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首页> 外文期刊>Environmental earth sciences >Possibilities of oil shale mining under the Selisoo mire of the Estonia oil shale deposit
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Possibilities of oil shale mining under the Selisoo mire of the Estonia oil shale deposit

机译:爱沙尼亚油页岩矿床Selisoo泥潭下的油页岩开采可能性

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摘要

The paper presents results of the study on oil shale mining (Estonia underground mine) possibilities under the Selisoo mire. The Selisoo area is 2,051 ha in extent, and most of the mire is in natural state. Peat layer consists of thick (4.4-6.5 m) oligotrophic peat. Mining under Selisoo will go at depths 65-70 m under the surface. The mining field of the Estonia mine was planned between Ahtme and Viivikonna fault zones. The lowest hydraulic conductivity of carbonate rocks 0.11 1/day per m~2 is found in the Oandu layer and for peat it is 0.35-0.0002 m/day. Therefore, together they form a good aquitard. When the annual rainfall amount is the highest, the difference between horizontal water inflow and runoff is positive with 127,000 m~3. Positive water balance is guaranteed in case of precipitation being at least 540 mm/year. The positive water balance is important for preserving the ecological system of Selisoo mire. For guaranteeing long-term stability of mine pillars, a new calculation method has been elaborated, based on the conventional calculation scheme, where the factor of safety is more than 2.3. Rheological processes are out of question, collapse of the pillars is impossible. Stability of the underground constructions and overburden rocks must be "eternal". The criteria were elaborated for oil shale mining and will guarantee preservation of mires in natural or close to natural state.
机译:本文介绍了在Selisoo泥潭下进行油页岩开采(爱沙尼亚地下矿山)可能性的研究结果。 Selisoo面积为2,051公顷,大部分泥潭处于自然状态。泥炭层由厚(4.4-6.5 m)的贫营养泥炭组成。 Selisoo下的采矿将在地下65-70 m的深度进行。爱沙尼亚矿的采矿场计划在Ahtme和Viivikonna断裂带之间。在Oandu层中发现的碳酸盐岩石最低的水力传导率为0.11 1 /天/ m〜2,对于泥炭来说,为0.35-0.0002 m /天。因此,它们一起形成了一个很好的水准。当年降水量最高时,水平水流入与径流量之差为正值,为127,000 m〜3。如果降水量至少为540毫米/年,则可以保证正水平衡。积极的水平衡对于维护Selisoo泥潭的生态系统非常重要。为了保证矿柱的长期稳定性,在安全系数大于2.3的传统计算方案的基础上,提出了一种新的计算方法。流变过程毫无疑问,支柱无法倒塌。地下建筑和覆岩的稳定性必须是“永恒的”。为油页岩的开采制定了标准,将确保保留自然或接近自然状态的泥潭。

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  • 来源
    《Environmental earth sciences》 |2013年第7期|3311-3321|共11页
  • 作者单位

    Department of Mining, Tallinn University of Technology, 5 Ehitajate Rd., 19086 Tallinn, Estonia;

    Department of Mining, Tallinn University of Technology, 5 Ehitajate Rd., 19086 Tallinn, Estonia;

    Department of Mining, Tallinn University of Technology, 5 Ehitajate Rd., 19086 Tallinn, Estonia;

    Department of Mining, Tallinn University of Technology, 5 Ehitajate Rd., 19086 Tallinn, Estonia;

    Department of Mining, Tallinn University of Technology, 5 Ehitajate Rd., 19086 Tallinn, Estonia;

  • 收录信息
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Selisoo mire; Underground mine; Peat; Hydraulic conductivity; Eternal;

    机译:Selisoo泥潭;地下矿山;泥炭;导水率永恒;

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