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棉短绒

与 棉短绒 相关的网络例句 [注:此内容来源于网络,仅供参考]

Arabian cotton; American short staple cotton;Levant cotton; herbaceous cotton

阿拉伯棉;美国短绒棉;黎凡特棉;草本棉

Herbaceous cotton; Levant cotton; American short staple cotton; Arabian cotton

草本棉;黎凡特棉;美国短绒棉;阿拉伯棉

American short staple cotton; Arabian cotton;herbaceous cotton; Levant cotton

美国短绒棉;阿拉伯棉;草本棉;黎凡特棉

Arabian cotton; American short staple cotton; Levant cotton; herbaceous cotton YdIZik F

阿拉伯棉;美国短绒棉;黎凡特棉;草本棉 8X278

American short staple cotton; Arabian cotton;herbaceous cotton; Levant cotton

美国短绒棉;阿拉伯棉;草本棉;黎凡特棉阿拉伯人一代又一代地分担着它的游牧主人的艰辛。

American short staple cotton; Arabian cotton; herbaceous cotton; Levant cotton

美国短绒棉;阿拉伯棉;草本棉;黎凡特棉分期偿付计划,分期偿付时间表

Herbaceous cotton; Levant cotton; American short

草本棉;黎凡特棉;美国短绒棉;阿拉伯棉

Levant cotton; herbaceous cotton; American short

列凡特海棉,草本棉,美国短绒棉,阿拉伯棉

American short staple cotton; Arabian cotton; herbaceous cotton; Levant cotton 3x+lf4

美国短绒棉;阿拉伯棉;草本棉;黎凡特棉%;'~TtW5分期偿付计划,分期偿付时间表 v76Gwu$d

The orthogonal experiment also indicates that the speed of cylinder., the speed of licker-in, the output speed of the carding sliver and the neps and short fibre. To further optimize the above four factors , a regress equation can be moleculed by the neps and the first three factors, Which can provide a theory for analyzhg neps controlling.

正交试验结果表明:锡林速度、刺辊速度、道夫速度、出条速度对棉结与短绒的影响不完全一致,在对这四个参数进行优化组合基础上,进一步建立棉结与锡林速度、刺辊速度、出条速度三个因素间的回归方程,为生条棉结控制提供了定性分析的理论依据。

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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。