• Journal of the Korean Crystal Growth and Crystal Technology
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• v.2 no.2
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• pp.47-52
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• 1992

결정화 유리에서의 결정화도 측정, 혹은 소결체에서의 잔류 유리량을 측정할 때 가장 유용한 방법을 찾아내기 위하여 현재까지 보고되어 있는 방법중에서 Ohlberg와 Benedetti의 XRD를 이용한 방법과 IR을 이용한 Hirose의 방법을 선정하여 코디어라이트 조성의 유리와 β-코디어라이트의 혼합물에 대하여 결정화도를 측정하였다. 이들 측정 방법중에서 Ohlberg의 방법은 표준시료가 준비되었을 경우 약 5%의 오차를 보였으며, Benedetti의 방법은 Ohlberg의 방법보다 큰 오차를 보였지만 표준시료를 필요로 하지 않았다. Hirose의 방법은 적은 결정화도 범위에서만 적용가능한 방법인 것으로 보여졌다.

• Korean Journal of Crystallography
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• v.9 no.1
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• pp.71-76
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• 1998

Crystal structure of Bis(ethylenediamine)palladium(II)-Bis(oxalato)palladate(II0 has been determined by X-ray crystallography. Crystal data : (Pd(C2H8N2)2.Pd(C2O4)2), Fw=509.04, Monocline, Space Group P21/c (no=14), a=6.959(2), b=13.506(2), c=15.339(2) Å, β=99.94(3), Z=4, V=1420 Å3, Dc=2.380 gcm-3, μ=25.46cm-1, F(000)=992. The intensity data were collected with Mo-Kα radiation (λ=0.7107 Å) on an automatic four-circle diffractometer with a graphite monochromater. The structure was solved by Patterson method and refined by full matrix least-square methods using unit weights. The final R and S values were R=0.021, Rw=0.030, Rall=0.032 abd S=2.1 for 1472 observed reflections. The essentially planar complex anions form diade of interplanar distances of 3.41 Å and their diads are stacked along aaxis with interplanar separation of 3.44 Å.

• The Journal of Engineering Geology
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• v.33 no.1
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• pp.61-68
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• 2023

This study analyzed and compared the physicochemical characteristics of topsoil and subsoil of Grade 1 soil from an igneous rock area on the ecological and nature map. The water content and pH of the collected soil samples were measured, and X-ray fluorescence and X-ray diffraction analyses were performed. The results showed that the water content of the topsoil was higher than that of the subsoil, and its pH was more acidic than that of the subsoil. According to the X-ray fluorescence analysis results, sample I9 was closest to kaolinite, while sample I7 was most distant from kaolinite. All other samples were located between samples I7 and I9. The X-ray diffraction analysis showed that the average content of clay minerals was higher in the topsoil than in the subsoil. The most notable clay minerals produced included illite, vermiculite, kaolinite, chlorite, and gibbsite. The results of this study will be used as a basic data for topsoil restoration to convert subsoil into topsoil.

• Journal of the Korean Chemical Society
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• v.30 no.6
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• pp.538-547
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• 1986

The 8 rare earth elements were determined in the monazite concentrates by X-ray fluorescence spectrometry. The spectral line overlapping interferences from the other elements were investigated and the correction methods of interferences were studied using line overlap coefficients. The coefficients were calculated from the ratios of the intensities measured at the diffracted angle (2${\theta}$) of the analytical lines of other elements to the intensity of pure rare earth oxide. The coefficients were used to correct the line overlaps by a regression analysis. The linearities of calibration curves from the corrected intensities were remarkably improved, and their standard deviations were decreased. The analytical results agreed with that of the inductively coupled plasma(ICP) spectrometry within an allowable error range.

• Proceedings of the Korean Powder Metallurgy Institute Conference
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• 1999.04a
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• pp.34-34
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• 1999

• Proceedings of the KSEEG Conference
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• 2007.04a
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• pp.180-182
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• 2007

• Korean Journal of Materials Research
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• v.4 no.1
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• pp.55-62
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• 1994

Co(A $I_{1- X}$C $u_{X}$ ) (0$\leq$0.40)합금계의 결정구조 및 자기적 특성을 X-선 회절분석기, 주사전자현미경 그리고 진동 시료형 자력계를 이용하여 조사하였다. X-선 결정구조 및 상분석 결과, 전조성 범위에서 주상은 격자상수가 약 2.86$\AA$인 규칙화한 B2(CsCI)구조를 가지고 있었으며, x $\geq$0.10범위에서는Cu함량이 많은 제 2상이 존재하였고 격자상수가 약 3.63$\AA$인 FCC 구조이었다. 자화측정결과 x $\geq$0.25범위에서는 강자성, x$\leq$0.10에서는 상자성 그리고 x=0.15, 0.20에서는 초상자성의 특성을 나타내었다. Cu함량(x)이 증가함에 따라 자화값은 증가하는 현상을 보여주었다. 본 합금계의 측정한 분자당 스핀자기 모멘트 값은 국부환경모델을 이용하여 각 조성에서 계산된 Co원소에 대한 스핀자기 모멘트 값과 잘 일치함을 보여주었다.다.

• Journal of the Korean Geotechnical Society
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• v.16 no.6
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• pp.51-58
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• 2000

울산지역에 널리 분포하고 있는 해성 퇴적토에 대하여 깊이별로 물리, 화학 그리고 광물학적 특성을 파악하였으며, 이 지역에서 채취된 시료에 대하여 깊이별로 퓨준압말시험을 실시하였다. 본 논문을 위하여 울산 해성 퇴적토의 생성과정을 추정하고, X-선 회절 분석, X-선 형광분석 및 에너지분산분광분석을 실시하여 깊이에 따른 변화를 비교하였다. 울산 해성 퇴적토의 점토광물에 대한 정량분석결과, 일라이트, 카올리나이트, 녹니석, 스멕타이트 순으로 많게 나타났음, 화학성분 분석결과, SiO$_2$, $Al_2$O$_3$그리고 Fe$_2$O$_3$가 대부분을 차지하는 것으로 나타났다. 주사전자현미경 관찰결과, 유공충과 규조류가 관찰되었다. 표준압밀시험 결과, 울산지역의 해성 퇴적 점토는 깊이에 따른 변형거동이 화학적, 광물학적 분석결과와 마찬가지로 깊이에 따른 변화를 보이지 않아 같은 시디에 퇴적인 것으로 판단된다.

• Journal of the Mineralogical Society of Korea
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• v.32 no.4
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• pp.303-312
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• 2019

In this study, X-ray diffraction, ICP analysis, and leaching experiments were performed to analyze the heavy metals and dissolution characteristics of Andong dam sediments. As a result of X-ray diffraction analysis, Andong dam sediment consists of quartz, plagioclase, chlorite and illite. ICP analysis of sediment showed very high concentrations of As and Cd. Leaching experiments were performed in aerobic and anaerobic condition in a disturbed state. The results of leaching experiment showed that more heavy metals were leached in aerobic than anaerobic conditions. Heavy metal that increased in concentration with time in aerobic conditions were Mn, Zn and Cd, and those in anaerobic conditions were Mn, Fe and As. The leaching ratio of heavy metal concentration in sediment was Mn > Cd > Zn > Ni > Cu > As > Pb ≒ Fe ≒ Cr and Mn > As > Cu > Ni > Zn > Pb ≒ Cd ≒ Fe ≒ Cr in aerobic and anaerobic conditions, respectively.

• Journal of the Korea Academia-Industrial cooperation Society
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• v.13 no.8
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• pp.3315-3318
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• 2012

In this study, Fe-base alloy powder was prepared by gas atomizing method. Shape and crystal structure of the powder were investigated by FESEM, X-ray diffraction, and DSC. The powder was produced in a spherical shape, with a size of 45 ~ 90 ${\mu}m$. X-ray diffraction analysis revealed that the powder was fully amorphous, showing typical broad amorphous peak. From DSC analysis, Tg and Tx that are generally found in a bulk amorphous alloy were also observed in the alloy powder. Tg and Tx of the powder were $530^{\circ}C$ and $560^{\circ}C$, respectively. These results suggest us that the bulk amorphous alloy (BMG) powder prepared in this study is applicable to laser welding.