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Natural zeolite is a type of mineralogical material containing large quantities of reactive SiO2 and Al2O3.
Exposure to increased temperatures and solar irradiance also causes zooxanthellae to manufacture abnormally large quantities of reactive oxygen species (molecules that contain oxygen and at least one unpaired electron), which are toxic to both the algae and their coral symbionts.
Background: in response to a variety of stimuli, phagocytes release large quantities of reactive oxygen species (ROS), which are essential for bacterial killing.
In an attempt to mitigate the hazards associated with storing large quantities of reactive metal hydrides, polymer composite materials were synthesized and tested under simulated usage and accident conditions.
Coastal wetlands have the capacity to retain and denitrify large quantities of reactive nitrogen (N), making them important in attenuating increased anthropogenic N flux to coastal ecosystems.
In response to endotoxin [ 42] or cytokines [ 43], neutrophils release large quantities of reactive oxygen species through respiratory burst, which is essential for killing invading microorganisms but also increases tissue damage [ 44].
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They can be primed and activated by different agents that can impair oxidative burst and phagocytosis with opposite effects: reduced capability to destroy bacteria or hyperactivation that induces the generation of large quantities of toxic reactive oxygen species, which can damage surrounding tissue and participate in inflammation.
The presence of large quantities of highly-reactive substances like oxygen would suggest that something interesting was going on, as there would be no known non-biological effect that could account for its presence.
However, storing large quantities of protons could have consequences in the formation of reactive oxygen species (ROS) that could be produced by back-up and leakage of electron transport [ 6].
Exposure to large quantities of hydrophobic nCB has been shown to induce cell injury, pyroptosis and generate reactive oxygen species (ROS) in cultured cells (Reisetter et al., 2011).
Explosive volcanic eruptions that inject large quantities of sulfur dioxide into the stratosphere facilitate the chemical conversion of chlorine into more reactive forms that destroy ozone.
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