Radon-222 from the island of Hawaii: deep soils are more important than lava fields or volcanoes

Wilkening MH. 1974. Radon-222 from the island of Hawaii: deep soils are more important than lava fields or volcanoes. Science. 183(4123):413-415

The mean flux of radon-222 atoms from the island of Hawaii is 0.45 atom per square centimeter per second. Lava fields occupy 50 percent of the land area, but their radon flux is only 1 percent of that from deep volcanic soils. The island yields approximately 10 curies of radon-222 per hour to the air surrounding it. The radon-222 contribution of volcanoes is negligible.

Type
Journal Article
Authors
Wilkening, M
Units
HAVO
Keywords
Chemical Analysis, Geochemistry, Hawaii (Big Island), Isotopes, Mauna Kea Volcano, Mauna Loa Volcano, Pedology, Radon (Rn), Rock, Soil

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