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Mobility of a remobilised parabolic dune in Kennemerland, The Netherlands

机译:荷兰肯纳梅兰的一个抛物线形沙丘的机动性

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摘要

A parabolic dune in the Netherlands was remobilised in December 1998 by removing vegetation and soil. The main aim of the experiment was ecological: to investigate whether permanent rejuvenation at the landscape scale is possible by restoration of natural processes. If processes can be reactivated at coarse scale, periodic rejuvenation of the landscape over the long term is possible, without the need for managers to interfere further. The experiment provides the opportunity to address another important question: can large parabolic dunes in the Netherlands be mobile in the present climate? Mobility of the dune is investigated by means of erosion pins, aerial photography and measurement of cross sections. Activity indices are derived from erosion pin recordings and correlated to weather conditions. From 1999 to 2001, displacement of the dune ranged from 0 to 12 m in east-northeasterly direction. Activity of the dune is related to wind conditions, but the relationship is strongly influenced by precipitation and therefore differs for wet and dry periods. Periods with extreme wind speeds resulted in much less geomorphic change than expected.
机译:1998年12月,荷兰的一个抛物线沙丘通过清除植被和土壤进行了修复。该实验的主要目的是生态学:研究通过恢复自然过程是否有可能在景观尺度上实现永久复兴。如果可以在较粗的规模上重新启动流程,则可以在长期内定期恢复景观,而无需管理人员进一步干预。该实验提供了解决另一个重要问题的机会:在目前的气候下,荷兰的大型抛物线沙丘可以移动吗?沙丘的流动性通过侵蚀销,航拍和横截面测量进行研究。活动指数来自侵蚀针记录,并与天气状况相关。从1999年到2001年,沙丘在东西向的位移范围为0到12 m。沙丘的活动与风况有关,但这种关系受降水的影响很大,因此在干湿两季都不同。风速极高的时期导致的地貌变化远少于预期。

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