Dynamics of tidal parameters depending on the landslide hazard condition of the salt mine roof

IF 0.6 Q4 GEOCHEMISTRY & GEOPHYSICS
A. M. Kutnyi, V. Pavlyk, T. M. Babych, V.P. Plis
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引用次数: 0

Abstract

The dynamics of tidal parameters were studied based on the results of tilt observations in 4 points of the landslide hazard zone, which was formed over the exhausted field of a salt mine in the city of Soledar, Donetsk region. The reduction in the thickness of the supporting walls of the salt mine led to the loss of their supporting stability, which led to the lowering of the ground, the destruction of the foundations and walls of residential and administrative buildings in a plot 1.3 km long and 0.5 km wide. To eliminate the risk of collapse, the used underground galleries were filled with salt in order to strengthen their retaining walls.Thus, the landslide hazard zone has become a unique training ground for studying the change in tidal parameters γ and Δϕ depending on the state of the mine roof. In total, 256 continuous hourly monthly series were processed using modern methods of excluding their linear drift and anomalous meteorological disturbances from the initial data at short observation intervals, which made it possible to significantly increase the accuracy of determining tidal parameters based on the results of harmonic analysis. For the first time in the global earth tide practice, the normalization of the tilt parameters during and after strengthening the collapsing roof of the mine was revealed. If before the strengthening of the supporting walls of the underground galleries, the tidal parameters assumed abnormal values (the amplitude factor γ by 30 %, and the phase factor Δϕ by 10—15 degrees differed from the regional analogues), then in the process of backfilling they began to approach their regional values, which they reached a year after the backfilling. The real possibility of using the earth tide method for monitoring and forecasting the landslide hazard and related phenomena of the ground has been proven.
取决于盐矿顶板滑坡危险条件的潮汐参数动力学
根据对滑坡危险区4个点的倾斜观测结果,研究了潮汐参数的动力学。滑坡危险区形成于顿涅茨克地区索莱达尔市一座盐矿的枯竭场上。盐矿支护墙厚度的减小导致其支护稳定性的丧失,导致地面下降,1.3公里长、0.5公里宽的地块内的住宅和行政建筑的地基和墙壁被毁。为了消除坍塌的风险,用过的地下通道被填充了盐,以加固它们的挡土墙。因此,滑坡危险区已成为研究潮汐参数γ和Δξ随矿井顶板状态变化的独特训练场。使用现代方法,在短观测间隔内从初始数据中排除线性漂移和异常气象干扰,总共处理了256个连续的每小时月序列,这使得根据谐波分析结果确定潮汐参数的准确性大大提高。在全球土潮实践中,首次揭示了该矿坍塌顶板加固过程中和加固后倾斜参数的归一化。如果在加固地下廊道的支撑墙之前,潮汐参数假设为异常值(振幅因子γ为30%,相位因子Δ为10-15度,与区域类似物不同),那么在回填过程中,它们开始接近其区域值,在回填一年后达到该区域值。证明了利用土潮法监测和预报滑坡灾害及地面相关现象的真实可能性。
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
Geofizicheskiy Zhurnal-Geophysical Journal
Geofizicheskiy Zhurnal-Geophysical Journal GEOCHEMISTRY & GEOPHYSICS-
自引率
60.00%
发文量
50
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