Abstract

ABSTRACTWind 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 to . The attenuation factor, , ranges from 0.7 to 1.3 for lower frequencies between 1 and 4 Hz, and increases to = 2.3 for the higher frequency peak around 5.25 Hz. Finally, we present an example of 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.

Highlights

  • Since the start of the energy transition, many wind turbines (WTs) have been installed to produce electricity without greenhouse emissions

  • The SMARTIE1 experiment characterizes the emission of seismic waves by a single WT and their impact on seismic stations at different distances

  • WT-induced seismic signals affect the recordings of seismic stations in a frequency range from 1 Hz up to around 10 Hz

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Summary

INTRODUCTION

Since the start of the energy transition, many wind turbines (WTs) have been installed to produce electricity without greenhouse emissions. Neuffer and Kremers (2017) analysed the impact of WTs on a seismic network in the vicinity of natural gas fields in Northern Germany They determined the azimuthal direction of incoming Rayleigh waves and observed that waves with back-azimuths pointing to WTs in operation dominate the wavefield in a frequency band of 3–4 Hz. Zieger and Ritter (2018) calculated attenuation factors for emitted seismic signals of wind farms in the area around the town of Landau, SW Germany, for the near and far fields of WTs. They determined the azimuthal direction of incoming Rayleigh waves and observed that waves with back-azimuths pointing to WTs in operation dominate the wavefield in a frequency band of 3–4 Hz. On the basis of the attenuation behaviour of the seismic signals and the emission of the WT, we introduce a propagation model which can be used to estimate a protection radii around seismic stations

SETTING
POLARIZATION PATTERNS OF A SINGLE WIND TURBINE AT DIFFERENT DISTANCES
EMISSION COEFFICIENT AT DIFFERENT WIND SPEEDS
A CONCEPT OF A PROTECTION RADIUS USING PROPAGATION MODELS
DISCUSSION AND CONCLUSIONS
Findings
DATA AVAILABILITY STATEMENT
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