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@ARTICLE{Liang:903178,
author = {Liang, Yan and Luo, Yonglu and Lu, Zhiwei and Klumpp, Erwin
and Shen, Chongyang and Bradford, Scott A.},
title = {{E}vidence on enhanced transport and release of silver
nanoparticles by colloids in soil due to modification of
grain surface morphology and co-transport},
journal = {Environmental pollution},
volume = {276},
issn = {0013-9327},
address = {Amsterdam [u.a.]},
publisher = {Elsevier Science},
reportid = {FZJ-2021-04898},
pages = {116661 -},
year = {2021},
abstract = {Natural soils have frequently been considered to decrease
the mobility of engineered nanoparticles (NPs) in comparison
to quartz sand due to the presence of colloids that provide
additional retention sites. In contrast, this study
demonstrates that the transport and release of silver
nanoparticles (AgNPs) in sandy clay loam and loamy sand
soils were enhanced in the presence of soil colloids that
altered soil grain surface roughness. In particular, we
found that the retention of AgNPs in purified soils
(colloid-free and acid-treated) was more pronounced than in
raw (untreated) soils or soils treated to remove organic
matter (H2O2 or 600 °C treated). Chemical analysis and
scanning electron microscopy (SEM) with energy-dispersive
X-ray spectroscopy demonstrated that the grain surfaces of
raw and organic matter-removed soils were abundant with
metal oxides and colloids compared to purified soil. Column
transport and release experimental results, SEM images, and
interaction energy calculations revealed that a significant
amount of concave locations on purified soils hindered AgNP
release by diffusion or ionic strength (IS) reduction due to
deep primary energy minima. Conversely, AgNPs that were
retained in soils in the presence of soil colloids were more
susceptible to release under IS reduction because the
primary minimum was shallow on the tops of convex locations
created by attached soil colloids. Additionally, a
considerable fraction of retained AgNPs in raw soil was
released after cation exchange followed by IS reduction,
while no release occurred for purified soil under the same
conditions. The AgNP release was highly associated with soil
colloids and co-transport of AgNPs and soil colloids was
observed. Our work is the first to show that the presence of
soil colloids can inhibit deposition and facilitate the
release and co-transport of NPs in soil by alteration of the
soil grain surface morphology and shallow primary minimum
interactions.},
cin = {IBG-3},
ddc = {690},
cid = {I:(DE-Juel1)IBG-3-20101118},
pnm = {2173 - Agro-biogeosystems: controls, feedbacks and impact
(POF4-217)},
pid = {G:(DE-HGF)POF4-2173},
typ = {PUB:(DE-HGF)16},
pubmed = {33592438},
UT = {WOS:000630774100015},
doi = {10.1016/j.envpol.2021.116661},
url = {https://juser.fz-juelich.de/record/903178},
}