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Primarily, the geochemical evolution of SGA groundwater occurs under CO2 open conditions, and the continuous uptake of CO2 is responsible for mineral dissolution, producing bicarbonate as the main anion, and calcium and magnesium in groundwater.
The continuous uptake of CO2 under open conditions leads to calcite precipitation, which in addition to ion exchange are responsible by Ca removal from groundwater and an increase in Na concentrations.
Like GS, in the physiological solution (0.9 % NaCl), there is a continuous uptake of PS which has been noticed by the hydrogel, and after certain time interval the absorption becomes stable.
Waters and Grusak (2008) suggested that, in Arabidopsis, continuous uptake and translocation of minerals to source tissues during seed fill are as important, if not more important, than remobilization of previously stored minerals.
It is accepted that minerals may be remobilized from vegetative sources (Hocking and Pate1977; Himelblau and Amasino2001), although a major portion of minerals in seeds are likely supplied through continuous uptake and translocation during reproductive growth to developing seeds.
In Arabidopsis, continuous uptake and translocation of minerals to source tissues during seed fill are as important, if not more important, than remobilization of previously stored minerals (Waters and Grusak 2008).
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More interestingly, the internalized LAT1 together with targeting nanoparticles could recycle back to the cell membrane within 3 h, guaranteeing sufficient transporters on cell membrane for continuous cellular uptake.
At times, when pure biosorptive metal removal is not feasible, application of a judicious consortium of growing metal-resistant cells can ensure better removal through a combination of bioprecipitation, biosorption and continuous metabolic uptake of metals after physical adsorption.
Experiments on adsorption kinetics indicate that after a fast surface adsorption process a continuous slow uptake occurs which may be explained by incorporation via surface dissolution and reprecipitation processes.
Nevertheless, in this study, the eight pulmonary infarctions exhibited a slight, thin and continuous FDG uptake in all cases, with a median SUVmax value of 3.6, which is close to those reported previously [5].
In conclusion, the rim sign, defined as a slight and continuous FDG uptake at the border of a peripheral lung consolidation, is easily recognisable at FDG-PET/CT and is strongly suggestive of pulmonary infarction.
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