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The natural denudation rate of the lowlands near the Ranger mine, Australia: A target for mine site rehabilitation

机译:澳大利亚Ranger Mine附近的低地的自然剥削率:矿场康复的目标

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摘要

This paper provides a robust estimate of the total natural denudation rate for the area surrounding the Ranger uranium mine in the Northern Territory, Australia. This rate will be used to assess whether the final rehabilitated landform of the Ranger mine will denude at the natural rate after the landform has stabilized. The approach adopted was to compile and analyze all existing estimates of the total denudation rate.(including both physical erosion rates and solution losses) from areas near the mine site. Where available, solution losses are based on local measurements. These were used to adjust estimates for other local sites, where only physical erosion rates are available. Adjustments were based on a global relationship between physical erosion and solution loss rates. The adjusted total denudation rate estimates were shown to have no statistically significant relationship with the time over which they have been estimated (the averaging time, maximum period about 59,000 years), which suggests that they conform to mass flux equilibrium. This form of equilibrium implies an equivalence between inputs and outputs of sediment and solutes for which there is some evidence. Because the denudation rates are independent of averaging times, the long-term average total natural denudation rate can be calculated from all of the data, giving a value of 0.075 +/- 0.013 mm year(-1) (75 mm 1000 years(-1), 75 m Ma(-1)). This value is almost twice the previously quoted rate of 0.04 +/- 0.03 mm year(-1) (40 +/- 30 mm 1000 years(-1)), which was calculated from a mixture of physical erosion rates and the total denudation rates including some from large river catchments. The derivation of a revised denudation rate provides confidence that the revised value, based on all available data, is representative of the region; and is therefore an appropriate value with which to assess the success of the rehabilitation of a post-mining landform. Crown Copyright (C) 2021 Published by Elsevier B.V. All rights reserved.
机译:本文提供了澳大利亚北部地区游侠铀矿周围地区的完全自然剥蚀速度的强大估计。此率将用于评估Ranger Mine的最终恢复地区是否会在地形稳定后以自然速度剥夺。采用的方法是编制和分析总剥削率的所有现有估计。(包括矿场附近的区域的物理侵蚀率和解决方案损失)。在可用的情况下,解决方案损耗基于本地测量值。这些用于调整其他本地位点的估计,其中只有物理侵蚀率可用。调整基于物理侵蚀和解决方案损失率之间的全球关系。调整后的总剥削速率估算显示出与估计其估计的时间(平均时间,大约59,000年的最大时间)没有统计上显着的关系,这表明它们符合质量通量平衡。这种形式的均衡意味着沉积物的输入和输出之间的等价性和溶质有一些证据。因为剥蚀速率与平均次数无关,所以可以从所有数据计算长期平均全自然剥蚀速率,从而提供0.075 +/- 0.013 mm年(-1)(75 mm 1000年( - 1),75米MA(-1))。该值几乎是先前引用率的两倍为0.04 +/- 0.03 mm年(-1)(40 +/- 30 mm 1000岁(-1)),从物理侵蚀率和总剥蚀的混合物计算房价包括大型河流集水区。修订后的剥削率的推导提供了基于所有可用数据的修订价值的信心是该地区的代表;因此,这是一个适当的价值,从而评估挖掘后地位的康复的成功。皇冠版权(c)2021由elsevier b.v出版。保留所有权利。

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