Using the experiential correlation method, sediment yield is calculated.

用经验相关法进行流域泥沙计算。

Scale transfer is the key of soil erosion and sediment yield modeling in different scales.

尺度转换是进行不同尺度间侵蚀产沙模拟的关键所在。

Slope length is one of the important geomorphologic factors affecting the surface runoff and sediment yield.

坡长是影响坡面径流和水流侵蚀产沙的重要地貌因素之一。

Slide erosion, the main resource of gully sediment yield, is one of the most important types of gravity erosion.

滑坡侵蚀是重力侵蚀的主要类型之一，是黄土高原陡坡侵蚀产沙和沟道侵蚀产沙的主要来源。

Erosion and sediment yield process of soil dumped by people have been analyzed by simulated rainfall experiments.

通过人工模拟降雨实验，研究分析了强降雨条件下人为弃土的侵蚀产沙量及侵蚀过程。

The results shows, the relationship between individual rainfall runoff depth and it's sediment yield is very close.

结果表明，次降雨径流深与其对应所产生的侵蚀量关系非常密切；

The result showed, that the fastigium of runoff yield and sediment yield were in accordance with the rainfall fastigium.

结果表明：径流小区产流、产沙量的高峰期与降雨量的高峰期相一致。

Slope sediment yield is under the impact of rainfall intensity, the change rules are similar to the runoff dynamic changes.

坡面产沙同样受降雨强度的影响，其变化规律同坡面产流的规律类似。

Results show that sediment yield decrease slightly but runoff yield increase obviously of Jinghe watershed nearly 50 years;

结果表明：泾河流域近50年来的输沙量略有下降，而径流量减少比较显著；

The features of erosion, sediment yield and sediment reduction by the comprehensive controlling are studied in Zhifang gully catchment.

该文以纸坊沟流域为例，分析了治理小流域侵蚀特征、产沙特征及综合治理减沙效益。

Space scales of soil erosion and sediment yield and scales transfer problems have become currently new fields in soil erosion researches.

侵蚀产沙的空间尺度及尺度转换问题已成为当前土壤侵蚀研究的前沿领域。

The trend of runoff and sediment yield in the Jihe watershed declined evidently first and then remained steady during the research period.

径流与泥沙在多年变化中均呈先下降后平缓趋势。

The impact of topography on the sediment yield and runoff generation is an important project and at the same time is an little studied problem.

地形对降雨量、产流量和产沙量的影响及其估算是一个十分重要的课题，同时也是一个相当困难和研究基础十分薄弱的课题。

Hyperconcentrated flows are an important factor responsible for the high-intensity erosion and sediment yield in the middle Yellow River basin.

高含沙水流搬运与重力侵蚀之间存在着很强的耦合关系，这是黄土高原高强度侵蚀产沙过程形成的重要因素。

The impacts of slope length on sediment yield under different conditions are experimentally studied by means of artificial rainfall simulation.

本研究通过一系列人工模拟降雨，研究了在不同条件下坡长对侵蚀产沙过程的影响。

The paper studied the runoff generation and sediment yield regulations of the natural slope-green-land in loess zone by the simulated rainfall.

通过野外模拟降雨试验，研究黄土区天然草坡的产流、产沙规律。

The average sediment yield rate and flow velocity decrease with the increase of coverage, but the influence of coverage on runoff is not remarkable.

草地坡面的平均输沙率及坡面流速随草地盖度的增大而减小，而盖度对草地坡面径流量的影响则不明显。

Through the analysis of characteristics of physic - chemistry and sediment yield produced by erosion in the area, the result show that the capacity...

通过对砒砂岩的理化及侵蚀产沙特性的分析表明，砒砂岩的产流和产沙能力均高于当地的黄土和风沙土。

In this research, soil erosion and sediment yield was calculated by runoff shear stress, runoff energy consumption and runoff power theory respectively.

分别利用坡面径流剪切力、坡面径流能耗和坡面径流单位水流功率理论对坡面土壤侵蚀发生过程进行了研究。

Results show that the visible difference of runoff yield and sediment yield and land cover pattern were found in the up of Huanjian, Heshuichuan and Ruihe.

结果表明：流域北部的环江上游、合水川与汭河的径流量和输沙量以及土地覆被空间格局分布差异显著；

Under the same other conditions, runoff generation, sediment concentration and sediment yield of the soil with smaller bulk density were relatively greater.

在其它条件相同时，容重较小的土质，其径流量、含沙量和产沙量相对较大。

And the relationship between sediment yield and its main influencing factors on the slopes of three different types of soil were established in the paper independently.

并分别建立了三种土质下产沙量与其主要影响因子的关系式。

The authors apply this method to the areas with high and coarse sediment yield of the Loess Plateau, and compartmentalize the river network into 4 grades and 37 regions.

将此方法应用于黄土高原多沙粗沙区的河网，按河网自然的拓扑形态和流域的天然分界将该地区河网划分为4级37区。

The study on regional distribution, area and sediment yield of different modulus of sediment transport provides a support to decide the coarse sand concentrated coming area.

研究不同输沙模数级的区域分布、面积及产沙量，为粗泥沙集中来源区界定提供支撑。

Understanding the methods of scale transfer in the processes of sediment yield is the base of soil erosion and sediment yield modeling in different scales and scale transfer.

认识侵蚀产沙过程中的尺度转换方法是进行不同尺度间侵蚀产沙模拟和尺度转换的基础。

The GIS-based soil erosion and sediment yield models, which can reflect the process of spatial distribution of soil erosion and sediment, will be the study focus in the future.

能反映侵蚀产沙时空过程的、基于GIS的分布式侵蚀产沙模型成为研究的重点。

Factors affecting the processes of soil erosion and sediment yield have more asymmetry and variability and enhance the complexity of modeling sediment yield in different scales.

影响侵蚀产沙过程的因素在时空上具有很大的不均匀性和变异性，增加了不同尺度间侵蚀产沙模拟的复杂性。

Almost all the sediment yield models of heavy rainfall built in recent years have adopted the assumption of sediment transport concentration of gullies and rivers being equal to 1.

近几年来建立的各类暴雨产沙模型，基本都采用沟道、河川泥沙的输移比等于1的假定。

This paper introduces soil erosion and sediment yield scale features, scale transfer styles and theory methods, and the necessity to pay attention to the problems of scale transfer.

本文在介绍了侵蚀产沙的尺度特征后，对侵蚀产沙尺度转换的类型和理论方法进行了总结，最后还强调了尺度转换中应注意的问题。

Further analysis of the root distribution pattern and the vertical sediment yield allowed establishment of a quantitative relationship between root biomass and vertical sediment yield.

通过进一步分析植被根系分布特征和土壤垂直侵蚀产沙之间的联系，建立了草地植被根系生物量与土壤垂直侵蚀产沙特征之间的定量关系。