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@ARTICLE{Zhang:820896,
author = {Zhang, Miaoyue and Bradford, Scott A. and Šimůnek, Jirka
and Vereecken, Harry and Klumpp, Erwin},
title = {{D}o {G}oethite {S}urfaces {R}eally {C}ontrol the
{T}ransport and {R}etention of {M}ulti-{W}alled {C}arbon
{N}anotubes in {C}hemically {H}eterogeneous {P}orous
{M}edia?},
journal = {Environmental science $\&$ technology},
volume = {50},
number = {23},
issn = {1520-5851},
address = {Columbus, Ohio},
publisher = {American Chemical Society},
reportid = {FZJ-2016-06160},
pages = {12713–12721},
year = {2016},
abstract = {Transport and retention behavior of multi-walled carbon
nanotubes (MWCNTs) was studied in mixtures of negatively
charged quartz sand (QS) and positively charged
goethite-coated sand (GQS) to assess the role of chemical
heterogeneity. The linear equilibrium sorption model
provided a good description of batch results, and the
distribution coefficients (KD) drastically increased with
the GQS fraction that was electrostatically favorable for
retention. Similarly, retention of MWCNTs increased with the
GQS fraction in packed column experiments. However,
calculated values of KD on GQS were around 2 orders of
magnitude smaller in batch than packed column experiments
due to differences in lever arms associated with
hydrodynamic and adhesive torques at microscopic roughness
locations. Furthermore, the fraction of the sand surface
area that was favorable for retention (Sf) was much smaller
than the GQS fraction because nanoscale roughness produced
shallow interactions that were susceptible to removal. These
observations indicate that only a minor fraction of the GQS
was favorable for MWCNT retention. These same observations
held for several different sand sizes. Column breakthrough
curves were always well described using an
advective-dispersive transport model that included retention
and blocking. However, depth-dependent retention also needed
to be included to accurately describe the retention profile
when the GQS fraction was small. Results from this research
indicate that roughness primarily controlled the retention
of MWCNTs, although goethite surfaces played an important
secondary role.},
cin = {IBG-3},
ddc = {050},
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},
UT = {WOS:000389557100022},
doi = {10.1021/acs.est.6b03285},
url = {https://juser.fz-juelich.de/record/820896},
}