• Information and Communications Magazine
• /
• v.14 no.12
• /
• pp.77-85
• /
• 1997

지금까지 access network에서의 xDSL의 위치를 살펴보고 DSL, HDSL, ADSL 및 VDSL을 중심으로 기술 및 최근의 표준화동향을 살펴보았다. ITU의 조사에 따르면 97년 기준으로 전세계 약 8억가구에 copper access line이 연결되어 있고 그중의 70%이상이 가정에 연결되어 있는데 증가추세도 북미의 경우 년3.5%, 서유럽과 태평양연안의 경우 년4.5%의 성장율을 보이고 있어 2000년경에는 10억가구에 다다를 전망이다. 미국은 97년기준 약 1억가구에 1억6000만 copper access line이 연결되어 있는데 Yankee Group이 조사한 바에 따르면 2000년을 기준으로 3백만가구에 ADSL/RADSL/SDSL이 연결되고 관련 revenue는 10억달러에 이를것으로 추산하고 있다. 전세계 xDSL 시장규모를 미국의 5배정도로 보면 2000년경에는 전세계 twist pair의 2%정도에 xDSL이 연결되어 ADSL/RADSL/SDSL 관련 세계시장규모가 50억달러에 이르고 시장성장률은 30%에 이를 것으로 보고 있다. 현재 이러한 xDSL의 표준화작업은 3장에서 언급한 바와 같이 ANSI T1, ETSI에서 주로 주도되고 있으나 ITU-T, IEEE, ADSL Forum, ATM Forum, DAVIC 등 다른 group과 활발한 liasion meeting 을 통해서도 협력안을 마련하려 노력하고 있다. 예를 들어 DAVIC은 long range(1.5Km이상) PMD규격으로 ADSL을, mid range($300m\sim1.5km$) PMD규격으로 VDSL을, short range(300m이하) PMD규격으로 CAP방식의 FTTC를 각각구정하여 xDSL을 수용하고 있다. Microsoft의 CEO인 Bill Gates가 'Bandwidth bottleneck. No question. that's the biggest obstacle.'이라고 천명한 바와 같이 정보사회로의 진전에 있어 bandwidth는 시급히 해결되어야 할 문제이다. 정보사회의 꿈을 실현하고자 1993년부터 시작된 In-formation Infrastructure의 구축노력이 그동안 다양하게 시도되어왔으나 숱한 우여곡절과 실패를 겪은 telco등의 서비스업자들이 이제는 너무 큰 꿈을 쫓기보다는 internet이라는 현실적인 시장에서 xDSL과 cablemodem을 바탕으로 차근차근 새로 시작하고 있다고 생각된다. 그동안 ADSL, Forum을 중심으로한 일부 technology evangelist들은 전세계 8억가구에 깔려있는 copper twist pair를 경제적인 'the last mile solution'으로 활용할 것을 줄기차게 주장해왔다. 그동안 xDSL은 VDSL이라는 차세대 대안을 제시하여 interim solution이라는 울타리를 벗어나는데 성공하였을 뿐만 아니라 IDSL, SDSL, RADSL등의 새로운 고객지향적 xDSL을 개발하여 선택의 폭을 넓혀주었다. xDSL vendor들간의 치열한 경쟁속에서 값싼 xDSL 시스템들이 속속 등장하고 있으며, DSLAM[8]과 같은 switch solution도 제시되어 기존의 copper twist pair를 이용해 값싸게 다양한서비스를 제공해 줄 수 있는 기틀을 마련한 것이 오늘날의 xDSL의 성공요인이라고 생각된다. 일찌기 Bell Atlantic의 CEO Ray Smith가 'Yes. ADSL is an interim solution that will be with us for forty years.'라고 간파한대로 xDSL은 fiber가 좀 더 값싼 해결책이 될 때까지 당분간 access network에서 확고한 자리를 구축할 것으로 보인다. 최근들어 우리나라의 초고속정보통신망도 ADSL 과 VDSL을 바탕으로 FTTH으로 진화하는 전략을 수립한것은 우리의 현실과 세계적인 추세를 반영한 일이라 여겨진다.

• Journal of Periodontal and Implant Science
• /
• v.32 no.1
• /
• pp.1-12
• /
• 2002

The periodontal ligament(PDL) is a unique tissue that is crucial for tooth function. However, little is known of the molecular mechanisms controlling PDL function. PDL-specific protein;PDLs22 had been previously identified as a novel protein isolated from cultured human PDL fibroblasts using subtraction hybridization between human gingival fibroblasts and PDL fibroblasts. The aim of this study was to examine the expression pattern and tissue localization of PDLs22 protein in embryonic and various postnatal stages of developing mouse using immunohistochemical staining. Embryos (E18) and postnatal (P1, P4, P5, P15, P18) were decapitated and the heads were fixed overnight in a freshly prepared solution of 4% paraformaldehyde. Some specimens were decalcified for $2{\sim}4$ weeks in a solution containing 10% of the disodium salt of ethylenediamine-tetraacetic acid (EDTA). Next, tissues were dehydrated, embedded in paraffin and sectioned serially at $6{\mu}m$ in thickness. Polyclonal antiserum raised against PDLs22 peptides, ISNKYLVKRQSRD, were made. The localization of PDLs22 in tissues was detected by polyclonal antibody against PDLs22 by means of immunohistochemical staining. The results were as follows; 1. Expression of PDLs22 protein was not detected in the tooth germ of bud and cap stage. 2. At the late bell stage and root formation stage, strong expression of PDLs22 protein was observed in developing tooth follicle, osteoblast-like cells, and subodontoblastic cells in the tooth pulp, but not in gingival fibroblasts, ameloblasts and odontoblasts of tooth germ 3. In erupted tooth, PDLs22 protein was intensely expressed in PDL and osteoblast-like cells of alveolar bone, but not in gingival fibroblasts, mature osteocytes and adjacent salivary glands. 4. In the developing alveolar bone and mid-palatal suture, expression of PDLs22 protein was seen in undifferentiated mesenchymal cells and osteoblast-like cells of developing mid-palatal suture, but not in mature osteocytes and chondrocytes. These results suggest that PDLs22 protein may play an important role in the differentiation of undifferentiated mesenchymal cells in the bone marrow and PDL cells, which can differentiate into multiple cell types including osteoblasts, cementoblasts, and PDL fibroblasts. However, more researches should be performed to gain a better understanding of the exact function of PDLs22 protein which related to the PDL cell differentiation.

• Proceedings of the Mineralogical Society of Korea Conference
• /
• 2003.05a
• /
• pp.66-66
• /
• 2003

King George island, Antarctica, is mostly covered by ice sheet and glaciers, but the land area is focally exposed for several thousand years after deglaciation. For a mineralogical study of chemical weathering in the polar environment, glacial debris was sampled at the well-developed patterned ground which was formed by long periglaclal process. As fresh equivalents, recently exposed tills were sampled at the base of ice cliff of outlet glaciers and at the melting margin of ice cap together with fresh bedrock samples. Fresh tills are mostly composed of quartz, plagioclase, chlorite, and illite, but those derived from hydrothermal alteration zone contain smectite and illite-smectite. In bedrocks, chlorite was the major clay minerals in most samples with minor illite near hydrothermal alteration zone and interstratified chlorite-smectite in some samples. Smectite closely associated with eolian volcanic glass was assigned to alteration in their source region. Blocks with rough surface due to chemical disintegration showed weathering rinds of several millimeter thick. Comparision between inner fresh and outer altered zones did not show notable change in clay mineralogy except dissolution of calcite and some plagioclase. Most significant weathering was observed in the biotite flakes, eolian volcanic glass, sulfides, and carbonates in the debris. Biotite flakes derived from granodiorite were altered to hydrobiotite and vermiculite of yellow brown color. Minor epitactic kaolinite and gibbsite were formed in the cleaved flakes of weathered biotite. Pyrite was replaced by iron oxides. Calcite was congruently dissolved. Volcanic glass of basaltic andesite composition showed alteration rim of several micrometer thick or completely dissolved leaving mesh of plagioclase laths. In the alteration rim, Si, Na, Mg, and Ca were depleted, whereas Al, Ti, and Fe were relatively enriched. Mineralization of lichen and moss debris is of much interest. They are rich of A3 and Si roughly in the ratio of 2:1 to 3:1 typical of allophane. In some case, Fe and Ti are enriched in addition to Al and Si. Transmission electron microscopy of the samples rich of volcanic glass showed abundant amorphous aluminosilicates, which are interpreted as allophane. Chemical weathering in the King George Island is dominated by the leaching of primary phyllosilicates, carbonates, eolian volcanic glass, and minor sulfides. Authigenesls of clay minerals is less active. Absence of a positive evidence of significant authigenic smectite formation suggests that its contribution to the clay mineralogy of marine sediments are doubtful even near the maritime Antarctica undergoing a more rapid and intenser chemical weathering under more humid and milder climate.

• The Korean Journal of Mycology
• /
• v.49 no.1
• /
• pp.57-66
• /
• 2021

Six strains among the shiitake varieties developed by the National Institute of Forest Science were used to select suitable varieties for sawdust block cultivation method. After 100 days cultivation (60 days in dark and 40 days in light), the weight loss rate of the sawdust block media was 14.4% (12.8% to 15.7%) in average. After 5 to 7 days of fruiting process, 2~36 primordia per medium were formed. The number of primordium formation was in the following order: Manchuhyang> Sansanhyang> Sanbaekhyang> Bambithyang> Sangjanghyang> Taehyanggo. The stipe length was 41~59 mm as followed by Taehyanggo (59 mm), Sanbackhyang (56 mm), Bambithyang (54 mm), Manchuhyang (53 mm), Sanjanghyang (45 mm) and Sansanhyang (41 mm). Among the strains, Sansanhyang had short and thick stipe. The average weight of fruiting bodies was 33~77 g as following order of Taehyanggo (77 g), Bambithyang (51 g), Sansanhyang (50 g), Manchuhyang (41 g), Sanjanghyang (34 g) and Sanbackhyang (33 g). Mushroom production per 2 kg medium was the highest in Sanbackhyang (473 g) followed by Bambithyang (287 g), Manchuhyang (175 g), Sansanhyang (109 g), Sanjanghyang (78 g) and Taehyanggo (60 g). The hardness of the cap was 1,218 to 1,839 g/10 mm. Taehyanggo was the hardest (1,839 g/10 mm) and Bambithyang was the softest (1,218 g/10 mm). In conclusion, in the cultivation condition of sawdust block medium, mushroom production was good in Sanbackhyang and Bambithyang. Sansanhyang showed good in terms of fruiting body shape.

• Geophysics and Geophysical Exploration
• /
• v.9 no.1
• /
• pp.30-36
• /
• 2006

Japan's first pilot-scale $CO_2$ sequestration experiment has been conducted in Nagaoka, where 10400 t of $CO_2$ have been injected in an onshore aquifer at a depth of about 1100 m. Among various measurements conducted at the site for monitoring the injected $CO_2$, we conducted time-lapse crosswell seismic tomography between two observation wells to determine the distribution of $CO_2$ in the aquifer by the change of P-wave velocities. This paper reports the results of the crosswell seismic tomography conducted at the site. The crosswell seismic tomography measurements were carried out three times; once before the injection as a baseline survey, and twice during the injection as monitoring surveys. The velocity tomograms resulting from the monitoring surveys were compared to the baseline survey tomogram, and velocity difference tomograms were generated. The velocity difference tomograms showed that velocity had decreased in a part of the aquifer around the injection well, where the injected $CO_2$ was supposed to be distributed. We also found that the area in which velocity had decreased was expanding in the formation up-dip direction, as increasing amounts of $CO_2$ were injected. The maximum velocity reductions observed were 3.0% after 3200 t of $CO_2$ had been injected, and 3.5% after injection of 6200 t of $CO_2$. Although seismic tomography could map the area of velocity decrease due to $CO_2$ injection, we observed some contradictions with the results of time-lapse sonic logging, and with the geological condition of the cap rock. To investigate these contradictions, we conducted numerical experiments simulating the test site. As a result, we found that part of the velocity distribution displayed in the tomograms was affected by artefacts or ghosts caused by the source-receiver geometry for the crosswell tomography in this particular site. The maximum velocity decrease obtained by tomography (3.5%) was much smaller than that observed by sonic logging (more than 20%). The numerical experiment results showed that only 5.5% velocity reduction might be observed, although the model was given a 20% velocity reduction zone. Judging from this result, the actual velocity reduction can be more than 3.5%, the value we obtained from the field data reconstruction. Further studies are needed to obtain more accurate velocity values that are comparable to those obtained by sonic logging.

• Tunnel and Underground Space
• /
• v.32 no.6
• /
• pp.491-501
• /
• 2022

Bentonite has been proposed as a buffer and backfill material for high-level radioactive waste repository. Under such repository environment conditions, bentonite is subjected to combined thermal, hydrological, mechanical, and chemical processes. This study evaluates the feasibility of applying X-ray CT technology on the characterization of bentonite under hydration conditions using a newly developed testing cell. The cylindrical cell is made of platic material, with a removable cap to place the sample, enabling to apply vertical pressure on the sample and to measure swelling pressure. The hydration test was carried out with a sample made of Gyeonju bentonite, with a dry density of 1.4 g/cm³, and a water content of 20%. The sample had a diameter of 27.5 mm and a height of 34 mm. During the test, water was injected at a constant pressure of 0.207 MPa, and lasted for 7 days. After one day of hydration, bentonite swelled and filled out the space inside the cell. Moreover, CT histograms showed how the hydration process induced an initial increase and later progressive decrease on the density of the sample. Detailed profiles of the mean CT value, CT standard deviation, and CT gradient provided more details on the hydration process of the sample and showed how the bottom and top regions exhibited a decrease on density while the middle region showed an increase, especially during the first two days of hydration. Later, the differences in CT values with respect to the initial state decreased, and were small at the end of testing. The formation and later reduction of cracks was also characterized through CT scanning.