2015
DOI: 10.1007/s12665-015-4090-7
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Hydrogeology of the Skadar Lake basin (Southeast Dinarides) with an assessment of considerable subterranean inflow

Abstract: The Skadar Lake basin is located in the southeastern part of the classical Dinaric karst region (northern Mediterranean). This region is well known for its highly developed karst and the presence of all types of karstic features. In addition to the high degree of karstification, the advantage of Skadar Lake's catchment area in terms of water resources is also reflected in the following factors: a large amount of precipitation, scarcity of soil and vegetation cover, favourable geological and geomorphological co… Show more

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Cited by 20 publications
(6 citation statements)
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“…1). The Lake Skadar is the largest lake on the Balkan Peninsula and is located in the area of Dinaric karst, with a surface area that seasonally fluctuates between 370 and 600 km 2 (Pe sić et al, 2018) The lake is well-known for the occurrence of numerous karstic springs (Radulović et al, 2015). Most of them are rheocrene and limnocrene springs.…”
Section: Study Area and Samplingmentioning
confidence: 99%
“…1). The Lake Skadar is the largest lake on the Balkan Peninsula and is located in the area of Dinaric karst, with a surface area that seasonally fluctuates between 370 and 600 km 2 (Pe sić et al, 2018) The lake is well-known for the occurrence of numerous karstic springs (Radulović et al, 2015). Most of them are rheocrene and limnocrene springs.…”
Section: Study Area and Samplingmentioning
confidence: 99%
“…The average annual precipitation on the area is relatively high (approximatively 2500 mm/year of which 80-85% of rainfall occurs between November and March [14]) due to its geographical position in relation to the Adriatic Sea and its terrain configuration. Despite that, there is no abundant surface water on this area neither a well-developed hydrographic network [15]. Almost all rainwater infiltrates rapidly into the permeable ground, percolating vertically until the water table, and the surface drainage network is poorly developed (limited to the abovementioned situations), with a small number of local watercourses that flow only in the rainiest period of the year [9].…”
Section: The Geo-hydrological Framework Of the Study Areamentioning
confidence: 98%
“…In addition to these, a third aspect must be considered: The lake is drained by the Buna River, just southward the city, and after few kilometres it receives the Drin River along the hydrographic left. The Drin River is the longest river of Albania (average flow rate of 360 m 3 /s, drainage basin of about 14,200 km 2 , length of 285 km out of a total of 335 km; [26]) and its flow rate, besides inducing floods in the southern plains [27], can create a hydraulic barrier for the waters that move out from the lake [12,15] up to induce flow inversions. This is a real possible scenario in case of very high-water tables originated by the natural flooding of the Drin or as consequence of extraordinary opening of the upstream dams during the management of very high-water levels [24].…”
Section: Figure 2 (A)mentioning
confidence: 99%
“…Elevation map of the study area with sampling locations for collecting precipitation (P1 and P2), Mareza spring water (S1, S2, S3, and S4), and surface water of the Zeta River (upstream, RU; downstream, RD). recharge area of the Skadar Lake karst aquifer is spread over a wide area in the karst plateaus, while the discharge area extends along the karst depressions and deep canyons [36]. According to the Institute of Hydrometeorology and Seismology of Montenegro's (IHMS) meteorological data, the mean monthly air temperature during the sampling period (from February 2017 to March 2018) in Podgorica was between 7.3 • C in December and 30 • C in July and August ( Figure 3).…”
Section: Study Areamentioning
confidence: 99%