耶路撒冷的西罗亚大的放射性碳测年与气候数据和主要的水利工程有关
Johanna Regev1, Nahshon Szanton2, Filip Vukosavović2
1Dangoor Research Accelerator Mass Spectrometer Radiocarbon Laboratory, Scientific Archaeology Unit, Weizmann Institute of Science, Rehovot 7610001, Israel.
概括
放射性碳测年显示耶路撒冷的西罗亚大建于公元前800年左右. 这种古老的水管理系统在气候压力时期加强了吉洪泉.
科学领域:
- 考古学
- 古气候学
- 古代的水系统
背景情况:
- 耶路撒冷的水基础设施对于其历史发展和生存至关重要.
- 之前的研究已经确定了各种水工程, 但缺乏关键结构的精确日期.
- 了解古老的水资源管理,可以了解社会对环境挑战的反应.
研究的目的:
- 为了确定西罗亚大建设的确切时间.
- 连接西罗亚大与耶路撒冷的其他当代水资源管理项目.
- 调查耶路撒冷水系统的环境驱动因素.
主要方法:
- 采用微考古采样技术从西罗亚大收集样本.
- 用放射性碳测年法来确定采集的样品的年龄.
- 分析公元前9世纪的古气候数据 (干旱和洪水).
主要成果:
- 确切的放射性碳日期为公元前800年.
- 这一日期确立了西罗亚大与同一时期的其他重要水利工程之间的时间联系.
- 气候数据显示在公元前9世纪末发生了严重的干旱和洪水.
结论:
- 西罗亚大建于公元前800年左右,作为一个更大的水资源管理战略的一部分.
- 建造的目的是要巩固吉宏泉并建立一个水库 (西罗亚池) 供水.
- 环境压力,包括气候变化,可能促使这些水系统的发展.
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