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单词 Crystalline water
释义

Crystalline water

原声例句
全球玩乐指南

In Ras Muhammad National Park, you can visit beaches with crystalline waters and coral reefs.

在拉斯穆罕默德国家公园，您可以参观拥有清澈海水的海滩和珊瑚礁。

全球玩乐指南

Its beautiful sands of dazzling white color And crystalline blue waters invite you to enjoy and rest peacefully.

美丽的白色沙滩和清澈湛蓝的海水诚邀您前来享受和宁静地休息。

加州的群山（上）

Here the tense, crystalline water is first dashed into coarse, granular spray mixed with dusty foam, and then divided into a diamond pattern by following the diagonal cleavage-joints that intersect the face of the precipice over which it pours.

在这里，紧张的结晶水首先冲入混合着灰尘泡沫的粗糙颗粒状喷雾，然后沿着与它倾倒的悬崖表面相交的对角线劈裂缝分成菱形图案。

中文百科

冰 Ice

（重定向自Crystalline water）
冰岛海岸上四吨重的浮冰
雪花
Frozen water in the form of an ordinary household ice cube. The white zone in the center is the result of tiny air bubbles.
The three-dimensional crystal structure of H2O ice Ih (c) is composed of bases of H2O ice molecules (b) located on lattice points within the two-dimensional hexagonal space lattice (a). The values for the H–O–H angle and O–H distance have come from Physics of Ice[2] with uncertainties of ±1.5° and ±0.005 Å, respectively. The black box in (c) is the unit cell defined by Bernal and Fowler.[3]

冰是水的固态形式。

冰是无色透明的固体，晶格结构一般为六方体，但因应不同压力可以有其他晶格结构。在常压环境下，冰的熔点为0℃。

0℃水冻结成冰时，体积会增大约1/11。据观测，封闭条件下水冻结时，体积增加所产生的压力可达2500大气压。

冰的熔点与压力存在着一种奇妙的关系：在2200大气压以下，冰的熔点随压力的增大而降低，大约每升高130个大气压降低1摄氏度；超过2200大气压后，冰的熔点随压力增加而升高：3530大气压下冰的熔点为-17℃，6380大气压下为 0℃，16500大气压下为 60℃，而20670大气压下冰在76℃时才熔化，称为名副其实的“热冰”。 冰在0℃下密度为0.917 g/cm³，而水的密度正常为1.00g/cm³，所以冰会浮于水上。

英语百科

Ice 冰

（重定向自Crystalline water）
Frozen water in the form of an ordinary household ice cube. The white zone in the center is the result of tiny air bubbles.
Snowflakes by Wilson Bentley, 1902. Snow is ice that grows from water vapor in Earth's atmosphere, which is why it usually displays crystal shapes.
The three-dimensional crystal structure of H2O ice Ih (c) is composed of bases of H2O ice molecules (b) located on lattice points within the two-dimensional hexagonal space lattice (a). The values for the H–O–H angle and O–H distance have come from Physics of Ice[2] with uncertainties of ±1.5° and ±0.005 Å, respectively. The black box in (c) is the unit cell defined by Bernal and Fowler.[3]
Frozen waterfall in southeast New York

Ice is water frozen into a solid state. Depending on the presence of impurities such as particles of soil or bubbles of air, it can appear transparent or a more or less opaque bluish-white color.

In the Solar System, ice is abundant and occurs naturally from as close to the Sun as Mercury to as far as away the Oort cloud objects. Beyond the Solar System, it occurs as interstellar ice. It is abundant on Earth's surface –particularly in the polar regions and above the snow line –and, as a common form of precipitation and deposition, plays a key role in Earth's water cycle and climate. It falls as snowflakes and hail or occurs as frost, icicles or ice spikes.
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更新时间：2025/6/25 14:01:27