Determination of Natural Background Levels and Threshold Values in the Neogene Aquifer (Flanders)

Author(s):  
Marleen Coetsiers ◽  
Kristine Walraevens
2008 ◽  
Vol 57 (5) ◽  
pp. 1155-1168 ◽  
Author(s):  
Marleen Coetsiers ◽  
Petra Blaser ◽  
Kristine Martens ◽  
Kristine Walraevens

2020 ◽  
Author(s):  
Rita Masciale ◽  
Stefano Amalfitano ◽  
Eleonora Frollini ◽  
Stefano Ghergo ◽  
Marco Melita ◽  
...  

<p>The European Water Directives (WDs, 2000/60/EC; 2006/118/EC) force Member States to proceed to the characterization of groundwater bodies in order to define their quantitative and chemical status and their environmental objectives. Since the earlier years of this century, the Department of Water Resources Management of the Apulia Region implemented the WDs by setting a wide groundwater monitoring network, delineating regional groundwater bodies and characterizing their status. The groundwater bodies characterization showed that the risk of not achieving a good status was generally related to salt contamination and the exceedance of the threshold values or the quality standards for some parameters (e.g., NO<sub>3</sub>, Fe, Mn), as expected for regions with a predominantly agricultural vocation and characterized by extensive coastal development. The main regional aquifers reside in the carbonate bedrock characterized by intense fracturing and karstification.</p><p>The groundwater Directive 2006/118/EC allows the evaluation of Natural Background Levels (NBLs) to be taken into account when establishing the relevant threshold values.</p><p>During the last years, the IRSA-CNR collaborated with the National Environmental Protection Agency (ISPRA) in defining scientifically based guidelines for the NBLs assessment and clarifying some methodological aspects. These guidelines suggest excluding water samples characterised by high levels of specific markers clearly indicating anthropogenic inputs.</p><p>The project "VIOLA - Natural background levels for the groundwater bodies of Apulia Region ", has been funded by the Department of Water Resources Management of the Apulia Region for carrying out the application and validation of the above mentioned methodologies and to develop and test methodologies better tailored for coastal aquifers. In particular, isotopic techniques will be used to discriminate between the anthropogenic and natural origin of the salinization and historical data of groundwater salinization will be processed in order to study its evolution in time. . Finally, the investigation of innovative microbiological techniques is envisaged to evaluate how changes in groundwater quality will affect the resident microbial community properties involved in C-flux.</p><p>The VIOLA project will last three years during which the IRSA-CNR will:</p><ul><li>collect and order all the background knowledge relating to the hydro-geo-chemical characteristics of the Apulian groundwater bodies,</li> <li>define adequate groundwater sampling procedures and assessment protocols for the NBLs,</li> <li>carry out field activities, aimed at sampling groundwater at a specific monitoring network and measuring values of main physico-chemical and microbiological parameters, in the study area of the coastal Murgia groundwater body, and</li> <li>produce tools to support the planning and management of groundwater resources integrated in a GIS environment.</li> </ul><p>This contribution aims at providing an overview at the ongoing activities at the regional scale, illustrating the groundwater bodies setting, the main pressures and the preliminary derivation of NBL using the historical data.</p>


2018 ◽  
Vol 54 ◽  
pp. 00027 ◽  
Author(s):  
I. Retike ◽  
J. Bikše

Intensive water consumption in former decades caused formation of large depression cone near city Liepāja and resulted with seawater intrusion into Upper Devonian Mūru-Žagaru confined freshwater aquifer. Area affected by seawater intrusion is delineated as separate groundwater body at risk (F5) and according to Groundwater Directive threshold values for groundwater bodies at risk must be established to assess the status of a body and identify possible trends. Correct estimation of background levels is significant for determination of threshold values. This study shows an updated so called “BRIDGE” methodology for determination of background levels. A two-step approach how to establish background levels in much stricter manner is presented. Also, data on major ion chemistry, biogenic and trace elements in groundwater and seawater from sampling campaign in 2017 are displayed. Dataset include unique seawater sample taken from Baltic Sea. Finally, the calculated seawater fraction results in groundwater samples shows up to 50 % presence of seawater which decrease with increasing distance from the coast and increasing screen interval.


Desalination ◽  
2008 ◽  
Vol 226 (1-3) ◽  
pp. 160-168 ◽  
Author(s):  
F. Wendland ◽  
G. Berthold ◽  
A. Blum ◽  
P. Elsass ◽  
J.-G. Fritsche ◽  
...  

Author(s):  
Claudia Avila-Sandoval ◽  
Hugo Júnez-Ferreira ◽  
Julián González-Trinidad ◽  
Carlos Bautista-Capetillo ◽  
Anuard Pacheco-Guerrero ◽  
...  

The presence of arsenic in groundwater constitutes a hazard for the environment and human health, and the determination of its source has become a global challenge, which can be approached by defining the natural background levels (NBL) in conjunction with the indicator kriging method, with the aim of delineating anthropogenically contaminated areas. However, having a unique value of NBL for large areas can generate interpretation errors. This research integrates the determination of the flow systems present in the Calera Aquifer, and the definition of the natural background levels in each flow system by making estimation maps in ArcGIS using two databases, 10 years apart, to evaluate the spatio-temporal variation of arsenic in groundwater. The results indicate a notable increase in the probability of exceeding the arsenic NBL, mainly in the intermediate flow, which may be due to movement resulting from mining activities as well as a mixture of regional and intermediate flows caused by the extraction of water for agriculture and drinking water supplies. The presented values exceed the maximum limits allowed for human consumption, as stated by the World Health Organization.


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