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Titlebook: Advances in Water Resources Engineering and Management; Select Proceedings o Rafid AlKhaddar,Ram Karan Singh,Madhuri Kumari Conference proc

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樓主: Corrugate
31#
發(fā)表于 2025-3-27 00:36:42 | 只看該作者
32#
發(fā)表于 2025-3-27 03:45:40 | 只看該作者
33#
發(fā)表于 2025-3-27 07:51:33 | 只看該作者
Agency: A Historical Perspectiveion on bridge piers has been found as one of the main causes for bridge collapse. The combined action of enhanced scouring at the base of the pier and increased hydrodynamic load is viewed as the main force driving the enhanced failure probability. It is therefore fundamental to understand the distr
34#
發(fā)表于 2025-3-27 11:20:28 | 只看該作者
Annals of Theoretical Psychologysider the real-time hydrological uncertain events. In this paper, a real-time operation model is presented for Tanahu Hydropower Reservoir System in Nepal. To handle the real-time hydrology, it has to predict the reservoir inflow, which is done by using genetic programming (GP). For this, GP-based i
35#
發(fā)表于 2025-3-27 14:50:57 | 只看該作者
Starting Points for Agency Researchder the?dynamic leadership and undergoing a transition between modernization and tradition. On the one hand, KSA is among the most stressed regions of the world from the water resource point of view; on the other hand, it is a country with the highest oil reserves in the world. The water footprint (
36#
發(fā)表于 2025-3-27 20:16:04 | 只看該作者
37#
發(fā)表于 2025-3-27 23:20:50 | 只看該作者
38#
發(fā)表于 2025-3-28 04:53:39 | 只看該作者
https://doi.org/10.1007/b108296 is incurred. Soil loss is one of such significant environmental problems. Various models such as USLE, RUSLE, USPED and LISEM are developed for rapid assessment of soil loss. Assessment of soil loss is considered as a significant, as it leads to loss of top layers of soil and thus reduces the ferti
39#
發(fā)表于 2025-3-28 06:40:35 | 只看該作者
40#
發(fā)表于 2025-3-28 10:25:46 | 只看該作者
Arthur Wingfield,Patricia A. Tunpacity of storm water drains is called urban flooding. Urbanization disrupts the natural water balance by increasing impervious areas and reduction in infiltration. This increases runoff from urban catchments and leads to higher flood peaks even for short-duration low-intensity rainfall. Such flash
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