RADON AND THORON DECAY PRODUCT AND PB-210 MEASUREMENTS AT JUNGFRAUJOCH, SWITZERLAND

被引:44
作者
GAGGELER, HW
JOST, DT
BALTENSPERGER, U
SCHWIKOWSKI, M
SEIBERT, P
机构
[1] PAUL SCHERRER INST, CH-5232 VILLIGEN, SWITZERLAND
[2] UNIV VIENNA, INST METEOROL & GEOPHYS, A-1190 VIENNA, AUSTRIA
[3] UNIV BERN, INST ANORGAN CHEM, CH-3000 BERN, SWITZERLAND
关键词
RADON DECAY PRODUCTS; THORON DECAY PRODUCTS; PB-210; JUNGFRAUJOCH; RADIONUCLIDES; FREE TROPOSPHERE; ATMOSPHERIC TRANSPORT; AEROSOLS; RESIDENCE TIME;
D O I
10.1016/1352-2310(94)00195-Q
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
During one year, the atmospheric activity concentrations of the short-lived ''radon'' (Rn-222) and ''thoron'' (Rn-220) decay products were measured at Jungfraujoch (3450 m a.s.l.). The measurements were performed using a modified epiphaniometer, with a time resolution of 1 h. In addition, also the long-lived radon decay product Pb-210 was measured with a time resolution of one month. Strong seasonal variations of ail activity concentrations were found, the average summer Values being a factor of ten higher than the average winter values. During summer time the activity concentrations of the radon and thoron decay products showed pronounced diurnal variations. During winter these diurnal variations were absent, and the activity concentrations were close to free tropospheric background values. From the ratio between the activity concentrations of the radon decay products Pb-214 and Pb-210 a mean residence time of aerosol particles in the atmosphere of about six days could be estimated. The average activity concentrations of the radon and thoron decay products at Jungfraujoch were found to be related to the regional soil temperatures at a near-by low altitude Swiss Midland site and to the static stability of the air mass between this Midland site and the Jungfraujoch. Furthermore, a significant correlation was found between the radon and thoron decay product activity concentrations and synoptic situations with higher than average activity concentrations for air flows from NE to SW and lower than average concentrations for air flows from W to N.
引用
收藏
页码:607 / 616
页数:10
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