Groundwater Background Values
Country / Region: Germany
Begin of project: April 1, 2005
End of project: December 31, 2014
Status of project: December 31, 2014
Fig. 1: Hydrogeochemical units of Germany
Background:
The achievement of a good chemical status of groundwater, which is one of the main objectives of the European Water Framework Directive (EU WFD), requires the knowledge of the hydrogeochemical groundwater background values.
To fulfill the requirements of the EU WFD, the Geological Surveys of the Federal States of Germany (SGD) founded the task force EU-WRRL (UAG EU-WRRL) as a coordinating committee. A main product of the activities of the UAG EU-WRRL is the Hydrogeological Map of Germany 1:200.000 (HÜK200).
A subdivision of the UAG EU-WRRL, the working group "groundwater background values" (PK HGW) has been engaged since 2005 in identifying and statistically evaluating groundwater background values for the upper aquifer.
Project aim and approach:
The main objective of the PK HGW was the nationwide compilation and visualization of aquifer based groundwater background values in Germany on the basis of over 50,000 groundwater samples collected between 1980 and 2005. In a first step, the hydrogeological units (about 1100) of the Hydrogeological Map of Germany (HÜK200) were aggregated into hydrogeochemical (HGC) units, which are defined as hydrogeological units with typical distributions of hydrogeochemical properties.
After every groundwater sample had been assigned to the appropriate HGC unit, the data were subdivided into 10 hydrogeological regions (Fig. 1) and statistically evaluated by the Geological Surveys of the Federal States (SGD) and the Federal Institute for Geosciences and Natural Resources (BGR). This resulted in a total of 186 HGC units, of which 112 units contained sufficient (at least 10) samples to perform the statistical analysis. The evaluated units cover about 97.5% of Germany.
The HGC units for the northern region 1 were generated from the area related hydrogeological sub-regions, hence covering 100% of the region. Due to the strongly depth related variations in groundwater quality in the northern unconsolidated aquifers, the evaluation for this region was reduced to groundwater samples from a depth < 50 m.
Since the first data collection in the year 2005 showed an insufficient territorial coverage of samples for a number of trace elements, a new data collection was performed in the year 2012 for relevant trace elements with available minor threshold values (see also LAWA (2004): arsenic, boron, barium, cadmium, cobalt, chromium, copper, fluoride, mercury, molybdenum, nickel, lead, antimony, selenium, thallium, uranium, vanadium, zinc).
Method:
The statistical evaluation of each parameter was performed semi-automatically using probability plots (WALTER et al., 2006). This method allows the identification of separate populations and anomalies compared to the background or normal population, as different populations can be distinguished through changes in inclination of the slope (Fig. 2). These anomalies (MARCZINEK et al., 2008) could be caused by anthropogenic influences, but also by local natural phenomena like ore mineralization, coastal and inland salinization or acidification of crystalline rocks regions.
Fig. 2: Example of statistical evaluation
From the trend of the normal population in the probability plot the statistical values (mean, standard deviation and percentiles) can be calculated. In this project the background value was defined as the 90th percentile.
For an efficient evaluation, an excel-tool was developed, which allows the determination of the range of data, which represent the normal population of a data set (Fig. 2). The results of the procedure were reviewed visually by a comparison of a histogram of the data to the calculated normal distribution. Goodness of fit was also tested by the correlation coefficient and the d’Agostino-Pearson-test for normality. These methods allow an easy verification, if the assumed distribution fits the actual distribution. It is also possible to determine if the data are best represented by a normal or lognormal distribution.
The statistical evaluations were controlled and, if necessary, modified by the geological surveys responsible for the respective HGC unit. The tables with the results were then included into the database of the HÜK200.
A more detailed description of the method can be found in WAGNER et al. (2014).
Fig. 3: Groundwater background values
Results:
The results of the data analysis are available for download via the BGR Product Center or can be accessed via the internet through a web map service (WMS) in the form of maps (Fig. 3) and info-queries (German only), showing the statistical values within the areal extent of each hydrogeochemical unit in the upper aquifer. In addition the WMS "HUEK200 HGW" is visualised in the BGR Geoviewer.
Up to 39 parameters (see Tab. 1) can be displayed, though for some parameters, especially trace elements, and for some small HGC units not enough samples were available to perform a statistical analysis (minimum requirement for statistical analysis: 10 samples).
Values for nitrate are not shown, because essentially all higher values of nitrate (> 10 mg/l) are of anthropogenic origin and nitrate is a seasonally very variable parameter, so that in most cases the statistic evaluation would not lead to representative background values.
A detailed description of the contents displayed in the WMS and more information about the project are given in WAGNER et al. (2014).
Geoviewer:
Maps:
Data:
Literature:
- BLA-GEO & LAWA (2015): Hydrogeochemische Hintergrundwerte im Grundwasser und ihre Bedeutung für die Wasserwirtschaft. 22 S. (PDF, 1 MB)
- DÖRHÖFER, G., HANNAPPEL, S. & VOIGT, H. - J. (2001): Die Hydrogeologische Übersichtskarte von Deutschland HÜK200. – Z. Angew. Geol., 47(4); Hannover.
- KUNKEL, R., WENDLAND, F., VOIGT, H.-J. & HANNAPPEL, S. (2004): Die natürliche, ubiquitär überprägte Grundwasserbeschaffenheit in Deutschland. - Schriften FZ Jülich, Reihe Umwelt, 47: 204 S.
- LAWA (2004): Ableitung von Geringfügigkeitsschwellenwerten für das Grundwasser. - Länderarbeitsgemeinschaft Wasser (Hrsg.), 33 S., Düsseldorf.
- MARCZINEK, S., BEER, A., BUDZIAK, D, DREHER, T., ELBRACHT, J., FRITSCHE, H.-G., HOT-ZAN, G., HÜBSCHMANN, M., PANTELEIT, B., PETERS, A., POESER, H., SCHUSTER, H., WAGNER, B., WALTER, T., WIRSING, G., WITTHÖFT, M. & WOLTER, R. (2008): Natürliche Hintergrundwerte im Grundwasser – Erste Ergebnisse. In: SAUTER, M., PTAK, TH., KAUFMANN-KNOKE, R., LODEMANN, M., VAN DEN KERKHOF, A. (Hg.): Grundwasserressourcen: Kurzfassungen der Vorträge und Poster; Tagung der Fachsektion Hydrogeologie in der DGG, Göttingen, 21. bis 25. Mai 2008; Hannover. (PDF, 20 KB)
- WAGNER, B., BEER, A., BITZER, F., BROSE, D., BRÜCKNER, L., BUDZIAK, D., CLOS, P., FRITSCHE, H.-G., HÖRMANN, U., HÜBSCHMANN, M., MOOSMANN, L., NOMMENSEN, B., PANTELEIT, B., PETERS, A., PRESTEL, R., SCHUSTER, H., SCHWERDTFEGER, B., WALTER, T. & WOLTER, R. (2014): Explanations to the Web Map Service (WMS) "Groundwater background values". 22 p.; Hof. (PDF, 920 KB)
- WAGNER, B., BEER, A., BROSE, D., BUDZIAK, D., CLOS, P., DREHER, T., FRITSCHE, H.-G., HÜBSCHMANN, M., MARCZINEK, S., PETERS, A., POESER, H., SCHUSTER, H., WAGNER, F., WALTER, T., WIRSING, G. & WOLTER, R. (2010): A Web Map Service of Groundwater Background Values in Germany. p. 714-715, Proceedings of the IAH-conference, 12. – 17. September 2010, Krakow, Poland.
- WAGNER, B., TÖPFNER, C., LISCHEID, G, SCHOLZ, M., KLINGER, R. & KLAAS, P. (2003): Hydrogeochemische Hintergrundwerte der Grundwässer Bayerns. – GLA Fachberichte, 21: 250 S.; München.
- WAGNER, B., WALTER, T., HIMMELSBACH, T., CLOS, P., BEER, A., BUDZIAK, D., DREHER, T., FRITSCHE, H.-G., HÜBSCHMANN, M., MARCZINEK, S., PETERS, A., POESER, H., SCHUSTER, H., STEINEL, A., WAGNER, F. & WIRSING, G. (2011): Hydrogeochemische Hintergrundwerte der Grundwässer Deutschlands als Web Map Service. - Grundwasser, 16(3): 155-162; doi: 10.1007/s00767-011-0161-1
- WALTER, T., BEER, A., BROSE, D., BUDZIAK, D., CLOS, P., DREHER, T., FRITSCHE, H.-G., HÜBSCHMANN, M., MARCZINEK, S., PETERS, A., POESER, H., SCHUSTER, H., WAGNER, B., WAGNER, F., WIRSING, G. & WOLTER, R. (2010): Determining Natural Background Values with Probability Plots.- p. 716-717. Proceedings of the IAH-conference, 12. – 17. September 2010, Krakow, Poland.
- WALTER, T., BEER, A., DREHER, T., ELBRACHT, J., FRITSCHE, H.-G., HÜBSCHMANN, M., KÄMMERER, D., KRINGEL, R., MARCZINEK, S., PANTELEIT, B., PAWLITZKY, M., PETERS, A., SCHUSTER, H, WAGNER, B. & WIRSING, G. (2006): Ermittlung und Darstellung der natürlichen Hintergrundwerte der Grundwässer in Deutschland. In: VOIGT, H.-J., KAUFMANN-KNOKE, R., JAHNKE, C., HERD, R. (Hg.): Indikatoren im Grundwasser: Kurzfassungen der Vorträge und Poster; Tagung der Fachsektion Hydrogeologie in der DGG, Cottbus, 24. bis 28. Mai 2006; Hannover. (PDF, 17 KB)
Partner:
- State Geological Surveys of Germany (SGD)
- German Working Group on Water Issues of the Federal States (LAWA)
- Federal Environment Agency (UBA)