河流泥沙工程学,river sediment engineering
1)river sediment engineering河流泥沙工程学
2)river sedimentation engineering河流泥沙工程学
3)river sediment engineering河流泥沙工程
4)sediment engineering泥沙工程学
5)sediment[英]['sed?m?nt][美]['s?d?m?nt]河流泥沙
1.Through the variation analysis of runoff and sediment transport capacity of Qiushuihe River from 1954 to 2000,the flow-sediment relationship of the river has shown a great change since 1978.通过对湫水河林家坪水文站20世纪50年代以来径流量和输沙量的变化分析,表明20世纪70年代中期以来,湫水河的水沙关系发生了较大变化,河流泥沙呈明显减少的趋势。
2.Combined with the optimum regularizafion technique inverse algorithm,the particle size distributions of sediments under different volume fractions and different particle size distribution were obtained according to the attenuation prediction of coupled-phase model plus a scattering model and experimental attenuation spectrum at fre- quencies ranges from 2 MHz to 7.宽频超声波通过河流泥沙悬浊液的声衰减谱包含了泥沙的颗粒粒度信息。
英文短句/例句

1.The Study of Physicochemical Process of Sediment Movement in River;河流泥沙运动物理化学过程初步研究
2.A Study about Impacts of Human Activities in the Mid-lower Yangtze on Fluvial Sediment Supply from River Basin and Sediment Discharge from the Yangtze into the Sea;长江中下游人类活动对河流泥沙来源及入海泥沙的影响研究
3.Surface Erosion in Upper Yangtze Region and River Sediment Transport长江上游流域地表侵蚀与河流泥沙输移
4.Response of Sediment to Correlative Significant Events and Policies of Hekou-Longmen Region in Huanghe River basin黄河河龙区间河流泥沙对相关重大事件与政策的响应
5.Many rivers carry silt toward the equator.许多河流带着泥沙流向赤道。
6.Analysis of Sediment Dispersal of the Huanghe(Yellow) River Mouth--A Case of Diaokouhe Lobe黄河河口泥沙扩散规律分析——以钓口河流路为例
7.Technical specifications for tidal current and sediment simulation of coasts and river mouths海岸与河口潮流泥沙模拟技术规程
8.Code for measurement of suspended sediment in open channels河流悬移质泥沙测验规范
9.Numerical Simulation of Wave, Tidalcurrent and Sediment of Estuary and Coast;河口、海岸波浪、潮流、泥沙数值模拟
10.The Research and Application of Mathematical Sedimentation Model for DuLiuJianhe River Estuary;独流减河口泥沙数学模型研究及应用
11.Development of Mathematical Model for Unsteady Sediment Transport of the Lower Weihe River;渭河下游非恒定流泥沙数学模型研究
12.Research on Regulation of Waterway on Mouth Bar in Guan River Estuary by a 2D Horizontal Current and Sediment Numerical Model;灌河口拦门沙航道治理潮流、泥沙数模研究
13.Analysis on erosion and deposition in Wujiadu-Xiaoliuxiang reach of the main stem Huaihe River淮河干流吴家渡至小柳巷河段泥沙冲淤分析
14.Study on the Basic Laws of Flow and Sediment Transport in Alluvial Channels冲积河流水流泥沙运动基本规律的研究
15.Evaluation of Runoff and Sediment from Daning River Watershed in Three Gorges Reservoir Region Based on AnnAGNPS Model City三峡库区大宁河流域径流泥沙的AnnAGNPS定量评价
16.Relationship between ion transport and sediment discharge in river河流水化学特性与流域泥沙输移的相关性研究
17.Technical specifications for current and sediment simulation of inland river navigation channels and ports内河航道与港口水流泥沙模拟技术规程
18.SCOUR-AND-FILL AND SILT DISTRIBUTION OF SILTS IN THE DIAOKOU CHANNEL OF THE HUANGHE RIVER EROM 1964 TO 1976黄河1964—1976年刁口流路泥沙冲淤及其分布特点
相关短句/例句

river sedimentation engineering河流泥沙工程学
3)river sediment engineering河流泥沙工程
4)sediment engineering泥沙工程学
5)sediment[英]['sed?m?nt][美]['s?d?m?nt]河流泥沙
1.Through the variation analysis of runoff and sediment transport capacity of Qiushuihe River from 1954 to 2000,the flow-sediment relationship of the river has shown a great change since 1978.通过对湫水河林家坪水文站20世纪50年代以来径流量和输沙量的变化分析,表明20世纪70年代中期以来,湫水河的水沙关系发生了较大变化,河流泥沙呈明显减少的趋势。
2.Combined with the optimum regularizafion technique inverse algorithm,the particle size distributions of sediments under different volume fractions and different particle size distribution were obtained according to the attenuation prediction of coupled-phase model plus a scattering model and experimental attenuation spectrum at fre- quencies ranges from 2 MHz to 7.宽频超声波通过河流泥沙悬浊液的声衰减谱包含了泥沙的颗粒粒度信息。
6)river sediment河流泥沙
1.Research of soil erosion and river sediment in Iran伊朗土壤侵蚀及河流泥沙研究
2.Analysis on suspended and bed-load ratio of river sediment for South Xinjiang新疆南疆地区河流泥沙推悬比分析研究
延伸阅读

河流泥沙河流泥沙riversediment河水挟带的岩土颗粒。泥沙输运是河流中重要的水文现象,它对于河流的变迁有重大的影响(见河床演变)。泥沙按输移特性分为推移质和悬移质。在悬移质泥沙中,部分细颗粒泥沙随水流一泻千里,不在河槽中沉降,不参与河床泥沙的交换,称冲泻质或非造床质,其余较粗颗粒则参与河床泥沙的交换和冲淤变化,称为床沙质或造床质。推移质一般仅占悬移质泥沙的5%~10%,在山区河流,有时可占10%~20%或更多。单位体积浑水中所含泥沙的数量称含沙量,单位为千克/米3。一定时段内通过河道某断面的泥沙数量称为该时段的输沙量,单位为千克或吨。河流含沙量随时间而变化。一年中最大含沙量出现在汛期,最小含沙量在枯水期。在一次洪水过程中,最大含沙量称沙峰。沙峰不一定与洪峰同时出现,一年中首场大洪水的沙峰常比洪峰出现早,以后则可能同时出现,也可能沙峰滞后于洪峰。含沙量沿水深的分布,通常在水面处最小,河底处最大。悬移质中粗粒泥沙含量近河底很大。自河底向上则急剧减小。较细的颗粒,如粉沙和粘土,沿水深的分布则较均匀。含沙量沿水深基本呈某种指数曲线分布,指数值与泥沙颗粒的大小和水流条件有关。由于水内各种副流的影响,最大的含沙量也可能不在靠近河底,而是在河底以上的某一位置。含沙量在河流横断面上的分布随断面上水流情况不同而异。如水流在断面上的分布比较均匀,含沙量的横向分布较均匀。如水流情况较复杂,则含沙量的横向分布往往很不均匀。含沙量沿河长的分布,一般从上游向下游递减,也取决于流域产沙特性、河道特性和支流汇入等因素的影响程度。黄河中游流经黄土高原,沿途有高含沙量的支流汇入,因而含沙量反而沿程增加,下游河床开阔,大量泥沙落淤,含沙量才趋向减小。中国主要河流输沙量见表。表:中国主要河流输沙量