Aktivierungs analyse in der Hydrogeologie, 1970, Buchtela K.

Carte hydrogéomorphologique, hydrogéologie et hydrochimie du karst de Dorvan (Ain), 1983, Gibert J. , Laurent R. , Maire R.

PRESENTATION OF THE HYDROGEOMORPHOLOGICAL MAP AT 1/100,000 ON KARST OF DORVAN (SOUTHERN JURA, AIN, FRANCE. Main researches about hydrology and hydrochemistry on this karst - The Dorvan massif is a low mountain Jurassian karst with a wet temperate climate and a little nival influence. The surface relief is covered with important decalcification clay. The drainage of the karst is assumed by superimposed systems, according to the excavation of the Torcieu watergap. The flow of the main outlet (Pissoir) is a pluvial type, which presents an annual cycle with a maximum in winter and a minimum in summer. The specific discharge is 31.4 l/s/km2. The dissolution rate is high: 81 mm/ky. 50% of the corrosion interests the epikarst, 50% interests the endokarst. During the Pleistocene, the glaciations played a direct or indirect role on the evolution of the Dorvan karst: nivo-karst during the Würm; fluvio-glacial up-building of the Torcieu watergap and correlated water logging of the lower karst during Würm and Tardiglacial periods; probable direct action of glaciers during the Riss.

Hydrogéologie karstique des Alpes-Maritimes, 1984, Baissas, P.

Karst hydrogeology in the Alpes-Maritimes - In the Marguareis, the systems penetrate very quickly by transverse faults, to reach the impermeable basement and then follow the dip. All the waters, even those on the French side, belong to the Pô basin. In the Roya arc, underflows are to be found going round the base of the Argentera-Mercantour. In the Nice arc, the karstification depends principally on tectonic factors and according to the places, the water follows either the overlaps or transverse faults. In the Grasse plateaus, the galleries follow at the outset the slopes and the dips of the synclinal hinges; the tectonic factors determine the location of the resurgences ; at depth, the karst is always phreatic, with relations between tectonic compartments during floods. In the cover of the Tanneron-Esterel basement and Barrot Dome, lithological factors determine flow.

Hydrogéologie karstique du poljé d'lrmene, Bodrum (Turquie), 1985, Canik, B.

KARSTIC HYDROGEOLOGY OF THE IRMENE POLJE - BODRUM (TURKEY) - The Irmene polje (25 km2) is located in the Bodrum peninsula, Turkey. The formation exposed, are coloured argilaceous schists, blackish shales and sandstones of a paleozoic age. They are overlapped by unconformable carbonate formations of Early Triassic to Late Jurassic. The karstification is mostly developed on the non-dolomitic parts of the fissured limestones. The groundwater flow is generally northwards, towards coastal or submarine springs. Thus, it is calculated that a discharge of about 40 l/s can be obtained from possible wells to supply water for the Irmene village. We propose to increase the infiltration rate within the karstic aquifer by building barriers, which would favour runoff towards natural wells or sinks not active for the moment.

Hydrogéologie de la région entre Araches et Flaine (Haute-Savoie), 1985, Sesiano, J.

NEW HYDROGEOLOGICAL INVESTIGATIoNS IN THE Massif de Platé BETWEEN ARACHES AND Flaine (HAUTE-SAVOIE, FRANCE) - During 1983 and 1984 several dye-tracing experiments have been performed in the French Prealps (Haute-Savoie). The studied area covered about 30 km2, with altitudes ranging between 500m and 2500m. An underground drainage model has been set up, taking into account the fact that there is a common water outlet. The model is based upon the regional tectonic setting, the drainage pattern following thrust and fault planes

L'accident de Tchernobyl : une retombée positive en hydrogéologie, 1986, Sesiano J. , Bueche M.

THE TCHERNOBYL ACCIDENT: A POSITIVE HYDROGEOLOGICAL ASPECT - As a continuation of dye-tracing studies of underground waters in Haute-Savoie, France, over the last few years, we have used the radioactive elements released by the Chernobyl nuclear accident as artificial tracers. The event happened simultaneously with the onset of the spring high waters. The response of the system was thus delayed by more than two weeks, the time for the water to percolate and for the aquifer to recharge. On the third week, a very faint signal was detected by gammametry and by liquid scintillation counters at the two surveyed springs.

Tätigkeitsbericht 1991 der Fachsektion Karsthydrogeologie des Verbandes österreichischer Höhlenforscher., 1992, Pavuza, R.

Tätigkeitsbericht 1991 der Fachsektion Karsthydrogeologie des Verbandes österreichischer Höhlenforscher, 1992, Pavuza, R.

Tätigkeitsbericht 1992 der Fachsektion Karsthydrogeologie des Verbandes österreichischer Höhlenforscher., 1993, Pavuza, R.

Tätigkeitsbericht 1992 der Fachsektion Karsthydrogeologie des Verbandes österreichischer Höhlenforscher, 1993, Pavuza, R.

Tätigkeitsbericht 1993 der Fachsektion Karsthydrogeologie des Verbandes österreichischer Höhlenforscher., 1994, Pavuza, R.

Tätigkeitsbericht 1993 der Fachsektion Karsthydrogeologie des Verbandes österreichischer Höhlenforscher, 1994, Pavuza, R.

Tätigkeitsbericht 1996 der Fachsektion Karsthydrogeologie des Verbandes österreichischer Höhlenforscher., 1997, Pavuza, R.

Tracer als Werkzeug in der Hydrogeologie, 1997, Wohnlich Stefan,

Tätigkeitsbericht 1996 der Fachsektion Karsthydrogeologie des Verbandes österreichischer Höhlenforscher, 1997, Pavuza, R.