Search results
Results from the WOW.Com Content Network
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.
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]
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.
Some water spirits in traditional African religion include: Mami Wata is a transcultural pantheon of water spirits and deities of the African diaspora. For the many names associated with Mami Wata spirits and goddess, see Names of Mami Wata. [1] Owu Mmiri of some riverine people of Nigeria are often described as mermaid-like spirit of water. [2]
A Simbi (also Cymbee, Sim'bi, pl. Bisimbi) is a Central African water and nature spirit in traditional Kongo religion, as well as in African diaspora spiritual traditions, such as Hoodoo in the southern United States and Palo in Cuba. Simbi have been historically identified as water people, or mermaids, pottery, snakes, gourds, and fire.
Get AOL Mail for FREE! Manage your email like never before with travel, photo & document views. Personalize your inbox with themes & tabs. You've Got Mail!
December 4, 2024 at 3:07 PM. How Your Cholesterol Could Indicate Dementia Risk Qi Yang - Getty Images. Typically, dementia is associated with classic symptoms like confusion and memory loss. But ...
The Arden Buck equations are a group of empirical correlations that relate the saturation vapor pressure to temperature for moist air.The curve fits have been optimized for more accuracy than the Goff–Gratch equation in the range −80 to 50 °C (−112 to 122 °F).