STUDIES ON THE ACTIVITY RATIOS OF PO-210 TO PB-210 AND THEIR DRY-DEPOSITION VELOCITIES AT BOMBAY IN INDIA

被引:35
作者
ANAND, SJS
RANGARAJAN, C
机构
[1] Pollution Monitoring Section, Bhabha Atomic Research Centre, Bombay, 400085, Trombay
关键词
D O I
10.1016/0265-931X(90)90017-P
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Atmospheric concentrations and dry fallout of 210Pb and 210Po have been measured at Bombay in India during 1985-1987 using air samplers and surrogate collectors respectively. The objective of these measurements was to compare the 210Po/210Pb activity ratios in surface air and dry fallout and to estimate the dry-deposition velocity, Vg, of the atmospheric particulates carrying these two radionuclides. The location of Bombay is eminently suitable for such studies in view of its continuous dry period of about eight months. An analysis of the collected data shows that the average 210Po/210Pb activity ratio in dry fallout (0·47 ± 0·39) is considerably higher than that in surface air (0·12 ± 0·08). This has been attributed to the higher values for 210Po (0.76 ± 0.48 cms-1) relative to 210Pb (0.14 ± 0.07 cm s-1). The higher Vg values for 210Po could be due to complementary sources of 210Po, such as resuspension of soil particles, etc., in addition to atmospheric 222Rn. A source apportionment has also been carried out for atmospheric 210Po using the 210Po/210Pb activity ratios, the Vg values for a range of radionuclides and their estimated atmospheric residence times. This calculation indicates that only about 17 ± 13% of 210Po may derive from atmospheric 222Rn, while 25 ± 10% is from soil and the rest from other sources. The Vg values from surrogate collectors reported here are useful as indices of deposition to other surfaces and give an idea of the relative magnitudes of Vg values for various species. © 1990.
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页码:235 / 250
页数:16
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共 32 条
[1]  
Abe, Abe, Trend in the chemical state of <sup>210</sup>Po in the atmosphere, Natural Radiation Environment III, pp. 9-430, (1980)
[2]  
Anand, Rangarajan, Mishra, Aerosols residence time calculations using Bismuth-210/Lead-210 activity ratios of atmospheric particulates, Lecture Notes in Physics on Atmospheric Aerosols and Nucleation, pp. 90-289, (1988)
[3]  
Bondietti, Brantly, Rangarajan, Examining accumulation-mode aerosol behaviour using natural and Chernobyl-derived radionuclides, Proc. 6th Int. Symp. of the Commission on Atmospheric Chemistry and Global Pollution on Global Atmospheric Chemistry, (1987)
[4]  
Burton, Stewart, Use of long-lived natural radioactivity as an atmospheric tracer, Nature, 186, pp. 584-589, (1960)
[5]  
Cambray, Fisher, Brooks, Peirson, Radioactive fallout in air and rain. Results to the middle of 1970, UK Atomic Energy Research Establishment Report AERE-R 6566, (1970)
[6]  
Eapen, Rangarajan, Efficiency of HV-70 filters for sampling short-lived radon daughter in atmospheric air, Health Physics, 39, pp. 354-358, (1980)
[7]  
Gopalakrishnan, Rangarajan, Joshi, Kapoor, Eapen, Measurements on airborne and surface fallout radioactivity in India, Report No. BARC-679, (1973)
[8]  
Gopalakrishnan, Eapen, Rangarajan, Fallout and atmospheric radioactivity measurements in India, Report No. HASL-328, (1977)
[9]  
Graustein, Turekian, <sup>210</sup>Pb and <sup>137</sup>Cs in air and soils measure the rate and vertical profile of aerosol scavenging, Journal of Geophysical Research, 91, pp. 14355-14366, (1986)
[10]  
Hicks, Wesely, Durhan, Critique of methods to measure deposition, Workshop Summary Report No. EPA-600/9-80-050, (1980)