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在格陵兰冰盖中发现来自切尔诺贝利事故的放射性
概括
来自切尔诺贝利事故的放射性被测量在格陵兰岛的雪中. 这会在极地冰川中形成一个独特的层,这对于测定冰芯年龄和测量积雪量是非常有用的.
科学领域:
- 环境科学 环境科学
- 放射化学 放射化学是指辐射化学.
- 冰川学的冰川学
背景情况:
- 切尔诺贝利事故向大气中释放了大量的放射性核化物.
- 远程大气传输是放射性核素分布的一个关键因素.
- 北极的雪和冰作为过去环境事件的档案.
研究的目的:
- 为了评估切尔诺贝利事故后北极地区的放射性核化物沉积.
- 调查北极雪层作为时间标记物的潜力.
- 为冰芯分析建立一个参考层.
主要方法:
- 在格陵兰雪样本中测量-134和-137同位素.
- 使用大气中远程运输模型.
- 分析积雪速率和冰芯层结构.
主要成果:
- 在格陵兰的雪中发现了一层明显的放射性 (-134和-137).
- 沉积模式与切尔诺贝利核灾后的情况相关.
- 鉴定到的层适合用作日期参考.
结论:
- 在北极雪中的放射性核素测量提供了对大气运输的洞察力.
- 极地冰川中的切尔诺贝利层为冰川学研究提供了有价值的工具.
- 这一发现提高了准确估计积雪率和日期冰芯样本的能力.
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