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Influence of wind turbines on seismic stations in the upper rhine graben, SW Germany

机译:风力涡轮机对莱茵河上莱茵河上莱茵河德国地震车站的影响

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Abstract By analysing long- and short-term seismological measurements at wind farms close to the town of Landau, SW Germany, we present new insights into ground motion signals from wind turbines (WTs) at local seismic stations. Because of their need to be located in similar regions with sparsely anthropogenic activities, wind turbines impact seismic stations and their recordings in a way that is not yet fully understood by researchers. To ensure the undisturbed recording tasks of a regional seismic array or a single station by a protected area around those endangered stations, it is very important to investigate the behavior of WTs as a seismic source. For that reason, we calculate averaged one-hour long spectra of the power spectral density (PSD) before and after the installation of a new wind farm within the investigated area. These PSD are ordered according to the rotation speed. We observe a clear increase of the PSD level after the WT installation in a frequency range of 0.5 to 10 Hz up to a distance of 5.5 km away from the WT. By analysing seismic borehole data, we also observe a decrease of the PSD of wind dependent signals with depth. The impact of wind-dependent signals is found to be much more pronounced for the shallower station (150 m depth) than for the deeper one (305 m depth). Using short-term profile measurements, we fit a power-law decay proportional to 1/ r _( b )to the main WT-induced PSD peaks and differentiate between near-field and far-field effects of ground motions. For low frequencies in the range from 1 to 4 Hz, we determine a b value of 0.78 to 0.85 for the far field, which is consistent with surface waves. The b value increases (up to 1.59) with increasing frequencies (up to 5.5 Hz), which is obviously due to attenuating effects like scattering or anelasticity. These results give a better understanding of the seismic wavefield interactions between wind turbines (or wind farms) with nearby seismic stations, including borehole installations
机译:摘要通过分析风电场的长期和短期地震测量,靠近Landau,SW德国镇,我们在当地地震站的来自风力涡轮机(WTS)的地面运动信号中提出了新的洞察。由于他们需要位于具有稀疏性活动的类似地区,风力涡轮机冲击地震站及其录音,以通过研究人员尚未完全理解的方式。为了确保在那些濒危站周围的受保护区域的区域地震阵列或单个站的不受干扰的录制任务,研究WTS作为地震源的行为非常重要。因此,在安装在调查区域内的新风电场之前和之后,我们计算了功率谱密度(PSD)的平均1小时长光谱。这些PSD根据轮换速度排序。我们在WT安装后观察到PSD水平的PSD水平,频率范围为0.5至10 Hz,距离WT有5.5公里的距离。通过分析地震钻孔数据,我们还观察到具有深度的风相信号的PSD减少。对较大的车站(深度深度为150米),发现依赖依赖信号的影响比深度更深(305米)更为显着。使用短期轮廓测量,我们将动力法衰减与1 / R _(b)成比例,到主要的WT诱导的PSD峰值,并区分地面运动的近场和远场效果。对于从1到4 Hz的范围内的低频,我们将B值为0.78至0.85的B值与表面波一致。 B值增加(高达1.59)随着频率的增加(高达5.5 Hz),显然是由于散射或四弹性等衰减效果。这些结果可以更好地了解与附近的地震站的风力涡轮机(或风电场)之间的地震波场相互作用,包括钻孔装置

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