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首页> 外文期刊>Near surface geophysics >Wind turbine induced seismic signals: the large-scale SMARTIE1 experiment and a concept to define protection radii for recording stations
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Wind turbine induced seismic signals: the large-scale SMARTIE1 experiment and a concept to define protection radii for recording stations

机译:风力涡轮机诱导地震信号:大规模的Smartie1实验和一个定义录音站保护半径的概念

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Wind turbines produce mechanical energy that can propagate to the ground and disturb sensitive measurements such as seismic recordings. The aim of the large-scale experiment Seismic Monitoring And Research of wind Turbine Induced Emissions (SMARTIE1) at a single wind turbine in Pfinztal (SW Germany) is to understand how wind turbines emit seismic signals under different operating conditions and how these seismic signals propagate through the local subsurface. The main objectives of SMARTIE1 are the investigation of wind turbine induced seismic signals, the characteristics of their propagation behaviour, as well as the radiation pattern of a single wind turbine as defined using particle motions. Moreover, we quantify the emission of the wind turbine induced seismic signals with respect to the wind speed. The combination of the wind turbine's emission into the subsurface and the attenuation behaviour of the seismic signals (ground motion velocity) can be used to estimate protection radii around seismic stations to ensure the recording of seismic signals without noticeable influences of the wind turbines. In this study, we detect several discrete wind turbine induced frequency peaks ranging from 1 to 10 Hz. We identify a radiation pattern of the wind turbine, which could give further insights into the interaction between the movement of the wind turbine's nacelle and the generation of the wind turbine induced seismic signals. Using profile measurements with a maximum distance of almost 3 km each, we fit a power-law decay for power spectral density proportional to1/rb. The attenuation factor,b, ranges from 0.7 to 1.3 for lower frequencies between 1 and 4 Hz, and increases tob= 2.3 for the higher frequency peak around 5.25 Hz. Finally, we present an example estimation of a protection radius around the seismic station of the Collm Observatorium that is part of the German Regional Seismic Network. The example protection radius around Collm Observatorium regarding this single wind turbine is reached at a minimum distance of 3.7 km.
机译:风力涡轮机产生可以传播到地面的机械能,并干扰敏感测量,例如地震记录。在Pfinztal(SW德国)的单个风力涡轮机上的大规模实验地震监测和对风力涡轮机诱导的排放(Smartie1)的目的是了解风力涡轮机如何在不同的操作条件下发出地震信号以及这些地震信号如何传播通过当地的地下。 Smartie1的主要目的是对风力涡轮机感应地震信号的研究,其传播行为的特性,以及使用颗粒运动限定的单个风力涡轮机的辐射图案。此外,我们量化了风力涡轮机诱导的震动信号的发射相对于风速。风力涡轮机的发射进入地下的组合和地震信号(地面运动速度)的衰减行为可用于估计围绕地震站的保护半径,以确保在不明显的风力涡轮机的情况下记录地震信号。在这项研究中,我们检测到几种离散的风力涡轮机感应峰值,范围为1至10Hz。我们识别风力涡轮机的辐射图案,其可以进一步了解风力涡轮机的机舱的运动与风力涡轮机诱导的地震信号之间的相互作用。使用具有最大距离近3英里的概况测量,我们适用于功率谱密度比例为1 / RB的电源衰减。衰减因子B为0.7至1.3的较低频率为1到4Hz,并且在较高频率峰值约为5.25Hz的较高频率峰值上增加Tob = 2.3。最后,我们介绍了在Collm Vispileatium的地震站周围的保护半径的示例估计,这是德国区域地震网络的一部分。关于该单个风力涡轮机的CollM观测结果周围的示例保护半径在3.7 km的最小距离到达。

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