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首页> 外文期刊>Earth Surface Processes and Landforms: The journal of the British Geomorphological Research Group >Reconstructing the development of sampled sites on fluvial island surfaces of the Tagliamento River, Italy, from historical sources
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Reconstructing the development of sampled sites on fluvial island surfaces of the Tagliamento River, Italy, from historical sources

机译:从历史来源重建意大利塔利亚门托河河流岛表面采样点的开发

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摘要

In parallel with research on surface sediment characteristics of evolving island features (patches) along an island-braided reach of the Tagliamento River, Italy, the present research reconstructed the development of the sampled sites using historical information coupled with field measurements. Since any field sediment sampling programme inevitably focuses on small areas (of the order of a few metres), the historical sources were assessed bearing in mind their spatial resolution and geographical accuracy in relation to the size of the sampled sites, and the information they could provide regarding the historical evolution of those sites. The analysis combined four sources of information: (i) river stage records revealed flood events that had the potential to reset bar surfaces and float in wood and seeds to initiate vegetation colonization; (ii) oblique ground photographs identified areas of the river's active corridor where riparian vegetation colonization appeared to have been initiated by specific flood events; (iii) dendrochronology was used to estimate the age of sampled sites; (iv) field-measured geographical locations of the sampled sites were combined with historical vertical areal imagery to further establish sampling site age and changes in vegetation cover from 1944 to 2012. A chronosequence of sampled sites (0, 2, 8, 12, 40years) was established. Vegetation colonization and island development showed a statistically significant development trajectory among sites of each age across the 40year period following formative floods in 1965-1966, 2000, 2004 and a flow pulse in 2010. The trajectory progressed through pioneer and building island stages until vegetated areas became part of established islands. Evidence from the younger sites indicates that the pioneer island phase lasts up to eight years. Evidence from the oldest site indicates a building island phase lasting a maximum of 30years, but probably a lot less. Copyright (c) 2014 John Wiley & Sons, Ltd.
机译:在与意大利塔利亚门托河沿岛辫状河段不断演变的岛屿特征(斑块)的表面沉积物特征进行研究的同时,本研究利用历史信息和现场测量结果重建了采样点的开发。由于任何野外沉积物采样计划都不可避免地将重点放在小区域(几米量级)上,因此在评估历史资源时要考虑到它们的空间分辨率和地理精度与采样地点的大小有关,以及它们所能提供的信息。提供有关这些网站的历史演变的信息。分析结合了四个信息来源:(i)河段记录显示洪水事件有可能重置杆表面并漂浮在木材和种子中以启动植被定殖; (ii)倾斜的地面照片确定了河流活动走廊的河岸植被定植似乎是由特定洪水事件引发的区域; (iii)用树轮年代学来估计采样地点的年龄; (iv)将实地测量的采样地点地理位置与历史垂直面图像相结合,以进一步确定采样地点的年龄和植被覆盖度(从1944年到2012年)。采样地点的时间序列(0、2、8、12、40年) 建立了。在1965年至1966年,2000年,2004年形成洪水和2010年的水流脉动之后的40年期间,植被定植和岛屿发展在各个年龄段的站点之间显示出统计上显着的发展轨迹。该轨迹经历了先驱和建岛阶段,直到植被恢复为止。成为既有岛屿的一部分。来自较年轻地点的证据表明,先锋岛阶段可持续长达八年。来自最旧站点的证据表明,一个建筑岛阶段最多可以持续30年,但可能要少得多。版权所有(c)2014 John Wiley&Sons,Ltd.

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