FMFrédéric A. Mathurin

Frédéric A. Mathurin

*This is an algorithmically generated author record based on publicly available information.

Current Organizations / Institutes

The organizations/institutes from the scholar's latest article


Frédéric A. Mathurin has a total of 4 co-authors. Here are the top co-authors by number of shared publications:

  • Birgitta E. Kalinowski

    Swedish Nuclear Fuel and Waste Management Co, Blekholmstorget 30, SE-101 24 Stockholm, Sweden

    1 shared publication
  • Eva-Lena Tullborg

    Terralogica AB, Östra Annekärrsvägen 17, SE-443 72 Gråbo, Sweden

    1 shared publication
  • Marcus Laaksoharju

    Nova FoU, Varvsgatan 15, SE-572 28 Oskarshamn, Sweden

    1 shared publication
  • Mats E. Åström

    Linnæus University, School of Natural Sciences, Barlastgatan 11, SE-391 82 Kalmar, Sweden

    1 shared publication

Latest Publications

  • Effect of Tunnel Excavation on Source and Mixing of Groundwater in a Coastal Granitoidic Fracture Network

    by Frédéric A. Mathurin, Mats E. Åström, Marcus Laaksoharju, Birgitta E. Kalinowski, Eva-Lena Tullborg

    The aim of this study was to assess how the excavation of the Äspö Hard Rock Laboratory tunnel has impacted on sources and mixing of groundwater in fractured crystalline (granitoidic) bedrock. The tunnel is 3600 m long and extends to a depth of 460 m at a coastal site in Boreal Europe. The study builds on a unique data set consisting of 1117 observations on chloride and δ18O of groundwater collected from a total of 356 packed-off fractures between 1987 and 2011. On the basis of the values of these two variables in selected source waters, a classification system was developed to relate the groundwater observations to source and postinfiltration mixing phenomena. The results show that the groundwater has multiple sources and a complex history of transport and mixing, and is composed of at least glacial water, marine water, recent meteoric water, and an old saline water. The tunnel excavation has had a large impact on flow, sources, and mixing of the groundwater. Important phenomena include upflow of deep-lying saline water, extensive intrusion of current Baltic Sea water, and substantial temporal variability of chloride and δ18O in many fractures.