厌学
- 与 厌学 相关的网络例句 [注:此内容来源于网络,仅供参考]
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Zeta potential was -44.23 millivolt. Viscosity was 1.83 mpa. All of which were coincided with physical desire. In addition, the tests of PHGF liposomes including irritation, hemolysis, pyrogen, anomaly toxicity and hypersensibility, proved that the preparation reached the standard of intravenous injection entirely. Taking glutamic pyruvic transaminase and malondialdehyde in mice as index, studies on pharmacodynamics after hepatic injure caused by tetrachloromethane in mice indicated that GPT level (P.001) and MDA yieldment P
以小鼠CCli急性中毒性肝损伤为模型,以动物血清中谷丙转氨酶(GP水平与肝脏中丙二醛p A烨成量为指标,进行PHGF脂质体的药效学试验,结果表明P**F脂质体能显著降低GP T水平o<0刀01)与MD A 生成量厌<o.05);大鼠组织形态的观察表明高剂量***F脂质体能使肝脏 0 内皮细胞增生活跃,提高肝细胞的免疫功能,对受损肝细胞具有修复作用;同样小鼠碳廓清试验也显示PHGF脂质体较市售粉针具有更好的机体免 p 疫作用o功刀01),达到制剂设计目的,获得较好的结果。
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Dissimilatory Fe oxide reduction under anaerobic condition is a process which is an anaerobic respiration with Fe as the terminal electron acceptor. This anaerobic respiration showed important environmental significances. Dissimilatory Fe reducers can use diverse electron acceptors including many toxic heavy metals and metalloids such as Mn、Cr、Co insides Fe. So these toxic metals were detoxified or were immobilized reductively.
这种厌氧呼吸作用具有重要的环境学和地学意义,Fe还原微生物可利用除Fe以外的许多其它电子受体包括许多有毒重金属和类金属,如Mn、Cr、Co等,从而对这些有毒重金属起到还原解毒或还原固定的作用;还原过程还可促进一些有机污染物的降解; Fe氧化物的还原偶联着Si、P等元素的变化,对提高这些营养元素的有效性发挥着重要作用。
- 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。