When Lava Meets the Sea -- Lava Haze or Laze Air Pollution

White laze plumes, southeast coast of Kilauea Volcano
Photograph by T.N. Mattox April 23, 1993
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Pahoehoe lava enters sea.
Extreme heat from lava entering the sea rapidly boils and vaporizes
seawater, leading to a series of chemical reactions. The boiling
and reactions produce a large white plume, locally known as
lava haze or laze, which contains a mixture of hydrochloric
acid (HCl) and concentrated seawater.
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In this photo, lava flows ooze into the sea on the southeast
coast of Kilauea Volcano; the discrete plumes form above the
most energetic entry sites. The red traffic cones on the left
side of the photograph were placed by rangers of the Hawai`i
Volcanoes National Park to mark the hazardous area where
lava is entering the sea.
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The hydrochloric acid (HCl) comes from the breakdown of seawater-derived
chlorides during sudden boiling. Because the lava is largely degassed by
the time it reaches the sea, any HCL coming from it is insignificant by
comparison. Analyzed samples of the plume show that is is a brine with a
salinity of about 2.3 times that of seawater and a pH of 1.5-2.0.
Key seawater chloride breakdown reactions that produce HCl gas
- MgCl2 (sea salt) + H2O
(steam) = MgO (periclase) + 2HCl (HCl gas)
- 2 NaCl (sea salt) + H2O
(steam) = Na2O (sodium oxide)
+ 2 HCL (HCl gas)
- CaCl2 (sea salt) +
H2O (steam) =
CaO (lime) + 2 HCL (HCl gas)
Laze plumes are very acidic

Photograph by C.C. Heliker February 10,
1994
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Avoid standing beneath a laze plume. Dense laze plumes
contain as much as 10-15 parts per million of hydrochloric acid.
These values drop off sharply as the plume moves away from the
lava entry areas. During along-shore or on-shore winds, this
plume produces acid rain that may fall on people and land along
the coast. This rain (pH 1.5 to 2), often more acidic that lime
juice or stomach acid, is very corrosive to the skin and clothing.
Visitors to the lava entry areas should avoid standing directly
in, under, or downwind of the laze plume.
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References
Gerlach, T.M., Krumhansl, J.L., Fournier, R.O.,
Kjargaard, J., 1989, Acid rain from the heating and
evaporation of seawater by molten lava: a new volcanic
hazard [abs.]: Transactions of the American Geophysical
Union (EOS), v. 70, p. 1421-1422.
Sutton, A.J., and Elias, T., 1993, Volcanic gases create air
pollution on the Island of Hawai`i: U.S. Geological Survey
Earthquakes and Volcanoes, v. 24, no. 4, pp. 178-196.
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U.S. Department of the Interior, U.S. Geological Survey, Menlo Park, California, USA
URL http://volcanoes.usgs.gov/Hazards/What/VolGas/Laze.html
Contact: VHP WWW Team
Last modification: 14 November 1999(SRB)