Due to the presence of boulders and different morphologies, mountain rivers contain various resistance sources. To correctly simulate river flow using 1-D hydrodynamic models, an …
Mountain-rivers are, by far, the most challenging case to model because of its bed characteristics and their energy dissipation mechanisms depending on its irregular …
Este trabajo de tesis compara el comportamiento que presentan diferentes funciones likelihoods de la metodología GLUE en la clasificación de coeficientes de rugosidad de ríos …
AO Alvarado Martinez - 2022 - dspace.ucuenca.edu.ec
The behavior of many physical systems is described by means of differential equations. These equations are usually derived from balance principles and certain modelling …
Tez kapsamında, üniform olmayan akımlarda su yüzeyi profilleri hem deneysel hem de sayısal olarak araştırılmıştır. Bu amaçla, Dokuz Eylül Üniversitesi İnşaat Mühendisliği …
W Artichowicz, D Prybytak - Archives of Hydro-Engineering and …, 2015 - sciendo.com
In this paper, energy slope averaging in the one-dimensional steady gradually varied flow model is considered. For this purpose, different methods of averaging the energy slope …
ER Sanchez Cordero, LM Timbe Castro… - 2021 - dspace-test.ucuenca.edu.ec
Due to the presence of boulders and different morphologies, mountain rivers contain various resistance sources. To correctly simulate river flow using 1-D hydrodynamic models, an …
Due to the presence of boulders and different morphologies, mountain rivers contain various resistance sources. To correctly simulate river flow using 1-D hydrodynamic models, an …
أحمد إبراهيم صابر, أحمد إبراهيم, شلبي… - مجلة کلية الآداب. جامعة …, 2021 - journals.ekb.eg
النهر ککتلة متحرکة من الماء لابد أن يکون له طاقة أو قوة تتوقف على العديد من المتغيرات الهيدروليکية والتي يصعب الفصل بينهما، ومع اختلاف هذه المتغيرات تتباين طاقة النهر من موقع …