Coupled hydraulic and mechanical model of surface uplift due to mine water rebound: implications for mine water heating and cooling schemes

IF 0.5 4区 地球科学 Q4 GEOLOGY Scottish Journal of Geology Pub Date : 2019-07-26 DOI:10.1144/sjg2018-028
F. Todd, C. McDermott, A. Harris, A. Bond, S. Gilfillan
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引用次数: 13

Abstract

In order to establish sustainable heat loading (heat removal and storage) in abandoned flooded mine workings it is important to understand the geomechanical impact of the cyclical heat loading caused by fluid injection and extraction. This is particularly important where significantly more thermal loading is planned than naturally occurs. A simple calculation shows that the sustainable geothermal heat flux from abandoned coal mines can provide less than a tenth of Scotland's annual domestic heating demand. Any heat removal greater than the natural heat flux will lead to heat mining unless heat storage options are also considered. As a first step, a steady-state, fully saturated, 2D coupled hydromechanical model of a generalized section of pillar-and-stall workings has been created. Mine water rebound was modelled by increasing the hydrostatic pressure sequentially, in line with monitored mine water-level data from Midlothian, Scotland. The modelled uplift to water-level rise ratio of 1.4 mm m−1 is of the same order of magnitude (1 mm m−1) as that observed through interferometric synthetic aperture radar (InSAR) data in the coalfield due to mine water rebound. The modelled magnitude of shear stress at the pillar corners, as a result of horizontal and vertical displacement, is shown to increase linearly with water level. Mine heat systems are expected to cause smaller changes in pressure than those modelled but the results provide initial implications on the potential geomechanical impacts of mine water heat schemes which abstract or inject water and heat into pillar-and-stall coal mine workings. Thematic collection: This article is part of the SJG Collection on Early-Career Research available at: https://www.lyellcollection.org/cc/SJG-early-career-research
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矿井水回弹引起的地表隆起的水力和力学耦合模型:对矿井水加热和冷却方案的影响
为了在废弃的淹没矿井中建立可持续的热负荷(排热和储热),了解流体注入和提取引起的循环热负荷的地质力学影响很重要。在计划的热负荷明显多于自然发生的热负荷的情况下,这一点尤为重要。一个简单的计算表明,废弃煤矿的可持续地热通量只能提供不到苏格兰年国内供暖需求的十分之一。除非考虑储热方案,否则任何大于自然热通量的排热都将导致热开采。作为第一步,建立了矿柱和失速工作面的广义截面的稳态、完全饱和、二维耦合流体力学模型。根据苏格兰Midlothian监测到的矿井水位数据,通过顺序增加静水压力来模拟矿井水反弹。模型抬升与水位上升比为1.4 毫米 m−1具有相同的数量级(1 毫米 m−1),与通过干涉合成孔径雷达(InSAR)数据在煤田中观察到的一样。作为水平和垂直位移的结果,柱角处的剪切应力的模拟大小显示为随水位线性增加。矿井热系统预计会导致比建模的压力变化更小的压力变化,但研究结果对矿井水热方案的潜在地质力学影响提供了初步启示,该方案将水和热抽运或注入矿柱和失速煤矿工作区。主题集:本文是SJG早期职业研究集的一部分,可在以下网站获取:https://www.lyellcollection.org/cc/SJG-early-career-research
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Scottish Journal of Geology
Scottish Journal of Geology 地学-地质学
CiteScore
1.70
自引率
0.00%
发文量
10
审稿时长
>12 weeks
期刊介绍: Although published only since 1965, the Scottish Journal of Geology has a long pedigree. It is the joint publication of the Geological Society of Glasgow and the Edinburgh Geological Society, which prior to 1965 published separate Transactions: from 1860 in the case of Glasgow and 1863 for Edinburgh. Traditionally, the Journal has acted as the focus for papers on all aspects of Scottish geology and its contiguous areas, including the surrounding seas. The publication policy has always been outward looking, with the Editors encouraging review papers and papers on broader aspects of the Earth sciences that cannot be discussed solely in terms of Scottish geology. The diverse geology of Scotland continues to provide an important natural laboratory for the study of earth sciences; many seminal studies in geology have been carried out on Scottish rocks, and over the years the results of much of this work had been published in the Journal and its predecessors. The Journal fully deserves its high reputation worldwide and intends to maintain its status in the front rank of publications in the Earth sciences.
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