尼日利亚中北部阿布贾Dei-Dei钻孔放射性监测

O. Maxwell , H. Wagiran , N. Ibrahim , S.K. Lee , S. Sabri
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引用次数: 4

摘要

由于公共供水不足,阿布贾Dei-Dei地区的居民消耗的地下水来自地下结构的不同岩性单元。这些水未经处理就被消耗掉了,在钻探过程中,它穿过了许多岩层,在一定程度上构成了需要评估的放射性元素。利用垂直电测深和航天飞机雷达地形图任务确定了电导率结构并绘制了地形图。利用地球物理测井资料钻了水文地质驱动井。用高分辨率同轴HPGe能谱仪分析活性浓度。232Th活性浓度为45±2 ~ 98±6 Bq kg-1, 238U活性浓度为18±2 ~ 37±4 Bq kg-1, 40K活性浓度为236±32 Bq kg-1 ~ 1195±151 Bq kg-1。在结构上,裂缝的连通性归因于某些层的低水平。活动水平是否在限制范围内,需要研究地下水活动水平和岩石地球化学。
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Radiological Monitoring of Borehole in Dei-Dei, Abuja, North Central Nigeria

Inhabitants in Dei-Dei area of Abuja consume groundwater that recharges from different lithologic units of subsurface structures due to inadequate public water supply.The water is consumed untreated and during drilling, it cuts across so many rock formations, to extents constitute radioactive elements which are to be evaluated. Vertical Electric Sounding and Shuttle Radar Topography mission was used to determine the structure of electric conductivity and map lineaments.Hydrogeologically motivated borehole with geophysical log data was drilled. Activity concentrations were analysed using high resolution co-axial HPGe gamma spectrometer system. The activity concentrations ranges from 45± 2 to 98 ± 6 Bq kg-1 for 232Th, 18 ± 2 to 37 ± 4 Bq kg-1 for 238U and 236 ± 32 Bq kg-1 to 1195±151 Bq kg-1 for 40K. Structurally, fractured interconnectivity attributed to low levels in some layers. Activity levels are within the limits, requires research within groundwater activity levels and rock geochemistry.

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