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The photocatalytic activities were examined by degradation of alizarin red in sunlight and ultraviolet light.

茜素红溶液进行了在紫外灯及太阳光下的光催化降解,测试催化剂的催化活性,确定催化剂制备条件。

After calcium induction, the alizarin red staining was performed to test the formation of calcium concentration.

并分别采用茜素红钙盐染色和油红O染色进行鉴定。

The adsorptions of alizarin red on four TiO2 pillared bentonite samples were also studied.

研究了茜素红在4种TiO2柱撑膨润土上的吸附行为。

In order to determine the carbonation interface properly, Alizarin yellow R is chosen as the acid base indicator.

研制了新的具有球形凹面的混凝土试块及相应模具,实现了混凝土碳化试块的非破坏测试;选择了茜素黄R作为酸碱指示剂,合理地确定了检测时的碳化界面。

An adsorptive voltammetric procedure for determination of trace copper at alizarin modified carbon paste electrode was described .

报道了采用茜素修饰碳糊电极测定痕量铜的阳极溶出伏安法。

Alizarin red staining results showed that the calcified nodules were produced after induction.

茜素红染色结果表明,诱导后出现钙化结节。

The bleaching action of fluorides is slow in the alizarin dye procedure .

茜素染料法中,氟化物的消色作用较慢。

Eurasian herb having small yellow flowers and red roots formerly an important source of the dye alizarin .

生于欧亚的一种药草,开小黄花,根呈红色,以前是染色茜素的重要来源。

The complex of Cu and alizarin red S gave a sensitive complexing adsorptive wave.

在HAc-NaAc(pH=3.50)的溶液中,Cu2+与茜素红S生成配合物,该配合物在滴汞电极上于-0.18 V产生一个灵敏的配合吸附波。

One method of preparation new membrane materials was presented with putting multi-wall carbon nanotube and carboxylic multi-wall carbon nanotube in collodion solution.

分别将碳纳米管和羧基化碳纳米管均匀分散在火棉胶溶液中,采用流涎法制备出碳纳米管复合膜;并用分光光度法对样液、滤液中的间苯二酚和茜素红的吸光度进行了对比测定,以考察膜的吸附性能。

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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。