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印度果阿邦河流、地下水、矿井水和降水中环境氚的分布情况。

Distribution of environmental tritium in rivers, groundwater, mine water and precipitation in Goa, India.

作者信息

Ansari Md Arzoo, Mohokar H V, Deodhar Archana, Jacob Noble, Sinha U K

机构信息

Isotope & Radiation Application Division, Bhabha Atomic Research Centre, Trombay, Mumbai 400085, India.

Isotope & Radiation Application Division, Bhabha Atomic Research Centre, Trombay, Mumbai 400085, India.

出版信息

J Environ Radioact. 2018 Sep;189:120-126. doi: 10.1016/j.jenvrad.2018.04.004. Epub 2018 Apr 13.

DOI:10.1016/j.jenvrad.2018.04.004
PMID:29656175
Abstract

Tritium concentration in rivers, groundwater, precipitation and mine pits water, all over Goa state was characterized to find out spatial and temporal variability of tritium. Twenty four water samples were collected during pre-monsoon and post-monsoon and analyzed for their tritium concentration. The mean tritium concentration in surface and sub-surface hydrosphere is 2.5 (±0.6) TU. The mean concentration of tritium in rivers, groundwater, mines pits water and rain water are 2.9 (±0.5) TU, 1.95 (±0.5) TU, 2.5(±0.3) TU and 3.1(±0.1) TU respectively. The tritium distribution in all the samples shows modern precipitation (post-1950) component in surface and sub-surface hydrosphere of Goa. The HYSPLIT4.0 air mass trajectory model and atmospheric circulation pattern suggest that the moisture origin was from the Arabian Sea and this low tritium moisture is diluting the tritium concentration of surface hydrosphere near the coastal area. The tritium concentration in surface hydrosphere shows more and more enrichment as one move inland (i.e. away from the coast). Significant seasonal change is observed in the surface hydrosphere. The pre-monsoon samples showed higher tritium concentration than post-monsoon samples. This may be due to high rate of re-evaporation of water and a reduction in the supply of oceanic moisture during the summer (pre-monsoon).

摘要

为了解氚的时空变异性,对果阿邦各地河流、地下水、降水和矿坑水中的氚浓度进行了表征。在季风前和季风后采集了24个水样,并分析了它们的氚浓度。地表和次表层水圈中的平均氚浓度为2.5(±0.6)TU。河流、地下水、矿坑水和雨水中氚的平均浓度分别为2.9(±0.5)TU、1.95(±0.5)TU、2.5(±0.3)TU和3.1(±0.1)TU。所有样品中的氚分布表明,果阿邦地表和次表层水圈存在现代降水(1950年后)成分。HYSPLIT4.0气团轨迹模型和大气环流模式表明,水汽来源是阿拉伯海,这种低氚含量的水汽正在稀释沿海地区地表水体的氚浓度。随着向内陆移动(即远离海岸),地表水体中的氚浓度越来越高。在地表水体中观察到显著的季节变化。季风前的样品显示出比季风后样品更高的氚浓度。这可能是由于夏季(季风前)水的再蒸发率高以及海洋水汽供应减少所致。

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