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Sand martins favour loess: How the properties of loess ground facilitate the nesting of sand martins/bank swallows/uferschwalben(Riparia riparia Linnaeus 1758)

机译:沙丁鱼有利于黄土:黄土地面的特性如何促进沙丁鱼/燕子/费城山的筑巢(Riparia riparia Linnaeus 1758)

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摘要

Sand martins/bank swallows (Riparia riparia Linnaeus 1758) nest in tunnels excavated in loess deposits. Loess is particularly suitable because of its cohesive properties, its ease of excavation, its ability to form vertical faces, its ready availability in small scale brick works. A low clay content is a requirement for suitable ground (palaeosols appear to have too much clay), and in sand deposits a low level of cementation. The selective nature of nesting behaviour may have some stratigraphic value, and it may be that loess availability affects the distribution of sand martins (they move away from river banks to brick pits). Soil crust formation may affect the inhabitability of nest tunnels (the same phenomenon may be important in loess deposit formation). Penetration resistance of the ground is required to be in a middle-range, not too hard, not too soft. This is the Heneberg compromise: a compromise between tunnel stability and ease of excavation and construction.
机译:沙马丁/河岸燕子(Riparia riparia Linnaeus 1758)在黄土沉积物开挖的隧道中筑巢。黄土之所以特别合适,是因为其具有粘结性,易于开挖,形成垂直面的能力以及易于在小型砖砌工程中使用。对于合适的地面(古土壤似乎含有太多的粘土),要求粘土含量低,而在砂土中的胶结程度低。筑巢行为的选择性性质可能具有一定的地层价值,可能是黄土的可利用性影响了沙丁鱼的分布(它们从河岸转移到砖坑)。土壤结皮的形成可能影响巢穴的可居住性(同样的现象在黄土沉积物形成中可能很重要)。地面的抗穿透性要求在中等范围内,不要太硬,也不能太软。这是Heneberg的折衷方案:在隧道稳定性与易于开挖和施工之间进行折衷。

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  • 来源
    《Quaternary International》 |2013年第16期|216-219|共4页
  • 作者单位

    Giotto Loess Research Group, Geography Department, Leicester University, University Road, Leicester LE1 7RH, UK;

    Giotto Loess Research Group, Geography Department, Leicester University, University Road, Leicester LE1 7RH, UK;

    Giotto Loess Research Group, Geography Department, Leicester University, University Road, Leicester LE1 7RH, UK;

    Institute of Geography and Regional Development, University of Wroclaw, Wroclaw, Poland;

    Laboratory for Palaeoenvironmental Reconstruction, University of Novi Sad, 21000 Novi Sad, Serbia;

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