Aleksandar Tanasković, Vesna Ristić Vakanjac, D. Polomcic, Jelena M. Močević
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引用次数: 0
摘要
要评估泉水(河流源头)的排水动态并计算其水平衡方程参数,需要足够长的日排水时间序列。本文假定,如果有至少 30 年的观测时间序列,就可以对集水区进行测量,但在塞尔维亚这种情况很少见。通常会进行为期一年的监测,以核实水源或泉水的储备情况。监测工作在最终报告编制完成后停止。本文旨在说明,如果没有足够长的时间序列,如果没有进行详细的水文地质调查,可能会出现的问题。本文以 Gornji Dušnik 泉水为例。该泉水流经苏瓦普兰纳山西部。多年前取水是为了向 Gadžin Han 镇及附近的 Donji Dušnik 和 Gornji Dušnik 村提供公共供水。
A contribution to the understanding of the discharge dynamics and water balance of the karst spring Gornji Dušnik (Suva Planina)
A sufficiently long time-series of daily discharges is needed to assess the discharge dynamics and calculate the water balance equation parameters of a spring (river source). The paper assumes that a catchment is gauged if a time-series of observations of at least 30 years is available, which is a rare case in Serbia. One-year monitoring is often set up to verify the reserves of a water source or spring intended for capture. Monitoring ceases after the final report is produced. The paper aims to show potential problems if there are no sufficiently long time-series and if no detailed hydrogeological investigations have been undertaken. The Gornji Dušnik Spring is used as an example. That spring drains the western parts of Suva Planina Mountain. It was captured many years ago to provide public water supply to the town of Gadžin Han and the nearby villages of Donji Dušnik and Gornji Dušnik.