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The fermentation conditions for producing chymosin with rhizopus have been investigated in this paper.

对根霉经发酵产凝乳酶的发酵条件进行研究。

The application of pH value in testing saccharide acidity in rhizopus starter production was studied.

比较研究pH值在根霉曲生产过程检验糖分和酸度中的应用方法。

The invention relates to a fungi Rhizopus arrhizus and its application in Pu'er tea production, belongs to the biotechnology field.

本发明涉及一种少根根霉真菌及其在普洱茶生产中的应用,属生物技术领域。

This paper at first separated the protoplast from rhizopus and yeast respectively, and then merged the protoplasts of them.

利用分离的根霉、假丝酵母菌种,首先各自进行菌体活化,原生质体制备,然后将两菌进行杂交融合。

One cellulase-production strain TC1 was screened. It was identified as Rhizopus sp. based on identification method of fungi.

筛选得到1株纤维素酶产生菌TC1,根据真菌的分类鉴定方法,鉴定为根霉属菌(Rhizopus sp。)。

The optimization of liquid state fermentation conditions of fibrinolytic enzyme produced by Rhizopus sp.

[目的]研究根霉Yc1以豆渣为原料经液态发酵产生纤溶酶的发酵条件。

Another popular product is tempeh, a soybean mash fermented by Rhizopus.

另一种产品是天培,一种用根霉发酵成的豆酱。

Cultivar resistance has been the most effective way to control Phytophthora root rot.

利用抗病品种是防治大豆疫霉根腐病最有效的方法。

Sharing economic loss of soybean industry is caused by Phytophthora root rot of soybean every year.

大豆疫霉根腐病是毁灭性病害之一,每年都会给大豆产业带来巨大的经济损失。

Phytophthora root rot of soybean caused by Phytophthora sojae is one of the most dangerous soybean disease.

大豆疫霉根腐病是一种毁灭性的大豆土传病害,由Phytophthora sojae引起。

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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。