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  • 标题:Factors controlling natural subsidence in the Po Plain
  • 本地全文:下载
  • 作者:Luigi Bruno ; Bruno Campo ; Bianca Costagli
  • 期刊名称:Proceedings of the International Association of Hydrological Sciences
  • 印刷版ISSN:2199-8981
  • 电子版ISSN:2199-899X
  • 出版年度:2020
  • 卷号:382
  • 页码:285-290
  • DOI:10.5194/piahs-382-285-2020
  • 摘要:Abstract. Understanding the causes and mechanisms of land subsidence is crucial, especially in densely populated coastal plains. In this work, we calculated subsidence rates (SR) in the Po coastal plain, averaged over the last 5.6 and 120 kyr, providing information about land movements on intermediate (103–105 years) time scales. The calculation of SR relied upon core-based correlation of two lagoon horizons over tens of km. Subsidence in the last 120 kyr appears to be controlled mainly by the location of buried tectonic structures, which in turn controlled sedimentation rates and location of highly compressible depositional facies. Numerical modelling shows that subsidence in the last 5.6 kyr is mainly due to compaction of the Late Pleistocene and Holocene deposits (uppermost 30 m).
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