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蒸発

9 件の記事

Water boiling at 99.3 °C (210.8 °F) at 215 m (705 ft) elevation

沸点とは何か？気圧による変化と化学的特性のメカニズム

沸点蒸気圧飽和温度気圧
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The amount of water vapor in Earth's atmosphere has risen over recent decades,[1] making heavy rainfall events more severe.[2]

水蒸気の科学地球の気候変動と宇宙における役割

水蒸気温室効果ガス湿度気候変動
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A typical phase diagram. The solid green line applies to most substances; the dashed green line gives the anomalous behavior of water

三重点とは何か？物質の状態が共存する特異な温度と圧力

三重点熱力学相図水
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Aerosol of microscopic water droplets suspended in the air above a cup of hot tea after the water vapor has sufficiently cooled and condensed. Water vapor is an invisible gas, but the clouds of condensed droplets refract and scatter the sunlight and are thus visible.

蒸発のメカニズムと日常生活への影響気化現象の科学的視点

蒸発気化熱水循環蒸気圧
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Rolling boil of water in an electric kettle

沸騰の科学液体から気体への相転移とその実用的活用

沸騰相転移沸点核沸騰
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Aerosol of microscopic water droplets suspended in the air above a cup of hot tea after the water vapor has sufficiently cooled and condensed. Water vapor is an invisible gas, but the clouds of condensed droplets refract and scatter the sunlight and are thus visible.

蒸発のメカニズムと日常生活への影響気化現象の科学

蒸発気化蒸気圧気化熱
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Water boiling at 99.3 °C (210.8 °F) at 215 m (705 ft) elevation

沸点とは何か？圧力と物質の特性が与える影響を詳しく解説

沸点蒸気圧飽和温度標準沸点
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Water cycle of the Earth's surface, showing the individual components of transpiration and evaporation that make up evapotranspiration. Other closely related processes shown are runoff and groundwater recharge.

蒸発散（ET）の仕組みと水資源管理への影響

蒸発散蒸発蒸散水サイクル
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The endorheic basin that feeds water into Üüreg Lake, Mongolia

内陸流域（エンドレイク）の仕組みと世界的な分布

内陸流域エンドレイク閉鎖流域塩湖
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