scispace - formally typeset
Journal ArticleDOI

Basalt weathering laws and the impact of basalt weathering on the global carbon cycle

TLDR
In this paper, the chemical weathering of basalts and the flux of carbon transferred from the atmosphere to the ocean during this major process at the surface of the Earth were investigated.
About
This article is published in Chemical Geology.The article was published on 2003-12-30. It has received 762 citations till now. The article focuses on the topics: Soil production function & Weathering.

read more

Citations
More filters
Journal ArticleDOI

Enhanced dissolution of basaltic glass in brackish waters: Impact on biogeochemical cycles

TL;DR: In this article, a series of alteration experiments of basaltic glass were performed at various degrees of salinity (from 0 to 3.5 g) in far-from-equilibrium conditions.
Journal ArticleDOI

Geochemical and isotopic data for restricting seawater intrusion and groundwater circulation in a series of typical volcanic islands in the South China Sea

TL;DR: A hydrogeologic investigation using combined hydrochemical and isotopic approaches was conducted in the coastal region of the South China Sea near the Leizhou peninsular to provide primary insight into seawater intrusion and groundwater circulation.
Journal ArticleDOI

Zn isotope compositions of the thermal spring waters of La Soufrière volcano, Guadeloupe Island

TL;DR: In this paper, the Zn isotope compositions of seventeen water samples from eight thermal springs and six gas samples from two fumaroles from La Soufriere, an active volcano on Guadeloupe Island (French West Indies, FWI), were analyzed using a method adapted for purifying Zn from Fe- and SO4-enriched thermal solutions.
References
More filters
Journal ArticleDOI

Global silicate weathering and CO2 consumption rates deduced from the chemistry of large rivers

TL;DR: In this article, newly compiled data on the 60 largest rivers of the world are used to calculate the contribution of main lithologies, rain and atmosphere to river dissolved loads, and the relationship between the chemical weathering rates of silicates and the possible controlling parameters are explored.
Journal ArticleDOI

The carbonate-silicate geochemical cycle and its effect on atmospheric carbon dioxide over the past 100 million years

TL;DR: In this article, a computer model has been constructed that considers the effects on the CO/sub 2/ level of the atmosphere, and the Ca, Mg, and HCO/sub 3/ levels of the ocean, of the following processes: weathering on the continents of calcite, dolomite, and calcium-and-magnesium-containing silicates; biogenic precipitation and removal of CaCO 3/from the ocean; removal of Mg from the ocean via volcanic-seawater reaction; and the metamorphic-magmatic decarbon
Journal ArticleDOI

Tectonic forcing of late Cenozoic climate

TL;DR: In particular, tectonically driven increases in chemical weathering may have resulted in a decrease of atmospheric C02 concentration over the past 40 Myr as discussed by the authors. But this was not shown to be the case for the uplift of the Tibetan plateau and positive feedbacks initiated by this event.
Journal ArticleDOI

Geocarb III: A Revised Model of Atmospheric CO2 over Phanerozoic Time

TL;DR: In this article, the GEOCARB model has been updated with an emphasis on factors affecting CO2 uptake by continental weathering, including the role of plants in chemical weathering and the application of GCMs to study the long-term carbon cycle.
Journal ArticleDOI

A negative feedback mechanism for the long‐term stabilization of Earth's surface temperature

TL;DR: In this article, it is suggested that the partial pressure of carbon dioxide in the atmosphere is buffered, over geological time scales, by a negative feedback mechanism, in which the rate of weathering of silicate minerals (followed by deposition of carbonate minerals) depends on surface temperature, which in turn depends on the carbon dioxide partial pressure through the greenhouse effect.
Related Papers (5)