Sentence examples for microbial dissolution of from inspiring English sources

Highly positive correlation between the extracted amounts of As and Fe implied that microbial dissolution of Fe(III -oxides, whether III -oxidesnd- and proton-promoted dissolution or reductive dissolution, might be dominantly responsible for the As release.

Microbial dissolution of metals involves direct adhesion/attack of the bacterial cell on the sulfide surface and/or allowing chemical oxidation of liberated sulfides by ferric iron generated microbially or through oxidation by air.

The answer to this question will help to complete the missing knowledge about microbial dissolution of arsenic-bearing minerals and will help to estimate the chance of the potential use of dissimilatory reducers in biomining and bioremediation.

For the Bangladesh and West Bengal aquifers, however, the most widely accepted mechanism for the cause of high aqueous arsenic concentrations is the microbial reductive dissolution of iron oxyhydroxides and concomitant release of arsenic.

Conversely, an increase in bone porosity, and related fluid circulation, could result in microbial attack and the dissolution of crystals, which could potentiate the deposition of exogenous DNA templates on the fraction of bone powder that appeared easily decalcified (here, TP1 and TP2 extracts) [ 27, 28].

That dissolution-of-youth thing was super-appealing.

A possible scenario would be that a microbial community was nurtured by the dissolution of chromite.

Thus, more DIC derived from the dissolution of root and microbial respired CO2 into soil water could have been transported to the rivers through flood runoff.

Stable sulfur and oxygen isotopes indicate that the primary source of sulfur is the partial dissolution of jarosite during microbial sulfate reduction.

SEM images indicated that morphological and compositional features of schwertmannite were dominated by: (1) framboid-like spheroidal clusters with Fe/S ratio > 5 that were preserved after crystallization and likely formed by dissolution of pyrite and microbial oxidation of Fe2 + by acidophilic bacteria and (2) fibrous spheres (0.3 3 μm) with filamentous morphology and a high degree of porosity.

The most common microbial arsenic mobilization processes involve oxidative dissolution of minerals through oxidation of iron, sulfur, or arsenic [ 6].