4.1. Wind Farm Errors Characterization and Modelling
This research work aims to determine the existence of a relation between the climatic variables that usually occur in a wind farm and the occurrence of the failure at the time each of them happens. This study, despite the fact it was initially analyzed in previous studies [
6,
11,
25], is a more detailed analysis of the relationship between a nonfailure and a failure has been attempted according to each of the climatic variables present at the time of the failure, as shown in
Table 5. This table shows the errors that, compared to the nonfailure, show for each of the climate variables a significance level close to 0.000, that is, they are different from the condition’s climate failure. From this table it can be inferred from an analysis of wind speed, that there is a clear difference in speed conditions under normal conditions and at the time error 1 (overproduction) occurs, and with a significance close to zero in error 32 (high winds), as shown in
Table 5.
On the other hand, during the study of the wind direction, you can differentiate in
Table 6 the time when stop failures occur by error 1 (overproduction), error 2 (anemometer overspeed), error 14 (gearbox temperature), error 22 (LG R-phase temperature), error 32 (high winds) and error 39 (right and left orientation forwarding), and the not failure conditions. Since ambient temperature has clear influences on conditions in the nacelle, we have established through its study a clear differentiation of the conditions when stop failures occur by error 1 (overproduction), error 2 (anemometer over speed), error 5 (LG overproduction), error 9 (emergency stop), error 15 (vibration sensor) and error 17 (excessive time orienting). This is reflected in the data in
Table 6.
Finally, relative humidity has a high number of associated faults when it reaches abnormal values. In this way, you can predict stops by error 1 (overproduction), error 3 (low voltage), error 9 (emergency stop), error 17 (excessive orientation time), error 22 (LG R-phase temperature) and error 32 (high winds).
These results are in line with the logical causes of the errors, as excessive wind top speed will cause problems, and the error 32 (high winds) and high wind conditions will present wind production excess that will lead to stops by power regulation. On the other hand, wind direction can lead to the above errors and, in addition, cause problems of transduction of the anemometer and temperature in the gearbox. Similarly, a very low or very high ambient temperature causes the freezing of anemometers or problems in the yaw mechanism causing too much time to orient.
This air mass, as noted above, can be associated with several of the most common errors such as stoppage by power regulation (error 1; 33% of failures) associated with abnormal values of the four climate variables simultaneous direction, high humidity (100%), temperature (30 °C) and speed peaks of 40 km/h (speed of 11.3 m/s). In the same way, the emergency stoppage (error 9; 5.2%) and excessive time orienting (error 17; 2%) are also associated very high humidity and temperature values as a result of the arrival of winds with this orientation.
First of all, it should be noted that, although these very frequent failures are the ones that have the greatest economic effects, you can only detect those associated with the climate and not many others, as they are the problems in the start-up. Indirectly, this evidence supports the study of significance previously conducted to define which climate variables can detect errors. In this way, we can conclude that the chosen location of a wind farm in the design period will determine, through its weather conditions, the most frequent types of breakdowns and their economic costs.
After defining which climate variables have abnormal values at the time of some failures and with the intention of being able to detect these same failures prematurely, we tested to determine the average values of those variables at the time such errors occur, as can be seen in
Table 7.
In this
Table 7, for example, it can be inferred that error 2 usually appears under average wind speed of 12.4 m/s, a wind direction of 208.7° N, an outdoor temperature of 8.2 °C and relative humidity of 85.2%. However, these average values cannot be used directly as a control algorithm for fault detection in wind farms, considering that each error is a function of climate variables and high deviation standard of each average value.
Unable to apply the above technique, we tested it with the use of control charts to identify the anomalous values of climate variables at the time when each of the linked errors occurs. However, almost none of the sampling values were found to be outside the control limits, set as the average plus/minus three times the standard deviation. Similarly, following the remaining control chart interpretation standards, a series of upstream or downtrend measurements was sought and has not allowed the anticipation of any kind of failure.
From these control charts, we observed that errors do not occur under abnormal weather conditions, and that the same conditions associated with failure also occur during the normal operation of the wind farm. This implies that we should not treat the study as deterministic based on the number of variables we handle, but it should be treated as a probabilistic study. In deterministic models, a good decision is judged according to the results. However, in probabilistic models, the technician is not only concerned with the results, but also with the amount of risk that each decision brings.
At this point, everything points towards a fateful combinatorial of climate variables, which is a new focus in our study. Therefore, there is a need for the use of data mining techniques to obtain interesting results for the maintenance of the wind farm.
In this way, we have used the methodology of response surfaces, which offers us the mathematical models that determine error 0 and 1 and error 0 and 2 depending on the climatic variables and those associated with the results obtained in the previous sections. This technique has been applied with annual and monthly sample values to determine which of the curves offers the best response.
The result has been really high for the huge mass of data, obtaining the following results with a correlation of almost 70%, very high value for annual and real values becoming higher than that shown in a bimonthly modelling. This is due to the smaller influence of failures with respect to normal operating conditions.
Attempting to validate these models with respect to the actual values obtained, we can conclude that, despite some tendency of the model to indicate a value greater than error 0, it does not reach the value 1 or 2. Somehow, the percentage obtained at the time of failure could be associated with the probability of failure at that time.
With this imprecise result obtained, a new approach to response surface analysis has had to be applied, modelling each of the failures based on a combination of climate variables that offer us the speed at which each of the errors would occur, as shown in Equations (6) and (8).
If we now use the limit speed to which each of the faults seems and represent it in a real wind speed diagram, we can define the time when each of the errors occurs, as shown in
Figure 4 and
Figure 6.
As can be seen, these results fit perfectly at the moment when an air mass with a given temperature, humidity and direction reaches its limit speed and causes the corresponding error.
Figure 4 and
Figure 6 confirm that this new approach provides us a reliable control algorithm for detecting time periods where a combination of values of weather conditions (wind speed and direction, outdoor temperature and relative humidity) with a high probability of error.
This new methodology does not seek to predict the exact moment of failure or an estimate of the hours remaining to the occurrence of the fault, but to inform the operators of the wind turbines, at which time of operation there are values of climatic variables that represent an alert for themselves due to a probability of error.
This represents valuable information and a new indicator to take into account in the decision-making of operational actions in wind turbines, in the choice of maintenance strategies to follow in wind farms and in the estimation of the productive capacity of a wind farm in its study phase.
4.2. Climate Technical Unavailability
This new indicator will be referred to herein after as “climate technical unavailability”, defined the same as the one where even if there are valid climatic conditions for wind turbines to generate electricity, will not be available because an error occurs.
As mentioned, this indicator can be taken into account in the implementation studies of the new wind farms, to make a more reliable estimate of the annual electricity production that they will develop over their useful life, and therefore a better approximation of the economic profitability of the wind farm that is planned.
The climate technical unavailability of a future wind farm can be calculated with the errors that are related to the climatic variables. In this sense, we can estimate the annual time that the wind turbines, in the location where they are intended to be installed, will be exposed to these critical weather conditions in which the probability of occurrence of each of these errors is presented.
With the estimation of the number of errors by the average stoppage time of each of them, we would have the time of climatic technical unavailability, and, in the same way with the number of errors and the associated cost for repair of each of them, we would have the associated costs and the loss of economic profitability involved.
Taking as an example one of the wind turbines to study and following the state coding of
Table 8, we represent in
Table 9 the number of minutes that remains in each state.
Using Equation (10) of the overall equipment effectiveness (OEE), its calculation is made by obtaining the OEE of this wind turbine:
Therefore, according to Equation (10), this wind turbine has an OEE of 97.17%. Assuming that the proposed methodology in the design phase had been applied to this wind turbine, the time of unavailability due to errors 1 and 2 whose linking has been demonstrated in this work could have been estimated. Considering that error 1 corresponds to the time encoded as H and error 2 is a percentage of the time encoded as F, we would have a stoppage time that implies a loss of availability of 0.7%. Being able to predict a not inconsiderable reduction of 0.7% gives an idea of the possibilities of the application of the control algorithm indicated in the present research paper.
On the other hand, error 1 occurs when the production of electricity exceeds the evacuation capacity of the point to which the wind farm is connected, that is, when there is an excess of production of the different wind farms connected to the same evacuation line.
Figure 3 and
Figure 4 show that we can determine in what climatic conditions there is the probability of occurrence of such overproduction, and, in the same way, if we are outside those conditions, that probability does not exist. Therefore, if you could modify the value of any of the climate variables, you could eliminate the combinatorial of variables that cause the error, while a priori this does not seem possible, if it is.
In order to modify the values of the variables, you can act on the value of the wind speed by modifying the angle of incidence of the wind turbine blades which would amount to operating with lower wind speed, and thus away from the risk-of-error conditions. Therefore, as indicated, this methodology can be used in the decision-making of operational actions.
When older, this action would have the immediate effect of the increase of the OEE of the wind farm when it is substantially reduced as there would be no downtime due to error 1. However, although increased availability has a double effect on electricity production, on the one hand, electricity production increases during the hours we have increased availability, on the other hand, and we see reduced electricity production when the error conditions are given as lower wind speed is used to avoid the probability of such an error.
Similarly, you can act on the outside temperature in error 2. This error largely associated with the freezing of the anemometer has been eliminated in many wind farms by installing heat resistors thus modifying the outside temperature of the same. In this way, the value of one of the climatic variables has been modified by eliminating the combinatorial of variables that cause the error, which somewhat validates this methodology. Finally, as noted, this indicator is useful in choosing the maintenance strategies to be followed in wind farms.
The action of the variation of the blade angle not only has the effect on the elimination of error 1, but avoids the stops in full production caused by this error that subject the wind turbine components to stresses that can cause over time breakdowns in them. Therefore, it has a self-protection effect on wind turbines that will lead to a lower incidence of breakdowns over time, an increase in mean time between failure (MTBF) and greater durability of the equipment. This will also have a direct link in the wind farm’s life cycle, increasing their useful life and reducing the costs of operating the wind farm. On the other hand, at the moment of weather conditions where there is a probability of error, we can establish preventive maintenance actions aimed at avoiding it. In error 2, for example, greasing and cleaning of the anemometers could be performed to prevent their blockage.
Both preventive maintenance work on the different components of wind turbines and corrective maintenance work to repair faults that do not involve wind turbine shutdown are carried out whenever possible in periods of calm, i.e., where sufficient wind speeds are not given for electricity generation. In the case of having to be performed in productive periods, these works could be performed when the combination of values of weather conditions means there is a high probability of error. In this way, the unavailability generated with preventive or corrective maintenance work could be compensated with the possible unavailability in the event of the error associated with those conditions.
Everything above gives us an idea of the importance of this new approach in the study of the influence of climate variables on the occurrence of errors and the multiple advantages it brings us.