Cave radon exposure, dose, dynamics and mitigation

IF 0.5 4区 地球科学 Q4 GEOSCIENCES, MULTIDISCIPLINARY
C. Waring, S. Hankin, S. Solomon, Stephen Long, A. Yule, Robert Blackley, S. Werczynski, A. Baker
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引用次数: 1

Abstract

Many caves around the world have very high concentrations of naturally occurring 222Rn that may vary dramatically with seasonal and diurnal patterns. For most caves with a variable seasonal or diurnal pattern, 222Rn concentration is driven by bi-directional convective ventilation, which responds to external temperature contrast with cave temperature. Cavers and cave workers exposed to high 222Rn have an increased risk of contracting lung cancer. The International Commission on Radiological Protection (ICRP) has re-evaluated its estimates of lung cancer risk from inhalation of radon progeny (ICRP 115) and for cave workers the risk may now (ICRP 137) be 4–6 times higher than previously recognized. Cave Guides working underground in caves with annual average 222Rn activity  1,000 Bq m3 and default ICRP assumptions (2,000 workplace hours per year, equilibrium factor F  0.4, dose conversion factor DCF  14 μSv (kBq h m3)1 could now receive a dose of  20 mSv y1. Using multiple gas tracers (dCCO2, Rn and N2O), linked weather, source gas flux chambers, and convective air flow measurements a previous study unequivocally identified the external soil above Chifley Cave as the source of cave 222Rn. If the source of 222Rn is external to the cave, a strategy to lower cave 222Rn by passively decreasing summer pattern convective ventilation, which draws 222Rn into caves, is possible without harming the cave environment. A small net annual average temperature difference (warmer cave air) due to geothermal heat flux produces a large net annual volumetric air flow bias (2–5:1) favoring a winter ventilation pattern that flushes Rn from caves with ambient air. Rapid anthropogenic climate change over decades may heat the average annual external temperature relative to the cave temperature that is stabilized by the thermal inertia of the large rock mass. Relative external temperature increases due to climate change (Jenolan Caves, 2008–2018, 0.17°C) reduces the winter pattern air flow bias and increases Rn concentration in caves.
洞穴氡暴露、剂量、动态和缓解
世界上许多洞穴都有非常高浓度的自然产生的222Rn,它可能随着季节和昼夜模式而发生巨大变化。对于大多数具有不同季节或日变化模式的洞穴,222Rn浓度受双向对流通风驱动,其响应外部温度与洞穴温度的对比。暴露在高222Rn环境中的洞穴探险者和洞穴工人患肺癌的风险增加。国际放射防护委员会(ICRP)重新评估了吸入氡子体的肺癌风险(ICRP 115),对于洞穴工人来说,现在的风险(ICRP 137)可能比以前认识到的高4-6倍。在年平均活度为222Rn的洞穴中工作的洞穴导游可以接受到的剂量为:年均工作时间为222Rn的工作时间为:年均工作时间为:222Rn;年均工作时间为:222Rn;年均活动时间为:222Rn;年均活动时间为:222Rn;年均活动时间为:1000bq m;先前的一项研究使用多种气体示踪剂(dC - CO2, Rn和N2O),联系天气,源气体通量室和对流气流测量,明确地确定Chifley洞穴上方的外部土壤是洞穴222Rn的来源。如果222Rn的来源是洞穴外部,那么在不损害洞穴环境的情况下,可以通过被动减少夏季模式对流通风来降低洞穴222Rn。由于地热热通量造成的年平均净温差较小(洞穴空气变暖),产生了较大的年净体积气流偏差(2-5:1),有利于冬季通风模式,即利用环境空气将Rn从洞穴中冲走。相对于由大岩体的热惯性稳定的洞穴温度,几十年来快速的人为气候变化可能使年平均外部温度升高。气候变化导致的相对外部温度升高(Jenolan Caves, 2008-2018, 0.17°C)减少了冬季气流偏置,增加了洞穴中的Rn浓度。
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来源期刊
Journal of Cave and Karst Studies
Journal of Cave and Karst Studies 地学-地球科学综合
CiteScore
1.90
自引率
0.00%
发文量
6
审稿时长
>12 weeks
期刊介绍: The Journal of Cave and Karst Studies is a multidisciplinary journal devoted to cave and karst research. The Journal is seeking original, unpublished manuscripts concerning the scientific study of caves or other karst features. Authors do not need to be members of the National Speleological Society, but preference is given to manuscripts of importance to North American speleology.
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