• KOMUNHWA
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• no.70
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• pp.5-15
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• 2007

Octagonal green glass bottle with long neck(녹유리장경각병) was found in the tomb of the princess Hwayu who was King Youngjo's daughter by a concubine while the tomb was exhumed and buried in another place around Bucheon City, Gyeonggi-do. This octagonal glass bottle is dark green. It was made in AD 1736-A1795 because it was cngraved an inscription of "건륭년제" the bottom. This glass bottle was taken an X-ray radiography and tested adhesives and restoration materials for the conservation. Loctite 401 was suitable as considering the translucency of the glass bottle, good adhesive property and reversibility of the adhesive so it was chosen. A minute piece of the glass was analyzed the composition and lead isotope ratio. Major chemical composition of the glass bottle consisted of SiO2, K2O, and PbO system and the ratio was 68: 18.5:5.7. Green color of glass bottle was due to Fe2O3 and CuO. When the glass bottle was made, quartz as raw material of silica and K2O as natural saltpeter(KNO3) were utilized. As a result of lead isotope ratio analysis, it was suggested that the galena as raw material of lead for glass making came from the southern part of China. These results are expected to become useful data in background of glass culture and circulation study of old glass.

• Journal of the Geological Society of Korea
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• v.54 no.5
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• pp.567-578
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• 2018

A nondestructive petrological investigation was carried out to identify the original location and form of the Gyeongju Seated Stone Buddha with Square Pedestals in the Blue House (so-called Stone Buddha in the Blue House). The Statue is a representative stone Buddha statue of Silla (9th century) but its original location is controversial and some parts were missing. Based on the petrological observation, magnetic susceptibility and gamma spectrometry, its stone material was identified as medium-grained alkali feldspar granite. This kind of granites are widely found in the Namsan, Gyeongju. It is very likely that the Namsan granites are the source of rock of the Stone Buddha. The Yudeoksa (Igeosaji temple site) and Namsan are possible to be the original home of the Buddha Statue since there are petrologically identical alkali feldspar granite outcrop distributed in Namsan and stone heritage made of the same stone type in both places. An investigation on the square middle stone base in the Chuncheon National Museum reveals that it is less likely to be the missing part of the Buddha statue as the stone base is fine- to medium-grained pink feldspar granite and has different magnetic susceptibility from the Buddha statue. This study confirmed the contribution and significance of petrological investigation to identification of stone heritage in Korea.

• Korean Journal of Heritage: History & Science
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• v.37
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• pp.349-369
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• 2004

Today, in the cultural properties research, there are several methods for knowing the culture of the past through a lot of information that remains and relics contain. Especially, statistical method like presumption of producing center were introduced from computer development at the early 20th century. This study showed the characteristic about firing historic sites presumed as a tile-kiln in the remains of Cheonwang temple sites, Hanam, Gyeonggi province. Also, I used nature scientific methods for correlation between tiles excavated at historic sites and circumference building and obtained there results as follows. First, soft tile parts showed similar water suction ratio(over 10%) like another tiles, except hard tile parts. Second, identification about mineral crystallization in a sample showing low water suction ratio confirmed a result that Mullite, Tridymite, Cristobalite as high temperature crystal form were presented. I know that firing temperature was higher than the other tile parts from this result. Third, statistical analysis from micro-component resulted that tiles excavated at firing historic sites and Cheonwang temple sites were closely connected. As the results, I knew that the tiles got a supply after the establishment of tile-kiln, not at a long distance at the period of Cheonwang temple construction.

• Economic and Environmental Geology
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• v.57 no.3
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• pp.343-352
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• 2024

Composition analysis and lead isotope ratio analysis were conducted to determine the coloring machanism on lead glaze used in Gyeongbokgung Palace and the provenance of the lead used as a flux. 31 blue tiles were classified into green, blue, and yellow. The chemical analysis of lead glazes on the blue tiles revealed that Pb, Si, and Cu were the main components, and trace amounts of Fe, Ca, Mg, and Al were detected. The Cu content was high in blue lead glaze, while Cu was not detected in yellow or brown lead glaze which instead had high Fe content. Therefore, it was found that lead was used as a flux and copper oxide as a coloring agent in the production of lead glaze. In addition, the lead isotope ratios of the lead glaze used in the blue tiles of Gyeongbokgung palace were plotted in zone 3 on the distribution map of lead isotope ratios on the Korean Peninsula, which includes Chungcheong-do and Jeolla-do. It is presumed that the flux for the lead glaze was sourced from galena found in these regions. The lead isotope ratios of the green glaze from the Three Kingdoms and Unified Silla period were mostly located outside the Korean Peninsula, showing that the provenance of lead had changed. In particular, the lead isotope ratios of the green glaze from the Three Kingdoms and Unified Silla period suggest exchange with neighboring countries. Also the lead isotope ratios of the green glazes from the same temple are different, so it is believed that they were made at different times or in different workshops.

• KOMUNHWA
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• no.60
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• pp.101-120
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• 2002

The floor tile on a coated green-glass was excavated from the Beobgwangsa Temple Site in the Pohang City. We analyzed using the MXRD, ICP-AES, EDXRF, TG/DTA and TIMS. As a result of microscope analysis, it was composed of quartz, feldspar and clay particl

• Journal of Korea Water Resources Association
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• v.41 no.6
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• pp.565-574
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• 2008

Fire-enhanced soil hydrophobicity often increases runoff and erosion in the mountain hillslope following severe wildfires. Estimation techniques for WEPP's parameters were studied in burnt mountain slopes. In burnt mountain slopes, the model over-predicted runoff in the small runoff and under-predicted runoff in the great runoff, and in the lower sediment runoff it had a tendency to over-predict soil loss. The effective hydraulic conductivity was most sensitive in the WEPP's runoff and its sediment runoff was mainly effected by the effective hydraulic conductivity, initial saturation, rill erodibility, and interrill erodibility. To improve the applicability of the WEPP, the adjustment coefficient of effective hydraulic conductivity was defined for runoff and the adjustment coefficient of rill erodibility and interrill erodibility was presented for sediment runoff. The adjustment coefficient of effective hydraulic conductivity in wildfire mountain slopes increased with maximum rainfall intensity of single storm and the vegetation height index. The adjustment coefficients of rill erodibility depended on soil components of size distribution curve and total rainfall depths in single storm. The adjustment coefficients of interrill erodibility decreased with increases of maximum rainfall intensity and vegetation height index. These results may be used in the application of WEPP model for wildfire mountain slopes.

• The Korean Journal of Zoology
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• v.23 no.4
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• pp.251-262
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• 1980

Two Neanurid species of Collembola, Lobella minuta n. sp., and Morulina triverrucosa Tanaka, 1978 were identified from collections of South-Western part of Korea. They were, in addition, confirmed to be genera of new record to the country. From their common structure of simple mouth parts it was postulated that they may have both hypertrophy and polytene development of salivary glands in the light of early evidences by Cassagnau. These assumptions were tested for the above two Korean species using cytological and histological techniques. The results of the investigations have proved to be positive for the postulations, thus supporting hypothetical correlations of simple mouth parts with polytene development, irrespective of taxa, not limited to Neanurini as indicated in early works. However the structurization of the polytene chromosomes was shown of different extent between the two, i.e., in Lobella minuta, clearly more differentiated than in Morulina triverrucosa in spite of the strong similarity of mouth parts, which are to be seen as a distinct convergence from two tribes, Neanurini and Morulini. It remains to be studied consequently to know whether there as any factor other than mouth part structure affecting polytene development and also if the parallelism among a few different taxa of mouth parts would be the case with polytene development of salivary glands either.

• Economic and Environmental Geology
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• v.43 no.6
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• pp.543-553
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• 2010

This study was focused on the mineralogical and geochemical characteristics of field soil of the Baekje Kingdom from K wongbawigol site in Jeongdongri, Buyeo and whether the bricks from Songsanri Tombs and Muryung's Royal Tomb were made of soil from this site. Soil samples show the similar size fraction as a silt loam and acidic soil, whereas some samples have the enrichment of organic matter, P and S. Also, they have similar geochemical behavior of elements and similar mineral phases consisting of quartz, plagioclase, orthoclase, vermiculite, mica and kaolinite. The enrichment of iron oxide is found in some soil layer, including the iron oxide mottling and precipitation along plant roots and they are attributed to repeat oxidation and reduction environments due to flooding and drainage of field soil. It's anthropogenic alteration by human activity. Especially, it is assumed that the concentration of the iron oxides found in bricks from Muryung's Royal Tomb and Songsanri Tombs is the additional evidence that soil in this study is probably the raw materials of those bricks.

• Proceedings of the Korea Water Resources Association Conference
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• 2012.05a
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• pp.816-816
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• 2012

최근 우리나라는 기후변화와 이상기후 현상 등의 영향으로 홍수에 대한 위험이 커지고 있다. 홍수에 의해 발생하는 인명 및 재산피해를 최소화하기 위해서는 구조적 및 비구조적 대책 등을 통한 치수정책 수립이 필요하며, 대표적인 비구조적 대책으로는 홍수위험지도(flood hazard map) 제작 등이 있다. 홍수위험지도는 홍수시 침수범위, 침수심 등의 정보를 지도상에 표시하고 있으므로 홍수피해가 발생가능한 공간적 범위를 나타내는 것이다. 홍수위험지도는 침수정보 뿐만 아니라 대피로, 대피처 등 홍수시 피난정보도 함께 나타낼 수 있으므로 홍수발생시 인명 피해를 최소화하기 위하여 활용될 수 있다. 또한 홍수피해 예상범위를 미리 추정할 수 있으므로 피해가능 지역의 특성을 고려하여 구조적 치수계획 수립의 적절한 기준을 제시할 수 있다. 즉, 침수 가능지구 내의 사회적, 경제적, 문화적 중요도를 평가함으로써 지역 특성을 고려한 선택적 홍수방어에 활용될 수 있는 것이다. 본 연구에서는 이러한 중요도 중 홍수피해 예상인구에 대한 현실적인 계산 방법을 제안하고자 한다. 홍수가 발생하여 침수가 예상되는 지역에서 사람이 실제 거주하는 면적을 고려하는 방법은 토지등기부의 지목을 활용하는 것이다. 토지지목은 토지의 종류를 사용목적에 따라 구분한 명칭이며,"측량, 수로조사 및 지적에 관한 법률" 제67조에서 전 답 과수원 목장용지 임야 광천지 염전 대(垈) 공장용지 학교용지 주차장 주유소용지 창고용지 도로 철도용지 제방(堤防) 하천 구거(溝渠) 유지(溜池) 양어장 수도용지 공원 체육용지 유원지 종교용지 사적지 묘지 잡종지 등 28가지 항목으로 구분된다. 여기서 대(垈) 지목은 영구적 건축물 중 주거 사무실 등의 부지를 의미하므로 상주인구가 거주하는 지역으로 가정할 수 있다. 침수가 예상되는 지역에서 대(垈) 지목의 면적을 고려하여 계산된 인구수와 단순 면적비로 계산된 인구수를 비교한 결과, 도시화의 비율이 높은 지역일수록 단순 면적비에 비해 인구수가 높게 계산되었고, 농경지 및 산지가 발달된 지역일수록 단순 면적비에 비해 인구수가 낮게 계산되었다. 따라서 침수가 예상되는 지역의 인구수를 예측할 경우 토지지목 중 대(垈) 지목의 면적을 고려하여 계산하는 것이 보다 합리적인 홍수피해 예상인구를 계산하는 방법으로 판단된다.

• Proceedings of the Korea Water Resources Association Conference
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• 2021.06a
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• pp.235-235
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• 2021

아시아 몬순기후의 영향에 의해 우리나라는 2020년 7월부터 9월까지 약 90일간의 장마로 인해 크고 작은 수재해가 발생하였다. 특히, 안성, 충주, 음성 그리고 곡성 등에서 인명피해가 발생하였으며, 그 외 13개소에서 많은 재산 피해가 발생하였다. 2020년 산사태/토석류 재해로 인한 전국적인 피해액은 약 3,900억으로 보고되고 있으며, 매년 집중호우에 의해 피해 양상이 변하고, 도시지역에서의 발생이 빈번하게 늘고 있다. 집중호우에 의한 산사태/토석류 전이 피해를 저감시키기 위해서는 발생 물질이 어디까지 이동할 수 있는지에 대한 위험범위확산에 대한 연구가 중요하며, 이런 연구를 기반으로 인명피해를 줄이기 위한 연구가 필요하다. 이를 위해 본 연구에서는 천수방정식, 유변학특성 식 그리고 연행침식 식을 조합하여 개발된 적응형 격자기반 2차원 토석류 모델을 이용하여 안성, 음성 그리고 단성지역에서 발생했었던 산사태/토석류 전이 피해 양상을 해석하였다. 산사태 발생 후 2~3일 이내에 지표 지질 및 지형 조사를 실시하였으며, UAV 및 항공사진을 이용하여 산사태 및 토석류의 형태를 맵핑하였다. 지질 및 지형조사 시 간이 Vein tester를 이용하여 야외에서 토양 물성관련 자료를 취득하였으며, 토석류의 이동 흔적(나무 등에의 토석류 타격 흔적)을 이용하여 조사지점에서의 최대 토석류 흐름 깊이를 추정하였다. 정확한 토석류의 유속에 대한 자료 부족으로 2011년 우면산에서 발생한 약 26m/s의 속도를 이용하여 토석류의 흐름 특성을 계산하였다. 이와 더불어 연행침식의 계산을 위해 발생지점 부터 토석류가 퇴적된 하류부까지 기반암의 노출 및 퇴적 정보를 통해 최대 침식 깊이를 추정하여 입력자료로 활용하였다. 토석류 맵핑자료와 비교 결과 정확도가 90%이상으로 나타났으며, 토석류 발생 후 안성 200초, 음성 180초 그리고 단성 180초 이내로 토석류가 하류까지 이동할 수 있는 것으로 계산되었다. 본 연구와 같이 산사태/토석류 발생 메커니즘 해석에 대한 지속적인 연구를 통해 산지 재해에 의한 인명 피해를 줄일 수 있는 토석류확산범위 해석에 대한 연구가 지속적으로 필요할 것으로 판단된다.