How to access the database?


To access the database and download data sets, you need to create an account at this address. When your account is validated, you can connect to the database interface or directly download data from the links available on the website using your login and password. Please, follow this tutorial for more information.

Description of the Emme site

This observatory site is located in Aeschau (region of Emmental, Switzerland). The study area (0.8 km2) lies in the Upper part of Emme River Valley, a pre-alpine, alluvial valley situated at the northern margin of the Alps. The underlying aquifer is formed by quaternary deposits, composed of sandy gravels and cobbles, with a variable proportion of silt, and contains lenses of coarse uniform gravel (Käser and Hunkeler, 2015). These features result in an extremely conductive unconfined aquifer. The bedrock underneath the aquifer -and the lower part of it (1-3 m thick)- is considered as an aquitard relative to the upper part of the alluvium. The saturated hydraulic conductivity (Ks) show higher values (5×10-3 m/s) predominantly in the upper 30-35 m of the valley fill, whereas smaller values, around 10-4 m/s or lower, occur mainly deeper (Blau, 1984, 1991; Blau and Muchenberger, 1997; Würsten, 1991).  

The monitored area is crossed by the Emme river, which provides the main source of recharge to the alluvial aquifer through its coarse gravel-bed. This segment of the river also exhibits a couple of small weirs designed for erosion control. The valley at this location has an average width of 400 m and a mean topography gradient of 0.9%.  

An important groundwater abstraction plant -which supplies the 45% of the drinking water for consumption of the city of Bern- is located at the site. The wellfield, consisting of 8 wells, is aligned in parallel to the river Emme in the so-called Ramsei Plain (left side of the river). The total groundwater abstraction rate is on average 24000 l/min (0.4 m3/s). This rate is substantially relative to the total water balance of the system, as it has been proved that the latter is clearly affected by pumping. By no means it can be higher than 50% of the total outflow (Schilling et al., 2017). The bedrock-sediment interface around the Ramsei Plain is on average as deep as 25 m, being the maximum depth 46 m (Würsten 1991). This mean value can be also considered a good estimate of the aquifer thickness for the rest of the study area.  

Regarding the climatic and hydraulic conditions of the site, the average annual precipitation is 1300 mm, the potential evapotranspiration 550 mm and mean annual air temperature 8ºC (Käser and Hunkeler, 2015). The long-term average discharge of the river is 4.4 m3/s. This value is typically higher during the snowmelt periods (March-April) and especially small throughout very dry summers or cold winters, when segments of the Emme river can dry completely dry (Würsten, 1991).


Data Available At The Emme Site


Access to the data from Google Earth module

The Google Earth module provides a site visualization and information on data available such as types of measurements, locations, dates, etc. This interface also provides an overview of geophysical maps and cross-sections, which can be directly downloaded from the available links. Data available through predefined requests can be downloaded from this interface too.  

To download the Google Earth file and access to the data of this site, click on the following link : 


Access to the data from database interface

All data inserted in the H+ database can be extracted using requests, which can be defined through this interface. For more information, please read the tutorial available here.


Access to the data from predefined requests

To help finding general data sets, predefined requests have been created and are regularly executed. Results can be downloaded from the links available below.




Site data

Spatialized data


Experimental bench


In situ measurements



Soil atmosphere exchange