德拉瓦河下游泥沙变化的评价

IF 0.6 Q4 ENGINEERING, CIVIL
Senlin Zhu, O. Bonacci, D. Oskoruš
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引用次数: 4

摘要

本文使用重新缩放的调整偏和(RAPS)方法评估了德拉瓦河下游泥沙状况的变化,并讨论了这些变化的可能原因。Drava河下游两个测量站的泥沙状况突然改变,悬浮泥沙浓度急剧下降,始于20世纪80年代。从1967年至1981年(0.922×106吨/年)到2003年至2017年(0.323×106吨/年。Donji Miholjac站的悬移质输沙量在1971年至1981年(1.383×106吨/年)和2007年至2017年(0.263×106吨/年)之间下降了约81%。水库的建设和运行是造成这些急剧变化的主要原因。通过提出一种新形式的泥沙定额曲线(SRC)来评估SSC和流量(Q)的关系。与传统的SRC方法相比,新形式的SRC可以更好地捕捉SSC在日和月时间尺度上的季节动态。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
ASSESSING SEDIMENT REGIME ALTERATION OF THE LOWER DRAVA RIVER
Alterations to the sediment regime of the lower Drava River were assessed using the rescaled adjusted partial sums (RAPS) method and possible causes of these changes are discussed in this paper. The sudden alteration to sediment regime and the sharp decreases of suspended sediment concentration (SSC) at the two gauging stations in the lower Drava River began in the 1980s. Suspended sediment load decreased about 65% between 1967–1981 (0.922×106 t/year) and 2003–2017 (0.323×106 t/year) for the Botovo station. For the Donji Miholjac station, suspended sediment load decreased about 81% between 1971–1981 (1.383×106 t/year) and 2007–2017 (0.263×106 t/year). The construction and operation of reservoirs were the main reasons for these sharp alterations. SSC and flow discharge (Q) relationships were assessed by proposing a new form of a sediment rating curve (SRC). Compared with the traditional SRC approach, the new form of the SRC can better capture seasonal dynamics of SSC at daily and monthly time-scales.
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