Hyun Na Kim

Prof. Hyun Na Kim

orcid

Research Focus & Metrics

Academic Career Length

18Years (2009-Present)

(Calculated once Scilit publication data is synced: current year − year of first publication + 1)

Representative Publications

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1 November 2013 in Geochimica et Cosmochimica Acta
Verified
Journal Article
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HKHyun Na Kim
Hyun Na Kim
SLSung Keun Lee
Sung Keun Lee

31 October 2019 in Minerals
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Journal Article
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HKHyun Na Kim
Hyun Na Kim
JKJin Woo Kim
Jin Woo Kim
MKMin Sik Kim
Min Sik Kim
BLBum Han Lee
Bum Han Lee
JKJin Cheul Kim
Jin Cheul Kim
The properties and preparation of talc have long been investigated due to its diverse industrial applications, which have expanded recently. However, its comminution behavior is not yet fully understood. Therefore, having better control of the particle size and properties of talc during manufacturing is required. In this study, we investigate the effect of the ball size in a high-energy ball mill on the comminution rate and particle size reduction. High-energy ball milling at 2000 rpm produces ultrafine talc particles with a surface area of 419.1 m2/g and an estimated spherical diameter of 5.1 nm. Increasing the ball size from 0.1 mm to 2 mm increases the comminution rate and produces smaller talc particles. The delamination of (00l) layers is the main comminution behavior when using 1 mm and 2 mm balls, but both the delamination and rupture of (00l) layers occurs when using 0.1 mm balls. The aggregation behavior of ground talc is also affected by the ball size. Larger aggregations form in aqueous solution when ground with 0.1 mm balls than with 1 mm or 2 mm balls, which highlights the different hydro-phobicities of ground talc. The results indicate that optimizing the ball size facilitates the formation of talc particles of a suitable size, crystallinity, and aggregation properties.

1 July 2013 in American Mineralogist: Journal of Earth and Planetary Materials
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HKHyun Na Kim
Hyun Na Kim
SLSung Keun Lee
Sung Keun Lee
Nanoparticles are known to have physical properties different from their bulk analogs, a characteristic that bears wide technological potential. Detailed knowledge of the atomic structures of diverse metastable/stable polymorphs in alumina nanoparticles with varying particle size is essential to understand their macroscopic properties and the behavior of their phase transitions. In this study, we report high-resolution solid-state 27Al 2D triple-quantum (3Q) magic-angle spinning (MAS) and 1D MAS nuclear magnetic resonance (NMR) spectra for alumina nanoparticles with varying temperature and particle size with an aim to explore the nature of phase transitions in alumina nanoparticles. Although the 27Al MAS NMR spectra of alumina nanoparticles cannot fully resolve all the crystallographically distinct Al sites for metastable aluminas such as γ-, δ-, and θ-Al2O3, the simulation of 27Al MAS NMR spectra collected at different magnetic fields following the Czjzek model allows us to obtain the quantitative fractions of alumina polymorphs in nanoparticles and the NMR characteristics of their Al sites. The 27Al 3QMAS NMR spectra resolved crystallographically distinct [6]Al and [4]Al sites in (γ,δ)- and θ-Al2O3 in the isotropic dimension for the first time. The fraction of θ-Al2O3 gradually increases up to ~1473 K at the expense of a decrease in (γ,δ)-Al2O3. The onset of formation of α-Al2O3 from metastable aluminas is observed above ~1493 K. Several phase transitions in alumina nanoparticles observed in the current study include, γ,δ → θ-Al2O3, γ,δ → α-Al2O3, and θ → α-Al2O3. Although the phase transition γ,δ → θ-Al2O3 occurs gradually with increasing annealing temperature from 873 to 1473 K, the phase transitions γ,δ → α-Al2O3 and θ → α-Al2O3 occur dramatically within a narrow temperature range between 1473 and 1573 K. The observed difference in temperature range (gradual vs. dramatic) for phase transition γ,δ → θ-Al2O3 and γ,δ,θ → α-Al2O3 originates from the different structural disorder in the metastable aluminas (i.e., γ-, δ-, θ-) and α-Al2O3. The effect of particle size on the phase transition (γ,δ) → θ-Al2O3 between 298 and ~1473 K is not observed significantly. On the other hand, the transition temperature for γ,δ,θ → α-Al2O3, where the 50% for alumina is α-Al2O3, apparently increases as the particle size increases (as evidenced by TEM observation), indicating a larger energy penalty for phase transitions into α-Al2O3 in larger alumina nanoparticles. This could be due to higher surface energy of θ-Al2O3 than that of α-Al2O3 and/or the fact that the transition from θ-Al2O3 to α-Al2O3 is kinetically favored for smaller nanoparticles. The mechanistic details of phase transitions among alumina polymorphs provided in the current study yield insights into the nature of the phase transition mechanisms for other oxide nanoparticles ubiquitous in the Earth’s surface environment.

1 April 2019 in Earth and Planetary Science Letters
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Journal Article
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NKNoriyuki Kawasaki
Noriyuki Kawasaki
CPChangkun Park
Changkun Park
NSNaoya Sakamoto
Naoya Sakamoto
SPSun Young Park
Sun Young Park
HKHyun Na Kim
Hyun Na Kim
HYHisayoshi Yurimoto
Hisayoshi Yurimoto

20 November 2009 in The Journal of Physical Chemistry B
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Journal Article
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Sung Bo LeeSung Bo Lee
Sung Bo Lee
HKHyun Na Kim
Hyun Na Kim
BLBum Han Lee
Bum Han Lee
HKHyo-Im Kim
Hyo-Im Kim
EKEun Jeong Kim
Eun Jeong Kim

1 October 2014 in American Mineralogist: Journal of Earth and Planetary Materials
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Journal Article
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HKHyun Na Kim
Hyun Na Kim
SLSung Keun Lee
Sung Keun Lee
Despite efforts to understand the amorphization mechanisms of zeolites upon heating and subsequent dehydration, little is known about the extent of Si-Al disorder and topological variations in both crystalline and amorphous phases during amorphization. In this study, we investigated the atomic structure and the extent of configurational disorder (e.g., Si-Al ordering) in Na-zeolite A and other dehydrated phases during their temperature-induced amorphization using multi-nuclear solid-state NMR. We also report the first multi-nuclear (17O, 29Si, and 27Al) NMR spectra of the intermediate amorphous phases. 29Si MAS NMR results confirm the prevalence of amorphous phases up to ~1073 K and variation in Q-species for the crystalline phases. The 27Al quadrupolar coupling constant of the [4]Al peak in Na-zeolite A and the intermediate amorphous phases increase with increasing temperature, which suggests an increase in the topological disorder associated with the structural distortion around [4]Al. 2D 17O 3QMAS NMR spectra resolve the crystallographically distinct Si-O-Al sites in Na-zeolite A and three types of oxygen linkages namely, Si-O-Al, Si-O-Si, and Al-O-Al in the intermediate amorphous phases, which provides an unambiguous experimental evidence for an increase in the Si-Al disorder during the amorphization of zeolite. The detailed structural changes in Na-zeolite A and other dehydrated phases at various temperatures provide insights into the structural changes of other aluminosilicates during amorphization, thereby highlighting the changes in Si-Al ordering.