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downward erosion相关的网络例句

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与 downward erosion 相关的网络例句 [注:此内容来源于网络,仅供参考]

According to the result of artificial rainfall, the character and factors affectedby soil, rainfall, chemicals, slope length, slope gradient and field mangment practices, for rainfall, runoff,infiltration, soil erosion and soil chemicals, such as NO_3~-, NH_4~+, PO_4~(3-), K~+ and Br~-, are investigated. Thedeterminate methods, influence factors and practical application of the mixing zone depth are also researched.The results can enrich the dynamics of soil, water and nutrient transport, evaluate the soil water and fertilizerefficiency, and theoretically benefit the research of agricultural NSP on loess hill slope. 1. According to the surface transport experiments of soil chemicals under the non-satuation soil and watererosion condiction, for adsorbed PO_4~(3-) and K~+, the time of sheet erosion and rill erosion initiation is coincidentthat of chemicals content in surface runoff climbs, and then their abundant export by surface runoff is urged.

本文以黄土坡地为研究对象,通过模拟降雨试验,研究土壤因素、降雨因素、化学物质理化性质、坡长坡度因素和农田管理措施等对坡地降雨—产流—入渗—土壤侵蚀—农田NO_3~-、NH_4~+、PO_4~(3-)、K~+和Br~-地表迁移的影响,研究非饱和土壤和水蚀条件下混合层深度的确定、影响因素和模拟,探讨其在黄土坡地的实际应用,为丰富坡地水分养分迁移动力学、提高旱地土壤水分养分利用率和深化农田非点源污染研究提供理论依据。

By using the programs to process water depth data,the erosion and accumulation area can be found by drawing the contour diagram and stereogram about erosion and accumulation,and the corresponding erosion and accumulation weight and area sizes can also be calculated.

经程序处理后的水深数据,可以找出其冲淤区、绘制冲淤等值线图和冲淤立体图;计算出其冲淤量和冲淤面积。

Based on observation data, the development process of the breach of landslide dams due to over topping may divided into 3 modes: vertical erosion, breadthwise extension and regression erosion of dam slope. A mathematical model describing the gradual failure process of the landslide dams is established based on the formula expressing the high intensity erosion obtained from experimental data, which can integrate the 3 modes of breach development process together. The validity of the model is verified by observation data.

根据一般滑坡堰塞坝特点和实际观测到的堰塞坝溃口发展规律建立了一个溃口扩展模式,并将溃口扩展过程归纳为溃口垂直下切、横向扩展和坝坡溯源冲刷3种主要表现形式,采用通过试验资料建立的高强度泥沙冲刷计算公式将这3种表现方式联系在一起,建立了堰塞坝逐渐溃决数学模型,并利用实测溃坝资料验证了模型的可靠性。

Instead, the erosion resistance is increased after FSP. The refined and uniformly distributed second phases, which are resulted from the FSP, can help to increase the hardness and further reduce the brittle fracture of the specimens. Si and nvAl3CuNi phases are usually found near or end of the grooves with little fracture. But the τ1 (Al9FeNi) phase is easier to be removed by the erodent cutting. It can be inferred that Si and nvAl3CuNi are useful to improve the erosion resistance of A384 aluminum alloy, but τ1 (Al9FeNi) phase is detrimental for the erosion resistance of A384 aluminum alloy.

经摩擦搅拌制程改质后,硬度提升,晶出相细化且均匀分布,降低脆性龟裂的现象发生,有助於改善A384铝合金的磨耗性质,其中,亦发现在冲蚀沟槽附近有残留和脆性破裂之共晶Si颗粒和nvAl3CuNiw晶出相,推测此两相为A384铝合金中有助提升磨耗阻抗的第二相;而τ1(Al9FeNi)晶出相则容易受到冲蚀颗粒的切削而被冲蚀颗粒移除,增加材料的重量损失,推测τ1(Al9FeNi)晶出相为A384铝合金中较不耐磨耗的晶出相。

The results showed, the intention of erosion of rock and soil has two sides: one is that object of erosion is mixture of rock and soil, that is, the micro-change of composition of soil surface is complexer; another is that the means and degree of erosion is different from original geomorphy.

结果表明,岩土侵蚀的内涵为:一是侵蚀的对象是岩土非均匀混合物,也就是说,地表组成物的微变化比较复杂;二是侵蚀的方式、程度与原地貌有明显的不同。

Among various affecting factors of gravity erosion,the topography and geomorphy,i.e.the gravity erosion provides the basic dynamic force and its behavior is the results of long-term action of gravity erosion.

在重力侵蚀的各种影响因素中,地形地貌既为重力侵蚀的发生提供基本动力,其形态又是重力侵蚀长期作用的结果。

Headward erosion is main cause of river captrue,but it is not only; Erodeless belt is not absolute erodeless; Erosion of below river can cut through the watershed by "erosion chain" at last,Erodeless belt is not obstacle to river ...

认为,河流袭夺概念有其特定含义,河流袭夺和河流侵并两种河流兼并现象并存不悖;溯源侵蚀是河流袭夺的主因,但不是唯一原因;无冲刷带并非绝对的无冲刷,低位河的侵蚀通过&侵蚀链&最终能够切穿分水岭,无冲刷带不是河流袭夺不可逾越的障碍。

2Analyzing the unstructural knowledge of factors influencing soil erosion in theresearch area.17 watersheds in Guizhou Province were chosen and the relationship betweeninfluent factors of soil erosion and soil erosion there was studied.

分析了研究区土壤侵蚀影响因子的非结构性知识。

The relationship of slope and upslope drainage area of the study area is S = 0.074 A-0.1895, and the gully initiation process is an interaction process of hydrological erosion, melt erosion and landslide erosion, the initiation threshold is increased by the biomass.

研究所得的切沟发育临界地形条件为S = 0.074 A-0.1895,研究区切沟发育的过程是受水力侵蚀、冻融侵蚀和重力侵蚀的交互影响的过程,而沟头植被覆盖的增大会导致切沟发育临界条件的增大。

The results show that an internal and mutual transformation of land-use types cause striking changes in soil erosion extent. The transition of cultivated land to woodland and grassland medicates erosion intensity, and the one from forestland to cultivated land and grassland aggravates erosion. In addition, land-use practices, including mainly human activities, have impacts on the content of suspended sediment.

研究表明,本区土地利用类型的内部转化和相互转化引起土壤侵蚀程度的明显变化;耕地向林地、草地的转化使侵蚀强度指数显著降低;林地向耕地、草地转化,均显著增加侵蚀强度指数;耕地、林地、草地的内部转化对土壤侵蚀也有少量影响。

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