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首页> 外文期刊>Earth Surface Processes and Landforms: The journal of the British Geomorphological Research Group >Restoring earth surface processes through landform design. A 13-year monitoring of a geomorphic reclamation model for quarries on slopes
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Restoring earth surface processes through landform design. A 13-year monitoring of a geomorphic reclamation model for quarries on slopes

机译:通过地形设计恢复地表过程。斜坡采石场地貌开垦模型的13年监视

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The application of geomorphic principles to land reclamation after surface mining has been reported in the literature since the mid-1990s, mostly from Australia, Canada and the USA. This paper discusses the reclamation problems of contour mining and quarries on slopes, where steep gradients are prone to both mass movement and water erosion. To address these problems simultaneously, a geomorphic model for reclaiming surface mined slopes is described. Called the ‘highwall-trench-concave slope’ model, it was fi rst applied in the 1995 reclamation of a quarry on a slope (La Revilla) in Central Spain.The geomorphic model does not reproduce the original topography, but has two very different sectors and objectives: (i) the highwall–trench sector allows the former quarry face to evolve naturally by erosion, accommodating fallen debris by means of a trench constructed at the toe of the highwall; (ii) the concave-slope base sector, mimicking the landforms of the surrounding undisturbed landscape, promotes soil formation and the establishment of self-sustaining, functional ecosystems in the area protected from sedimentation by the trench. The model improves upon simple topographic reconstruction, because it rebuilds the surfi cial geology architecture and facilitates re-establishment of equilibrium slopes through the management and control of geomorphic processes.Thirteen years of monitoring of the geomorphic and edaphic evolution of La Revilla reclaimed quarry confi rms that the area is functioning as intended: the highwall is backwasting and material is accumulating at the trench, permitting the recovery of soils and vegetation on the concave slope. However, the trench is fi lling faster than planned, which may lead to run-off and sedimentation on the concave slope once the trench is full. The lesson learned for other scenarios is that the model works well in a twodimensional scheme, but requires a three-dimensional drainage management, breaking the reclaimed area into several watersheds with 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,其中大部分来自澳大利亚,加拿大和美国。本文讨论了斜坡上等高线采矿和采石场的填海问题,在这些斜坡上,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,描述了用于开采地表采矿边坡的地貌模型。它被称为``高墙-沟槽-凹面斜坡''模型,该模型首次用于1995年西班牙中部斜坡(La Revilla)采石场的填海中。地貌模型没有复制原始的地形,但有两个截然不同的地方部门和目标:(i)高墙-沟渠部门使前采石场面因侵蚀而自然演化,并通过在高墙趾部构造的沟渠容纳掉落的碎屑; (ii)模仿周围未受干扰景观的地形的凹面坡道基部,可促进土壤形成,并在受沟渠沉积保护的区域内建立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,因为它可以重建表面地质结构,并通过对地貌过程的管理和控制来促进平衡坡的重建。监测La Revilla回收采石场确认的地貌和水生演化的十三年该区域的功能达到了预期的效果:高墙正在倒水,沟渠中积聚了材料,可以恢复凹面斜坡上的土壤和植被。但是,沟槽的装填速度比计划的快,一旦沟槽装满,可能会导致径流和凹面斜坡上的沉降。在其他情况下获得的经验教训是,该模型在二维方案中效果很好,但是需要三维排水管理,将开垦区划分为具有流道的多个分水岭。

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