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单词 Solid water
释义

Solid water

英语例句库

The great viscosimetry onusseit, its solid water with high, in the small, cohesion, bond strength can vary widely.

粘度大的胶粘剂,其固体含里高,水分少,内聚力大,粘结强度也大。

原声例句
PBS趣味科普

Okay. Do you remember the weirdest property of solid water?

你还记得固态水最奇怪的特性吗?

双语版 TED-Ed 演讲精选

This is what solid water, ice, looks like on the molecular level.

固态水、 冰、从分子图上是这样的。

双语版 TED-Ed 演讲精选

But solid water, a. k. a. ice, is somehow less dense than liquid water.

但是,不知为何,固态水,又称冰,密度比液态水小。

英国学生科学读本

The ice or snow was solid water. The heat changed it into liquid water, such as we drink.

冰和雪都是“固态”水。热量让固态水变成了“液态”水,就是我们喝的水。

英国学生科学读本

Tom soon found that he could run about on the solid water, and very quickly he ran across the pond and claimed his penny.

汤姆很快发现, 他可以在凝固的水上来回跑了。他飞快地跑过池塘, 挣到了那个便士。

中文百科

冰 Ice

(重定向自Solid 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]

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Solid 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:2025/6/19 11:17:42