武汉市中心城区地表形变与洪涝灾害防治新策略

Detection of the Urban Surface Deformation and New Strategy for Flood Prevention in Wuhan Central District

  • 摘要: 武汉市2013年和2016年的城市洪涝暴露了城市基础设施应对洪涝灾害的严重不足。水面锐减导致传统的抽排模式受到越来越大的挑战。如果利用土壤的水容能力,既可以资源化雨洪利用,又能改善土壤圈生态,将是一种新的城市防洪方向,为此,查明城市地表形变规律和土壤非饱和信息至关重要。基于2015-04—2016-04 InSAR (interferometric synthetic aperture radar)数据和110个基准点信息,获得武汉市中心城区的地面沉降数据,与长江水面进行对比分析,研究水面变化与地表形变的相关性。研究发现,武汉市中心城区的地面上升达到18 mm/a,主要是土壤水的物理化学膨胀作用,指示了土壤的不饱和状态,其潜在的防洪能力远大于其他方法。另外,城市地面上升呈现带状分布,也指示了雨水的径流方向。

     

    Abstract:
      Objectives  The urban floods occurred in 2013 and 2016 exposed the serious shortages of Wuhan infrastructures to resist weathering disasters. Traditional drainage of Wuhan against urban flood enfaces the challenges due to the sharp decrease of water area. A large amount of rainwater flows into the Yangtze River, aggravating the downstream flood.
      Methods  A new strategy is proposed to control the urban rainwater by using the "thirsty" soil to absorb rainwater. The expansion of soil moisture characterizes the water absorption capacity of soil. In principle, the saturated soil expanses and raises ground surface; on the contrary, the thirsty soil shrinks in volume and results into ground subsidence. It becomes a better strategy to control urban flood by utilizing this absorption capacity of thirsty soil, not only transforming the rainwater disaster into water resources, but also improving the ecology of urban pedosphere. The natural fluctuation of urban ground deformation is measured to roughly estimate the potential capability of water absorption. We took use of InSAR (interferometric synthetic aperture radar) data and 110 datum points in Wuhan center to inverse the surface deformation during the temporal window of 2015-04 to 2016-04.
      Results  The measured results demonstrated that the uplift of Wuhan urban area reached 18 mm/a. The current drainage capacity of Wuhan is equivalent to 140 mm/d rainfall, the water capacity of lakes is 250 mm/d rainfall, and the flood resistance capacity of soil sponge is only 30 mm rainfall. If soil's water absorption capacity is fully utilized, the soil sponge of 10 m soil layer can absorb 4 500 mm/d rainfall.
      Conclusions  The uplift of the urban land surface was caused by physical and chemical expansions of soil water; its potential capacity of flood control is much bigger than other methods. In addition, the zonings of surface rise indicate the runoff directions of the groundwater.

     

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