Oxygen consuming substances in European rivers

Indicator Assessment
Prod-ID: IND-20-en
Also known as: CSI 019 , WAT 002
expired Created 11 Oct 2010 Published 20 Dec 2010 Last modified 11 Sep 2015
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Concentrations of BOD and total ammonium have decreased in European rivers in the period 1992 to 2009 (Fig. 1), mainly due to general improvement in wastewater treatment. See also WISE interactive maps:   Mean annual BOD in rivers and Mean annual Total Ammonium in rivers

Key messages

Concentrations of BOD and total ammonium have decreased in European rivers in the period 1992 to 2009 (Fig. 1), mainly due to general improvement in wastewater treatment.

See also WISE interactive maps:

 Mean annual BOD in rivers and Mean annual Total Ammonium in rivers




Is organic matter and ammonium pollution in European rivers decreasing?

Biochemical Oxygen Demand (BOD5) and total ammonium concentrations in rivers between 1992 and 2008

Note: Concentrations are expressed as the average of annual mean concentrations. Up to 3-year gaps of missing values have been interpolated or extrapolated. Only complete series with no missing values after this interpolation/extrapolation are included. Number of river monitoring stations included in analysis per country is noted in brackets. BOD7 data has been recalculated into BOD5 data.

Data source:
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BOD5 concentrations in rivers between 1992 and 2008 in different geographic regions of Europe

Note: Concentrations are expressed as the average of annual mean concentrations. Up to 3-year gaps of missing values have been interpolated or extrapolated. Only complete series with no missing values after this interpolation/extrapolation are included. The number of river monitoring stations included in the analysis per geographic region is noted in brackets. BOD7 data (Estonia, Finland, Lithuania (1996-2008), Latvia (1996-2001)) has been recalculated into BOD5 data.

Data source:

Waterbase - Rivers (version 10)

http://www.eea.europa.eu/data-and-maps/data/waterbase-rivers-6

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Total ammonium concentrations in rivers between 1992 and 2008 in different geographic regions of Europe

Note: Concentrations are expressed as the average of annual mean concentrations. Up to 3-year gaps of missing values have been interpolated or extrapolated. Only complete series with no missing values after this interpolation/extrapolation are included. Number of river monitoring stations included in analysis per country and region is noted in brackets.

Data source:
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BOD5 concentrations in rivers between 1992 and 2008 in different sea regions of Europe

Note: Geographical coverage: Atlantic Ocean, Baltic Sea, Black Sea, Mediterranean Sea and the North Sea.

Data source:
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Total ammonium concentrations in rivers between 1992 and 2008 in different sea regions of Europe

Note: Geographical coverage: Atlantic Ocean, Baltic Sea, Black Sea, Mediterranean Sea and the North Sea.

Data source:
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Introduction
Organic matter, measured as Biochemical Oxygen Demand (BOD) and ammonium, are key indicators of the oxygen content of water bodies. Concentrations of these parameters normally increase as a result of organic pollution caused by discharges from waste water treatment plants, industrial effluents and agricultural run-off. Severe organic pollution may lead to rapid de-oxygenation of river water, a high concentration of ammonia and the disappearance of fish and aquatic invertebrates.

The most important sources of organic waste load are: household wastewater; industries such as paper industries or food processing industries; and silage effluents and manure from agriculture. Increased industrial and agricultural production, coupled with a greater percentage of the population being connected to sewerage systems, initially resulted in increases in the discharge of organic waste into surface water in most European countries after the 1940s. Over the past 15 to 30 years, however, the biological treatment (secondary treatment) of waste water has increased, and organic discharges have consequently decreased throughout Europe. See also CSI 024: Urban waste water treatment.


Overall trend in BOD and total ammonium (Fig. 1)
In European rivers, the oxygen demanding substances measured as BOD and total ammonium have decreased by 50 % (from 4.7 mg/l to 2.4 mg O2/l) and 66 %  (from 800 to 275µg N/l),respectively, from 1992 to 2009 (Fig. 1). The decrease is due mainly to improved sewage treatment resulting from the implementation of the Urban Wastewater Treatment Directive. The economic downturn of the 1990s in central and eastern European countries also contributed to this fall, as there was a decline in heavily polluting manufacturing industries. In recent years, however, the downward trends in BOD across Europe have generally levelled. This suggests that either further improvement in wastewater treatment is required or that other sources of organic pollution, for example from agriculture, require greater attention, or both.

Overall there has been a significant decrease in BOD concentrations at 55.8% of the stations (an additional 6.1 % marginally significant) on the European rivers between 1992 and 2009, while there has been a significant increase at only 2.9 % of the stations (an additional 0.8% marginally significant). Similarly, there has been a significant decrease in total ammonium concentrations at 54.4 % of the stations (an additional 5.2 % marginally significant), while there has been a significant increase at only 3.7 % of the stations (an additional 1.1 % marginally significant).

BOD and total ammonium time series and trends per geographic regions (Fig. 2 and Fig. 3)

The largest decrease of BOD from 1992 to 2009 has occurred in the southern European rivers (63 %), represented by the Spanish rivers only (Figure 2). However, their concentrations are still higher than concentrations in other regions except for the southeastern Europen rivers with the highest concentrations in Europe (above 4 mg O2/l). The second largest decrease has occurred in the western European rivers (48 %) with the lowest concentrations since 2001 (below 2 mg O2/l). The decrease is similar in the southeastern (42 %) and the eastern European rivers (43 %). The northern European rivers have the lowest decrease (24 %). Their concentrations are represented by the Finnish rivers with low concentrations since 1992 (around 2 mg O2/l).

The largest proportion of monitoring stations with significant or marginally significant negative trend in BOD is found for the western and the southern European rivers, while the lowest proportion is found for the northern European rivers. Based on the sum of significant and marginally significant trends the trends for the rivers in different geographic regions are: West: 68.1 % negative, 0.7 % positive, South: 62.7 % negative, 1.9 % positive, East: 58.6 % negative, 7.2 % positive, Southeast: 50 % negative, 8.8 % positive, North: 26.7 % negative, 6.7 % positive). Countries with more than 60 % of the stations with negative trend in BOD are Hungary, the United Kingdom, Spain, the Czech Republic, Luxembourg, Ireland, Austria, France, Denmark, Slovakia and Slovenia.

The decrease of total ammonium from 1992 to 2009 is the largest in the eastern (77 %) and the western European rivers (75 %), followed by the decrease in the southeastern European rivers (66 %) (Figure 3). The concentrations in the southern European rivers (Spanish rivers, respectively) have decreased by 47 %. These concentrations are very fluctuating and the highest in Europe (above 900 µg N/l since 2006). On the contrary, concentrations in the northern European rivers are the lowest (below 40 µg N/l since 2007) and relatively stable with a decrease of 22 %.
The largest proportion of monitoring stations with significant or marginally significant negative trend in total ammonium is found for the western and eastern European rivers, while the lowest proportion is found for the northern European rivers as follows: West: 71.2 % negative, 3.0 % positive, East: 64.5 % negative, 2.8 % positive, Southeast: 62.1 % negative, 2.1 % positive, South: 54.1 % negative, 7 % positive, North: 27.8 % negative, 11.5 % positive (sum of significant and marginally significant trends). Countries with 60 % or more stations with negative trend in total ammonium are Norway, Austria, Bulgaria, France, Latvia, Luxembourg, FYR of Macedonia, Belgium, Poland, Ireland, the United Kingdom, Germany, Lithuania and Slovenia.

BOD and total ammonium time series and trends per sea regions (Fig.  4 and Fig. 5)
The largest decrease of BOD from 1992 to 2009 has occurred in the rivers draining to the Mediterranean Sea (72 %), followed by the decrease in the rivers draining to the Black Sea (52 %) (Figure 4). The decrease is somewhat lower in the rivers draining to the Greater North Sea (34 %) and the Celtic Seas, the Bay of Biscay and the Iberian Coast (30 %). The lowest decrease has occurred in the rivers draining to the Baltic Sea (24 %) with more or less stable concentrations since 1992 (around 2 mg O2/l). The concentrations among rivers in different sea catchments have become similar in recent years (Baltic Sea - Mediterranean Sea: below 2 mg O2/l; Greater North Sea - Black Sea: above 2 mg O2/l), except for the rivers draining to the Celtic Seas, the Bay of Biscay and the Iberian Coast. Their concentrations are the highest in Europe (about 3 mg O2/l) and have increased since 2005.

The trend analysis also shows that the largest proportion of monitoring stations with significant or marginally significant negative trend in BOD is found for the rivers draining to the Mediterranean Sea, while the lowest proportion is found for the rivers draining to the Baltic Sea (Mediterranean Sea: 80.4 % negative, 4.2 % positive, Black Sea: 70.9 % negative, 1.5 % positive, Greater North Sea: 59.4 % negative, 2.8 % positive, Celtic Seas, Bay of Biscay, Iberian Coast: 42.7 % negative, 1.9 % positive, Baltic Sea: 39.9 % negative, 11.9 % positive; sum of significant and marginally significant trends).

The largest decrease of total ammonium from 1992 to 2009 has occurred in the rivers draining to the Black Sea, the Greater North Sea, the Mediterranean Sea (all 74 %) and the Baltic Sea (73 %) (Figure 5). Concentrations in these sea catchments have become similar in recent years (between 130 and 300 µg N/l). Furthermore, the decrease is similar for the rivers draining to the Arctic Ocean (48 %), and the Celtic Seas, the Bay of Biscay and the Iberian Coast (46 %). The concentrations of the first are the lowest in Europe (about 5 µg N/l), while the concentrations of the second are very fluctuating and the highest in Europe (above 800 µg N/l since 2006).

The largest proportion of monitoring stations with significant or marginally significant negative trend in total ammonium is found for the rivers draining to the Greater North Sea and the lowest proportion is found for the rivers draining to the Arctic Ocean (Greater North Sea: 69.6 % negative, 2.8 % positive, Black Sea: 59.9 % negative, 3.0 % positive, Mediterranean Sea: 59.2 % negative, 4.9 % positive, Celtic Seas, Bay of Biscay, Iberian Coast: 58.2 % positive, 7.0 % negative, Baltic Sea: 54.3 % negative, 6.3 % positive, Arctic Ocean: 30.8 % negative, 7.7 % positive; sum of significant and marginally significant trends).

BOD and total ammonium present concentrations by countries

See WISE interactive maps for information displayed for countries, for river basin districts (BOD) and for individual stations: 

Mean annual BOD in rivers and Mean annual Total Ammonium in rivers

Countries with more than 50 % of all river stations with the lowest BOD concentrations (class 1: < 1.4 mg O2/l) for 2009 or the latest reported year are the United Kingdom, Latvia, Austria, Croatia, Spain, the Netherlands, Ireland, Denmark and Slovenia. Countries with more than 20 % of the stations with the highest BOD concentrations (class 5: >= 4 mg O2/l) are Lithuania, Romania, Hungary, Belgium, Bulgaria, Sweden, Albania, Turkey and FYR of Macedonia.

Countries with more than 50 % of all river stations with the lowest total ammonium concentrations (class 1: < 0.04 mg N/l) for 2009 or the latest reported year are Spain, Austria, Cyprus, Croatia, Sweden, Bosnia and Herzegovina, Ireland, Slovenia, Finland, the United Kingdom, Iceland, Liechtenstein and Norway. Countries with 20 % or more stations with the highest total ammonium concentrations (class 5: >= 0.4 mg N/l) are FYR of Macedonia, Greece, Romania, Bulgaria, Luxembourg, Albania and Belgium.





Indicator specification and metadata

Indicator definition

This indicator illustrates current biochemical oxygen demand (BOD) and concentrations of total ammonium (NH4) in rivers, and examines trends in both. The key indicator for the oxygenation status of water bodies is BOD, which is the demand for oxygen resulting from organisms in water that consume oxidisable organic matter.

Units

The units used in this indicator are annual average BOD after 5 or 7 days incubation (BOD5/BOD7), expressed in mg O2/l, and annual average total ammonium concentrations expressed in µg N/l.


Policy context and targets

Context description

There are a number of EU directives that aim to improve water quality, and reduce the loads and impacts of organic matter. First, the Water Framework Directive requires the achievement of good ecological status or good ecological potential of rivers across the EU by 2015 and repeals, step-by-step, several older water related directives. Alongside this, the following directives stay in place: the Nitrates Directive (91/676/EEC), aimed at reducing nitrate and organic matter pollution from agricultural land; the Urban Waste Water Treatment Directive (91/271/EEC), aimed at reducing pollution from sewage treatment works and certain industries (see also CSI24 Urban waste water treatment); and the Integrated Pollution Prevention and Control Directive (96/61/EEC), aimed at controlling and preventing the pollution of water by industry.

Targets

This indicator is not related directly to a specific policy target but shows the efficiency of waste water treatment (see also the Urban waste water treatment indicator).

The environmental quality of surface waters with respect to organic pollution and ammonium, and the reduction of the loads and impacts of these pollutants are, however, objectives of several directives. These include the Surface Water for Drinking Directive (75/440/EEC), which sets standards for the BOD value of surface water intended for the abstraction of drinking water. The level should not exceed 3 mg O2/l if the water is intended for abstraction with simple physical treatment and disinfection only, e.g. rapid filtration and disinfection.

A subsequent Drinking Water Directive 98/83/EC does not set guideline or mandatory values of BOD but defines indicator limits for ammonium: remedial actions for improving drinking water quality should be taken if an indicator value of 500 µg NH4/l (i.e. 388 µg N/l) is exceeded.

The guide values of BOD and ammonium are also set in the Fish Directive (2006/44/EC) and focus on supporting fish life, while also aiming at improving and maintaining freshwater quality from an ecological and economic point of view. BOD values should not exceed 3 mg O2/l in salmonid waters and 6 mg O2/l in cyprinid waters, while ammonium concentrations should not exceed 40 µg NH4/l (i.e. 31 µg N/l) in salmonid waters and 200 µg NH4/l (i.e. 155 µg N/l) in cyprinid waters.

Related policy documents

Methodology

Methodology for indicator calculation

Data source
The data on water quality on rivers in Waterbase are collected annually through the WISE SoE — Water Quality (WISE-4) data collection process. It includes data on nutrients, organic matter, hazardous substances and general physico-chemical parameters, as well as biological data. This reporting obligation is an Eionet core data flow. A request is sent to National Focal Points and National Reference Centres every year with reference to templates to use and guidelines. As of 2015, WISE SoE — Water Quality (WISE-4) supersedes Eurowaternet reporting on river quality (EWN-1).

The data in Waterbase are a sub-sample of national data assembled for the purpose of providing comparable indicators of the pressures, state and impact of waters on a Europe-wide scale. The data sets are not intended for assessing compliance with any European directive or any other legal instrument. Information on the sub-national scales should be sought from other sources.

Monitoring sites selection
Data from all reported monitoring sites are extracted for the indicator assessment. Some data are excluded following the QC process (see QC below). The time series and trend analysis are based on complete time series only (see Inter/extrapolation and consistent time series below).

Determinants
The determinands selected for the indicator and extracted from Waterbase are BOD5, BOD7 and ammonium.

Most countries monitor BOD5. Finland monitors BOD7. Lithuania monitored BOD5 up to 1995 and started monitoring BOD7 in 1996. Latvia monitored BOD7 from 1996 to 2001. Estonia has monitored BOD5 since 2010, replacing BOD7 which was monitored until 2009. 'BOD' is commonly used for BOD5. To be comparable the data of BOD7 have been converted to BOD5 (BOD7=1.16 BOD5).

All countries reported total ammonium until 2006. In 2007, Greece and Liechtenstein started reporting ammonium instead of total ammonium. Instead of total ammonium, Cyprus, Lichtenstein and Slovenia began reporting ammonium in 2008, as did Austria and the Netherlands in 2009, Bulgaria and Latvia in 2010, and Estonia, Norway and Poland in 2011. Besides total ammonium, Slovakia also started to report ammonium for some stations in 2008. Belgium, Germany, Italy, Luxembourg, Slovakia and the United Kingdom report either ammonium or total ammonium for an individual station in a selected year from 2008. Data for either of the two determinands were included in the assessment. For those stations in Slovakia where both were reported, total ammonium data were included in the assessment.

Mean
Annual mean concentrations are used as a basis in the present concentration and indicator analyses. Unless the country reports aggregated data, the aggregation to annual mean concentrations is done by the EEA. Countries are asked to substitute any sample results below the limit of quantification (LOQ) by a value equivalent to half of the LOQ before calculating the site annual mean values. The same principle is applied by the EEA.

The annual data in most cases represent the whole year, but data are used also if they represent shorter periods. Up until 2012, data could be reported at different temporal aggregation levels. Here, annual data have been selected, but if these were not available, seasonal data were selected according to a specific order of preference.

Quality control (QC)
An automatic QC procedure is applied when data are reported. Automatic outlier tests based on z-scores are also applied, both to the disaggregated and aggregated data, excluding data failing the tests from further analysis. In addition, a semi-manual procedure is applied to identify issues that are not identified in the automatic outlier tests. The focus is particularly on suspicious values having a major impact on the country time series and on the most recently reported data. This comprises e.g.:
• values deviating strongly from the whole time series;
• values not so different from values in other parts of the time series, but deviating strongly from the values closer in time;
• consecutive values deviating strongly from the rest of the time series (including step changes);
• whole  time series deviating strongly in level compared with other time series for that country and determinand;
• where values for a specific year are consistently far higher or lower than the remaining values for that country and determinand.
Such values are removed from the analysis (both time series/trend and present state analysis) and checked with the countries. Depending on the response from the countries, the values are corrected, flagged as outliers or flagged as confirmed valid. Any response affecting the indicator analysis is corrected in the next update of the indicator.


Inter/extrapolation and consistent time series

For time series and trend analyses, only series that are complete after inter/extrapolation (i.e. no missing values in the monitoring site data series) are used. This is to ensure that the aggregated time series are consistent, i.e. including the same monitoring sites throughout the time series. In this way, assessments are based on actual changes in concentration rather than changes in the number of monitoring sites. For the trend analysis, it is essential that the same time period is used for the different monitoring sites, so that the results are comparable.

Changes in methodology: Monitoring site selection and inter/extrapolation
Until 2006, only complete time series (values for all years from 1992 to 2004) were included in the assessment. However, a large proportion of the monitoring sites were excluded by this criterion. To allow the use of a considerably larger share of the available data, it was decided in 2007 (i.e. when analysing data up until 2005) to include all time series with at least 7 years of data. This was a trade-off between the need for statistical rigidity and the need to include as many data as possible in the assessment. However, the shorter series included might represent different parts of the whole time interval and the overall picture may therefore not be reliable.

In 2009, it was decided to inter/extrapolate all gaps of missing values of 1-2 years for each monitoring site. At the beginning or end of the data series, one missing value was replaced by the first or last value of the original data series, respectively. In the middle of the data series, missing values were replaced by the values next to them for gaps of 2 years and by the average of the two neighbouring values for gaps of 1 year.

In 2010, this approach was modified, allowing for gaps of up to 3 years, both at the ends and in the middle of the data series. At the beginning or end of the data series, up to 3 years of missing values were replaced by the first or last value of the original data series, respectively. In the middle of the data series, missing values were replaced by the values next to them, except for gaps of 1 year and for the middle year in gaps of 3 years, where missing values are replaced by the average of the two neighbouring values.

In 2018, this approach was slightly modified using linear interpolation for gap filling in the middle of the time series. Moreover, if data were available from 1989-1991 these were applied in the gap filling procedure, making it possible to interpolate instead of extrapolating at the beginning of the time series.

Only time series with no missing years for the whole period from 1992 (or from 2000) after such inter/extrapolation are included in the assessment. This gap filling procedure increases the number of monitoring sites that can be included in the time series/trend analysis. Using the shorter time period starting in 2000 allows for the inclusion of more monitoring sites, making the analysis more representative. Still, the number of monitoring sites in the time series/trend analysis is markedly lower compared with the analysis of the present state, where all available data can be used.

Aggregation of time series
The selected time series (see above) are aggregated to country and European level by averaging across all monitoring sites for each year.

Trend analyses
Trends are analysed by the Mann-Kendall method (Jassby and Cloern 2013) in the free software R (R Core Team 2019), using the wq package. This is a non-parametric test suggested by Mann (1945) and has been extensively used for environmental time series (Hipel and McLeod, 2005). Mann-Kendall is a test for monotonic trend in a time series y(x), which in this analysis is nutrient concentration (y) as a function of year (x). The test is based on Kendall's rank correlation, which measures the strength of monotonic association between the vectors x and y. In the case of no ties in the x and y variables, Kendall's rank correlation coefficient, tau, may be expressed as tau=S/D where S=sum_{i<j} (sign(x[j]-x[i])*sign(y[j]-y[i])) and D=n(n-1)/2. S is called the score and D, the denominator, is the maximum possible value of S. The p-value of tau is computed by an algorithm given by Best and Gipps (1974). The tests reported here are two-sided (testing for both increasing and decreasing trends). Data series with p-value <0.05 are reported as significantly increasing or decreasing (very positive/negative), while data series with p-value >= 0.05 and <0.10 are reported as marginally significant (marginally positive/negative). The results are summarised by calculating the percentage of monitoring sites within each category relative to all monitoring sites within the specific aggregation (Europe or country). The test analyses only the direction and significance of the change, not the size of the change.

The size of the change is estimated by calculating the Sen slope (or the Theil or Theil-Sen slope) (Theil 1950; Sen 1968) using the R software. The Sen slope is a non-parametric method where the slope m is determined as the median of all slopes (yj−yi)/(xj−xi) when joining all pairs of observations(xi, yi). Here the slope is calculated as the change per year for each monitoring site. This is summarised by calculating the average slope (regardless of the significance of the trend) for all monitoring sites in Europe or a country. The relative change per year (Sen slope %) is calculated as the Sen slope relative to the time series average. Again, this is summarised for Europe or individual countries by averaging across monitoring sites. The Sen slope was introduced for this indicator in 2013.

The Mann-Kendall method or the Sen slope will only reveal monotonic trends, and will not identify changes in the direction of the time series over time. Hence a combination of approaches is used to describe the time series: a visual inspection of the time series, describing whether the general impression is a monotonic trend, no apparent trend, clear shifts in direction of the trend or high variability with no clear direction; an evaluation of significant versus non-significant and decreasing versus increasing monotonic trends using the Mann-Kendall results; an evaluation of the average size of the monotonic trends using the Sen slope results.

Present concentration distributions
For analysis of the present state, average concentrations are calculated across the last 3 years. Outliers and suspicious values are removed before averaging. In this case all monitoring sites can be used, which is a far higher number than those that have complete time series after inter/extrapolation. The 3-year average is used to remove some inter-annual variability. Also, since data are not available for all monitoring sites each year, selecting data from 3 years will give more sites. The average value thus represents 1, 2 or 3 years.

The sites are assigned to different concentration classes and summarised per country (count of sites per concentration class). The classes defining values are based on the range of concentrations found in Waterbase and only give an indication of the relative distribution of values of BOD and ammonium in each country.

Methodology for gap filling

The methodology for gap filling is described under inter/extrapolation and consistent time series.

Methodology references

  • Hipel, K.W. and McLeod, A.I., (2005). Time Series Modelling of Water Resources and Environmental Systems. Electronic reprint of our book orginally published in 1994. 
  • Mann, H.B. (1945). Nonparametric tests against trend, Econometrica, 13, 245-259.
  • Jassby, A.D. and Cloern (2013) Mann-Kendall test and the Sen slope.R package version 0.3-10.
  • R Core Team (2019). R: A language and environment for statistical computing. R Foundation for Statistical Computing, Vienna, Austria.
  • Sen, Pranab Kumar (1968). "Estimates of the regression coefficient based on Kendall's tau", Journal of the American Statistical Association 63: 1379–1389
  • Theil, H. (1950). "A rank-invariant method of linear and polynomial regression analysis. I, II, III", Nederl. Akad. Wetensch., Proc. 53: 386–392, 521–525, 1397–1412

Uncertainties

Methodology uncertainty

The methodologies used for aggregating and testing trends in concentrations illustrate the overall European trends. Organic and oxygen conditions vary throughout the year, depending especially on flow conditions, affected by weather events etc. Hence, the annual average concentrations should ideally be based on samples collected as often as possible. Using annual averages representing only part of the year introduces some uncertainty, but it also makes it possible to include more river sites, which reduces the uncertainty in spatial coverage. Moreover, the majority of the annual averages represent the whole year.

Data sets uncertainty

This indicator is meant to give a representative overview of oxygenation availability in European rivers. This means it should reflect the variability in conditions over space and time. Countries are asked to provide data on rivers according to specified criteria.

The datasets for rivers include almost all countries within the EEA, but the time coverage varies from country to country, both through the analysed period and within the year for which the aggregated mean value is provided. It is assumed that the data from each country represents the variability in space in their country. Likewise, it is assumed that the sampling frequency is sufficiently high to reflect variability in time. In practice, the representativeness will vary between countries.

Waterbase contains a large amount of data collected throughout many years. Ensuring the quality of the data has always been a high priority. A revision of Waterbase reporting and the database-composition process took place in the period 2015–2017. This included restructuring of the data model and corresponding reporting templates; transformation of the legacy data (i.e. data reported in the past, for the period up to and including 2012); re-definition of specific data fields, such as aggregation period defining the length of aggregation in a year; update of the datasets according to correspondence with national reporters; re-codification of monitoring site codes across Eionet dataflows; and connection of the legacy data time series with the newly-reported data in restructured reporting templates (i.e. for the period 2013–2017). Still, suspicious values or time series are sometimes detected and the automatic QA/QC routines exclude some of the data. Through the communication with the reporting countries, the quality of the database can be further improved.

Rationale uncertainty

Biochemical oxygen demand and total ammonium show oxygen consumption and are thus well suited to illustrating water pollution. However, using annual average values may not fully illustrate the severity of low oxygen conditions.

Data sources

Metadata

Topics:

information.png Tags:
, , , , , , , ,
DPSIR: State
Typology: Descriptive indicator (Type A - What is happening to the environment and to humans?)
Indicator codes
  • CSI 019
  • WAT 002
Temporal coverage:

Dates

Frequency of updates

Updates are scheduled once per year

EEA Contact Info

Peter Kristensen
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