在卡拉布拉吉区的石头样本的深度分布中确定放射性,卡纳塔卡,印度
Nagraj Channappa1, Jayashri Mutagar1, Basavaraj Rachappa Kerur1
1Department of Physics, Gulbarga University, Kalaburagi 585106, Karnataka, India.
Radiation protection dosimetry
|July 17, 2024
概括
这项研究测量了来自印度卡拉布拉吉的土壤样本中的放射性. 结果显示,-238 (238U),-232 (232Th) 和-40 (40K) 的度显著,深度有所不同.
科学领域:
- 环境科学 环境科学
- 核地质物理学 核地质物理学
背景情况:
- 土壤中的放射性是环境的一个关键问题.
- 了解与深度相关的变化对于准确的风险评估至关重要.
研究的目的:
- 为了确定土壤中自然存在的放射性核化物 (238U,232Th,40K) 的活性度.
- 调查深度对卡拉布拉吉地区放射性水平的影响.
- 计算K/Th和K/U比率来评估基本关系.
主要方法:
- 使用了高分辨率的马射线光谱学.
- 收集并分析了深度地形土壤样本.
- 活动度和元素比率被计算出来.
主要成果:
- 观察到显著的活性度,贾亚纳加的样本显示高水平的238U (51.64 ± 0.50 Bq kg-1),232Th (58.77 ± 0.23 Bq kg-1),和40K (313.92 ± 3.57 Bq kg-1).
- 放射性水平随着深度的变化而变化.
- 从表面样本中估计了K/Th和K/U比率,可能与深层样本有所不同.
结论:
- 该研究强调了卡拉布拉吉土壤中显著的自然放射性.
- 深度是影响放射性核素度的关键因素.
- 需要进一步的研究来理解这些发现的含义.
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