作者: Răzvan Bătinaş , Gheorghe Şerban , Daniel Sabӑu
DOI: 10.1007/978-3-030-22320-5_16
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摘要: The strong precipitation and cool climate render the Apuseni Mountains a real “water castle” with complex, radial development of river network. density network has an average value between 0.6 1.0 km/km2, higher than values found in Eastern Southern Carpathians; deviation from these occurs karstic areas where surface drainage is replaced by underground one: 0.4–0.5 km/km2 Pădurea Craiului Mountains, Vascău Plateau Trascău (Pascu 1983). hydrographic result climate; therefore, quantitative differences two slopes are also manifested specific flow rate: 20–40 l/s km2 on west side 10–20 1/s eastern side. According to this parameter, entire mountain region among country’s water-surplus areas. moderate water resources belong peripheral depression areas, 5–10 km2. evaluation done analyzing hydrological regime, respectively establishing balance calculating aridity index, rated for Romania I. Ujvari, since 1972. introductory chapter presents aspects related general organization available resources, followed assessment factors determining flow. observations parameters were analyzed third part study, including details about liquid