1. Latent EEects in a Hydrogeological Problem In the present study we investigate the data provided by the karstwater level monitoring system, set up in the Transdanubian Mountains, more precisely in the Bakony, the Keszthelyi Mountains and the Balaton-Highland. (Here, like in the sequel, the term karstwater is used for groundwater in karstic areas.) The detailed description of the monitoring s...

bazargan and poldasht plains are located in the north of west azarbaijan, northwest of iran. in this area, groundwater supplies main water demands. aim of this research is assessment of aquifer vulnerability for contamination potential on the basis of hydrogeological conditions of the study area. for this purpose the combined use of the drastic and geographical information system (gis) demonstr...

CO2 geological storage (CGS) is one of the most promising technologies to address the issue of excessive anthropogenic CO2 emissions in the atmosphere due to fossil fuel combustion for electricity generation. In order to fully exploit the storage potential, numerical simulations can help in determining injection strategies before the deployment of full scale sequestration in saline aquifers. Th...

8 Climate change is one if not the most pressing challenge modern society faces. Increasing temperatures are observed 9 all over the planet and the impact of climate change on the hydrogeological cycle has long been shown. However, so 10 far we have insufficient knowledge on the influence of atmospheric warming on shallow groundwater temperatures. 11 While some studies analyse the implication c...

Water percolation through infiltration ponds is creating significant synergies for the broad adoption of water reuse as an additional non-conventional supply. Despite apparent simplicity soil aquifer treatment (SAT) approaches, complexity site-specific hydrogeological conditions and processes occurring at various scales require exhaustive understanding system’s response. The non-saturated zone ...

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in march 2004, a fluxgate gradiometer survey was conducted over tepe ghabristan, covering approximately 6ha of ground. it identified further areas of the iron age cemetery with possible grave pits (areas b and c). in addition, an irrigation channel was discovered which could be contemporary to these iron age graves (area d). the anomalies in area e can be interpreted as buried structural remain...