Radon as a natural tracer for underwater cave exploration

被引:10
|
作者
Csondor, Katalin [1 ]
Eross, Anita [1 ]
Horvath, Akos [2 ]
Szieberth, Denes [3 ]
机构
[1] Eotvos Lorand Univ, Inst Geog & Earth Sci, Dept Phys & Appl Geol, Parzmany Peter Setany 1-C, H-1117 Budapest, Hungary
[2] Eotvos Lorand Univ, Inst Phys, Dept Atom Phys, Parzmany Peter Setany 1-A, H-1117 Budapest, Hungary
[3] Budapest Univ Technol & Econ, Dept Inorgan & Analyt Chem, Muegyetem Rakpart 3, H-1111 Budapest, Hungary
关键词
Radon; Hypogenic; Underwater cave; Mixing; Tracer; BUDA THERMAL KARST; GROUNDWATER-FLOW; RADIONUCLIDES; HUNGARY; RN-222; VENTILATION; AQUIFERS; RECHARGE; SYSTEM;
D O I
10.1016/j.jenvrad.2016.10.020
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
The Molnar Janos cave is one of the largest hypogenic caves of the Buda Thermal Karst (Budapest, Hungary) and mainly characterized by water-filled passages. The major outflow point of the waters of the cave system is the Boltiv spring, which feeds the artificial Malom Lake. Previous radon measurements in the cave system and in the spring established the highest radon concentration (71 BqL(-1)) in the springwater. According to previous studies, the origin of radon was identified as iron-hydroxide containing biofilms, which form where there is mixing of cold and thermal waters, and these biofilms efficiently adsorb radium from the thermal water component. Since mixing of waters is responsible for the formation of the cave as well, these iron-hydroxide containing biofilms and the consequent high radon concentrations mark the active cave forming zones. Based on previous radon measurements, it is supposed that the active mixing and cave forming zone has to be close to the spring, since the highest radon concentration was measured there. Therefore radon mapping was carried out with the help of divers in order to get a spatial distribution of radon in the cave passages closest to the spring. Based on our measurements, the highest radon activity concentration (84 BqL(-1)) was found in the springwater. Based on the distribution of radon activity concentrations, direct connection was established between the spring and the Istvan-room of the cave, which was verified by an artificial tracer. However, the distribution of radon in the cave passages shows lower concentrations (18-46 BqL(-1)) compared to the spring, therefore an additional deep inflow from hitherto unknown cave passages is assumed, from which waters with high radon content arrive to the spring. These passages are assumed to be in the active cave formation zone. This study proved that radon activity concentration distribution is a useful tool in underwater cave exploration. (C) 2016 Elsevier Ltd. All rights reserved.
引用
收藏
页码:51 / 57
页数:7
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