Chemical weathering of basalt in southwest Iceland: effects of runoff, age of rocks and vegetative/glacial
ABSTRACT. River, ground, and peat water from a basaltic catchment area, Laxa ́ in Kjós Southwest Iceland, were sampled and analyzed for major element concentrations to define the effect of glassy versus crystalline basalt, the formation of secondary minerals, and runoff on fluxes of dissolved eleme...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.547.2112 2023-05-15T16:47:50+02:00 Chemical weathering of basalt in southwest Iceland: effects of runoff, age of rocks and vegetative/glacial Sigurdur R. Gíslason The Pennsylvania State University CiteSeerX Archives 1996 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.547.2112 http://earth.geology.yale.edu/~ajs/2001/Jun/qn060100513.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.547.2112 http://earth.geology.yale.edu/~ajs/2001/Jun/qn060100513.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://earth.geology.yale.edu/~ajs/2001/Jun/qn060100513.pdf text 1996 ftciteseerx 2016-01-08T11:20:30Z ABSTRACT. River, ground, and peat water from a basaltic catchment area, Laxa ́ in Kjós Southwest Iceland, were sampled and analyzed for major element concentrations to define the effect of glassy versus crystalline basalt, the formation of secondary minerals, and runoff on fluxes of dissolved elements to the ocean. The proportions of the dissolved solids in the water samples derived from precipitation, air, and rock weathering were estimated. The amounts of Na, Mg, Ca, K, and S originating from precipitation were calculated from the respective solute/Cl marine ratios and the estimated aqueous Cl originated from precipitation, which was calculated using measured B content of the waters and B/Cl molal marine and rock ratios. The rock contribution from weathering ranged from 22 to 46 percent of the total dissolved solids of the waters. Iron and Al showed low mobility compared to Na. This was primarily due to consumption of these elements by ferrihydroxides, allophane, imogolite, and clay minerals. Also, Si and to a lesser degree Ca show apparent slightly lower mobility than Na. These results are in good agreement with these phases being dominant in the soils Text Iceland Unknown Laxa ENVELOPE(-17.055,-17.055,65.344,65.344) |
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Unknown |
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ftciteseerx |
language |
English |
description |
ABSTRACT. River, ground, and peat water from a basaltic catchment area, Laxa ́ in Kjós Southwest Iceland, were sampled and analyzed for major element concentrations to define the effect of glassy versus crystalline basalt, the formation of secondary minerals, and runoff on fluxes of dissolved elements to the ocean. The proportions of the dissolved solids in the water samples derived from precipitation, air, and rock weathering were estimated. The amounts of Na, Mg, Ca, K, and S originating from precipitation were calculated from the respective solute/Cl marine ratios and the estimated aqueous Cl originated from precipitation, which was calculated using measured B content of the waters and B/Cl molal marine and rock ratios. The rock contribution from weathering ranged from 22 to 46 percent of the total dissolved solids of the waters. Iron and Al showed low mobility compared to Na. This was primarily due to consumption of these elements by ferrihydroxides, allophane, imogolite, and clay minerals. Also, Si and to a lesser degree Ca show apparent slightly lower mobility than Na. These results are in good agreement with these phases being dominant in the soils |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
Sigurdur R. Gíslason |
spellingShingle |
Sigurdur R. Gíslason Chemical weathering of basalt in southwest Iceland: effects of runoff, age of rocks and vegetative/glacial |
author_facet |
Sigurdur R. Gíslason |
author_sort |
Sigurdur R. Gíslason |
title |
Chemical weathering of basalt in southwest Iceland: effects of runoff, age of rocks and vegetative/glacial |
title_short |
Chemical weathering of basalt in southwest Iceland: effects of runoff, age of rocks and vegetative/glacial |
title_full |
Chemical weathering of basalt in southwest Iceland: effects of runoff, age of rocks and vegetative/glacial |
title_fullStr |
Chemical weathering of basalt in southwest Iceland: effects of runoff, age of rocks and vegetative/glacial |
title_full_unstemmed |
Chemical weathering of basalt in southwest Iceland: effects of runoff, age of rocks and vegetative/glacial |
title_sort |
chemical weathering of basalt in southwest iceland: effects of runoff, age of rocks and vegetative/glacial |
publishDate |
1996 |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.547.2112 http://earth.geology.yale.edu/~ajs/2001/Jun/qn060100513.pdf |
long_lat |
ENVELOPE(-17.055,-17.055,65.344,65.344) |
geographic |
Laxa |
geographic_facet |
Laxa |
genre |
Iceland |
genre_facet |
Iceland |
op_source |
http://earth.geology.yale.edu/~ajs/2001/Jun/qn060100513.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.547.2112 http://earth.geology.yale.edu/~ajs/2001/Jun/qn060100513.pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
_version_ |
1766037930774626304 |