1. Introduction
With the global warming, the infrastructures in China’s power grids suffer from more serious meteorological events. According to statistics released recently by Chinese government, more than 20 convective weather events took place in east China in each year including a certain proportion of ruinous tornado disasters, leading to many steel transmission towers’ collapses. As failures of transmission lines seriously harm the economic development of the region and the normal life of the general public, useful techniques for protecting steel transmission towers against tornados are expected from the engineering circle.
A good approach to deal with the structural failures of transmission towers in strong winds is to develop good structural health monitoring (SHM) systems. In history, some innovative SHM strategies have been formulated in this circle. For example, Fei et al. [
1] proposed to use the decreased modal frequencies measured on the transmission towers to inverse the wind speeds on location and give the alarms to the cases with the identified speeds crossing the critical threshold. The rationality behind this practice is the rule observed that the fundamental modal frequency calculated for a transmission tower dramatically decreases when the applied static wind load is increased to the instability critical value. Ref. [
2] proposed to use a static force equilibrium equation to calculate the whole structure’s real-time stress distribution according to its real-time behavior, as captured by the global positioning system in SHM of transmission towers. Ref. [
3] reconstructed the global displacements of a transmission tower based on the simultaneous acceleration and strain measurements in corporation with the Kalman filter based data fusion algorithm to evaluate the structural performance.
Although the above mentioned methods developed are proven to be effective in use, we should note that they are all targeted for protecting the towers against the traditional atmospheric boundary layer (ABL) wind actions. In fact, tornados are different from ABL winds due to its strong non-stationary nature. According to Ref. [
4], the time-consuming computational fluid dynamics technique was utilized to generate the non-stationary tornadic wind load samples for the required dynamic analyses to take place. The authors in [
5] developed a non-stationary analytical method for tornadoes acting on structures with reference to some early observations and calculated the tornado-induced dynamic responses of several buildings. Refs. [
6,
7,
8] used an advanced small-scaled non-stationary vortex simulation facility to undertake physical tests of tornadic events. In nature, the small-scale core vortex of the tornado travels along an unpredictable route during the tornadic event, leading to the changes of the distribution patterns of the loads acting on the affected tower with time. Therefore, the monitoring strategy for towers affected by tornados should be different from those subjected to ABL winds with the determinate load patterns. We suppose the focus of SHM methods proposed for transmission towers against tornados should be the real-time load distribution identifications which will facilitate accurate calculations of the transient whole-field stress on the structure for the effective reliability estimations of the real-time structural conditions, as per Ref. [
2].
With the engineering background of a 131-m high free-standing transmission tower located in east China, this article first applies the finite-element (FE) model updating technique to the identification of load magnitude of the traditional ABL wind based on a field modal experiment. Then a novel SHM oriented load distribution identification practice for transmission towers against tornados based on the real-time mode shape measurement and FE model updating is proposed, supposing the target tower is subjected to a typical tornado. Via the numerical simulation, the effectiveness of the new method is validated. To the writer’s knowledge, these works have not been reported by the engineering community so far, but their practical significance is immeasurable.
2. Engineering Background and Numerical Model
A self-supported transmission tower located in east China is chosen as the engineering background, which has a 26 m × 26 m base and a height of 131 m (see
Figure 1). Its main body consists of four upright main chords interconnected via cross bars, diagonal bracings and web members. Four cross arms are attached to the top part of the main body in order to shoulder the transmission lines.
In according with the design drawings, the transmission tower’s 3D FE model is established using a commercial numerical platform. A beam-truss hybrid element simulation approach is adopted with members connected by flanges and welds modeled by beam elements and those connected by bolts modeled by truss elements to ensure their correct end stiffness respectively (see
Figure 2).
After the FE model is so established, a modal analysis is followed with the calculated results listed in
Table 1 and presented in
Figure 3.
Table 1 compares the calculated modal frequencies and those measured on location using the modal experiment reported in Ref. [
9], which suggests the comparatively good agreement in between them. As can be seen in
Figure 3, the 1st~8th modes calculated are 1st sway, 1st bending, 1st torsion, 2nd sway, 2nd bending, 2nd torsion, 3rd sway, 3rd bending, respectively.
3. Field Modal Experiment in Moderate ABL Wind
As reported in Ref. [
9], before putting into operation, a field modal experiment was conducted on the target free-standing tower without electric conductors installed using moving sensor modal test method by Southeast University (see
Figure 4). 11 × 4 measuring points were arranged on the 11 tower floors (see
Figure 1) and in 4 positions on each floor to measure the longitudinal and lateral directional structural vibrations. 4 channels were available for measuring the two-directional structural responses at one shifting measuring point and at an immobile reference measuring point simultaneously. The overall structural responses excited by the environmental loads, mainly moderate ABL wind, were recorded in the form of velocity time-histories.
Two directional time-histories and their auto-spectra measured at 2nd measuring point and 6th measuring point (immobile reference measuring point) are shown in Figs. 5 and 6, respectively. As can be seen, the velocity responses are greater at the higher floor (the 6th measuring point), and the first a few modal frequencies are identifiable on all power-spectral density (PSD) plots shown in
Figure 5 and
Figure 6. Cross-spectra between time-histories measured at 2nd and 6th measuring points are shown in
Figure 7, which indicates that the signs of the longitudinal and the lateral fundamental modes should be minus and plus on the 2nd point, respectively, according to
Appendix A. Following the steps introduced in
Appendix A, the low-order modal frequencies (see
Table 1) and mode shapes (see
Figure 8 for 1st~3rd modes) are successfully identified from the field modal test for further use. The modes shown in
Figure 8 agree with those calculated via modal analysis (
Figure 3a–c).
4. Load Magnitude Identification Using Structural Modal Frequency Measurement
Different from the traditional practice of using modal parameters to identify the structural parameters via the FE model updating, Ref. [
1] proposed the method of using modal parameters to identify the external loads acting on the structure based on the new observation that the fundamental modal frequency calculated for a transmission tower decreases when the applied static wind load is increased (see
Section 1). In this portion of study, the magnitude of the wind loading on the transmission tower (or the mean wind speed on location) at the time the field modal test has been undertaken (see
Section 3) is identified using the numerical model established in
Section 2 following the model updating practice. It is assumed that the mean wind velocity profile (or the wind load distribution pattern) is determinate in accordance with the Chinese design standard [
10] which can be expressed using a power-law formula with an exponent of 0.16. Regarding an overall amplification factor of the design wind loads applied to the FE model and the stiffness of the three-dimensional supports at the tower bottom as the updated parameters and the root-mean-square value between the calculated and the measured 1st and 2nd modal frequencies as the objective function, dynamic FE model updating is conducted using the first order method (see
Appendix C) via minimizing the penalty function-based unconstrained objective function by iteratively changing the updated parameter. The objective function is gradually minimized and converged after seven iterations (
Figure 9). The optimized overall amplification factor is obtained as being 0.338, and the basic wind speed at the height of 10 m is therefore calculated as being 13.2 m/s which is close to the result measured on location using a handheld anemometer (≈10 m/s). This proves the effectiveness of the dynamic model updating approach in load magnitude identification for traditional ABL wind events. Besides, it is found that the model with the optimized three-dimensional supports arranged at the tower bottom can generate commensurate modal analysis results with a model with the foundation modeled in detail, which also indicates the effectiveness of the performed FE model updating.
5. Tornadic Velocity Model
The tornadic velocity model traditionally employed in structural analyses in history is the two dimensional Rankine’s model, which wrongfully ignores the axial flow movements. The three dimensional model proposed by Wen [
11] which well considers the axial flow movements is more rational in this regard. According to Wen’s model, the thickness of the tornadic boundary layer
can be written as:
in which,
;
is the distance from the targeted position to the center of the tornado;
is the radium corresponding to the maximum tangential velocity;
is the thickness of the tornadic boundary layer for
, which is chosen as being
according to the general practice.
As shown in
Figure 10, the boundary layer interface divides the tornadic flow field into two parts. Therefore, the nature of the flow depends on the height of the targeted position (the
z coordinate). Above the interface (
), the following equations can describe the velocity components along the three directions:
Below the interface (
), the velocity components are formulated as:
in which,
,
,
are the tangential velocity, the radial velocity, the vertical velocity, respectively;
is the maximum tangential velocity;
;
;
z is the vertical distance from the ground to the targeted position.
According to Ref. [
12], when calculating the tornadic velocity time-history at a targeted position on the tornado passage,
T and
R formulated in Equations (2) and (3) should be adjusted to consider the net effect of the no-zero translating of the tornado with velocity
VT (see
Figure 11 for the required adjustments). With reference to Ref. [
11], the F3 grade tornado with
and
is selected for the following case study of the tornado-induced structural response of a free-standing transmission tower. With reference to the F3 tornado observed in Mullinville, KS on 7 May 2002 [
13],
VT is chosen as being 5.7 m/s for the case study. As shown in
Figure 11, the free-standing transmission tower described in
Section 2 is assumed to be located on the pass of the F3 grade tornado with its front directly facing the tornado for the case study.
6. Calculation of Structural Responses to Tornadic Actions
An earlier research (Ref. [
14]) has calculated the structural response of the tower to tornadic loads in the same event based on Wen’s velocity model described in
Section 5. According to Ref. [
14], the process of the calculation include the following steps: (1) calculate the tornadic velocity field based on Wen’s model; (2) calculate the time-varying tornadic loads acting on the tower using the standard formula stipulated in standards to transform the velocity samples to load samples; (3) conduct the time-history analysis via applying the loads to the FE model. In this course of the dynamic calculation, the main software function employed is Newmark-β method whose details of analysis are presented in
Appendix D.
The present calculation process basically follows the above, but with an appropriate improvement on a weak point of the calculation conducted by Ref. [
14], i.e., only the low-frequency fluctuations are taken into account in calculating the tornadic velocity/load samples based on the time-varying means calculated using Wen’s model, while the high-frequency fluctuations are ignored in their dynamic analysis. The reason behind their treatment is that no empirical model has been proposed to describe the high-frequency fluctuations of the tornadic velocities for use so far due to the limited field measurements of tornados.
As the alternative method, we use the conventional ABL spectrum to generate the high-frequency velocity fluctuations for the tornado which are then added to the time-varying means to obtain the tornadic velocity samples with both high-frequency and low-frequency components included. The ABL velocity fluctuations are generated according to the method described in Ref. [
14]. After that, the longitudinal and the lateral load samples at 20 heights are calculated from velocity samples in accordance with the practice adopted by Ref. [
14], and FE time-history analysis is then conducted using the Newmark-β method with 0.1 s time step via applying the load time-histories to the tower body of the model assuming that the tornado travels from an upstream position at 200 m in front of the tower to a downstream position at 200 m behind the tower.
The lateral and longitudinal displacement responses so calculated at the tower top are shown in
Figure 12. As can be seen, at the beginning, the lateral displacement gradually increases and reaches the maximum value (0.5 m) when the tornado is at an upstream position of around 50m in front of the tower. Then, the lateral response significantly decreases. After the tornado passes the transmission tower, the lateral displacement changes its direction. When the tornado moves away from the tower, the lateral displacement first significantly increases and subsequently gradually decreases. In addition, as shown, the longitudinal response is negligible throughout the loading process. These observations agree well with those reported in Ref. [
14]; however, a noticeable difference is also observed between the displacement responses calculated for the present study and those shown in Ref. [
14], i.e., high-frequency fluctuations can be seen on the response curves shown in
Figure 12, which were not seen on those shown in Ref. [
14]. This is obviously due to the present treatment in calculating the tornadic velocity samples with both high-frequency and low-frequency components included. In addition,
Figure 12 also compares the velocity samples calculated at 113-m height against the responses so obtained at the tower top. As shown, they show similar variation tendencies in both longitudinal and lateral directions.
The displacement responses shown in
Figure 12 are then transformed into acceleration responses which are processed using the wavelet analysis with complex Morlet wavelet function. Following the modal parameter identification practice with wavelet analysis reported in Ref. [
15] which has the advantage of disclosing the variations of the modal frequencies with time for the non-stationary events, the time-varying fundamental natural frequencies of in both lateral and longitudinal directions are identified in view of the maxima in time-frequency energy spectra obtained using the wavelet analysis from the acceleration responses calculated at the tower top (
Figure 13). As can be seen, the first order modal frequencies for both the lateral and the longitudinal directions are at the lowest value (≈0.7 Hz) in the time interval [25 s, 40 s], suggesting that the static wind loading effects are most significant in this duration (the overall wind force acting on the structure is the largest). This is supported by the rule that the fundamental modal frequency for a transmission tower decreases when the applied static wind load is increased [
1]. Therefore, the following studies focus on identifying the tornadic load patterns on the tower at the local time 25 s.
7. Load Distribution Identification Using Structural Mode Shape Measurement
Section 4 is basically to deal with ABL winds whose velocity profiles are comparatively determinate that have already been measured by many researchers and generalized into empirical formulae for direct use. Therefore, distribution patterns of wind loads acting on the structure are determinate for ABL winds, and as a result, the load identification work undertaken in
Section 4 merely focuses on the magnitude of the load without considering the load pattern. In order to fulfill the purpose of
Section 4, only the fundamental frequency of the structure is employed as there is only one load parameter (the magnitude of the reference velocity) to identify. However, with regard to the present research focusing on the tornados, the load distribution pattern consisted of many concentrated forces is changeable over time, which should be simultaneously identified using the modal parameters. As it is found that the structural mode shape contains much more information concerning the load distribution applied to the structure comparing to the structural modal frequency, possibly meeting the need of identifying multiple parameters, the load pattern identification approach employed by the present study is based on the measurement and the utilization of the mode shape.
To obtain the mode shape via the modal experiment, 10 accelerometers are supposedly uniformly arranged at 5 heights along the vertical direction to measure the longitudinal and the lateral structural responses at these positions (see
Figure 1). It is supposed that 10 structural acceleration samples are generated by the 10 sensors during the short time interval [22.5 s, 27.5 s] for use, which are actually obtained from the calculated results in
Section 6 and presented in
Figure 14.
Using the Frequency Domain Decomposition (FDD) method with its theories described in
Appendix B, the modal parameters are identified for the tower subjected to the tornado at 25 s based on the structural acceleration samples shown in
Figure 14. As a nonparametric approach in frequency domain, the modal parameter identification using FDD approach requires the manual peak picking on the first singular values of the PSD matrix calculated for the structural responses, and the peaks of the PSD of the structural response (
Figure 15) are reasonably picked to identify the structure’s 1st and 2th modal parameters (this step will be automatically executed in actual applications). The 1st and the 2th natural frequencies so identified are 0.625 Hz and 0.6641 Hz respectively which are found to be much smaller than the corresponding results calculated for the tower without external loads in
Section 2 (0.809 Hz and 0.827 Hz, respectively). This observation agrees the rule reported in Ref. [
1]. The 1st and 2th normalized mode shapes so identified are shown and compared with those calculated in
Section 2 for the structure without undertaking wind actions in
Figure 16. From
Figure 16, it can be learnt that the fundamental lateral (1st) modes for the tower with and without tornadic actions are close together, while the 2nd (fundamental longitudinal) modes calculated are noticeably different between the tornadic case and the case without wind actions. It is therefore suggested that the 2nd mode identified for the tornadic case contains more information concerning the transient load distribution than the 1st mode identified does. In addition, the resemblance between the actual lateral velocity profile (see
Figure 9) and the fundamental lateral mode of the structure without loads is greater than that between the actual longitudinal velocity profile (
Figure 9) and the corresponding longitudinal mode of the structure without loads. Therefore, we suppose the reason behind the above-mentioned observation that the 1st mode does not change much after the tornadic loads are applied to the structure is that only for the cases that the applied load distributions are noticeably different from the modes of the original structures, the mode shapes significantly alter after the structures are subjected to the external loads. As can be seen in
Figure 16, the 2nd mode identified for the tower with loads at 25 s during the tornadic event resembles the actual longitudinal velocity profile (
Figure 9) to some extent.
With the mode shapes identified for the tower subjected to the tornado at 25 s, the transient tornadic load distributions at that local time are identified using the FE model updating on ANSYS platform. In detail, the first order optimization algorithm provided by the ANSYS platform with its theories presented in
Appendix C is employed. During the optimization process, the wind loads are applied to the numerical modal, and the 1st and 2th modes are calculated via the modal analysis in each iteration. The updated parameters are chosen to be the longitudinal and the lateral tornadic loads acting on the main body of the tower at 20 heights (2 × 20 = 40 parameters in total). The initial values of the updated parameters are set to be the design values according to the Chinese structural design standard DLT5154-2002 [
10] for the case of the 45 degrees skewed wind. The constraints of the updated parameters are set to be [0.5 × initial value, 1.5 × initial value]. The constrained objective functions are set to be
= 2 − MAC1 − MAC2 (MAC1 and MAC2 are the longitudinal and the lateral Modal Assurance Criteria (MAC) values [
16] between the modes calculated in the current iteration and the identified modes shown in
Figure 16, respectively). The state-variables were the first two order modal frequencies whose lower/upper bounds were ±20% based on the values identified above for the tower subjected to the tornado at 25 s. Model updating using first order optimization technique was utilized to minimize the penalty function-based unconstrained objective function through the iterations. The objective function was gradually decreased and converged after 9 iterations (see
Figure 17). With the optimized parameters (40 concentrated forces acting on the tower body), both the longitudinal and the lateral tornadic velocity profiles at 25 s are calculated, and compared with the accurate profiles in
Figure 18. As can be seen, the longitudinal profile identified via the model updating is close to the accurate profile along the height; while the lateral profile so identified is partly different from the accurate profile at the middle and the upper parts.
8. Comparison with Conventional Method in Load Distribution Identification
The conventional method for load distribution identification basically relies on wind measurement using the anemometer and empirical velocity model. It is supposed that the longitudinal and the lateral velocities have been measured at 25 s by an anemometer arranged at the free-end of a lower cross-arm, which are 18.03 m/s and 63.61 m/s, respectively, based on the input to the numerical calculation described in
Section 6. As shown in
Figure 19, the maximum tangential velocity of the tornado
and the radium corresponding to the maximum tangential velocity
are assumed to be correctly provided by the timely local weather forecast (74.1 m/s and 50 m, respectively), and the distance from the target tower to the center of the tornado
and the inclined angle between the line connecting the target tower and the center of the tornado and the transmission lines
are regarded as the two unknown parameters to be identified. By feeding the known parameters to Equation (3), an equation system with two unknowns (
and
) are obtained. By solving the equation system using a numerical method, the
and
are identified for the time 25 s as being 55.82 m and −7.36 degrees respectively with 2.92% and 2.04% relative errors from the accurate values. Using the two identified unknowns, the lateral and the horizontal tornadic velocities profiles at the target position at 25 s are identified and compared with the accurate ones in
Figure 20, which suggests that their agreements are comparatively good.
Figure 20 further compares tornadic velocity profiles identified using the approach based on wind measurement and empirical velocity model (the traditional method) with those of the proposed method. As can be seen, better effectiveness is achieved for the load distribution identification method based on the flow measurement than for the method based on structural mode shape measurement. However, the traditional method is subjected to the issue that accurate prior knowledge concerning detailed information of the tornado (the maximum tangential velocity of the tornado and the radium corresponding to the maximum tangential velocity) must be provided by the local weather station. Therefore, its applicability is limited with respect to the fact that the meteorological information of a tornado cannot be forecasted with up-to-date measurement techniques at present.