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与 结冰的 相关的网络例句 [注:此内容来源于网络,仅供参考]

Some apples are dried, frozen, or made into specialty products such as "apple butter"(a spread prepared by stewing apples in cider, sugar, and spices).

有些苹果被烘乾,结冰或者被做成专业产品例如"苹果butter"(炖准备的传播在萍果汁、糖和香料的苹果)。

Accretion of aduct-diameter and emission speed also can freeze more axial area, but for the influence of radial thickness close-by orifice ,it is less.

管径和出口流速增大均能使结冰区域的轴向范围增大,但对近排放口处的厚度影响较小。

Ice appeared in snowflake patterns and crackled over the Vice Admiral's desk.

雪花状的图案象结冰一样在中将的桌子上破裂般伸展。

At this time of year, the waters around the elvish island of Vori freeze.

一年里的这个时期,凡里岛的周围水域都结冰了。

The system is designed such that it can be operated by its own and has the advantage of fast ice making.

本海水液体冰制冰机器则是利用抽水马达抽水,经过冰筒冷却,将内部的水降温后使用冰刀将冰由冰筒下方往上推动,再将其刮出后再回到原来的容器,一直循环到完成结冰为止。

The unusually long period of cold weather has shown how even warm climates can sometimes freeze over.

异常的长期寒冷天气表明,即使是温暖的气候有时也会结冰。

In winter across the northlands, you can see fishermen sitting on ice-covered lakes near holes in the ice.

在北国的冬天,你可以看到钓客坐在结冰湖面凿出的洞口附近。

All exposed instrumentation must be specially designed to remain ice-free.

各种在气流中的仪表都必须专门设计的以防结冰。

The initial freezing and re-freezing of the igloo takes place at end of the igloo's construction.

冰屋的持续结冰发生在建筑过程的末尾。

Practically Possible Lowest Unfrozen Temperature of water or of a surface is defined.

本文首次提出了水以及表面的实际最低不结冰温度的概念。

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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。

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。

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。