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Hantu Air, Puaka Air or Mambang Air is the Malay translation for Spirit of the Water or Water Ghost, which according to animist traditions in Maritime Southeast Asia, is the unseen inhabitant of watery places such as rivers, lakes, seas, swamps and even ditches. [1]
A Rusalka (plural: rusalki) was a female ghost, water nymph, succubus or mermaid-like demon that dwelled in a waterway. А Berehynia in ancient Ukrainian folklore is a goddess spirit that guarded the edges of waterways, while today it is used as a symbol for Ukrainian nationalism. Moryana is a giant sea spirit from Russian folklore.
The difference is whether the relative abundance is with respect to all the nitrogen, i.e. 14 N plus 15 N, or just to 14 N. Since the atmosphere is 99.6337% 14 N and 0.3663% 15 N, a is 0.003663 in the former case and 0.003663/0.996337 = 0.003676 in the latter.
Most water in Earth's atmosphere and crust comes from saline seawater, while fresh water accounts for nearly 1% of the total. The vast bulk of the water on Earth is saline or salt water, with an average salinity of 35‰ (or 3.5%, roughly equivalent to 34 grams of salts in 1 kg of seawater), though this varies slightly according to the amount of runoff received from surrounding land.
Water god in an ancient Roman mosaic. Zeugma Mosaic Museum, Gaziantep, Turkey. A water deity is a deity in mythology associated with water or various bodies of water.Water deities are common in mythology and were usually more important among civilizations in which the sea or ocean, or a great river was more important.
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The name Kuraokami combines kura 闇 "dark; darkness; closed" and okami 龗 "dragon tutelary of water". This uncommon kanji (o)kami or rei 龗, borrowed from the Chinese character ling 龗 "rain-dragon; mysterious" (written with the "rain" radical 雨, 3 口 "mouths", and a phonetic of long 龍 "dragon") is a variant Chinese character for Japanese rei < Chinese ling 靈 "rain-prayer ...
Data in the table above is given for water–steam equilibria at various temperatures over the entire temperature range at which liquid water can exist. Pressure of the equilibrium is given in the second column in kPa. The third column is the heat content of each gram of the liquid phase relative to water at 0 °C.