查询词典 capillary rise
- 与 capillary rise 相关的网络例句 [注:此内容来源于网络,仅供参考]
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It is similar to the force that causes a liquid to rise in a capillary tube - the capillary attraction, or capillarity.
这是内聚力作用于液体表面的结果;正如引起液体沿毛细管上升的毛细引力。
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Capillary discharge ; Rise time ; Peak of current pulse ; Pulse width ; Soft X-ray laser
毛细管放电;上升时间;电流脉冲峰值;脉冲宽度;软X射线激光
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When crude oil content up to 1%, capillary water doesn't rise.
含油量≥1%的原油污染土壤毛细水上升高度为零。
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Mercury contained in a bulb at the bottom of a graduated sealed capillary tube expands with a rise in temperature causing a thin thread of mercury to rise in the tube .
在密封的毛细管内的底部有装有水银的球状物,向上通有小管随着温度的上升水银会上升。
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A similar suggestion was made by Robert Boyle (25 Jan. 1627 - 30 Dec 1691), who thought that a very narrow bore tube would allow a liquid to rise continually by capillary effects.
类似的建议是由罗伯特波义耳( 1627年1月25日-1 691年1 2月3 0日),谁想到一个非常狭窄的口径钢管将允许液体不断上升的毛细管作用。
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The results showed that the maximum height of the capillary water rise of layered soil was mainly determined by the sand soil texture, position, thickness and their mutual relationship, and they also were closer connected with other soil texture in the profile.
针对目前层状土体剖面夹层土质对毛管水分最大上升高度的影响存在较大分歧,以沙土夹层为例,从土坡水动力学的角度,通过实验和理论分析,分不同情况对层状土城的毛管水最大上升高度进行了系统研究。
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Green-Ampt model can be applied in analyzing capillary water rise process of homogeneous soil. A laboratory experiment was conducted for capillary soil transport characteristics of homogeneous soil.
将Green-Ampt模型用于均质土壤毛管水上升过程分析中,通过室内土柱模拟试验,对均质土毛管水运动特性进行了研究。
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The results showed that there was power function relationship between the capillary water rise height and groundwater supply quantity and the time. There was linear function relationship between capillary water rise height and groundwater supply quantity and a power function between them and the time. There was linear function relationship between the capillary water rise velocity and the groundwater supply rate. Parameters could be calculated by measured data, which showed that it is possible to simulate capillary water rise process of homogeneous soil by Green-Ampt model.
结果表明:均质土毛管水上升高度和地下水补给量均与时间之间为幂函数关系,毛管水上升速度和地下水补给速率也均与时间呈幂函数关系,毛管水上升高度与地下水补给量之间呈明显的线性关系,毛管水上升速度与地下水补给速率也呈线性关系;通过试验资料可以推求有关参数;说明入渗条件下的Green-Ampt模型用于模拟均质土的毛管水上升过程是可行的。
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The results of the test show that the whole intensity and comprehensive stability of subgrade made a good progress because the capillary water cant rise by using the insulating layer. In the prior condition of taking insulating layer thickness as 0.2m, choosing insulating layer 0.5m, 0.8m, below the pavement, the stability of seasonal frozen soil subgrade is analyzed. The results of the test also show that the optimal position of the insulating layer is 1.0m~1.5m .
试验表明,由于隔离层的作用使得毛细水无法迁移,对路基整体的强度和综合稳定性都有了很大程度上的提高,同时试验还表明在隔离层厚度为0.2m的前提下,设置在距路面以下1.0m~1.5m位置,即路基表面以下0.5m~0.8m处对路基的稳定性最为有利。
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Some of the liquid spills out through the capillary constantly with the rise of the temperature of the content. Wipe away the overflown liquid with a piece of filter paper at any time until the fluid does not overflow anymore. Remove the pycnometer from the water bath rapidly. Proceed as described under method (1), starting from the words "clean off any material on the outside with a piece of filter paper…".
取洁净、干燥并精密称定重量的比重瓶,装满供试品(温度应低于20°C或各品种项下规定的温度)后,插入中心有毛细孔的瓶塞,用滤纸将从塞孔溢出的液体擦干,置20°C(或各品种项下规定的温度)恒温水浴中,放置若干分钟,随着供试液温度的上升,过多的液体将不断从塞孔溢出,随时用滤纸将瓶塞顶端擦干,待液体不再由塞孔溢出,迅即将比重瓶自水浴中取出,照上述(1)法,自"再用滤纸将比重瓶的外面擦净"起,依法测定,即得。
- 推荐网络例句
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Finally, according to market conditions and market products this article paper analyzes the trends in the development of camera technology, and designs a color night vision camera.
最后根据市场情况和市面上产品的情况分析了摄像机技术的发展趋势,并设计了一款彩色夜视摄像机。
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Only person height weeds and the fierce looks stone idles were there.
只有半人深的荒草和龇牙咧嘴的神像。
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This dramatic range, steeper than the Himalayas, is the upturned rim of the eastern edge of Tibet, a plateau that has risen to 5 km in response to the slow but un stoppable collision of India with Asia that began about 55 million years ago and which continues unabated today.
这一引人注目的地域范围,比喜马拉雅山更加陡峭,是处于西藏东部边缘的朝上翻的边框地带。响应启始于约5500万年前的、缓慢的但却不可阻挡的印度与亚洲地壳板块碰撞,高原已上升至五千米,这种碰撞持续至今,毫无衰退。