首页> 外文OA文献 >Restoring earth surface processes throughudlandform design. A 13-year monitoringudof a geomorphic reclamation model forudquarries on slopes
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Restoring earth surface processes throughudlandform design. A 13-year monitoringudof a geomorphic reclamation model forudquarries on slopes

机译:通过 ud恢复地球表面过程地形设计。长达13年的监控 ud ud的地貌填海模型斜坡上的采石场

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摘要

The application of geomorphic principles to land reclamation after surface mining has been reported in the literatureudsince the mid-1990s, mostly from Australia, Canada and the USA. This paper discusses the reclamation problems of contourudmining and quarries on slopes, where steep gradients are prone to both mass movement and water erosion. To address theseudproblems simultaneously, a geomorphic model for reclaiming surface mined slopes is described. Called the ‘highwall–trench–udconcave slope’ model, it was fi rst applied in the 1995 reclamation of a quarry on a slope (La Revilla) in Central Spain.udThe geomorphic model does not reproduce the original topography, but has two very different sectors and objectives: (i) theudhighwall–trench sector allows the former quarry face to evolve naturally by erosion, accommodating fallen debris by means of audtrench constructed at the toe of the highwall; (ii) the concave-slope base sector, mimicking the landforms of the surroundingudundisturbed landscape, promotes soil formation and the establishment of self-sustaining, functional ecosystems in the areaudprotected from sedimentation by the trench. The model improves upon simple topographic reconstruction, because it rebuildsudthe surfi cial geology architecture and facilitates re-establishment of equilibrium slopes through the management and control ofudgeomorphic processes.udThirteen years of monitoring of the geomorphic and edaphic evolution of La Revilla reclaimed quarry confi rms that the area isudfunctioning as intended: the highwall is backwasting and material is accumulating at the trench, permitting the recovery of soilsudand vegetation on the concave slope. However, the trench is fi lling faster than planned, which may lead to run-off and sedimentationudon the concave slope once the trench is full. The lesson learned for other scenarios is that the model works well in a twodimensionaludscheme, but requires a three-dimensional drainage management, breaking the reclaimed area into several watershedsudwith stream channels.
机译:自1990年代中期以来,已有文献报道了地貌原理在地面采矿后在土地开垦中的应用,主要来自澳大利亚,加拿大和美国。本文讨论了坡度较高的边坡,采石场和采石场的填海问题,在这些坡度上,陡峭的坡度容易引起土体运动和水蚀。为了同时解决这些问题,描述了一种用于开采地表开采边坡的地貌模型。它被称为“高墙-沟槽- udconcave坡度”模型,该模型首先在1995年西班牙中部斜坡(La Revilla)上的采石场开垦中应用。 ud地貌模型不能复制原始地形,但具有两个部门和目标截然不同:(i) udwallwall-trench部门允许前采石场面通过侵蚀自然演化,并通过在highwall趾部构造的 udtrench容纳下落的碎片; (ii)凹面坡道的基础部分模仿了周围 udundisturbed景观的地貌,促进了土壤的形成,并在该地区 un了免受沟槽沉积影响的地区建立了自我维持的功能性生态系统。该模型在简单的地形重建方面进行了改进,因为它可以重建 uduric地质结构,并通过管理和控制预算变形过程来促进平衡坡的重建。 ud监测La Revilla地貌和水生演化的十三年采石场确认该区域已达到预期的功能:高墙被浪费,沟渠中积聚了材料,从而使凹面斜坡上的土壤和植被得以恢复。但是,沟槽的装填速度比计划的快,一旦沟槽装满,可能会导致径流和沉淀在凹面斜坡上。在其他情况下获得的经验教训是,该模型在二维方案中运行良好,但需要三维排水管理,将开垦区划分为数个流域河流。

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