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甜香

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Introduction】 Deep plummy red color. Mint and mulberries on the nose, followed through on the palate supported by well integrated, ripe tannins.

酒色呈深李子红色,有着薄荷和成熟的法国浆果气息,比如黑加仑子色樱桃\\子以及李子干的甜香气息,单宁适中,有架构。

The wine with strong personality , complex aroma with a ripe fruity over a background of herbs , sundried apricot .

回荡在口中复杂的香气令人赞叹,细腻的香料香、干燥后的杏子香、像是可可豆的甜香以及矿物质的味道都可以在这里发现。

In August, the garden is filled with the sweet and fragrant flavor of the sweet-scented osmanthus.

八月的花园里,空气中充满了木樨花的甜香味道。

Odor Characteristics—Sweet, aldehydic, orange, waxy and citrus rind.

香气特征:甜香,醛香,甜橙香,蜡香和柑橘皮香。

Taste Characteristics— 10ppm. Floral, citrus, orange, sweet, aldehydic with a slight mandarinnuance.

味觉特征:在10ppm 时,有花香,柑橘香,甜橙香,甜香,带有轻微红桔的醛香味。

Taste characteristics— 10ppm. Sweet, floral, fruity, aldehydic with a terpy nuance.

味觉特征:在10ppm 时,有甜香,花香,果香,带有萜烯的醛香味。

Description: sweet, anisic odor; green vegetable; berry-currant; melon-like.

香气描述:甜香,茴香香气,绿色蔬菜;桨果-黑醋栗;似甜瓜。

Chimonanthus fragrans , in English the Winter-sweet, should have a place of honour.

对于腊梅,英语叫做冬季甜香,应该给予尊敬。

The made tea fertilized with organic fertilizers possessed higher contents of geraniol, geranic acid,phenyl ethanol,linalool and its oxides,and the aroma was characterizd as of "keemum geraniol," with sweet smelling.

全年施用有机肥的红茶中,香叶醇、香叶酸、苯乙醇、芳樟醇及其氧化物含量高,红茶甜香,具有明显的&祁门香&特征

A sweet, smooth, and zesty smoke.

甜香,平滑的,讓人性質很高的烟雾。

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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。