The share of electronic water meters installed in households has increased sharply in recent years. However, the current regulations are in large parts still tailored to traditional mechanical water meters. Electronic meters have already been included in the common standards, but reviews and various adaptions are still missing. An important point to be reviewed is the impact of the sampling interval of the electronic water meters on the measurement accuracy of the captured water volume. In this study, the error caused by the sampling interval is investigated by using measured data sets and stochastic water consumption data. It is shown that the error caused by sampling depends on the starting point of the sampling and the observation period. The studies show that for a billing period of one year, which is common in Germany, the sampling interval should be 14 s or less to always ensure a sampling-related error of less than 0.5%. Based on the results, input for further regulations is derived.

  • What influence does the type of interpolation in electronic water meters have on the accuracy of measurement?

  • Is there a type of interpolation that provides always the smallest measurement error?

  • What influence does the starting point of the sampling have on the measuring accuracy of a water meter?

  • What influence does the observation period have on the measurement accuracy of an electronic water meter?

Graphical Abstract

Graphical Abstract

Digitization is advancing in all areas worldwide and is also becoming increasingly important in the water supply sector. Since the launch of the first ultrasonic water meter in 2008 (Diehl Stiftung & Co. KG 2021), the share of electronic water meters installed, e.g., in households, has increased steadily in recent years (Doucet 2019). This trend is also visible in the global smart water metering market. The market was valued at $4.91 billion in 2020, and is projected to reach $9.73 billion by 2030, growing at a CAGR of 7.5% from 2021 to 2030 (Rake et al. 2021). However, it should be noted that in market analyses on smart water metering, electronic meters and mechanical meters with electronic add-on devices are often jointly considered. In addition, electronic water meters and flow meters with the same measuring principle are often grouped together. A general trend towards increasing use can be derived from this and is also reflected in the growing number of type approvals for electronic water meters. The reasons for an increased use of those meters are for example integrated additional functionalities such as leakage detection, a wider measuring range or less susceptibility to certain types of disturbances and installation situations. An up-to-date and comprehensive overview of electronic water meters, their measuring principles, aspects of remote reading and additional functionalities can be found in a brochure by DVGW (German association of the gas and water industry) (DVGW 2022).

‘Electronic water meters’ means here meters, which, due to the active measuring principle, require a secured power supply (internal battery) for determining water consumption. A significant difference between electronic and mechanical water meters concerns how and what they measure. Electronic meters do not measure the volume (m3) with moving mechanical parts as traditional water meters do. With electronic water meters the flow (L/h) is measured based on Faraday's law (magnetic-inductive water meters) or the run time of ultrasonic waves (ultrasonic water meters). Here, the measurement principle is based on the transit-time difference of the ultrasonic signal passing in the direction and in the opposite direction of the water flow. Electronic water meters were developed by several companies in parallel. The measuring principles are shown in Figure 1. Further details on the measurement principles can be found for example in Furness (1989).
Figure 1

(a) Measuring principle of an ultrasonic water meter; (b) measuring principle of a magnetic-inductive meter.

Figure 1

(a) Measuring principle of an ultrasonic water meter; (b) measuring principle of a magnetic-inductive meter.

Close modal

Both measuring principles used by electronic meters measure at discrete points in time in contrast to mechanical meters, which measure continuously. The consumed volume, which is needed for billing purposes, is calculated internally based on the integration of each determined flow through the cross-sectional area over time.

Independent from the measurement principle the manufacturers of water meters must demonstrate that the water meters are capable to measure the consumption correctly according to legal requirements. For this, amongst others the battery life of electronic water meters must be ensured for a defined period of time. A typical value is 15 years. However, since each measurement consumes energy, an attempt is made to keep the number of measurements at an absolutely necessary level to ensure a longer battery life. In normative documents such as ISO 4064:2014 or OIML R49:2013 no specifications are included for the frequency of measurements because the current versions were foremost developed for mechanical meters. Since electronic water meters came up at a later stage there are no regulations or recommendations for a sampling interval so far. The sampling interval can be set up by the manufacturer in dependence of the measurement principle for instance. For the magnetic-inductive method a quite short sampling interval could be defined because it is possible to measure the voltage, which is proportional to the flow, with a high temporal resolution. In contrast, the ultrasonic method has a restriction regarding the minimum sampling interval. Based on information by two water meter manufacturers (one among them Kamstrup A/S) and a water supplier (bnNETZE GmbH), the ultrasonic system requires at least 2 seconds for each calculation, which means that the highest feasible sampling interval for this type of meter is 2 seconds.

The sampling interval may have an influence on the measurement accuracy (measurement error) of the meter under real consumption conditions and depending on the considered time period. It is currently unclear how large the impact may be on the total captured volume. Currently, the measurement errors of water meters are determined (e.g. according to ISO 4064:2014 resp. OIML R49: 2013) from constant flow rates. For a constant flow, the effect of the sampling interval is negligible (van der Wiel et al. 2021). An error can arise because the start and end of the test do not need to be equal with the first or last discrete measuring point. This means that it is possible that at the beginning and at the end some volume would not be detected. However, a constant flow does not correspond to real conditions. Water meters operating under real consumption conditions where dynamic water flows are typical may have a larger measurement error due to the sampling interval. Under real conditions there may be periods with large deviations from the mean flow rate that will not be detected if they occur between single measurements. This would result in an under- or over-registration of the volume.

Till now there is no study about the impact of the sampling interval of a water meter on the measurement error at operating conditions. So far, a simple study on a washing machine fill cycle (66 s with 3.35 L) was done by Holmes-Higgin (2019). He shows that in this case due to a sampling interval of 4 seconds an error between −31.34 and +25.37% occurs in the measured volume depending on the start of the first measurement. For comparison the maximum permissible error (MPE) of a water meter at lower flow rates is maximum ±5% (OIML R 49 2013). Holmes-Higgin (2019) demonstrates in his study that there is a significant difference if the first measured value is equal to the start of the filling cycle, or if it is shifted between 1 and 3 seconds.

This simple study already illustrates that there may be a significant impact of the sampling interval and starting point on the accuracy of a discrete measurement. In a further study Eff (2020) shows something similar. In his study, a simple flow profile of a dispensing process is used to show the dependence of the measurement error by sampling interval on the starting point of the sampling. Additionally, he demonstrates that the measurement error is getting smaller with a longer observation period. For this, he used the simple flow profile as before but replicated it up to 500 times. He also carried out this investigation for the three test profiles of the EMPIR project 17IND13 ‘Metrology for real-world domestic water metering’ (MetroWaMet 2018), for which he obtained comparable results.

The studies by Holmes-Higgin (2019) and Eff (2020) are a good starting point, but in order to make reliable estimates of the effects of the sampling interval on the measurement accuracy of electronic water meters, further research with longer consumption profiles without cyclicities is needed. This was the motivation to address the issue more comprehensively. Several aspects were investigated in this study using real consumption profiles. The first part of the study focuses on the influence of the interpolation method used to calculate the total volume that passed the meter. Two simple interpolation types (rectangular and linear) are considered. In the second part the influence of the sampling interval itself on the measured volume is investigated. In addition, the influence of the observation period on the measurement error is addressed. Finally, the influence of the starting point of the sampling is studied.

Used data sets

Two different types of data sets, stochastic consumption data and consumption data measured in households, were used for the study. The consumption data directly measured in households are important, because for getting information about the effect of the sampling interval under real-world conditions without restrictions, only real consumption profiles can show the impact. The data used comes from a DVGW study from 2017 (Martin et al. 2017). For this study the water consumption in different houses (detached houses (DH) and apartment houses (AH)) of different German cities, were measured between 2014 and 2016. The consumption was monitored for time periods between 23 and 84 days with a resolution of 1 Hz. For the measurement in the DHs ultrasonic water meters with a permanent flow rate (Q3) of 4 m3/h and a ratio R of permanent flow rate to minimum flow rate (Q1) of 160 were used. Due to higher flow rates in AHs ultrasonic water meters with Q3 = 16 m3/h and R = 160 were deployed. This results in a good database of in total 58 consumption time series of different lengths (Schumann 2019). Out of the consumption of all DHs a real-world profile with a duration of one year can be derived. Since the data was recorded in different cities and in different years there exists no measured database for one house for one year. However, the database is sufficient for the aim of the investigations carried out here. Previous studies showed that there is neither a significant difference between countries nor a relevant seasonal effect on the water consumption (Schumann et al. 2021). For this reason, it is possible to put together a one year-long profile from different houses measured at different times.

For the AH it is possible to realize a data set of nine months (except January, February, and July). This means that a shorter observation period is considered, but this should be sufficient to show basic effects of the sampling interval on the measurement accuracy.

The second type of data is stochastic data. Schumann (2019) developed an algorithm, which can be used to derive stochastically assured consumption profiles out of measured consumption data. The stochastic data sets are based on the previously mentioned measured consumption data. With the algorithm an approximately 1 day-long profile (86,472 s) and an approximately 1 week-long profile (604,920 s) were generated. The day-long profile comprises flow data with a minimum flow duration of 3 s and a maximum of 108.33 s. The 1 with the length of approximately 1 week has also a maximum flow duration of 108.33 s but a minimum of 1 s. All stochastic data provides the duration of every flow point up to three digits, which, in contrast to the real data set, would allow an examination of the sampling interval smaller than 1 second in further studies.

The benefit of the stochastic profiles is that not only one house is considered, because the data reflects the consumption of all 58 houses. Furthermore, those stochastic profiles can be made accessible for everyone in contrast to the data directly measured at households and as such are classified as personal data. With those stochastic profiles novel water meters or measuring techniques can easily be tested for the influence of the sampling interval on the measuring accuracy. In addition, it is possible to conduct simple studies on the influence of changes in consumer behaviour, e.g., due to climate change with a reasonable effort.

Interpolation analyses

Since electronic water meters measure discretely, the flow between the individual measuring points must be interpolated to obtain the total quantity registered by the meter. The volume calculated in this way is shown on the meter's display and is used for billing. Therefore, the effect of interpolation on the total volume obtained is of interest. In a first step, it is necessary to be able to calculate the volume of each consumption profile previously described, which would theoretically be measured with a sampling interval tS (time between two measurement points). For this purpose, a script was written that can create time series with defined sampling intervals. Each time step is assigned the flow rate present at that time in the original data. The volume that would theoretically be displayed by the meter is calculated by the script in a second step. In this investigation two interpolation types are considered. One is the assumption of a constant flow rate between the measurement points (rectangular function) and the other is the assumption of a linear progression between two measurement points. Figure 2 schematically shows the flow rate Q assuming the two different types of interpolation. In addition, the volume V, which would result from each assumption is shown. The volume is corresponding to the area under the curve of the flow Q.
Figure 2

Schematic representation of the interpolation methods and the resulting volume.

Figure 2

Schematic representation of the interpolation methods and the resulting volume.

Close modal
The script calculates the theoretically measured volume under the assumption of a constant flow between the measuring points (rectangular) by using the sampling interval and the flow from the previously generated data according to Equation (1):
(1)

In case of the linear progression the volumes correspond to the surface area under the curve of the measuring points, too. This volume can be determined by the integral of the function, in which the measuring points are connected linearly. This integral is calculated by the data analysis and visualization program Origin (OriginLab Corporation 2022).

For the further investigations it is necessary to know the exact volume in addition to the volume calculated assuming the different types of interpolation. Therefore, the script determines similarly the real volume by using the exact duration of any flow from the original 1 s data:
(2)

Due to the recording frequency of 1 Hz this data has already a small error, which is unknown. In the study the 1 Hz recording is used as real consumption. Also, the stochastic data has this unknown error because the stochastic data results out of the 1 s data.

Table 1

Investigated sampling intervals

Sampling interval /s
10 
30 
60 
90 
120 
150 
180 
210 
240 
270 
300 
600 
Sampling interval /s
10 
30 
60 
90 
120 
150 
180 
210 
240 
270 
300 
600 

As can be seen in Figure 2, the different types of interpolation lead to different volumes. For the comparison of the linear and rectangular interpolation types the difference of the error based on the sampling interval is calculated for each sampling interval from Table 1 by:
(3)
Table 2

Overview of the investigations and data sets used

InvestigationMethodUsed profile
Influence of the interpolation types (linear and rectangular) Comparison of the error due to the sampling interval (2–600 s) with linear and rectangular interpolation Day-long stochastic profile 
Week-long stochastic profile 
Week-long measured profile 
Measured profile (AH over 55 days) 
Influence of the observation period Comparison of error changes when repeating the same profile up to 120 times Day-long stochastic profile 
Comparison of error changes when repeating the same profile up to 20 times One month of measured data (AH) 
Comparison of error changes by using different observation periods Real-world profile DH (from one month to one year) 
Influence of the starting point Comparison of error changes due to different sample times Day-long stochastic profile 
Week-long stochastic profile 
Real-world profile DH (one year) 
Real-world profile AH (nine month) 
InvestigationMethodUsed profile
Influence of the interpolation types (linear and rectangular) Comparison of the error due to the sampling interval (2–600 s) with linear and rectangular interpolation Day-long stochastic profile 
Week-long stochastic profile 
Week-long measured profile 
Measured profile (AH over 55 days) 
Influence of the observation period Comparison of error changes when repeating the same profile up to 120 times Day-long stochastic profile 
Comparison of error changes when repeating the same profile up to 20 times One month of measured data (AH) 
Comparison of error changes by using different observation periods Real-world profile DH (from one month to one year) 
Influence of the starting point Comparison of error changes due to different sample times Day-long stochastic profile 
Week-long stochastic profile 
Real-world profile DH (one year) 
Real-world profile AH (nine month) 

Sampling interval and observation time

In contrast to mechanical meters, where typical reasons for measurement deviations are the friction and abrasion of mechanical components, measurement deviations in ultrasonic meters can be caused by the sampling interval in addition to deposition and abrasion effects.

The measurement error due to the sampling interval ε is calculated from the ratio of the difference of the directly measured volume to the theoretically measured volume (corresponds to or ) according to:
(4)
The error calculated here represents the error caused only by the sampling interval for one special case. Furthermore, in the study several cases like different months are considered. When considering multiple cases, the maximum error of all considered cases is of interest in assessing the sampling interval, since a water meter must always measure in legal limits, regardless of the time of observation:
(5)

The maximum error is used to identify the sampling intervals where the error exceeds defined limits, e.g. 1%, in the data set under consideration for the first time. For this purpose, the use of is very suitable, because for the same sampling interval smaller errors than can occur when considering several profiles. These smaller errors are not relevant for an evaluation in this study. The maximum error is used to investigate the influence of the observation period, and the start of the sampling on the error.

To assess the impact of the observation period the stochastic profiles and a directly measured consumption profile of an AH were multiplied several times. The stochastic profiles were replicated up to 120 times to simulate different observation lengths and to investigate if the maximum error becomes smaller when longer observation intervals are considered as found by Eff (2020). Although the stochastic profile has a duration of slightly longer than 1 day by 72 s), cyclical effects can still occur if the sampling interval has no residual at the end of the profile. To avoid those cyclical effects the profile was shifted at each repetition for 1/120 of the sampling interval. Sampling intervals between 2 and 120 s in 1 s steps were used. The profile of the AH was replicated up to 20 times. Due to the exact length of one month, there are more cases with no balancing effects. To avoid those cases, the profile was shifted at each replication for 1/120 of the sampling interval, as was done for the stochastic profile.

In a next step the real-world profile was considered with different lengths of the observation time (one month up to one year) to assess the influence of the observation period under real consumption conditions.

Additionally to the length of the period under consideration and the length of the sampling interval itself, the point in time of the sampling may also affect the determined volume and thus provide an additional error source (Holmes-Higgin 2019). To gain more insights into this error source under real consumption conditions the points in time at which samples were taken were changed and the impact on the total volume considered. For this, the starting point of the profile was shifted. In all cases the consumption data before the new starting point was added at the end. This has the consequence that in all instances the total consumption is identical independent from the starting point. For the day-long stochastic profile the starting point of the sampling was shifted exemplarily once by 1803 s (∼30 min) and 43,341 s (∼12 h). Analogously the stochastic week-long profile was obtained. Due to the longer profile, the starting point was additionally shifted by 86,168 s (∼24 h). For the investigation of directly measured consumption the real-world profile of a DH was used. The real-world profile was shifted three times by three months (one quarter) to start the sampling at a different season of the year. To gain insights into the effect of only small time shifts, the time at which the samples are taken was shifted for 1 s, 2, 5 and 10 s for the real-world profile.

Table 2 provides an overview of which investigations were conducted using which data in the present study.

Effect of the interpolation types

To evaluate the effect of the two types of interpolation, linear and rectangular, which were discussed previously, the resulting volumes are compared. The error based on the sampling interval is calculated for the stochastic day and week profiles. Both stochastic profiles yield comparable results. Figure 3 shows the results for the stochastic day-long profile exemplarily.
Figure 3

(a) Theoretical measurement error obtained for different time steps for linear progression and rectangular function used as interpolation method for the stochastic day-long profile and the difference between those progressions. (b) Detailed view for sampling intervals up to 60 s.

Figure 3

(a) Theoretical measurement error obtained for different time steps for linear progression and rectangular function used as interpolation method for the stochastic day-long profile and the difference between those progressions. (b) Detailed view for sampling intervals up to 60 s.

Close modal

From Figure 3(b) it can be seen that the type of interpolation has a negligible influence on the measurement error at timesteps smaller than 60 s (). At timesteps greater than 60 s the difference between linear and rectangular interpolation becomes slightly larger (up to 0.93% difference at a sampling interval of 600 s). The difference between linear and rectangular interpolation is becoming almost linearly larger with larger sampling intervals.

Furthermore, the influence of the interpolation method on a directly measured consumption profile of an AH over 55 days was also considered. The error obtained for the real-world profile is less affected by the interpolation type as the stochastic profiles. In this case even at larger timesteps the influence of the interpolation is quite low. At the largest timestep of 600 s the difference between the interpolations is only 0.25%. As before, the difference is becoming almost linearly larger with a larger sampling interval. One possible reason for the smaller difference could be the longer observation time of 55 days instead of 1 day or 1 week. This assumption is confirmed, as a measured profile of 1 week shows comparable differences as the stochastic profile with the same length.

Based on these results, the rectangular function is used in the subsequent investigations, because the calculations can be performed much faster using the rectangular function as interpolation method. Furthermore, the focus is on sampling intervals below 120 s in the error determination, since in this range the differences between the interpolation types are very small.

Influence of the observation period

As already seen in the comparison of the interpolation types, the observation period has an influence on the difference between the error of linear and rectangular interpolations. Whether the observation period also influences the measurement error is examined in the following. In a first step, the stochastic day profile is investigated regarding the influence of the observation period. Since the error ɛ due to the sampling interval varies around zero in all cases, the absolute value of the error is used in Figure 4(a) for an easier assessment of the sampling interval. For sampling intervals shorter than 16 s an error below 0.5% is caused. A maximum error of 5% occurs at a sampling interval of 113 s. The stochastic 1 week-long profile shows a similar behaviour, but the error of the original profile exceeds the error limit of 0.5% after 30 s for the first time. It follows that the longer observation period for the stochastic 1 week-long profile compared to the stochastic 1 day-long profile already leads to smaller errors.
Figure 4

(a) Errors due to the sampling interval derived from the stochastic 1 day-long profile (b) Impact on the maximum overall occurring error due to number of repetitions of the stochastic 1 day-long profile.

Figure 4

(a) Errors due to the sampling interval derived from the stochastic 1 day-long profile (b) Impact on the maximum overall occurring error due to number of repetitions of the stochastic 1 day-long profile.

Close modal

The results shown in Figure 4(b) confirm the expectation that due to averaging the error becomes smaller for longer observation periods.

The overall occurring maximum error based on the sampling interval is getting smaller with each repetition. After 120 repetitions the maximum error due to the sampling interval is still larger than 0.4%. The maximum error is becoming smaller but there seems to be a limit so that the error never gets close to zero or many more repetitions are needed for getting an error close to zero.

Analogously, a profile of an AH with a duration of one month was considered. The errors of all sampling intervals, which have a residual at the end of the profile, are again getting smaller with a higher number of repetitions.

To obtain a general overview of the influence of the sampling interval on the thereby arising errors of the real-world consumption profile (DH), intervals up to 600 s in 1 s steps were considered (Figure 5). The start time (1st of January) is identical for all sampling intervals.
Figure 5

Errors due to the sampling interval derived from the real-world profile (DH) of one year length and linear fit; sampling intervals between 2 and 600 s were considered.

Figure 5

Errors due to the sampling interval derived from the real-world profile (DH) of one year length and linear fit; sampling intervals between 2 and 600 s were considered.

Close modal

Figure 5 shows that in this case for a sampling interval of 28 s the error exceeds 1% for the first time, but even at a sampling interval of 600 s the error based on the sampling interval amounts to only 0.08% in this example. However, at a sampling interval in between the error can reach an order of magnitude of several percent. Overall, the errors fluctuate quite strongly depending on the sampling interval. For example, a sampling interval of 565 s causes an error of 8.23% and an interval of 566 s results in an error of 0.24%. The linear regression, which is a crude approach shows the trend, that with larger sampling intervals the error is generally getting larger.

Sampling intervals larger than a few seconds seem not conceivable, because the error in previous cases exceeds 1% for a sampling interval of 28 s for the first time. In order to exclude that in other cases possible compensatory effects have a significant influence, e.g., the 1% limit is exceeded the first time for a longer sampling interval, and the following investigations are nevertheless carried out for sampling intervals up to 120 s.

The averaging effect, which occurs for the data set consisting of a repeated daily stochastic profile, should be visible for the real-world profile based on the data of different detached houses too. Four different profile lengths were considered (one month, three months, half a year and one year) corresponding to different (theoretical) billing periods. For one month, three months and half a year observation periods the maximum error for sampling intervals between 2 and 120 s is shown in Figure 6(a)–6(c). In Figure 6(d) the error due to the sampling interval is given for one year with the start of the sampling on 1st of January. In all diagrams in Figure 6 a linear trend of the error depending on the sampling interval for the different observation periods can be seen. The error again becomes smaller with longer observation periods. The maximum overall occurring error for an observation time of one month (a) is 16.69%, for three months (b) 8.36% and for one year (d) a mere 2.53%.
Figure 6

Impact of the maximum error for different observation periods Additionally, the linear regression of the maximum errors for each observation period is shown.

Figure 6

Impact of the maximum error for different observation periods Additionally, the linear regression of the maximum errors for each observation period is shown.

Close modal

Typically, one year is used as billing period for potable water consumption, e.g. in Germany. During this time the error of the meter based on the sampling interval must be negligible, because additionally each meter has always an unknown measurement error. If the error based on the sampling interval is close to the permitted limit it cannot be guaranteed that the water meter is measuring the volume within the tolerance range correctly. Based on the examples shown in Figure 6 the error of the sampling interval exceeds the limits in Table 3 at different times. With longer observation periods, the limit values are exceeded first at a larger sampling interval.

Table 3

Overview at which sample interval the error exceeds the first time the limits given in the first row

Observation periodεmax > 0.25%εmax > 0.5%εmax > 1%εmax > 1.5%εmax > 2%
One month 3 s 4 s 8 s 12 s 12 s 
Three months (quarter) 5 s 7 s 14 s 20 s 27 s 
Half-a year 9 s 12 s 27 s 38 s 43 s 
One year 10 s 26 s 28 s 84 s 86 s 
Observation periodεmax > 0.25%εmax > 0.5%εmax > 1%εmax > 1.5%εmax > 2%
One month 3 s 4 s 8 s 12 s 12 s 
Three months (quarter) 5 s 7 s 14 s 20 s 27 s 
Half-a year 9 s 12 s 27 s 38 s 43 s 
One year 10 s 26 s 28 s 84 s 86 s 

Influence of the start of the sampling

So far only the effect of the sampling interval was considered, but the starting point was kept identical.

Because also the start of the sampling has an influence on the error, the start of the sampling was shifted. The error due to the sampling interval of the three considered starting points (not shifted, shifted by 1803 and 43,341 s) is shown in Figure 7(a). The error caused by the sampling interval is also not single-sided (cf. Figure 7(a)) for the stochastic day-long profile. For an easier interpretation the points are connected in Figure 7(a). Please note that the maximum error shown in Figure 7(b) serves only for illustration. It represents only the error which occurs for those three cases. With other shifts of the starting point different errors may result.
Figure 7

(a) Error of the 1 day-long stochastic profile. (b) Total error of the stochastic 1 day-long profile.

Figure 7

(a) Error of the 1 day-long stochastic profile. (b) Total error of the stochastic 1 day-long profile.

Close modal

Depending on the starting point of the sampling a notable difference in the error is arising. For example, a sampling interval of 87 s causes for the original profile an error of −3.46% and for the shifted profile an error of 5.34%. For the considered cases the maximum occurring error is increasing with the length of the sampling interval. As expected, the stochastic 1 week-long profile yields comparable results to the 1 day-long profile.

The impact of the time shift on the real-world profile is shown in Figure 7. The influence of small time shifts is shown in Figure 7(a). For an easier interpretation the points are connected in Figure 7(a) and 7(c) analogous to Figure 7(a).

The starting time of the sampling has also a large influence in case of the directly measured consumption profile. Due to the different starting points the error limits from Table 3 were reached partly earlier as can be seen in Figure 8(d). The 0.25% limit is reached the first time already at a sampling interval of 7 s (instead of 10 s) and the 0.5% limit at a 14 s sampling interval (instead of 26 s). Furthermore, with a sampling interval of 67 s, the 1.5% limit is reached instead of 84 s.
Figure 8

(a) & (c) Error due to the sampling interval with different starts of the sampling (b) Difference in the errors between the original profile and different small time shifts (d) maximum occurring error of the time shifts of c; please note the different scaling of the y-axis.

Figure 8

(a) & (c) Error due to the sampling interval with different starts of the sampling (b) Difference in the errors between the original profile and different small time shifts (d) maximum occurring error of the time shifts of c; please note the different scaling of the y-axis.

Close modal

That even small time shifts of a few seconds cause a different error becomes visible in Figure 8(b). The difference between the errors of the original one-year profile with a sampling start on 1st of January at midnight and a 1 s shifted profile causes a change of the error up to 0.79% for a sampling interval of 117 s. However, even at small sampling intervals the difference is not negligible (0.19% at a sampling interval of 10 s). The time shifts of 2, 5 and 10 s have a similar influence. Depending on the limit value to be complied with, a shift in the start time can already lead to errors outside the tolerance range of Table 3, but in comparison to Holmes-Higgin (2019) the differences due to small time shifts are quite small. A possible reason could be the longer observation time and the associated higher water consumption.

The analysis concerning the starting point of the sampling was repeated for consumption profiles of AHs. Here, comparable results were obtained to those discussed previously.

This study was carried out to get first insights into the influence of the sampling interval of electronic water meters on the determined consumption volume and the associated error. For this purpose, consumption profiles based on real measured data and stochastic consumption profiles were investigated regarding the influence of the interpolation between two samples, the influence of the starting point of the sampling and the length of the observation period (=billing period). The investigations are intended to help clarify the question of whether requirements should be placed on the interpolation type or the length of the sampling interval when data from electronic water meters are used for consumption billing.

In principle, stochastic and real data lead to comparable results in all investigations as should be expected.

The comparison of the interpolation types shows that linear and rectangular interpolation between samples lead to comparable results for timesteps lower than 120 s. The difference between those interpolation types grows linearly with the duration of the sampling interval and becomes smaller with longer observation times. Regarding the interpolation method, no further requirements seem to be necessary.

A clear dependence on the start time of the sampling is found. Already with small time shifts (even 1 s) the error due to the sampling interval can change significantly. Thus, by looking at a single start time, no conclusion can be drawn about the error caused by the discrete measurement. From this it follows that for an evaluation of different profiles it is necessary to look at different start times of the sampling.

With longer observation times the sampling related error is generally getting smaller, although it can happen that for individual sampling intervals due to compensation effects the resulting error is smaller for short observation periods than for longer. However, it turns out that the considered limit values of the error between 0.25 and 2% are exceeded earlier for short observation periods than for longer ones. From the cases studied it follows that for an observation period of one year and a sampling interval of 14 s or below, the error is less than 0.5%. For an observation period of one month, the sampling interval must be less than 4 s to ensure an error of less than 0.5%. Measuring 0.5% too much or too little has different effects on billing depending on the country. The average water price per cubic meter was 3.4 € for a consumption of 120 m3 per year. However, the price in Europe varies widely, from free water in Ireland to 9 €/m3 in Denmark. Additionally, water consumption per capita per day varies widely, ranging from 85 L in Lithuania to 240 L in Italy (EurEau 2017). Considering the average values, an error of 0.5% means that the customer would pay 2.04 € less. At the moment, the impact on costs seems relatively small, but it is likely to increase in the coming years due to rising energy costs, further increasing the importance of accurate billing.

All the investigations carried out here show the fundamental influences of the sampling interval on the total volume recorded by the meter based on European consumption behaviour. The results cannot be applied to the world market without further verification. Actions are needed in defining the maximum sampling interval. When determining the limit value, it must be considered that the assumption of an ideal water meter was made in this study. Under real conditions other influencing factors such as temperature, air bubbles or particle load also affect the meter's measurement accuracy. The future challenge will be to define a sampling interval that ensures that the maximum error that occurs never exceeds a predefined limit. Which limit for the maximum error is acceptable must be determined by the relevant standardization bodies.

Data cannot be made publicly available; readers should contact the corresponding author for details.

The authors declare there is no conflict.

bnNETZE GmbH Digitale Funkwasserzähler – das sollten Sie wissen (Digital water meters what you should know)
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