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Published on: June 30, 2020
基底碎片对冰川流动的影响
Neal R Iverson1, Denis Cohen, Thomas S Hooyer
1Department of Geological and Atmospheric Sciences, Iowa State University, Ames, IA 50011, USA. niverson@iastate.edu
概括
冰川内部的碎片显著抵制运动,产生大量的剪切引力. 在冰下碎片层中的高孔水压可以减少摩擦,导致冰滑过碎片.
科学领域:
- 冰川学的冰川学
- 地球科学 地球科学 地球科学
- 地质物理学 地质物理学
背景情况:
- 冰川运动受到基底条件的影响,包括亚冰川碎片的存在和特性.
- 碎片在抵制冰川运动和基底摩擦方面的作用在历史上一直被低估.
研究的目的:
- 为了研究碎片丰富的冰在基岩接口上施加的剪切引力.
- 为了确定孔水压力对冰下碎片层和冰碎片相互作用的机械行为的影响.
主要方法:
- 在厚厚的滑动冰川下进行实验.
- 在光滑的岩床上测量了冰的剪切引力,其中有2-11%的碎片.
- 将孔水压力 (60-100%的正常应力) 应用于冰下碎片层.
主要成果:
- 富含碎片的冰 (2-11%的碎片) 产生了60-200kPa的剪切引力,相当于总基底剪切引力.
- 碎片层中的孔水压力增加显著降低了剪切引力,停止了碎片变形.
- 当孔水压达到正常应力的60-100%时,冰在碎片层上滑落,这表明滑动阻力低于碎片剪切阻力.
结论:
- 冰川底层碎片在冰川基本阻力中起着至关重要的作用,这与以前的微不足道摩擦假设相反.
- 孔水压力是调节亚冰川摩擦的关键因素,可能导致基底滑动并影响冰川动态.
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