Effect of Environmental Factors on the Chemical Weathering of Plagioclase in Hawaiian Basalt
نویسندگان
چکیده
Much of the literature that analyzes the effect of various factors on basaltic weathering rates does not assess the synergistic effects of several factors at once. Those studies that do address such synergies generally report their results in formats that are difficult to integrate into geographic analysis. The research outlined in this paper employs multivariate statistics to assess the effect of several environmental variables on the weathering rate of basalts on the Island of Hawaii. The presence of lichens on the surface of the basalt increases weathering rate by an order of magnitude. Weathering that occurs in the absence of lichen cover is regulated by high elevation/low temperature conditions, moisture availability, and the age of the flow. Weathering that occurs in the presence of lichen cover is regulated primarily by moisture availability only. The statistical results reported here are consistent with the results of a geochemical-style analysis of the same dataset reported elsewhere, suggesting that a multivariate approach is appropriate for assessing the simultaneous effects of multiple weathering factors on the weathering rate. A multivariate statistical approach allows for the construction of quantitative weathering rate models that build on previously published qualitative models for describing geographic variation in weathering rates. [
منابع مشابه
دگرسانی کانیها در دو بستر سنگی متفاوت و خاک حاصل از آنها در ناحیهی لاهیجان
Microscopical studies were carried out, in addition to physico-chemical and mineralogical analysis, in order to evaluate the effect of parent material and weathering on soil genesis in forest regions of Lahijan. Two representative soil pedons in mountain landform developed on granite and andesitic basalt located about 8 km southeast of Lahijan were selected and sampling were taken from each hor...
متن کاملEnhanced chemical weathering and organic carbon burial as environmental recovery factors of the OAE2; a case study in the Koppeh-Dagh Basin (NE Iran)
A late Cenomanian-early Turonian interval (Hamam-ghaleh section) adjusted with the transition of Aitamir and Abderaz formations has been investigated in the east of Koppeh-Dagh Basin to examine environmental perturbations related to the oceanic anoxic event 2. The dark shale of the upper Aitamir Formation indicate higher organic matter concentrations especially in the two intervals at the end o...
متن کاملFactors controlling present weathering rates: new contributions from basalt erosion studies
As chemical weathering of silicate rocks acts as a sink for atmospheric CO2 and as greenhouse effect gases such as CO2 have a leading role in climate regulation, much of river geochemical studies now focus on chemical and mechanical riverine erosion and on their controlling parameters. Moreover, weathering has probably had a dominating influence in the climatic evolution of the Earth, and studi...
متن کاملTiming of acid weathering on Mars: A kinetic-thermodynamic assessment
[1] Weathering of olivine basalt by H2SO4-HCl aqueous solutions at the conditions of early Mars was investigated through numerical modeling in a system open with respect to CO2 and O2 only. The model includes dissolution rates of primary and secondary minerals and oxidation rate of aqueous Fe, as well as chemical equilibration among solutes, dissolved gases, and precipitates. The results reveal...
متن کاملTracing Continentalweathering Using Lithium and Magnesium Isotopes: Insights from the Chemical Weathering of Columbia River Basalts and Mass Balance Modeling
Title of Document: TRACING CONTINENTALWEATHERING USING LITHIUM AND MAGNESIUM ISOTOPES: INSIGHTS FROM THE CHEMICAL WEATHERING OF COLUMBIA RIVER BASALTS AND MASS BALANCE MODELING Xiao-Ming Liu, Ph.D., 2013 Directed By: Professors Roberta L. Rudnick & William F. McDonough, Department of Geology Chemical weathering is an important mechanism that changes the mass and composition of the continental c...
متن کامل