1991
DOI: 10.1016/0022-1694(91)90004-2
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Contribution à l'étude des courbes de récession des sources karstiques: Exemples du pays Hellénique

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Cited by 37 publications
(16 citation statements)
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“…A simple karst unit exhibits a normal distribution on a probabilistic graph while its duration curve is presented by a straight line with a certain slope (Soulios 1985;1991). In complex karst units; overflow or discharge loses towards an adjacent unit, or a supplementary recharge results in the differentiation of the duration curve, i.e., the change of its inclination (Soulios 1985;1991).…”
Section: Resultsmentioning
confidence: 99%
See 1 more Smart Citation
“…A simple karst unit exhibits a normal distribution on a probabilistic graph while its duration curve is presented by a straight line with a certain slope (Soulios 1985;1991). In complex karst units; overflow or discharge loses towards an adjacent unit, or a supplementary recharge results in the differentiation of the duration curve, i.e., the change of its inclination (Soulios 1985;1991).…”
Section: Resultsmentioning
confidence: 99%
“…The discharge duration curves are also used to investigate karst systems and their distinction into simple, isolated to the adjacent ones and complex (Soulios 1985;1991).…”
Section: Methodological Approachmentioning
confidence: 99%
“…Recession coefficients that increase with time have been observed in southern France (Bailly-Comte et al, 2010), Greece (Soulios, 1991), the Dineric Karst (Mangin, 1975;Bonacci, 1987 and1993), and, recently, in northwest Arkansas. Three models have been proposed for recession coefficients that increase with time: 1) Spring basins with two lithologies of contrasting permeabilities, which creates a lag-time for the inflow of water to the spring orifice (Soulios, 1991), 2) changes in storageoutflow relations created by temporarily flooded cave passages or ponor retention ponds that are drained by smaller diameter conduits (Bonacci, 1987 and1993), and 3) water exchange and pressure transfer between the matrix and conduit when antecedent water levels in the aquifer matrix are medium to high compared to those of the conduits prior to rainfall (Bailly-Comte et al, 2010).…”
Section: Karst-spring Recession Analysismentioning
confidence: 99%
“…Three models have been proposed for recession coefficients that increase with time: 1) Spring basins with two lithologies of contrasting permeabilities, which creates a lag-time for the inflow of water to the spring orifice (Soulios, 1991), 2) changes in storageoutflow relations created by temporarily flooded cave passages or ponor retention ponds that are drained by smaller diameter conduits (Bonacci, 1987 and1993), and 3) water exchange and pressure transfer between the matrix and conduit when antecedent water levels in the aquifer matrix are medium to high compared to those of the conduits prior to rainfall (Bailly-Comte et al, 2010). Bonacci (1987 and1993) proposed that when the water levels in a cave chamber or a ponor retention pond rise above the surrounding ground-water table in the aquifer, the capacity of the conduits draining these features is exceeded.…”
Section: Karst-spring Recession Analysismentioning
confidence: 99%
“…Other studies are based on the difference response separation method or on the analysis of transfer functions between input and output; the karst aquifer is considered to be a blackbox. Bonacci (1993) and Soulios (1991) and Kovács et al (2005) directly analysed the form of the whole discharge flow recession, which is influenced by the size and the hydrodynamic characteristics of the karst system. Other authors employed the hydrograph component separation with different models to obtain some information about the behaviour of the aquifer (e.g.…”
Section: Introductionmentioning
confidence: 99%