2 research outputs found
Influence of Ligand–Precursor Molar Ratio on the Size Evolution of Modifiable Iron Oxide Nanoparticles
During the synthesis of nanoparticles
via thermal decomposition
of iron precursors, the capping ligand–precursor ratio influences
the resulting size of the iron oxide nanoparticles. As the molar ratio
of aliphatic amines to iron precursor is increased, the average diameter
of the synthesized iron oxide nanoparticles decreases. This trend
is opposite to previously reported results. We investigated this phenomenon
by independently varying the ligand chain length, the ligand–precursor
molar ratio, and the degree of saturation of the aliphatic chain.
Nuclear magnetic resonance spectra of the precursor illustrated the
presence of a primary amine peak before heating and the peak absence
after heating, potentially indicating that the primary amine acts
as reducing agent to promote the decomposition of the iron precursor.
We hypothesize that the amine groups play a dominant role in the nucleation
of the particles, while the chain length and degree of aliphatic saturation
have only a minor effect on particle size. The nanoparticles’
size and crystallinity were characterized with high-resolution transmission
electron microscopy, dynamic light scattering, and X-ray diffraction,
and the magnetic properties were characterized by magnetometry
An Early Mesozoic transcontinental palaeoriver in South China: evidence from detrital zircon U–Pb geochronology and Hf isotopes
<p>Detrital zircon geochronology reveals that Late Triassic–Early Jurassic fluvial sandstones from the major basins of the South
China Craton have similar age patterns and define four populations at 2.6–2.4 Ga, 2.0–1.7 Ga, 850–700 Ma and 480–210 Ma. The
late Palaeoproterozoic group is predominant in all of the five samples, and yielded remarkable age peaks at <em>c</em>. 1.85 Ga. These zircons have ϵ<sub>Hf</sub>(t) values between −22.5 and +3.6, suggesting derivation from reworked Archaean crust and minor juvenile crustal additions
in the late Palaeoproterozoic. These characteristics differ from those of the Yangtze Block but correlate well with those
of samples from the eastern Cathaysia Block. Palaeocurrent analysis of the Early Mesozoic sandstones shows predominant west-
and NW-directed palaeoflows, supporting derivation of the sediments from the Cathaysia Block. The remarkable similarities
in provenance signatures and spatial changes of lithofacies of the Triassic–Jurassic around the South China Craton delineate
an east–west-trending sedimentary zone extending from Korea to West China. Accumulation of these sediments was probably related
to the development of an active continental margin produced by westward subduction of the Palaeo-Pacific Plate. A <em>c</em>. 2000 km long westerly draining transcontinental palaeoriver probably had existed in the Early Mesozoic and fed the basins
in Korea, South China and West China.
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