• Medical Lasers
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• 제8권2호
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• pp.87-89
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• 2019

Post inflammatory hyperpigmentation (PIH) is a reactive hypermelanosis of the skin that occurs as a result of various inflammatory responses such as surgical procedure, trauma, and many inflammatory conditions. There are several reported studies of various modality in managing PIH. However, the treatment of PIH can prove to be challenging. In this report, we treated a patient with PIH using picosecond-domain Nd:YAG lasers. After ten sessions of 1,064-nm picosecond-domain Nd:YAG laser treatment, the patient presented considerable improvement with no remarkable side effects or recurrence over the duration of 6 months. We suggest that a 1,064-nm picosecond-domain Nd:YAG laser can be effectively and safely used for treating pigmented lesions resulting from surgical procedure in the skin of Asian patients.

• 한국자기학회:학술대회 개요집
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• 한국자기학회 2007년도 The 1st International Symposium on Advanced Magnetic Materials
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• pp.28.2-28.2
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• 2007

• 한국광물학회:학술대회논문집
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• 한국광물학회.한국암석학회 2005년도 공동학술발표회 논문집
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• pp.64-64
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• 2005

• 한국세라믹학회지
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• 제33권9호
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• pp.1031-1037
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• 1996

• 한국암석학회:학술대회논문집
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• 한국암석회.한국광물학회 2009년도 공동학술발표회 논문집
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• pp.88-90
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• 2009

• 대한피부과학회지
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• 제56권10호
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• pp.649-651
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• 2018

• 자원환경지질
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• 제22권4호
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• pp.371-379
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• 1989

서산지역의 변성퇴적암류에 대한 변성온도 및 압력 조건이 공존하는 변성광물에 대한 분석결과로부터 측정될 수 있었다. 석류석과 흑운모 지온계 (Ferry and Spear, 1978; Ganguly and Saxena, 1984)를 이용한 온도 측정 결과, 서산층에 서는 $620{\pm}40^{\circ}C$이며, 대산층에서는 $520{\pm}20^{\circ}C$인 것으로 나타났다. 석류석-사장석-$Al_2SiO_5$- 석영 지압계 (Newton and Haselton, 1981; Gangul and Saxena, 1984)을 이용한 압력 측정 결과, 두 층 모두 5-6kb로, 유사한 압력 조건을 보여주고 있다. 이같은 결과는 같은 압력 조건 아래에서 서산층이 대산층보다 상대적으로 높은 온도의 변성작용을 받았음을 제시해 준다. 서산층과 대산층에서 Fe, Mg, Mn 등 주원소에 대한 석류석의 chemical zonation은 서로 다른 양상을 보여 주는데, 아마도 두 층이 다른 열적 변성과정(thermal history)을 받아온 결과인 것같다.

• 한국해양학회지
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• 제7권2호
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• pp.59-73
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• 1972

The heavy minerals of a barred estuarine and lagoonal sediments along the North Carolina coast have been studied with more than one hundred samples. Currents, salinity, and pH exhibit well-developed gradients from the upstream parts of the estuaries on the west toward the open ocean on the east. Twenty- four heavy minerals were identified in sediments of the study area. However, less than half of these occur frequently and the remainder exist only in minor quantities or trace amounts. Heavy minerals usually comprise less than 1% of the sample but vary from sample to sample. The maximum amount of heavy minerals in sediments of sounds and estuaries is 2.4% and in sediments of Outer Banks is 16.7%. Opaque minerals range from 10 to 85% of the total heavy mineral assemblage. Garnet and sillimanite are relatively more abundant in the eastern part than the western part in the area. Garnet more abundant in the northern part than the southern part, whereas sillimanite is more abundant in the southern part than the northern part, because the garnet source is in the northern part and one of the sillimanite source is in the southern part in the study area. The results of heavy mineral study indicate that the source of sediments is the Blue Ridge and Piedmont crystalline complex, and Coastal Plain formations. Some portions of sediments are transported from the Atlantic Ocean by the landward currents. They further indicate that the sediments of the Atlantic coast in the study area are transported mainly from the northern part to southern part by longshore littoral currents, and some portions of sediments are transported from the southern part to the northern part by the Gulf Stream.

• 한국자기학회지
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• 제3권2호
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• pp.143-148
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• 1993

열 분해법으로 $Bi_{x}Dy_{3-x}Al_{1}Fe_{4}O_{12}$(x=1, 1.2, 1.5) 자기 가넷 박막을 유리기판 위에 제조하였다. Bi 치환량을 증가시켰을 때 $M_{s}$ 값은 5 emu/cc에서 12 emu/cc로 증가하였고, 제조된 모든 박막이 수직 자기 이방성을 나타내었다. Bi 양의 증가에 따라 파장 780 nm의 광원을 사용했을 때 패러디 회전각이 $0.11^{\circ}/\mu\textrm{m}$에서 $0.20^{\circ}/\mu\textrm{m}$로 증가 하였으며 가넷 결정화 온도는 $660^{\circ}C$에서 $630^{\circ}C$로 감소하였다. 또한 보자력은 1200 Oe에서 600 Oe로 감소하였으며 결정립의 크기가 증가하였다. 박막의 두께를 $2000\;{\AA}$에서 $4000\;{\AA}$으로 증가시킴에 따라 $H_{c}$가 1750 Oe에서 1200 Oe로 감소했으며 ${\theta}_F$는 반사광의 간섭 효과에 의해 증가하였다.

• 한국광물학회지
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• 제2권1호
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• pp.26-36
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• 1989

Clinopyroxene in the Geodo mine belongs to diopside-hedenbergite series. It is widely distributed throughout the mine area together with garnet and is also closely related with Fe-mineralization. Clinopyroxenes in the Geodo mine including two samples from the sangdong and Ulchin Mines are studied using polarized microscope, EPMA, XRD, and IR spectroscopy for occurrence, chemistry, structure, and crystal chemistry. Especially, variations in unit-cell parameters are examined in relation with the substitution scheme between Fe and Mg cations. Clinopyroxenes in the Geodo mine occur in both endoskarn and exoskarn zone. It is mostly anhedral to subhedral with fine- to medium-grained in texture, but some have bigger crystals of short prismatic or columnar habits. Clinopyroxene occurs as monomineralic or is associated with mostly garnet and sometimes with actinolite, magnetite, epidote, and chlorite. Chemical analysis reveals that the Geodo clinopyroxene is diopsidic in composition (Di: 65-96%). This fact is in good contrast with garnet chemistry showing mostly andraditic (An: 41-82%). Especially, clinopyroxene coexisting with magnetite belongs to nearly end member diopside (Di: 97-99%). Thus, diopside-andradite pair indicates that Geodo skarns were formed under the reduced environment. X-ray diffraction analysis shows unit-cell parameters vary with increase of Fe contents: a = 9.765-9.838$\AA$, b = 8.943-9.020$\AA$, c= 5.240-5.253$\AA$.$\beta$ = 105.70-104.83$^{\circ}$, and V =440.64-448.19$\AA$3. It is noted from the least square regression that a, b and V increase linearly with increase of Fe content, while $\beta$ slightly decreases and c remains nearly unchanged as change in Fe content. These trends are to difference between synthetic and natural clinopyroxenes. This fact is also recognized in IR spectra which show a slight shift of several absorption bands toward lower wavenumber region with increasing Fe content.