Environmental Engineering Reference
In-Depth Information
ultimate disposition of NMs in the environment (e.g., ocean, ocean sediments, lake/river
sediments). The concepts required for addressing linked biogeochemical or
physicochemical processes and transport processes are discussed in Section 16.6.
Table 16.1 Summarize of processes potentially influencing NMs in aqueous
environmental settings.
Process
Representative Effects on NM Fate
in the Environment
Description
Aggregation
Interactions of colloids with resulting low net
energies of repulsion will “stick” together into larger
colloids
Aggregated NMs may result in more rapid
sedimentation out of water columns
Biodegradation
Bacteria (heterotrophic or autotrophic) gain
metabolic energy from a substrate (organic or
inorganic, respectively)
Organic capping ligands on quantum dots may
biodegrade and change the surface charge
characteristics of the metal core.
Bioaccumulation
Passage of a pollutant up and through a food chain
Partitioning of hydrophobic fullerenes in lipids may
biomagnify their detrimental effects in higher trophic
states
Dissolution
Phase transformation from solid to dissolved in
water
Nano-silver partially dissolves into silver ion in water
(Benn and Westerhoff submitted)
Facilitated
transport
Dissolved pollutant sorption onto colloids affect
their fate and toxicity
In the presence of TiO2 NMs, compared to no TiO2,
higher levels of arsenic and cadmium were observed in
fish (Sun et al., 2007; Zhang et al., 2007)
Filtration
Removal of colloids from water passing by fixed
collectors (i.e., sand) due to interception,
sedimentation or diffusion from streamlines
followed by chemical attachment to the collector
The velocity and ionic strength of water conveying
fullerenes and metal NMs affects their removal on
quartz collectors (Lecoanet et al., 2004; Lecoanet and
Wiesner, 2004)
Flocculation
Processes (diffusion, fluid shear, differential
settling) that bring colloids into contact with each
other and when a fraction of the colloids aggregate
together
Rapid and slow mixing of metal oxide NMs causes
increasing particle sizes to form over time (Zhang et al.,
in-press-a)
Magnetism
Attraction of oppositely charged paramagnetic
materials or aggregation in a magnetic field
Iron oxide NMs (5-12 nm) exhibit high magnetic
attraction (Mayo et al., 2007)
Nucleation
Increased rate of crystal formation of a chemical
precipitate due to presence of “seed” colloid
Calcite seed particles increase rate of calcium
precipitation (Chao and Westerhoff , 2002)
Oxidation
An increase in valence state, which may include
oxygen incorporation, that occurs via abiotic or
biotic reactions
Photo-oxidation of fullerenes incorporates oxygen-
containing functional groups which may change surface
chemistry (Lee et al., 2007)
Partitioning
Division of pollutant between two phases
Hydrophobic fullerenes partition from aqueous
solutions via non-specific uptake mechanisms in
hydrophobic lipid bilayers (Qiao et al., 2007)
Reduction
A reduction in valence state that occurs via abiotic
or biotic mechanisms
Bacteria can adhere onto metal surfaces and, via
enzymatic processes, facilitate their dissolution
(Shashikala and Raichur, 2002; Stack et al., 2004)
Sedimentation
Removal of particles from water as gravitational
forces exceed buoyant and drag forces
Increases in metal oxide NM diameter leads to more
rapid rates and extent of removal by sedimentation
(Zhang et al., 2008a)
Stabilization
NMs suspended in water columns over long periods
are stable. Destabilized particles may rapidly
aggregate. The degree of stabilization is related to
the surface charge and surface properties of NMs.
Dissolved organic matter facilitates increased
“dissolved” concentrations of fullerenes in water
(Hyung et al., 2007)
Volatilization
Transfer of material from water or solids into the air
Oceanic whitecaps which are the largest source of
aerosol particles on earth, accounting for approximately
10 12 g of sea salt particles annually, and have diameters
of 40 to 120 nm (Bates et al., 1998; Lewis and
Schwartz, 2004)
 
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