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中国沙漠 ›› 2003, Vol. 23 ›› Issue (4): 471-475.

• 学术讨论 • 上一篇    

沙纹弹道成因理论评析

孙显科1, 张凯2, 张大治2, 吕亚军1, 喻利华1   

  1. 1. 辽宁省林业厅 科技处, 辽宁 沈阳 110036;
    2. 辽宁省林业工作总站, 辽宁 沈阳 110036
  • 收稿日期:2002-03-27 修回日期:2002-05-13 出版日期:2003-08-20 发布日期:2003-08-20
  • 作者简介:孙显科(1929-),男(汉族),辽宁省黑山县人,研究员,主要从事风沙地貌、风沙移动规律和机械固沙措施的研究。

Review on Trajectory Theory of Sand-ripple Formation

SUN Xian-ke1, ZHANG Kai2, ZHANG Da-zhi2, LÜ Ya-jun1, YU Li-hua1   

  1. 1. Science and Technology Division, Forestry Department of Liaoning Province, Shenyang 110036, China;
    2. Forestry Technology Spreading Station of Liaoning Province, Shenyang 110036, China
  • Received:2002-03-27 Revised:2002-05-13 Online:2003-08-20 Published:2003-08-20

摘要: 运用风沙地貌蚀积原理对长期风靡于风沙地貌学研究领域的R·A·拜格诺跃移质冲击起动学说进行了评析,在肯定该学说正确方面和历史贡献的同时,对其中的沙纹弹道成因理论提出了异议。在分析弹道理论特点后认为,跃移质等量、等高、等距的三等特性是拜氏冲击起动学说在沙纹成因上的具体运用和观点的集中体现。分析认为沙粒跃移特性轨迹只存在于少量的跃移质中,且很少具有连续性;它不能取代普遍存在于风沙移动之中沙粒的3种运动形式,也无法体现沙粒两种起动的相互关系和沙粒在移动中所表现出来的高低不一,移距长短不同的差异性和分选性。评析强调沙粒起动和沙粒运移的多样性,在寻求它们的规律时,不应简化其多样性,或追求运动的单一性和特殊性。实验证明,沙纹无论在初始的形成阶段,还是在后续的演进阶段,均有风力起动和冲击起动的参与,而不是跃移质单一冲击的结果。沙纹有规则的排列主要是贴地夹沙气流周期性脉动的反映,而不是跃移质特性轨迹的重演。

关键词: 沙纹成因, 弹道理论, 跃移质特性轨迹, 冲击起动置换率, 沙地蚀积原理

Abstract: Bagnold's saltation impact start theory was reviewed by use of the theory on aeolian landform's erosion or deposition.While agreed to the correct aspects and its contribution,the author doubted the theory of sand-ripple trajectory formation cause.The property of equal-quantity,equal-height and equal-distance of saltation start is the concrete application and embodiment of the Bagnold's ideas.But the property contrail of sand particles can be only found in a few fluid particles and few has continuity.The contrail cannot substitute the three kinds of sand particles movement,and also be unable to show the correlativity of two kinds of sand particles start and the difference in sand movement.Author emphasized the diversity in sand particles start and movement.Experiment showed that wind start and impact start combined whether in the beginning or the sequent developmental phases.The regular arrange of sand lines is the reflection of the cycle pulsation of sand-bearing airflow,but not the replay of the characteristic contrail of the fluid start.

Key words: sand-ripple formation cause, theory of sand trajectory, characteristic contrail of sand particles, replacement rates of sand impact start, sandy land deposit or erosion theory

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