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@ARTICLE{Liang:864359,
author = {Liang, Yan and Bradford, Scott A. and Šimůnek, Jiří and
Klumpp, Erwin},
title = {{M}echanisms of graphene oxide aggregation, retention, and
release in quartz sand},
journal = {The science of the total environment},
volume = {656},
issn = {0048-9697},
address = {Amsterdam [u.a.]},
publisher = {Elsevier Science},
reportid = {FZJ-2019-04155},
pages = {70 - 79},
year = {2019},
abstract = {The roles of graphene oxide (GO) particle geometry, GO
surface orientation, surface roughness, and nanoscale
chemical heterogeneity on interaction energies, aggregation,
retention, and release of GO in porous media were not fully
considered in previous studies. Consequently, mechanisms
controlling the environmental fate of GO were incompletely
or inaccurately quantified. To overcome this limitation,
plate-plate interaction energies were modified to account
for these factors and used in conjunction with a
mathematical model to interpret the results of GO
aggregation, retention, and release studies. Calculations
revealed that these factors had a large influence on the
predicted interaction energy parameters. Similar to previous
literature, the secondary minimum was predicted to dominate
on smooth, chemically homogeneous surfaces that were
oriented parallel to each other, especially at higher ionic
strength (IS). Conversely, shallow primary minimum
interactions were sometimes predicted to occur on surfaces
with nanoscale roughness and chemical heterogeneity due to
adsorbed Ca2+ ions, especially when the GO particles were
oriented perpendicular to the interacting surface.
Experimental results were generally consistent with these
predictions and indicated that the primary minimum played a
major role in GO retention and the secondary minimum
contributed to GO release with IS reduction. Cation exchange
(Na+ replacing Ca2+) enhanced GO release with IS reduction
when particles were initially deposited in the presence of
Ca2+ ions. However, retained GO were always completely
recovered into the excess deionized water when the sand pore
structure was destroyed during excavation, and this
indicates that primary minima were shallow and that the pore
structure also played an important role in GO retention.
Further evidence for the role of pore structure on GO
retention was obtained by conducting experiments in finer
textured sand and at higher input concentrations that
induced greater aggregation. In both cases, greater GO
retention occurred, and retention profiles became more
hyperexponential in shape.},
cin = {IBG-3},
ddc = {610},
cid = {I:(DE-Juel1)IBG-3-20101118},
pnm = {255 - Terrestrial Systems: From Observation to Prediction
(POF3-255)},
pid = {G:(DE-HGF)POF3-255},
typ = {PUB:(DE-HGF)16},
pubmed = {pmid:30502736},
UT = {WOS:000455039600008},
doi = {10.1016/j.scitotenv.2018.11.258},
url = {https://juser.fz-juelich.de/record/864359},
}