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http://dbpedia.org/ontology/abstract Is är vatten i sitt fasta aggregationstill … Is är vatten i sitt fasta aggregationstillstånd. Ordet is används i överförd betydelse om den fasta formen av ämnen som i rumstemperatur är gaser, då de ofta ser ut som vattenis. För att undvika missförstånd brukar man kalla fast koldioxid för torris. Vatten kan med metan bilda en isliknande förening kallad metanhydrat eller metanklatrat. Denna fasta fas är stabil vid högt tryck och temperatur från 0°C och några grader högre. Metanhydrat förekommer på Jorden i permafrost och på stora havsdjup, samt i de kallare yttre delarna av solsystemet.i de kallare yttre delarna av solsystemet. , Pas soladach é oighear, criostalach de ghnáth, de ábhar neamh-mhiotalach atá mar leacht nó mar ghás ag teocht an tseomra, mar shampla, uisce, oighear dé-ocsaíd charbóin (oighear tirim), oighear amóinia, nó oighear .[1] , IJs is de vaste vorm van water en kan zeer uiteenlopende vormen aannemen, variërend van een ijsberg, gletsjer of ijspegel, tot hagel of sneeuw. , الجليد هو الحالة الصلبة المتبلورة غير الفل … الجليد هو الحالة الصلبة المتبلورة غير الفلزية لمادة قد تكون سائلة أو غازية في درجة حرارة الغرفة، ومن الأمثلة عليها الجليد المائي أو جليد الأمونيا. وفي اللغة الإنجليزية كلمة جليد تعني غالباً جليداً مائياً. يتكون الجليد في أي مكان في حال اجتمع وجود ماء وجو بارد، فيتحول الماء ببساطة إلى جليد. ويُمكن أن تتكون أحيانا جبال أو أنهار جليدية أو مجرد أرض متجمدة، وكثيراً ما تتجمد البحيرات (أو بالأحرى أسطح البحيرات، فبالرغم من أن طبقة سميكة من سطح البحيرة تتجمد أحياناً إلى أنه لا يُمكن أن تتجمد بحيرة بالكامل). تقريباً ثلاثة أرباع الماء العذب في العالم مُخزّن على شكل جليد، موزع بين قارة أنتركتيكا وجزيرة غرينلاند والقطب الشمالي وقمم الجبال الشاهقة وفي أماكن أخرى حول العالم. المحيط المتجمد الشمالي يشغل 7% من مساحة المحيطات على الأرض. وله أهمية ضخمة مناخياً لأنه يعكس معظم الأشعة الشمسية الساقطة عليه. لكن الدلائل المُشاهدة في القطب الشمالي حالياً تدل على أنه يَرقّ ويضمحل بسبب ظاهرة الاحتباس الحراري. ونماذج المحاكاة الحاسوبية تدل على أن الجليد في هذا المحيط سوف يختفي تماماً خلال فصل الصيف (لكنه سوف يعود في الشتاء) بحلول الثمانينيات من هذا القرن.في الشتاء) بحلول الثمانينيات من هذا القرن. , Gelo (do latim gelus) é o estado sólido da … Gelo (do latim gelus) é o estado sólido da água cristalizada no sistema cristalino hexagonal. Seu aspecto é vítreo e semitransparente. A sua densidade é inferior à da água, ficando em 0,9178 grama por centímetro cúbico. O seu ponto de fusão é de 0 grau Celsius a uma atmosfera de pressão. A mesma massa de água em estado líquido ou em estado sólido tem volumes diferentes, pois, ao passar de um estado para o outro, o volume aumenta cerca de 9 por cento: ao contrário da maioria dos outros sólidos, o gelo, no seu ponto de fusão, apresenta-se mais dilatado do que a sua forma líquida até atingir os 4 graus Celsius. Seu ponto de formação é usado como valor de referência em termodinâmica. O gelo tem pelo menos dezessete fases cristalinas conhecidas e três fases amorfas (não cristalinas), que existem em diferentes temperaturas e pressões. A estrutura extremamente aberta das moléculas do gelo faz com que ocupe maior volume — e, por isso, seja menos denso — do que a água.or isso, seja menos denso — do que a água. , Eis ist der dritte Aggregatzustand, die fe … Eis ist der dritte Aggregatzustand, die feste Phase von Wasser. Flüssiges reines Wasser erstarrt zu Eis bei einer Temperatur unter dem Gefrierpunkt, der bei Normaldruck in Anwesenheit von Kristallisationskeimen bei 0 °C liegt. Als natürlich vorkommender kristalliner Festkörper mit einer definierten chemischen Zusammensetzung zählt Eis zu den Mineralen. Aufgrund seiner chemischen Struktur H2O gehört Eis zur Stoffgruppe der Oxide. Unter atmosphärischen Bedingungen kristallisiert Eis im hexagonalen Kristallsystem und tritt in der Natur in verschiedenen Erscheinungsformen auf: von Schneeflocken, Graupel- und Hagelkörnern, Reif und Raureif über Raueis und Klareis, Eiszapfen und Eisblumen, Kammeis und Haareis, Firn und Nilas, Eisdecken stehender und fließender Gewässer, Grundeis, Treibeis, Packeis, Festeis, Schelfeis bis zu Gletschern, Eiskappen und Eisschilden. Die Dichte von hexagonalem, gewöhnlichem Eis ist mit 0,918 g/cm³ (reines, luftfreies Eis-Ih bei 0 °C) geringer als die von flüssigem Wasser, was auch Dichteanomalie des Wassers genannt wird. Auf Grund dessen schwimmt Eis auf der Wasseroberfläche und bildet dort Eisdecken, Eisschollen und Eisberge. Hierbei befindet sich nur rund ein Zehntel des Eisvolumens über der Wasseroberfläche, die übrigen rund 90 Volumenprozent tauchen unter. Von einem 100 Meter dicken Tafeleisberg liegen daher etwa 90 Meter unter Wasser (die im Auftrieb verdrängte Wassermasse entspricht der Gewichtskraft des Eises). In reiner Form besteht Eis aus farblosen, transparenten Kristallen. Wenn bei der Bildung der Eiskristalle feine Luftbläschen in Eisblöcke eingeschlossen wurden, erscheinen diese durch vielfache Lichtbrechung weißlich. Eis besteht als chemischer Stoff aus H2O und zeichnet sich durch eine Reihe besonderer Eigenschaften des Wassers aus. Bei zahlreichen meteorologischen Phänomenen spielt Eis eine wesentliche Rolle. Polare Eiskappen und Vergletscherungen von Polarregionen mit Ausbildung von Eisschilden haben entscheidenden Einfluss auf das Klima des Planeten Erde. Dauerhafte Eisbedeckungen in der Polarregion kennzeichnen ein Eiszeitalter. Die im Eis gebundene Wassermenge ist ein wichtiger Speicher im globalen Wasserkreislauf; sie beeinflusst auch die Zugänglichkeit von verschiedenen Regionen als Lebensräumen. Als die feste Form von Wasser ist Eis von besonderer Bedeutung für unsere Biosphäre. Die Wissenschaft von Formen, Auftreten und Eigenschaften von Eis und Schnee ist die Glaziologie.en von Eis und Schnee ist die Glaziologie. , El gel o glaç és l'estat sòlid de l'aigua … El gel o glaç és l'estat sòlid de l'aigua (H₂O), el qual es forma quan aquest es troba en una temperatura inferior a 0 °C (273,15 K, 32 °F), que és el seu punt de congelació. El gel també és considerat un mineral. Quant al seu nom, Pompeu Fabra proposava una redistribució semàntica, gel, quan és artificial, i glaç, quan és natural.an és artificial, i glaç, quan és natural. , Lód – minerał z gromady tlenków o wzorze chemicznym H2O. Jest to stan stały wody. , Лід, кри́га — вода в твердому кристалічному стані, замерзла вода. , La glace est l'eau (de formule chimique H2 … La glace est l'eau (de formule chimique H2O) lorsqu'elle est à l'état solide. Cet élément est très étudié dans la nature et en laboratoire, par les scientifiques, à commencer par les glaciologues, les physiciens de la matière condensée et autres cryologues de spécialités différentes : il contient souvent beaucoup d'impuretés ou d'inclusions, d'origine diverse. Les météorologues suivent la formation des flocons à partir de vapeur d'eau entrant en atmosphère froide plus ou moins poussiéreuse, géologues et minéralogistes, rejoints par les spéléologues, ne le retrouvent pas seulement dans les endroits communément englacés, mais sous des formes insolites dans les déserts secs et arides, des lieux plus secs et abrités des montagnes comme au fond des grottes profondes et cavités glacées, où la glace subsiste longtemps.s glacées, où la glace subsiste longtemps. , ( 설빙은 여기로 연결됩니다. 기업에 대해서는 설빙 (기업) 문서를 참고하십 … ( 설빙은 여기로 연결됩니다. 기업에 대해서는 설빙 (기업) 문서를 참고하십시오.)( 수빙은 여기로 연결됩니다. 나무 서리에 대해서는 상고대 문서를 참고하십시오.) 얼음(영어: Ice)은 물이 얼어 고체가 된 상태를 말한다. 수빙(水氷)이라고도 하며, 또 눈에서 생긴 얼음은 설빙(雪氷)이라고 한다. 흔히 얼음이라 하면 지구 상에서 압도적으로 많은 얼음 Ih를 가리키는데, 현재 알려진 바로는 17가지 종류의 서로 다른 상이 존재한다. 흔히 볼 수 있는 종류의 얼음은 투명하거나 공기 등의 불순물이 섞여 약간 푸르스름한 흰 빛을 띠며, 물은 1 기압 하에서 0 °C(273.15 K, 32 °F)에 얼어서 이 종류의 얼음이 된다. 하지만 수증기로부터 액체 상태를 거치지 않고 바로 얼음이 될 수도 있다. 1 기압에서 언 얼음의 특수한 성질은, 액체 상태인 물 보다 8% 가량 밀도가 작다는 것이다. 즉, 물은 0 °C에서 0.9998 g/cm³정도의 밀도를 지니는 데 반해, 얼음은 동일한 온도에서 0.9167 g/cm³정도의 밀도를 지닌다. 이러한 특성을 지닌 물은 얼 때 부피가 늘어나는 이제까지 알려진 유일한 비금속이다. 물은 4 °C에서 1.00 g/cm³가량으로 가장 밀도가 크며, 온도가 0 °C로 내려감에 따라 육방형의 결정을 형성하기 시작하는 것. 이러한 이유는 물 분자 간에 수소 결합이 형성되기 때문이며, 따라서 물이 얼게 될 때 분자가 보다 비효율적으로 나열되게 되어 부피가 늘어나게 되는 것이다.될 때 분자가 보다 비효율적으로 나열되게 되어 부피가 늘어나게 되는 것이다. , Led (chemický vzorec H2O) je pevné skupenství vody. Pokud vznikl přírodním procesem, je považován za minerál, v některých mineralogických systémech se však neuvádí vůbec nebo pouze okrajově. , El hielo es agua en estado sólido, uno de … El hielo es agua en estado sólido, uno de los tres estados naturales del agua que forman parte de los cuatro estados de agregación de la materia. Se reconoce por su temperatura, su color blanco níveo y su flotabilidad. El agua pura se congela a 0 °C cuando se halla sometida a una atmósfera de presión. El hielo es el nombre común del agua en estado sólido; otras denominaciones son la nieve, la escarcha, el granizo, etc.​n la nieve, la escarcha, el granizo, etc.​ , Glacio estas la solida formo de akvo. La a … Glacio estas la solida formo de akvo. La akvo fariĝas glacio, kiam likva akvo estas malvarmigita sub 0 °C (273 K, 32 °F) ĉe normala atmosfera premo. Glacio povas formiĝi je pli altaj temperaturoj en pliprema medio, kaj akvo daŭros likva aŭ gasa ĝis -30 °C ĉe malpliprema medio. Glacio formita ĉe alta premo havas malsaman kristalformon kaj densecon ol normala glacio.stalformon kaj densecon ol normala glacio. , 冰，也就是凍結成固態的水。或者是由甲烷和二氧化碳形成，取決於冰內含的雜質（如土壤或氣 … 冰，也就是凍結成固態的水。或者是由甲烷和二氧化碳形成，取決於冰內含的雜質（如土壤或氣泡顆粒），冰可以是透明的、或著帶有一點不透明的藍白色。 在太陽系中冰的含量非常豐富。從最接近太陽的水星，到離太陽極遠的歐特雲，都會生成冰。在太陽系以外的地方，英文稱“凍結成固態的水”為"interstellar ice"（星際冰）。冰在地球表面存量極大，尤其是在極地地區和雪線以上。而且，作為地表沉澱物和沉積物的一種常見形式，冰在地球的水循環和氣候上起著關鍵的作用。它可能以雪花、冰雹、霜、冰錐或冰柱等形式出現。 冰分子可依溫度和壓力，表現出高達19種不同的形態（分子堆疊形狀）。當水被迅速冷卻後，根據其經過的壓力和溫度，可生成多達三種不同型態的“冰”。當水慢慢冷卻，到達20K以下（約−253.15℃）時，量子穿隧效應可能引起宏觀的量子現象。幾乎所有在地球表面和大氣層裡的冰，都是六角形晶體結構; 相較之下，地表只會產生微量的立方體形冰。其中最常見的生成方式為：當液態水在標準大氣壓（1atm）下冷卻到低於0°C（273.15K，32°F）時，產生六角形晶體冰。冰也可通過水蒸汽直接沉積（凝華），如霜的形成就是一個很好的例子。從冰變成水的過程被稱為熔化，而從冰直接變成水蒸的過程則被稱為昇華。 冰在各種地方都被廣泛地運用著，包括製冷、冬季運動、和做成冰雕等。過程則被稱為昇華。 冰在各種地方都被廣泛地運用著，包括製冷、冬季運動、和做成冰雕等。 , Izotza, ur solidoaren 15 faseak izendatzeko hitza da. Egoera hau 0 °C-tik behera agertzen da. Antartika, "izoztutako kontinentea", izotzaren eremu handiena da munduan. , Ice is water frozen into a solid state, ty … Ice is water frozen into a solid state, typically forming at or below temperatures of 0 degrees Celsius or 32 °F (0 °C; 273 K) 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 away as 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 and aggregates from snow as glaciers and ice sheets. Ice exhibits at least eighteen phases (packing geometries), depending on temperature and pressure. When water is cooled rapidly (quenching), up to three types of amorphous ice can form depending on its history of pressure and temperature. When cooled slowly, correlated proton tunneling occurs below −253.15 °C (20 K, −423.67 °F) giving rise to macroscopic quantum phenomena. Virtually all ice on Earth's surface and in its atmosphere is of a hexagonal crystalline structure denoted as ice Ih (spoken as "ice one h") with minute traces of cubic ice, denoted as ice Ic and, more recently found, Ice VII inclusions in diamonds. The most common phase transition to ice Ih occurs when liquid water is cooled below 0 °C (273.15 K, 32 °F) at standard atmospheric pressure. It may also be deposited directly by water vapor, as happens in the formation of frost. The transition from ice to water is melting and from ice directly to water vapor is sublimation. Ice is used in a variety of ways, including for cooling, for winter sports, and ice sculpting.ing, for winter sports, and ice sculpting. , Es (bahasa Belanda: ijs) adalah air yang d … Es (bahasa Belanda: ijs) adalah air yang dibekukan menjadi bentuk padat. Bergantung pada adanya seperti partikel tanah atau gelembung udara, dapat terlihat transparan atau kebiru-biruan yang kurang lebih . Pembekuan ini umumnya terjadi bila air didinginkan di bawah suhu 0 °C (273.15 K, 32 °F) pada tekanan atmosfer standar. Es dapat terbentuk pada suhu yang lebih tinggi dengan tekanan yang lebih tinggi juga, dan air akan tetap sebagai cairan atau gas sampai -30 °C pada tekanan yang lebih rendah. Di Tata Surya, es berlimpah dan muncul secara alami dari Merkurius hingga sejauh objek awan Oort. Di luar Tata Surya, es terbentuk sebagai . Es berlimpah di permukaan bumi – khususnya di daerah kutub dan di atas garis salju – dan, sebagai bentuk umum presipitasi dan memainkan peran kunci dalam siklus air dan iklim Bumi. Es jatuh dari atmosfer sebagai butiran salju dan hujan es atau terjadi sebagai es atau . Molekul es memiliki delapan belas atau lebih fase berbeda yang bergantung pada suhu dan tekanan. Ketika air didinginkan dengan cepat (pendinginan), hingga tiga jenis dapat terbentuk tergantung pada sejarah tekanan dan suhunya. Ketika didinginkan, penerowongan proton yang berkorelasi lambat terjadi di bawah -253,15 °C (20 K, −423,67°F) memunculkan . Hampir semua es di permukaan bumi dan di atmosfernya adalah struktur kristal yang dilambangkan sebagai es Ih (diucapkan sebagai "es satu h") dengan jejak kecil es kubus yang dilambangkan sebagai es Ic. Transisi fase paling umum ke es Ih terjadi ketika air cair didinginkan di bawah 0°C (273,15 K, 32°F) pada tekanan atmosfer standar. Es juga dapat langsung oleh uap air, seperti yang terjadi pada pembekuan. Transisi dari es menjadi air cair dan dari es langsung menjadi uap air adalah sublimasi. Es digunakan dalam berbagai cara, termasuk pendinginan, olahraga musim dingin, dan . pendinginan, olahraga musim dingin, dan . , Ghiaccio è il nome comune usato per design … Ghiaccio è il nome comune usato per designare l'acqua allo stato solido. È un solido cristallino trasparente: a pressione atmosferica standard (101 325 Pa) la transizione di fase avviene quando l'acqua liquida viene raffreddata sotto lo 0 °C (273,15 K, 32 °F).ffreddata sotto lo 0 °C (273,15 K, 32 °F). , 氷（冰、こおり）とは、固体の状態にある水のこと。 なお、天文学では宇宙空間に存在する一酸化炭素や二酸化炭素、メタンなど水以外の低分子物質の固体をも氷（誤解を避けるためには「○○の氷」）と呼ぶこともある。また惑星科学では、天王星や海王星の内部に存在する高温高密度の水や、アンモニアの液体のことを氷と呼ぶことがある。さらに日常語でも、固体の二酸化炭素をドライアイスと呼ぶ。 この記事では、水の固体を扱う。 , Лёд — вода в твёрдом агрегатном состоянии. Льдом иногда называют некоторые вещества в твёрдом агрегатном состоянии, которым свойственно иметь жидкую или газообразную форму при комнатной температуре; в частности, сухой лёд, аммиачный лёд или метановый лёд. , Πάγος ονομάζεται το στερεής κατάστασης καθ … Πάγος ονομάζεται το στερεής κατάστασης καθαρό νερό, είναι δηλαδή η στερεά κατάσταση στην οποία μετατρέπεται το νερό όταν βρεθεί σε θερμοκρασία 0 °C (273,15 °K ή 32 °F) υπό κανονική ατμοσφαιρική πίεση. Στην αρχαία Ελλάδα «πάγος» ονομαζόταν και κάθε μεγάλων διαστάσεων γυμνός βράχος π.χ. Άρειος Πάγος ο επ' αριστερά της εισόδου της Ακρόπολης των Αθηνών, βράχος. εισόδου της Ακρόπολης των Αθηνών, βράχος.
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http://dbpedia.org/property/caption An ice block, photographed at the Duluth Canal Park in Minnesota
http://dbpedia.org/property/compressiveStrength 24
http://dbpedia.org/property/density 0.9167
http://dbpedia.org/property/dielectricConstant ~3.15
http://dbpedia.org/property/footnotes The properties of ice vary substantially with temperature, purity and other factors.
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rdfs:comment El gel o glaç és l'estat sòlid de l'aigua … El gel o glaç és l'estat sòlid de l'aigua (H₂O), el qual es forma quan aquest es troba en una temperatura inferior a 0 °C (273,15 K, 32 °F), que és el seu punt de congelació. El gel també és considerat un mineral. Quant al seu nom, Pompeu Fabra proposava una redistribució semàntica, gel, quan és artificial, i glaç, quan és natural.an és artificial, i glaç, quan és natural. , Лід, кри́га — вода в твердому кристалічному стані, замерзла вода. , Pas soladach é oighear, criostalach de ghnáth, de ábhar neamh-mhiotalach atá mar leacht nó mar ghás ag teocht an tseomra, mar shampla, uisce, oighear dé-ocsaíd charbóin (oighear tirim), oighear amóinia, nó oighear .[1] , 冰，也就是凍結成固態的水。或者是由甲烷和二氧化碳形成，取決於冰內含的雜質（如土壤或氣 … 冰，也就是凍結成固態的水。或者是由甲烷和二氧化碳形成，取決於冰內含的雜質（如土壤或氣泡顆粒），冰可以是透明的、或著帶有一點不透明的藍白色。 在太陽系中冰的含量非常豐富。從最接近太陽的水星，到離太陽極遠的歐特雲，都會生成冰。在太陽系以外的地方，英文稱“凍結成固態的水”為"interstellar ice"（星際冰）。冰在地球表面存量極大，尤其是在極地地區和雪線以上。而且，作為地表沉澱物和沉積物的一種常見形式，冰在地球的水循環和氣候上起著關鍵的作用。它可能以雪花、冰雹、霜、冰錐或冰柱等形式出現。 冰分子可依溫度和壓力，表現出高達19種不同的形態（分子堆疊形狀）。當水被迅速冷卻後，根據其經過的壓力和溫度，可生成多達三種不同型態的“冰”。當水慢慢冷卻，到達20K以下（約−253.15℃）時，量子穿隧效應可能引起宏觀的量子現象。幾乎所有在地球表面和大氣層裡的冰，都是六角形晶體結構; 相較之下，地表只會產生微量的立方體形冰。其中最常見的生成方式為：當液態水在標準大氣壓（1atm）下冷卻到低於0°C（273.15K，32°F）時，產生六角形晶體冰。冰也可通過水蒸汽直接沉積（凝華），如霜的形成就是一個很好的例子。從冰變成水的過程被稱為熔化，而從冰直接變成水蒸的過程則被稱為昇華。 冰在各種地方都被廣泛地運用著，包括製冷、冬季運動、和做成冰雕等。過程則被稱為昇華。 冰在各種地方都被廣泛地運用著，包括製冷、冬季運動、和做成冰雕等。 , IJs is de vaste vorm van water en kan zeer uiteenlopende vormen aannemen, variërend van een ijsberg, gletsjer of ijspegel, tot hagel of sneeuw. , Gelo (do latim gelus) é o estado sólido da … Gelo (do latim gelus) é o estado sólido da água cristalizada no sistema cristalino hexagonal. Seu aspecto é vítreo e semitransparente. A sua densidade é inferior à da água, ficando em 0,9178 grama por centímetro cúbico. O seu ponto de fusão é de 0 grau Celsius a uma atmosfera de pressão. A mesma massa de água em estado líquido ou em estado sólido tem volumes diferentes, pois, ao passar de um estado para o outro, o volume aumenta cerca de 9 por cento: ao contrário da maioria dos outros sólidos, o gelo, no seu ponto de fusão, apresenta-se mais dilatado do que a sua forma líquida até atingir os 4 graus Celsius.ma líquida até atingir os 4 graus Celsius. , Ghiaccio è il nome comune usato per design … Ghiaccio è il nome comune usato per designare l'acqua allo stato solido. È un solido cristallino trasparente: a pressione atmosferica standard (101 325 Pa) la transizione di fase avviene quando l'acqua liquida viene raffreddata sotto lo 0 °C (273,15 K, 32 °F).ffreddata sotto lo 0 °C (273,15 K, 32 °F). , La glace est l'eau (de formule chimique H2 … La glace est l'eau (de formule chimique H2O) lorsqu'elle est à l'état solide. Cet élément est très étudié dans la nature et en laboratoire, par les scientifiques, à commencer par les glaciologues, les physiciens de la matière condensée et autres cryologues de spécialités différentes : il contient souvent beaucoup d'impuretés ou d'inclusions, d'origine diverse. Les météorologues suivent la formation des flocons à partir de vapeur d'eau entrant en atmosphère froide plus ou moins poussiéreuse, géologues et minéralogistes, rejoints par les spéléologues, ne le retrouvent pas seulement dans les endroits communément englacés, mais sous des formes insolites dans les déserts secs et arides, des lieux plus secs et abrités des montagnes comme au fond des grottes profondes et cavités glacées, où la gltes profondes et cavités glacées, où la gl , Ice is water frozen into a solid state, ty … Ice is water frozen into a solid state, typically forming at or below temperatures of 0 degrees Celsius or 32 °F (0 °C; 273 K) 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. Ice is used in a variety of ways, including for cooling, for winter sports, and ice sculpting.ing, for winter sports, and ice sculpting. , Eis ist der dritte Aggregatzustand, die fe … Eis ist der dritte Aggregatzustand, die feste Phase von Wasser. Flüssiges reines Wasser erstarrt zu Eis bei einer Temperatur unter dem Gefrierpunkt, der bei Normaldruck in Anwesenheit von Kristallisationskeimen bei 0 °C liegt. Als natürlich vorkommender kristalliner Festkörper mit einer definierten chemischen Zusammensetzung zählt Eis zu den Mineralen. Aufgrund seiner chemischen Struktur H2O gehört Eis zur Stoffgruppe der Oxide. Die Wissenschaft von Formen, Auftreten und Eigenschaften von Eis und Schnee ist die Glaziologie.en von Eis und Schnee ist die Glaziologie. , Πάγος ονομάζεται το στερεής κατάστασης καθ … Πάγος ονομάζεται το στερεής κατάστασης καθαρό νερό, είναι δηλαδή η στερεά κατάσταση στην οποία μετατρέπεται το νερό όταν βρεθεί σε θερμοκρασία 0 °C (273,15 °K ή 32 °F) υπό κανονική ατμοσφαιρική πίεση. Στην αρχαία Ελλάδα «πάγος» ονομαζόταν και κάθε μεγάλων διαστάσεων γυμνός βράχος π.χ. Άρειος Πάγος ο επ' αριστερά της εισόδου της Ακρόπολης των Αθηνών, βράχος. εισόδου της Ακρόπολης των Αθηνών, βράχος. , El hielo es agua en estado sólido, uno de … El hielo es agua en estado sólido, uno de los tres estados naturales del agua que forman parte de los cuatro estados de agregación de la materia. Se reconoce por su temperatura, su color blanco níveo y su flotabilidad. El agua pura se congela a 0 °C cuando se halla sometida a una atmósfera de presión. El hielo es el nombre común del agua en estado sólido; otras denominaciones son la nieve, la escarcha, el granizo, etc.​n la nieve, la escarcha, el granizo, etc.​ , Es (bahasa Belanda: ijs) adalah air yang d … Es (bahasa Belanda: ijs) adalah air yang dibekukan menjadi bentuk padat. Bergantung pada adanya seperti partikel tanah atau gelembung udara, dapat terlihat transparan atau kebiru-biruan yang kurang lebih . Pembekuan ini umumnya terjadi bila air didinginkan di bawah suhu 0 °C (273.15 K, 32 °F) pada tekanan atmosfer standar. Es dapat terbentuk pada suhu yang lebih tinggi dengan tekanan yang lebih tinggi juga, dan air akan tetap sebagai cairan atau gas sampai -30 °C pada tekanan yang lebih rendah. Es digunakan dalam berbagai cara, termasuk pendinginan, olahraga musim dingin, dan . pendinginan, olahraga musim dingin, dan . , Лёд — вода в твёрдом агрегатном состоянии. Льдом иногда называют некоторые вещества в твёрдом агрегатном состоянии, которым свойственно иметь жидкую или газообразную форму при комнатной температуре; в частности, сухой лёд, аммиачный лёд или метановый лёд. , Glacio estas la solida formo de akvo. La a … Glacio estas la solida formo de akvo. La akvo fariĝas glacio, kiam likva akvo estas malvarmigita sub 0 °C (273 K, 32 °F) ĉe normala atmosfera premo. Glacio povas formiĝi je pli altaj temperaturoj en pliprema medio, kaj akvo daŭros likva aŭ gasa ĝis -30 °C ĉe malpliprema medio. Glacio formita ĉe alta premo havas malsaman kristalformon kaj densecon ol normala glacio.stalformon kaj densecon ol normala glacio. , 氷（冰、こおり）とは、固体の状態にある水のこと。 なお、天文学では宇宙空間に存在する一酸化炭素や二酸化炭素、メタンなど水以外の低分子物質の固体をも氷（誤解を避けるためには「○○の氷」）と呼ぶこともある。また惑星科学では、天王星や海王星の内部に存在する高温高密度の水や、アンモニアの液体のことを氷と呼ぶことがある。さらに日常語でも、固体の二酸化炭素をドライアイスと呼ぶ。 この記事では、水の固体を扱う。 , Izotza, ur solidoaren 15 faseak izendatzeko hitza da. Egoera hau 0 °C-tik behera agertzen da. Antartika, "izoztutako kontinentea", izotzaren eremu handiena da munduan. , ( 설빙은 여기로 연결됩니다. 기업에 대해서는 설빙 (기업) 문서를 참고하십 … ( 설빙은 여기로 연결됩니다. 기업에 대해서는 설빙 (기업) 문서를 참고하십시오.)( 수빙은 여기로 연결됩니다. 나무 서리에 대해서는 상고대 문서를 참고하십시오.) 얼음(영어: Ice)은 물이 얼어 고체가 된 상태를 말한다. 수빙(水氷)이라고도 하며, 또 눈에서 생긴 얼음은 설빙(雪氷)이라고 한다. 흔히 얼음이라 하면 지구 상에서 압도적으로 많은 얼음 Ih를 가리키는데, 현재 알려진 바로는 17가지 종류의 서로 다른 상이 존재한다. 흔히 볼 수 있는 종류의 얼음은 투명하거나 공기 등의 불순물이 섞여 약간 푸르스름한 흰 빛을 띠며, 물은 1 기압 하에서 0 °C(273.15 K, 32 °F)에 얼어서 이 종류의 얼음이 된다. 하지만 수증기로부터 액체 상태를 거치지 않고 바로 얼음이 될 수도 있다.. 하지만 수증기로부터 액체 상태를 거치지 않고 바로 얼음이 될 수도 있다. , Led (chemický vzorec H2O) je pevné skupenství vody. Pokud vznikl přírodním procesem, je považován za minerál, v některých mineralogických systémech se však neuvádí vůbec nebo pouze okrajově. , الجليد هو الحالة الصلبة المتبلورة غير الفل … الجليد هو الحالة الصلبة المتبلورة غير الفلزية لمادة قد تكون سائلة أو غازية في درجة حرارة الغرفة، ومن الأمثلة عليها الجليد المائي أو جليد الأمونيا. وفي اللغة الإنجليزية كلمة جليد تعني غالباً جليداً مائياً. يتكون الجليد في أي مكان في حال اجتمع وجود ماء وجو بارد، فيتحول الماء ببساطة إلى جليد. ويُمكن أن تتكون أحيانا جبال أو أنهار جليدية أو مجرد أرض متجمدة، وكثيراً ما تتجمد البحيرات (أو بالأحرى أسطح البحيرات، فبالرغم من أن طبقة سميكة من سطح البحيرة تتجمد أحياناً إلى أنه لا يُمكن أن تتجمد بحيرة بالكامل). تقريباً ثلاثة أرباع الماء العذب في العالم مُخزّن على شكل جليد، موزع بين قارة أنتركتيكا وجزيرة غرينلاند والقطب الشمالي وقمم الجبال الشاهقة وفي أماكن أخرى حول العالم. الجبال الشاهقة وفي أماكن أخرى حول العالم. , Is är vatten i sitt fasta aggregationstill … Is är vatten i sitt fasta aggregationstillstånd. Ordet is används i överförd betydelse om den fasta formen av ämnen som i rumstemperatur är gaser, då de ofta ser ut som vattenis. För att undvika missförstånd brukar man kalla fast koldioxid för torris. Vatten kan med metan bilda en isliknande förening kallad metanhydrat eller metanklatrat. Denna fasta fas är stabil vid högt tryck och temperatur från 0°C och några grader högre. Metanhydrat förekommer på Jorden i permafrost och på stora havsdjup, samt i de kallare yttre delarna av solsystemet.i de kallare yttre delarna av solsystemet. , Lód – minerał z gromady tlenków o wzorze chemicznym H2O. Jest to stan stały wody.
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