Control of particle size via chemical composition: Structural and magnetic characterization of Ni–Co alloy nanoparticles encapsulated in lamellar mixed oxides

2008 ◽  
Vol 107 (1-2) ◽  
pp. 202-211 ◽  
Author(s):  
K.A. Tarasov ◽  
V.P. Isupov ◽  
B.B. Bokhonov ◽  
Yu.A. Gaponov ◽  
B.P. Tolochko ◽  
...  
2018 ◽  
Author(s):  
G. Saravanan ◽  
V. Asvini ◽  
R. K. Kalaiezhily ◽  
I. Mubeena Parveen ◽  
K. Ravichandran

The Analyst ◽  
2018 ◽  
Vol 143 (21) ◽  
pp. 5191-5201
Author(s):  
Borja Cantero-Tubilla ◽  
Larry P. Walker

Fourier Transform InfraRed (FTIR) spectroscopy is a very powerful technique for the characterization of the chemical composition of biomass and its modifications occurring during thermochemical and chemical pretreatments.


2014 ◽  
Vol 42 (10) ◽  
pp. 1393-1401 ◽  
Author(s):  
Qinghong Wang ◽  
Guangxu Yan ◽  
Bin Cai ◽  
Chunmao Chen ◽  
Shaohui Guo

Minerals ◽  
2021 ◽  
Vol 11 (3) ◽  
pp. 276
Author(s):  
Lei Pan ◽  
Sean Golden ◽  
Shoeleh Assemi ◽  
Marc Freddy Sime ◽  
Xuming Wang ◽  
...  

Respirable coal mine dust (RCMD) particles, particularly the nano-sized fraction (<1 μm) of the RCMD if present, can cause severe lung diseases in coal miners. Characterization of both the particle size and chemical composition of such RCMD particles remains a work in progress, in particular, with respect to the nano-sized fraction of RCMD. In this work, various methods were surveyed and used to obtain both the size and chemical composition of RCMD particles, including scanning electron microscopy (SEM), scanning transmission electron microscopy (S-TEM), dynamic light scattering (DLS), and asymmetric flow field-flow fractionation (AsFIFFF). It was found that the micron-sized fraction (>1 μm) of RCMD particles collected at the miner location, from an underground coal mine, contained more coal particles, while those collected at the bolter location contained more rock dust particles. Two image processing procedures were developed to determine the size of individual RCMD particles. The particle size distribution (PSD) results showed that a significant amount (~80% by number) of nano-sized particles were present in the RCMD sample collected in an underground coal mine. The presence of nano-sized RCMD particles was confirmed by bulk sample analysis, using both DLS and AsFIFFF. The mode particle size at the peak frequency of the size distribution was found to be 300–400 nm, which was consistent with the result obtained from SEM analysis. The chemical composition data of the nano-sized RCMD showed that not only diesel particles, but also both coal and rock dust particles were present in the nano-sized fraction of the RCMD. The presence of the nano-sized fraction of RCMD particles may be site and location dependent, and a detailed analysis of the entire size range of RCMD particles in different underground coal mines is needed.


2006 ◽  
Vol 150 (1) ◽  
pp. 11-14 ◽  
Author(s):  
Xingyu Gao ◽  
Swee Ching Tan ◽  
A.T. S. Wee ◽  
Junhua Wu ◽  
Lingbing Kong ◽  
...  

1994 ◽  
Vol 9 (11) ◽  
pp. 2993-2997 ◽  
Author(s):  
Dale L. Perry ◽  
Paul Berdahl ◽  
Charles Perrino

SQUID magnetometer characterization of Ca–Ni–K–O catalyst materials reveals complex magnetic behavior. The magnetic properties are generally determined by the antiferromagnetic material NiO, but samples with traces of elemental nickel show marked effects of ferromagnetism. Potassium doping enhances the formation of metallic nickel. Further deviations from bulk NiO properties can be attributed to NiO particle size effects (superparamagnetism) and to the presence of paramagnetic impurities, possibly Ni3+ ions.


Minerals ◽  
2020 ◽  
Vol 10 (2) ◽  
pp. 142
Author(s):  
Maite Garcia-Valles ◽  
Pura Alfonso ◽  
Salvador Martínez ◽  
Núria Roca

This research characterizes the kaolinitic clays from Cretaceous–Paleocene lateritic deposits of Terra Alta (south Catalonia) to evaluate their possible applications. The outcrops and quarries belong to the Horta de Sant Joan and Pinell de Brai areas. The chemical composition, mineralogy, rheological behavior, particle size distribution and plasticity are determined. The Fe and Ti4+ contents prevent them from being directly used as raw material for white ceramics. The mineralogy consists of kaolinite with quartz, illite, hematite, and minor K-feldspar and calcite. Most of the area comprises medium plastic clays that are classified as fired clays and can be used as ceramic and construction materials. In Horta de Sant Joan, a kaolinitic-rich level, up to 75 wt % of kaolinite, is highly crystalline with low plasticity and can be classified as flint clay, useful as a refractory clay. The evaluated kaolinitic clays can also be used to obtain a triaxial ceramic when they are mixed with feldspar to act as a fluxing agent and chamotte.


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