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Ground motion in areas of abandoned mining: application of the intermittent SBAS (ISBAS) to the Northumberland and Durham coalfield, UK

机译:废弃采矿区的地面运动:间歇式SBAS(ISBAS)在英国诺森伯兰郡和达勒姆煤田的应用

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摘要

In this paper, we investigate land motion and groundwater level change phenomena using differential interferometric synthetic aperture radar (DInSAR) over the Northumberland and Durham coalfield in the United Kingdom. The study re-visits earlier research that applied a persistent scatterers interferometry (PSI) technique to ERS (European Remote Sensing) and ENVISAT (Environmental Satellite) data. Here, the Intermittent Small Baseline Subset (ISBAS) DInSAR technique is applied to ERS, ENVISAT and Sentinel-1 SAR datasets covering the late 1990s, the 2000s and the mid-2010s, respectively to increase spatial coverage, aid the geological interpretation and consider the latest Sentinel-1 data. The ERS data identify surface depressions in proximity to former collieries, while all three data sets ascertain broad areas are experiencing regional scale uplift, often occurring in previously mined areas. Uplift is attributed to increases in pore pressure in the overburden following the cessation of groundwater pumping after mine closure. Rising groundwater levels are found to correlate to ground motion measurements at selected monitoring sites, most notably in the surrounding area of Ashington. The area is divided by an impermeable EW fault; to the south, surface heave was identified as groundwater levels rose in the 1990s, whereas to the north, this phenomenon occurred two decades later in the 2010s. The data emphasize the complexity of the post-mining surface and subsurface environment and highlight the benefit that InSAR, utlizing the ISBAS technique, can provide in its charaterization.
机译:在本文中,我们使用差分干涉合成孔径雷达(DInSAR)研究了英国诺森伯兰郡和达勒姆煤田上的土地运动和地下水位变化现象。该研究重新访问了先前的研究,该研究将持久性散射体干涉测量(PSI)技术应用于ERS(欧洲遥感)和ENVISAT(环境卫星)数据。在这里,间歇性小基线子集(ISBAS)DInSAR技术分别应用于覆盖1990年代末,2000年代和2010中期的ERS,ENVISAT和Sentinel-1 SAR数据集,以增加空间覆盖率,帮助地质解释和考虑最新的Sentinel-1数据。 ERS数据确定了以前煤矿附近的地面凹陷,而所有这三个数据集都确定了广阔的区域正在经历区域规模的抬升,这通常发生在以前的开采地区。隆起归因于矿山关闭后停止抽水后上覆岩层中孔隙压力的增加。发现地下水位上升与选定监测点的地面运动测量值相关,最明显的是在阿辛顿周边地区。该区域被不可渗透的EW断层划分;在南部,1990年代地下水水位上升表明了地面起伏,而在北部,则在20年代后的2010年代出现了这种现象。数据强调了开采后地表和地下环境的复杂性,并强调了利用ISBAS技术的InSAR在表征方面可以提供的好处。

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