SEDIMENT TRANSPORT MODELING IN WATERSHED AND RIVER FOR THE LOESS ZONE IN CHINA

机译：中国黄土区流域泥沙迁移模型

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Based on a large amount of field data of erosion and sediment yield in loess zonewith different natural and social circumstances, the runoff in depth and the sedimentyield in a small watershed for one storm were derived. A large basin can be dividedinto a series of small watersheds linked by rivers. The universal river and reservoirsedimentation model was adopted. With the equations in small watersheds andexisting mathematical river model, a mathematical model for prediction of sedimentyield in a large basin for one storm has been established. The calibration of its resultsof the model is satisfactory.

机译：根据大量自然和社会环境不同的黄土带侵蚀和泥沙产量的现场数据，得出了一场暴雨的小流域的径流深度和产沙量。一个大盆地可以分为一系列由河流相连的小流域。采用通用河流和水库沉积模型。利用小流域方程和现有的数学河模型，建立了一个大流域一次暴雨的产沙量预测数学模型。模型结果的校准令人满意。

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来源
《Congress of the International Association for Hydraulics Research;Biennial congress of the International Association for Hydraulics Research》|1999年|p.1-6|共6页
会议地点 Graz(AT);Graz(AT)
作者
CAO WENHONG;
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作者单位

CN-7611Member of IAHRSenior Engineer DirectorDivision of Soil and Water ConservationDepartment of Sediment ResearchChina Institute of Water Resources and Hydropower ResearchP. O. BOX 366 Beijing ChinaTelephone: 0086-10-68415522 extension 6633Fax: 0086-10-68416371E-mail: erosion@iwhr.com;

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关键词
runoff; ; sediment yield; ; watershed; ; river; ; storm;

机译：径流; ;泥沙产量;分水岭;河; ;风暴;

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1. Piecewise prediction model for watershed‐scale erosion and sediment yield of individual rainfall events on the Loess Plateau, China [J] . Guo‐Qiang Yu, Mao‐Sheng Zhang, Zhan‐Bin Li, Hydrological ProcHydrological Processesrnesses . 2014,第21期

机译：黄土高原各降雨事件流域尺度侵蚀与产沙量的分段预测模型
2. Spatial scale effect on sediment dynamics in basin-wide floods within a typical agro-watershed: A case study in the hilly loess region of the Chinese Loess Plateau [J] . Le-Tao Zhang, Zhan-Bin Li, Shan-Shan Wang The Science of the Total Environment . 2016,第deca1期

机译：典型农业流域内流域范围洪水对沉积物动力学的空间尺度影响-以黄土高原丘陵区为例
3. Modeling the daily suspended sediment concentration in a hyperconcentrated river on the Loess Plateau, China, using the Wavelet-ANN approach [J] . Qian-Jin Liu, Zhi-Hua Shi, Nu-Fang Fang, Geomorphology . 2013,第MARa15期

机译：利用小波神经网络方法模拟黄土高原高浓度河流的日悬浮泥沙浓度
4. SEDIMENT TRANSPORT MODELING IN WATERSHED AND RIVER FOR THE LOESS ZONE IN CHINA [C] . CAO WENHONG Biennial congress of the International Association for Hydraulics Research . 1999

机译：中国黄土区流域和河流的沉积物运输建模
5. Modeling sediment transport in eddy recirculation zones of the Colorado River in Grand Canyon. [D] . Akahori, Ryosuke. 2007

机译：模拟大峡谷科罗拉多河涡流区的泥沙输送。
6. Sediment sources of Yangou watershed in the Loess Hilly region China under a certain rainstorm event [O] . Xue-xuan Xu, Tong-jun Ju, Shi-qing Zheng -1

机译：黄土丘陵区暴雨事件下盐沟流域的泥沙来源。
7. Influence of Landscape Pattern Changes on Runoff and Sediment in the Dali River Watershed on the Loess Plateau of China [O] . Yan Zhang, Zhilei Bi, Xin Zhang, 2019

机译：景观格局变化对中国黄土高原大理流域径流和沉积物的影响
8. Discrete Linear Models for Runoff and Sediment Discharge from the Loess Plateauof China [R] . Guang-Te, W., Smith, V. P., Changling, G., 1991

机译：中国黄土高原径流泥沙排出的离散线性模型

SEDIMENT TRANSPORT MODELING IN WATERSHED AND RIVER FOR THE LOESS ZONE IN CHINA

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