凍結成冰 的英文怎麼說
中文拼音 [dòngjiēchéngbīng]
凍結成冰
英文
glaciation-
If the ices had been rapidly vaporized by an impacting object, the expanding gases might have helped the ejected fragments reach escape velocity
如果這種（永久凍結）冰由於物體的沖擊力而迅速汽化，則形成的體積不斷膨脹的氣體可能有助於排出的碎片達到逃逸速度。In the low - temperature - freezing stage, the water is frozen as ice phase, while the solute precipitate as the salt phase. the velocity of ice phase growth ( vf ) in the solution and the velocity of solute diffusion ( vd ) decide that whether the heavy segregation of solute appears
當低溫冷凍時，水以冰的形式凍結，溶質則以鹽的形式析出，形成冰鹽兩相;冰相生長速率和溶質擴散速率決定了溶質鹽是否發生大的偏聚。In the cold geotechnical engineering, when the rock containing a mount of water was frozen, the inner water swells, and the freezing swollen force is emerged, in turn the rock became a multi damage material containing water, ice, air, rock
在寒區巖土工程中，巖體中含有一定量的水，凍結后，水冰相變體積膨脹，產生巨大的凍脹力，巖體成為水、冰、巖，氣的多相損傷介質。For to stay, though the hours burn in the night, is to freeze and crystallize and be bound in a mould
因為留下來只會被冰凍，結成塊狀，盡管深夜的時光正如火炙。Either they are hot and passionate, or when they become tired and bored with this heat, they turn to the opposite - - they become an ice - cold saint, frozen
要麼他們熱情似火，要麼是他們厭倦這種熱情之後轉向對立面他們變成冰冷的聖徒，已經凍結。Based on the damage mechanics theory, during the freezing and thawing, the ct measurement technology is used to observe the water transference, ice formation, inner microdamage propagation principle and the corresponding damage structure variability
從細觀損傷力學理論出發，利用ct識別先進的試驗技術研究巖石在凍結融化過程中，水分的遷移，冰的形成，內部細觀損傷擴展機理及相應損傷結構的變化。When water freezes and turns to ice, it expands
當水受凍結成冰，就會膨漲。The results show that the auto - conversion of frozen drops and graupels ( cnfh, cngh ) are the main sources of the hailstones in the strong convective storm studied in the paper, but the contribution of frozen drops is greater than that of graupels. hailstones mainly depend on the processes of collecting supercooled water ( clch, clrh ) to grow. the relatively simple mass continuous equation was used to calculate vertical velocity, and use radial projection relation of dual - doppler radar to retrieve the case ' s three - dimensional wind field
同時模擬分析了冰雹形成的微物理過程，結果表明，本個例模擬雹雲中，冰雹粒子主要由凍滴和霰轉化（ cnfh ， cngh ）形成，但凍滴對冰雹形成的貢獻要比霰大得多，冰雹含水量中心的發展演變與凍滴含水量中心的發展演變相一致，冰雹主要是通過撞凍過冷水過程（ clch ， clrh ）而進一步長大的。If the cold plate temperature is higher than a certain critical value, for instance, - 12 c under our observed experimental conditions, the higher the air relative humidity is, the bigger the water droplets concreting on the cold plate, and the later the water droplets froze. however, if the cold plate temperature is lower than a certain critical value, the influence of air relative humidity on the frozen time of water droplets was not observed. if the cold plate temperature is higher than a certain critical value, for example, - 20 c under our observed experimental conditions, frost deposition is through condensation, or condensation frosting
結果表明，冷壁面溫度越低，水珠凍結時間越短，且凍結的冰珠越小;當冷壁面溫度高於某一臨界值，譬如，在我們給定的實驗條件下， - 12 c時，空氣相對濕度越大，冷壁面上凝結的水珠越大，水珠凍結越晚，但當冷壁面溫度較低時，幾乎觀察不到空氣相對濕度對水珠凍結時間的影響;冷壁面溫度高於某一臨界值，譬如，在我們給定的實驗條件下， - 20 c時，發生凝結成霜，冷麵溫度低於這一臨界值時，發生凝華成霜;隨著實驗工況的不同，觀察到的霜晶呈現八種不同的形態。The cycle of snow and ice melting and refreezing can form ice dams that prevent water from draining during a refreeze cycle
冰雪融化和重新結凍的循環可能形成冰的屏障，在此重新結凍循環的過程中能夠阻止水排出。Comparing frozen material with freeze - dried apple, the ice area with low grey value in the beginning became the loosen pore area with high grey value after freeze - drying
對比凍結物料和凍干物料的灰度值曲線，可見剛開始灰度值較低的冰區，在凍干結束后變成灰度值相對較高的孔疏區。Freezes targets, inflicting ice damage immediately and heavy damage during a certain amount of time
凍結目標，直接造成冰傷害並在一段時間內持續造成大量傷害。The polar regions are now in a temperate climate where they begin to melt where temperate regions are in the polar regions where they freeze and build up ice
極地現在處在它們開始融化溫和的區域，溫和的區域成了它們凍結並且冰塊累累的極地。The waters hide themselves and become like stone, and the surface of the deep is frozen
30諸水隱藏，凍結如石頭，深淵表面凝結成冰。分享友人