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@ARTICLE{Liang:139933,
author = {Liang, Yan and Bradford, Scott A. and Simunek, Jiri and
Heggen, Marc and Vereecken, Harry and Klumpp, Erwin},
title = {{R}etention and {R}emobilization of {S}tabilized {S}ilver
{N}anoparticles in an {U}ndisturbed {L}oamy {S}and {S}oil},
journal = {Environmental science $\&$ technology},
volume = {47},
number = {21},
issn = {1520-5851},
address = {Columbus, Ohio},
publisher = {American Chemical Society},
reportid = {FZJ-2013-05900},
pages = {12229 - 12237},
year = {2013},
abstract = {Column experiments were conducted with undisturbed loamy
sand soil under unsaturated conditions (around $90\%$
saturation degree) to investigate the retention of
surfactant stabilized silver nanoparticles (AgNPs) with
various input concentration (Co), flow velocity, and ionic
strength (IS), and the remobilization of AgNPs by changing
the cation type and IS. The mobility of AgNPs in soil was
enhanced with decreasing solution IS, increasing flow rate
and input concentration. Significant retardation of AgNP
breakthrough and hyperexponential retention profiles (RPs)
were observed in almost all the transport experiments. The
retention of AgNPs was successfully analyzed using a
numerical model that accounted for time- and depth-dependent
retention. The simulated retention rate coefficient (k1) and
maximum retained concentration on the solid phase (Smax)
increased with increasing IS and decreasing Co. The high k1
resulted in retarded breakthrough curves (BTCs) until Smax
was filled and then high effluent concentrations were
obtained. Hyperexponential RPs were likely caused by the
hydrodynamics at the column inlet which produced a
concentrated AgNP flux to the solid surface. Higher IS and
lower Co produced more hyperexponential RPs because of
larger values of Smax. Retention of AgNPs was much more
pronounced in the presence of Ca2+ than K+ at the same IS,
and the amount of AgNP released with a reduction in IS was
larger for K+ than Ca2+ systems. These stronger AgNP
interactions in the presence of Ca2+ were attributed to
cation bridging. Further release of AgNPs and clay from the
soil was induced by cation exchange (K+ for Ca2+) that
reduced the bridging interaction and IS reduction that
expanded the electrical double layer. Transmission electron
microscopy, energy-dispersive X-ray spectroscopy, and
correlations between released soil colloids and AgNPs
indicated that some of the released AgNPs were associated
with the released clay fraction.},
cin = {IBG-3 / PGI-5},
ddc = {050},
cid = {I:(DE-Juel1)IBG-3-20101118 / I:(DE-Juel1)PGI-5-20110106},
pnm = {246 - Modelling and Monitoring Terrestrial Systems: Methods
and Technologies (POF2-246) / 424 - Exploratory materials
and phenomena (POF2-424)},
pid = {G:(DE-HGF)POF2-246 / G:(DE-HGF)POF2-424},
typ = {PUB:(DE-HGF)16},
UT = {WOS:000326711300045},
pubmed = {pmid:24106877},
doi = {10.1021/es402046u},
url = {https://juser.fz-juelich.de/record/139933},
}