西萨尔斯卡洞穴(摩拉维亚)环境中空气离子的浓度和迁移

Z. Roubal, Z. Szabó, R. Kadlec, L. Zdražil
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摘要

在本文中,作者讨论了在低电平电荷测量领域中获得的信号的传感和评估。测量是在Cisarska洞穴(摩拉维亚)在特定的温度和湿度条件下进行的。与传统方法相比,该方法具有较低的标准偏差,并分析了产生杂散振荡的原因。该传感方法是通过控制负离子载流子通过的电容式传感传感器进行测量。评估负离子浓度的长期变化。石灰石壁在介电常数和导电性方面具有非常有益的材料特性,对洞穴空间的评价也很重要。维护干净的石灰石表面对于保持洞穴的愈合性能非常重要;石灰石的表面已经用离子进行了详细的测试。维护干净的石灰石表面对于保持洞穴的愈合性能非常重要;石灰石的表面已经用离子进行了详细的测试。低测量不确定度是正确测定饱和特性所必需的。由此计算了空气离子的迁移谱。根据饱和度特征重新计算得到的结果表明,洞穴中空气离子的来源令人惊讶,其中唯一的来源可能不是放射性氡,但破碎水滴的贡献也很重要。如果没有提出的测量方法,这些结果是不可能得到的。
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Concentration and Mobility of Air Ions in the Environment of the Cisarska Cave (Moravia)
In this paper, the authors deal with the sensing and evaluation of signals obtained in the field of low-level electric charge measurements. The measurement took place in the Cisarska cave (Moravia) under specific temperature and humidity conditions for a long time. Compared to conventional techniques, the proposed method shows a lower standard deviation and analyzes the causes of spurious oscillations. The sensing method was based on measurement by a capacitive sensing sensor with controlled passage of negative ion carriers. Long-term changes in negative ion concentration are evaluated. The limestone walls, which have very beneficial material properties in terms of permittivity and electrical conductivity, are also important for the evaluation of the cave space. The maintenance of a clean limestone surface is important in terms of preserving the healing properties of the cave; the surface of the limestone has been tested in detail in terms of ions. The maintenance of a clean limestone surface is important in terms of preserving the healing properties of the cave; the surface of the limestone has been tested in detail in terms of ions. Low measurement uncertainties are necessary for the correct determination of the saturation characteristics. From this, the mobility spectrum of air ions is calculated. The obtained results of the recalculation from the saturation characteristics show the surprising origin of air ions in the cave, where the only source may not be radioactive radon, but the contribution of splintering water droplets is also significant. These results could not have been obtained without the proposed measurement methodology.
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