Giammanco S, Immè G, Mangano G, Morelli D, Neri M
Istituto Nazionale di Geofisica e Vulcanologia, Sezione di Catania, Piazza Roma, 2, 95123 Catania, Italy.
Appl Radiat Isot. 2009 Jan;67(1):178-85. doi: 10.1016/j.apradiso.2008.09.007. Epub 2008 Sep 26.
Three different methodologies were used to measure Radon ((222)Rn) in soil, based on both passive and active detection system. The first technique consisted of solid-state nuclear track detectors (SSNTD), CR-39 type, and allowed integrated measurements. The second one consisted of a portable device for short time measurements. The last consisted of a continuous measurement device for extended monitoring, placed in selected sites. Soil (222)Rn activity was measured together with soil Thoron ((220)Rn) and soil carbon dioxide (CO(2)) efflux, and it was compared with the content of radionuclides in the rocks. Two different soil-gas horizontal transects were investigated across the Pernicana fault system (NE flank of Mount Etna), from November 2006 to April 2007. The results obtained with the three methodologies are in a general agreement with each other and reflect the tectonic settings of the investigated study area. The lowest (222)Rn values were recorded just on the fault plane, and relatively higher values were recorded a few tens of meters from the fault axis on both of its sides. This pattern could be explained as a dilution effect resulting from high rates of soil CO(2) efflux. Time variations of (222)Rn activity were mostly linked to atmospheric influences, whereas no significant correlation with the volcanic activity was observed. In order to further investigate regional radon distributions, spot measurements were made to identify sites having high Rn emissions that could subsequently be monitored for temporal radon variations. SSNTD measurements allow for extended-duration monitoring of a relatively large number of sites, although with some loss of temporal resolution due to their long integration time. Continuous monitoring probes are optimal for detailed time monitoring, but because of their expense, they can best be used to complement the information acquired with SSNTD in a network of monitored sites.
基于被动和主动探测系统,使用了三种不同的方法来测量土壤中的氡((222)Rn)。第一种技术由CR - 39型固态核径迹探测器(SSNTD)组成,可进行积分测量。第二种由用于短时间测量的便携式设备组成。最后一种由放置在选定地点用于长期监测的连续测量设备组成。同时测量了土壤(222)Rn活度以及土壤钍射气((220)Rn)和土壤二氧化碳(CO₂)通量,并将其与岩石中的放射性核素含量进行了比较。2006年11月至2007年4月期间,在佩尔尼卡纳断裂系统(埃特纳火山北翼)上调查了两条不同的土壤气体水平剖面。用这三种方法得到的结果总体上相互一致,反映了所研究区域的构造背景。最低的(222)Rn值恰好记录在断层面上,而在断层轴两侧距其几十米处记录到相对较高的值。这种模式可以解释为由土壤CO₂高通量导致的稀释效应。(222)Rn活度的时间变化主要与大气影响有关,而未观察到与火山活动有显著相关性。为了进一步研究区域氡分布,进行了现场测量,以确定具有高氡排放的地点,随后可对其进行氡的时间变化监测。SSNTD测量允许对相对大量的地点进行长时间监测,尽管由于其长积分时间会损失一些时间分辨率。连续监测探头最适合进行详细的时间监测,但由于成本较高,它们最好用于补充在监测站点网络中用SSNTD获取的信息。