Permeability evolution during progressive development of deformation bands in porous sandstones

[1] Triaxial deformation experiments were carried out on large (0.1 m) diameter cores of a porous sandstone in order to investigate the evolution of bulk sample permeability as a function of axial strain and effective confining pressure. The log permeability of each sample evolved via three stages: (1) a linear decrease prior to sample failure associated with poroelastic compaction, (2) a transient increase associated with dynamic stress drop, and (3) a systematic quasi-static decrease associated with progressive formation of new deformation bands with increasing inelastic axial strain. A quantitative model for permeability evolution with increasing inelastic axial strain is used to analyze the permeability data in the postfailure stage. The model explicitly accounts for the observed fault zone geometry, allowing the permeability of individual deformation bands to be estimated from measured bulk parameters. In a test of the model for Clashach sandstone, the parameters vary systematically with confining pressure and define a simple constitutive rule for bulk permeability of the sample as a function of inelastic axial strain and effective confining pressure. The parameters may thus be useful in predicting fault permeability and sealing potential as a function of burial depth and faul

Numerical simulations of seismicity-induced fluid flow in the Tjornes Fracture Zone, Iceland

We use high-resolution simulations to analyze fluid flow, pore pressure, and fault permeability evolution in the seismically active Tjornes Fracture Zone (TFZ), a major transform fault zone in the North of Iceland. Our results show that the TFZ is characterized by four distinct areas where pore pressures are above hydrostatic, consistent with geophysical observations. Basement and faults, which are assumed to have low permeabilities, often display pore pressures close to lithostatic. Fault permeabilities are allowed to vary freely as a function of the effective fault normal stress. They hence inflate periodically to release excess pore pressure in a few minutes. This is accompanied by an increase in permeability of over seven orders of magnitude and causes short-lived fluid fluxes of more than 0.01 m s(-1). After pore pressures have dissipated, fault permeabilities decay back to their original values in 2 to 3 years as the effective fault normal stress increases. This behavior is consistent with a toggle switch mechanism and could have two important implications for fluid flow in seismically and hydrothermally active oceanic crust. First, the rapid changes in fault permeability and pore pressure provide an explanation for distinct cyclical geochemical changes observed on a similar timescale in thermal waters near the town of Husavik in the TFZ before and after a magnitude 5.8 M-w earthquake. Second, our results provide another line of evidence in the growing number of observations that crustal permeabilities are constantly evolving and geological processes in hydrothermal systems can be dominated by short-lived and extreme flow events.</p

Teores e características da matéria orgânica de solos hidromórficos do Espírito Santo

Os teores e as características da matéria orgânica do solo (MOS) são resultados das taxas de produção e incorporação, decomposição ou alteração e mineralização, de acordo com as condições do ambiente. Nos solos hidromórficos, a dinâmica da MOS é influenciada pelo déficit de oxigênio, o que diminui a taxa de decomposição e gera produtos diferenciados em relação aos solos bem drenados. O presente trabalho teve por objetivo determinar os teores e características da matéria orgânica do solo em três diferentes localidades do Estado do Espírito Santo. Foram realizadas determinações de C orgânico total (COT) por três métodos, além de fracionamento das substâncias húmicas (SH), com determinação de teores das frações humina (FHU), ácidos húmicos (FAH) e ácidos fúlvicos (FAF), e determinações de matéria orgânica leve (MOL) e resíduos mínimos. Os resultados mostraram altos teores de C orgânico para a maioria dos horizontes superficiais dos perfis estudados, com ocorrência de material de constituição orgânica; altos valores na relação SH/COT e baixos valores para EA/FHU, indicando a fração humina como a predominante entre os compartimentos da MOS; maior mobilidade da fração ácidos fúlvicos, expressa por teores relativamente maiores em subsuperfície; e altos teores de MOL, indicando incipiente humificação, em razão do hidromorfismo.Soil organic matter (SOM) contents and characteristics are results of production, incorporation, decomposition, alteration, and mineralization rates, according to environmental conditions. In hydromorphic soils, SOM dynamics are regulated by O2 deficit, lowering the decomposition rates and producing substances different from those in well-drained soils. This article aimed to determine SOM contents and characteristics at three locations in the State of Espirito Santo, Brazil. Total organic carbon (TOC) was quantified by three methods, besides partitioning humic substances (HS) and determining the humin (FHU), humic (FAH) and fulvic acid (FAF) fraction contents, light organic matter (LOM), and minimum residues. Results indicated high organic C in most surface horizons and material with organic constitution. High values of SH/TOC and low values of EA/FHU ratios indicated the humin fraction as the most important fraction of SOM compartments. The mobility of fulvic acid fraction was higher than of the others, expressed by relatively higher contents in the subsurface. The high LOM content indicated a low humification degree, due to the hydromorphic conditions