability to detect and measure particle showers produced by the interaction of cosmic rays in water with good confidence. To the best of our knowledge, this experiment has never been conducted before. Our approach offers a low-cost and easy-to-use alternative to more sophisticated cosmic ray detectors, making it accessible to a wider range of researchers and students.
用老式探测器和罗西方法探索宇宙射线与水的相互作用
宇宙射线空气阵雨是一种可以在地球上观察到的现象,当来自外太空的高能粒子与地球大气层相撞时。这些太空中的高能粒子被称为初级宇宙射线,主要由质子(约89%)、氦核(10%)和更重的核(1%)组成。大气中相互作用产生的粒子被称为次级宇宙射线。大气中空气阵雨的组成可以包括几种高能粒子,如介子、电子、介子、光子等,这取决于主要宇宙射线的能量和类型。除了空气之外,初级宇宙射线在与任何类型的物质相互作用时也会产生粒子雨;例如,粒子阵雨也会在没有大气层的行星的土壤中产生。以同样的方式,次级宇宙粒子可以在任何物质中引发三级粒子的阵雨。20世纪30年代,布鲁诺·罗西进行了一项实验,测量二次宇宙射线穿过薄金属片时的能量损失。令人惊讶的是,他观察到随着金属片厚度的增加,金属中出现的颗粒数量也增加了。然而,通过添加更多的金属薄片,颗粒的数量最终会减少。这与宇宙射线与金属中的原子相互作用并失去能量以产生多个次级粒子的预期是一致的。在本文中,我们描述了一种利用宇宙射线望远镜和罗西方法测量水中粒子雨的新-旧方法。我们的仪器由四个盖格-迈勒管(GMT)组成,用来探测μ子和粒子阵雨。GMT传感器是高度敏感的设备,能够探测能量从几十keV到几十MeV的电子和伽马射线。由于罗西研究了宇宙射线穿过金属时所引起的影响,我们想知道同样的过程是否也会发生在水中。我们展示了用该仪器进行的一系列实验的结果,证明了它能够很有信心地探测和测量由宇宙射线在水中相互作用产生的粒子阵雨。据我们所知,这个实验以前从未进行过。我们的方法为更复杂的宇宙射线探测器提供了一种低成本和易于使用的替代方案,使更广泛的研究人员和学生可以使用它。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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