• Proceedings of the Korean Vacuum Society Conference
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• 2011.02a
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• pp.150-151
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• 2011

양자점 Laser Diode(LD)는 낮은 문턱전류, 높은 미분 이득을 갖으며 또한 온도변화에도 안정적이기 때문에 광통신분야에서 광원으로 양자점 LD를 사용하기 위한 연구가 계속되고 있다. 양자점은 fill factor가 낮기 때문에 양자점의 밀도를 높이거나 양자점을 적층 성장하여 fill factor를 높인다. 그러나 양자점을 적층 성장하면 각 층간의 응력, 수직적 결합, 전기적인 결합이 생기며 이는 양자점의 전기적, 광학적 특성에 영향을 미친다. 본 연구에서는 metal organic chemical vapor deposition (MOCVD)을 이용하여 InP기판 위에 자발성장 법으로 InAs 양자점을 다주기 성장하였으며 photoluminescence (PL)을 이용하여 광학적 특성을 분석하였다. precursor는 trimethylindium (TMI), trimethylgalium (TMGa), $PH_3$, $AsH_3$를 사용하였으며 carrier gas는 $H_2$를 사용하였다. InAs 양자점은 1100 nm의 파장을 갖는 InGaAsP barrier 위에 성장하였고, InAs와 InGaAsP의 성장온도는 $520^{\circ}C$이며 InAs 양자점 성장시 V/III 비는 3.66으로 일정하게 유지하였다. 그림 1은 양자점 성장시간을 0.11분으로 고정하여 3주기(A), 5주기(B), 8주기(C) 성장한 구조이며 그림 2는 양자점 성장시간을 3주기마다 0.01분씩 줄여가며 3주기는 0.11분${\times}$3(D), 6주기는 0.11분${\times}$3+0.10분${\times}$3(E), 9주기는 0.11분${\times}$3+0.10분${\times}$3+0.09분${\times}$3(F) 으로 성장한 성장구조이다. 각 성장한 시료는 PL을 이용하여 파장과 반치폭을 측정하였다. 그림 3은 양자점 성장시간을 고정한 시료 A, B, C의 PL파장과 PL반치폭 데이터이다. PL파장은 A, B, C 시료 각각 1504 nm, 1571 nm, 1702 nm이며 반치폭은 각각 140 meV, 140 meV, 150 meV이다. PL파장과 반치폭은 각각 3주기에서 6주기로 증가할 때 67 nm, 0 meV 6주기에서 9주기로 증가할 때는 131 nm, 10 meV 증가하였다. 다음 그림4는 양자점 성장시간을 조절하여 성장한 양자점 시료 D, E, F의 PL파장과 PL반치폭 데이터이다. PL파장은 D, E, F 시료 각각 1509 nm, 1556 nm, 1535 nm이며 반치폭은 각각 137 meV, 138 meV, 144 meV이다. PL파장과 반치폭은 각각 3주기에서 6주기로 증가할 때 47 nm, 1 meV 증가하였고, 6주기에서 9주기로 증가할 때는 21 nm 감소, 6 meV 증가하였다. 양자점 성장시간을 고정하여 다주기를 성장하였고 또 3주기마다 양자점 성장시간을 달리하여 다주기를 성장하였으며 PL을 이용해 광학적 특성을 연구하였다. 성장된 양자점의 PL 파장과 PL 반치폭 변화를 통해 적층구조에서 성장 주기가 늘어날수록 양자점의 크기가 증가하는 것을 확인하였고 또한 적층성장을 할 때 양자점 성장시간을 줄임으로써 양자점의 크기 변화를 제어 할 수 있었다.

• Economic and Environmental Geology
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• v.55 no.6
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• pp.633-648
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• 2022

Gravity data were analyzed to identify the cause of clustered seismicity that occurred intensively in Yeoncheon, located in the central part of the Korean Peninsula. Our analysis suggests that the En echelon faults developed in the northwest-southeast direction. In addition, in the eastern part of the Dongducheon Fault, it was interpreted that high-density lower bedrock intermittently lifts close to the surface due to vertical tectonic movement accompanied by a flower structure. The fracture zone of the Dongducheon Fault is estimated that the width is about 200 m, the depth is at least 5 km, and the density is about 15% lower than the adjacent rocks. It is analyzed that the shallow earthquakes that occurred within 5 km depth was concentrated along the low-density En echelon fault fracture zone developed between the high-density rocks intruding close to the surface. Therefore, the earthquakes can be interpreted as the result that the north-south stress caused by the dextral tectonic movement of the Dongducheon Fault activated the En echelon fault in the northwest-southeast direction.

• KSCE Journal of Civil and Environmental Engineering Research
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• v.6 no.1
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• pp.1-11
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• 1986

Welded connectors of the cover plates, the transverse stiffeners of the plate girders, and the gusset plates of the plates girders or box girders, were selected as studying objects. A simplified method of drawing the S-N curves in these welded joints by a computer program without the direct fatigue tests was established. The plots on the S-N curve using the values from the practical fatigue tests were compared with the results from the method of the computer programming. The results of these studies are as follows. It appeared that the fatigue life by calculation method was a little less than the practical fatigue life from the actual tests. The latter values included both life $N_c$ of occurrence of initial crack $a_i$ and the life $N_p$ of propagation of critical crack. On the other hand, the former values included only the life $N_p$. Therefore, these results should be considered as justifiable ones. Since the difference between the two results was not significant, the results by calculation method should be in the conservation side when the safety of the structures was considered. Consequently, the results by calculation method should be applicable to the fracture fatigue design of structure. For reference, the same fatigue tests were performed with the specimens of 3 pieces in each case made of the low-strength steel, SS 41. The results went unexpected showing that the fatigue strength was lower in the case of low-strength steel. That is, in the case of the cover plate, the fatigue strength became slowly higher than the case of high-strength steel, SWS 50. That was observed when the maximum testing stress was higher than $14kg/mm^2$. In addition, in the case of the transverse stiffener, the fatique strength became rapidly higher than the case of SWS 50. That was observed when the maximum testing stress was lower than $31kg/mm^2$. It was thought that more such fatigue tests should be performed for more reliable results.

• Ocean and Polar Research
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• v.34 no.4
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• pp.413-430
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• 2012

To understand the scales of the spatial distribution and temporal duration of the subsurface chlorophyll-a maximum (SCM) observed in the Ulleung Basin of the East Sea, we analyzed physical and chemical data collected during the East Asian Seas Time-series-I (EAST-I) program. The SCM layer occurred at several observation lines from the Korea Strait to $37.9^{\circ}N$ in the Ulleung Basin during August of 2008 and 2011. At each observation line, the SCM layer extended from the coast to about 200 km off the coast. The SCM layer was observed between 30 and 40 m depth in the Ulleung Basin as well as in the northwestern Japan Basin along $132.3^{\circ}E$ from $38^{\circ}N$ to $42.3^{\circ}N$ during July 2009, and was observed around 50 m depth in the northeastern Japan Basin ($135-140^{\circ}E$ and $40-45^{\circ}N$) during July 2010. From these observed features, we hypothesize that the SCM layer observed in the Ulleung Basin may exist in most of the East Sea and may last for at least half-year (from the early May to late October). The nutrient supply mechanism for prolonged the SCM layer in the East Sea was not known, but it may be closely related to the horizontal advection of the nutrient rich and low oxygen waters observed in the Korea Strait between a 50 m depth to near the bottom. The prolonged development of the SCM layer in the Ulleung Basin may result in high primary production and would also be responsible for the high organic carbon content observed in the surface sediment of the region.

• Journal of the Korean earth science society
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• v.36 no.1
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• pp.1-15
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• 2015

In order to outline the kinematics and movement history of a new Quaternary fault, Jingwan Fault in Dangjin, West Korea, we analyzed the geometry of the fault zone composed of a few gouge zones, and made ESR dating for fault gouge materials. The $N55^{\circ}E$ striking Jingwan Fault is a normal fault and exhibits a gradual change in dip (gentle in the lower part, steep in the upper part), indicating a listric fault. As for the fault gouge zone, its thickness varies and reaches 2~3 cm in the lower part or between basement rocks, and 20~30 cm in the middle-upper part or between the basement and Quaternary deposit. It is observed in the latter case that more than three gouge zones develop with different colors, and branch out and re-merge, or they are partly superimposed, indicating different movement episodes. The cumulative displacement is estimated to be about 10 m using the geological cross-sections, from which it is inferred that the total length of fault may be about 2.5 km on the basis of the empirical relation between cumulative displacement and fault length. Therefore, a more study would be needed to verify the entire fault length. The results of ESR dating for three gouge samples at different spots along the fault yields ages of $651{\pm}47$, $649{\pm}96$, and $436{\pm}66ka$, indicating at least two movement episodes. Slickenlines observed on the fault planes indicate a pure dip slip (normal faulting), which suggests that the ENE-WSW trending Jingwan Fault was presumably moved under a NNW-SSE extensional environment.