Using DCIP and TEM to investigate the geology of the Alnarp Valley in southwestern Scania, Sweden
In southwestern Scania there is a paleovalley, the Alnarp Valley, which holds a confined aquifer called Alnarpsströmmen. Its geology consists mainly of sand and gravel and it is generally confined by one or more layers of clayey till above, and the limestone bedrock below. In collaboration with Region Skåne and SGU, this thesis aims to gather information about Alnarpsströmmen using two geophysical
