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Autophagy is a major process controlled by the Vps15/Vps34 complex in yeast and mammalian cells (Simonsen and Tooze, 2009), though the level of regulation and the in vivo implications are unclear and require further work.
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There is a general consensus that adsorption/desorption (i.e. sorption) is the major process controlling dissolved PO4.
Sandwave climbing, which combines progradation and accretion, is the major process controlling the growth of the ridge.
In view of the results of our experimental simulations, it is clear that the major process controlling the nutrient dynamics at the FSI, besides the mixing that takes place between the two different water bodies, is the seasonal variation between seawater intrusion (salinization) in summer and flushing of the aquifer (freshening) in winter.
The isotope fractionation factors (αC) for the degradation of the m/p-xylene (1.0015) and ethylbenzene (1.0021) obtained from the field observations were similar to factors previously determined for the anaerobic degradation of toluene and o-xylene in laboratory experiments, and suggest that in situ biodegradation is one major process controlling the fate of these contaminants in this aquifer.
The result of saturation index calculated by Visual MINTEQ software combined with Gibbs diagram and IBE findings indicate that, dolomite and calcite dissolution and reverse ion exchange can be a major process controlling the water chemistry in the study area.
Epithelial-mesenchymal transition (EMT) is a major process controlling multiple events during development.
For example, the assessment of δ13C and 87Sr/86Sr ratios suggested that carbonate dissolution is one of the major processes controlling the water chemistry within some aquifers.
Evaporation and ion exchange were the major processes controlling groundwater chemistry in this area.
All groundwater resources are alkaline; major processes controlling water quality are silicate weathering, mineral dissolution and cation exchange.
The major processes controlling the inventory of bioavailable N in the ocean are fixation of N2 gas, which supplies new N to the food web, and denitrification and anaerobic ammonia oxidation, which remove it.
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