Đetinja流域河情与水平衡分析

D. Milijašević, A. Milanović
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引用次数: 2

摘要

本文利用Đetinja河1978 ~ 2008年30年的水位和流量资料,分析了该河的水情和水平衡。Đetinja水位分析显示,8月平均水位最低,3、4月平均水位最高,年平均水位为53 cm。1978—2008年观测期内,圣戈尔日附近Đetinja年平均流量为5.60 m3/s。年平均流量与月平均低潮和月平均高潮的年平均值基本一致。结论认为Đetinja河属于雨-湖相的中度大陆变异。研究结果表明,Đetinja流域形成水量约为5.60 m3/s,比径流量为10.95 l/s/km2。虽然降水量不低,年降水量在875毫米左右,但由于蒸发量高达60%以上,河流入水量较小。有分析认为,考虑到离河口8.2公里的森戈尔里水文站,以及2002年停止使用的斯塔帕里水文站,在河道和更大的支流上建立水文站是很有意义的。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Analysis of river regime and water balance in the Đetinja River Basin
Water regime and water balance of the Đetinja River were analysed in this paper on the basis of a thirty-year data series on water level and discharge in the period from 1978 to 2008. The analysis of the Đetinja water level showed the mean annual water level of 53 cm in the mentioned period, whereas the lowest mean monthly water levels were in August, and the maximum mean monthly water levels in March and April. The average mean annual discharge of the Đetinja near Sengolj was 5.60 m3/s of the observation period 1978-2008. The annual value of the average discharges was similar to the annual value of the mean monthly low and high waters. It has been concluded that the Đetinja River belongs to the moderate-continental variance of the pluvial-nival regime. The results of the research have shown that about 5.60 m3/s of water is formed in the Đetinja Basin with specific runoff of 10.95 l/s/km2. Even though precipitation is not so low and ranges around 875 mm per year, the amount of the river inflow is smaller due to high evaporation of over 60%. Considering that the Sengolj hydrological station has been situated at 8.2 km from the mouth, and the station Stapari stopped working in 2002, there is an opinion that it would be significant to put the hydrological station in the part of the river course, as well as on larger tributaries. .
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