• Geomechanics and Engineering
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• 제32권3호
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• pp.347-359
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• 2023

With the development of infrastructure, there is a critical shortage of filling materials all over the word. However, a large amount of silt accumulated in the lower reaches of the Yellow River is treated as waste every year, which will cause environmental pollution and waste of resources. Microbial induced calcium carbonate precipitation (MICP) technology, with the advantage of efficient, economical and environmentally friendly protection, is selected to solidify the abandoned Yellow River silt with poor mechanical properties into high-quality filling material in this paper. Based on unconfined compressive strength (UCS) test, determination of calcium carbonate (CaCO₃) content and scanning electron microscope (SEM) test, the effects of cementation solution concentration, treatment times and relative density on the solidification effect were studied. The results show that the loose silt particles can be effectively solidified together into filling material with excellent mechanical properties through MICP technology. The concentration of cementation solution have a significant impact on the solidification effect, and the reasonable concentration of cementation solution is 1.5 mol/L. With the increase of treatment times, the pores in the soil are filled with CaCO₃, and the UCS of the specimens after 10 times of treatment can reach 2.5 MPa with a relatively high CaCO₃ content of 26%. With the improvement of treatment degree, the influence of relative density on the UCS increases gradually. Microscopic analysis revealed that after MICP reinforcement, CaCO₃ adhered to the surface of soil particles and cemented with each other to form a dense structure.

• 한국토양환경학회지
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• 제4권2호
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• pp.3-10
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• 1999

The unknown amount of thiolane retained on different soil matrix was characterized by employing an uniquely designed glass vessel, which was forced to purge the prepared slurry sample so that thiolane may diffuse into Tenax/charcoal tube. Thiolane can be recovered ranging from approximately 89 % at 1 ppm regardless of soil types, which was not consequently affected by potential biodegradation during sample preparation. For 5 ppm. thiolane is more recoverable up to 92 % for sand, whereas it was poorly recovered as low as 85 % for clay. It strongly suggests that controls should be considered when soil types varied in a concerned area. The technique was eventually capable of determination of thiolane for the samples taken from the site which led to be taken into consideration for proper site remediation.

• 원예과학기술지
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• 제17권2호
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• pp.148-152
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• 1999

본 연구는 단풍색이 황색인 느티나무 신품종을 육성하기 위해, 선발된 개체들의 생육특성 및 단풍시기, 엽내 안토시아닌 및 엽록소 함량 등의 생리적 특성을 구명하고 접목에 의한 단풍색의 접목후대 특성을 조사하고자 실시하였다. 황색 단풍이 드는 계통으로 선발된 'S-4'는 수령 28년생으로 수고 7m, 수관폭은 6m였으며, 엽내 안토시아닌의 함량이 다른 개체들에 비해 높고 단풍이 아름답고 단풍기간이 긴 것으로 나타났다. 또한 'S-14'와 'S-32' 역시 엽내 안토시아닌의 함량이 다른 개체들에 비해 높고 단풍이 황색으로 아름답고 단풍기간이 긴 것으로 나타났다. 선발된 개체들의 접목묘들 공히 모두 엽내 안토시아닌의 함량이 높고 단풍색이 황색으로 나타나 모본의 형질이 접목 후대에 유전되는 것을 알 수 있었다. 본 연구에서 선발된 개체들은 접목을 통해 번식시킨 후 조경용 소재로 보급할 수 있을 것으로 판단되었다.

• 한국대기환경학회지
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• 제18권4호
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• pp.317-325
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• 2002

An air pollution monitoring station has been operated at Tokchok Island since April 1999 to characterize the background atmosphere in the vicinity of the Yellow Sea. In this study, eight chemical species in PM$_{2.5}$ and three gaseous species were analyzed. A total of 53 samples were collected for the analysis of PM$_{2.5}$ and gaseous species from April, 1999 to April, 2001. The overall mean mass concentration of PM$_{2.5}$ was 20.8 $\mu\textrm{g}$/㎥ and the eight soluble ionic species accounted for about 46.8% of PM$_{2.5}$ mass. Approximately 80% of samples appeared to experience the chloride loss effect. Air pollutant sources of PM$_{2.5}$ measured at Tokchok Island were qualitatively identified by the principal component analysis. It was found that five principal components are secondary aerosol, soil, incineration, phase change of nitrate, and ocean.and ocean.

• 보존과학회지
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• 제38권4호
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• pp.327-333
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• 2022

Sri Lanka has four types of mural painting styles; Classic, Late Classic, Kandyan, and Southern styles, but there is little research on scientific analysis for mural paintings. In this study, we analyze white, yellow, and red clay pigments which were collected from ancient producing sites. Analyzing pigment samples shows that samples are containing aluminum oxide(Al₂O₃) and silicon dioxide(SiO₂) which are connected to the soil. And a degree of iron oxidation determines yellow or red colors. To understand the characteristics of clay pigment samples, we go over previous pigment analyses of mural paintings in Sri Lanka. Kaolin is identified after the 17^th century, yellow and red ochre are applied in early periods, Classic and Late Classic styles. The change in raw materials of pigments occurred in the 17^th century.

• 한국응용곤충학회지
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• 제25권1호
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• pp.47-51
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• 1986

유용자원(有用資源) 확보(確保)와 농업용(農業用) 항생물질(抗生物質) 탐색(探索)을 위(爲)한 기초자료(基礎資料)를 얻기 위해 전국(全國)에서 채집(採集)한 토양(土壤) 200점(點)에 대(對)해 방선균중(放線菌中) Streptomyces속(屬) 균주(菌株)의 분포(分布)를 조사(調査)한 결과(結果), 1. 지대별(地帶別) 균분포(菌分布)는 밭과 임야(林野)에서 비슷한 분포(分布) 를 나타내었으나 밭에서는 $5.6{\times}10^5\;colonies/g$ 으로 임야(林野)보다 더 많이 분포(分布)되어 있었고 논에서는 $2.2{\times}10^5\;colonies/g$ 으로 가장 적게 분포(分布)되어 있었다. 2. 토양(土壤) 심도별(深度別) 균주분포(菌株分布)에서는 토양(土壤) 표면(表面)에서 $1.05{\times}10^6\;colonies/g$ 으로 가장 많이 분포(分布)되어 있었고 대체로 5cm 이내에 많은 분포(分布)를 보였으며 5cm 이하(以下)에서는 심도별(深度別)로 감소(減少)하는 경향(傾向)이었다. 3. 토색(土色)에 따른 균주(菌株) 분포(分布)에서는 채취토양(採取土壤)의 색(色)이 olive yellow 토양(土壤)에서 $9.2{\times}10^5\;colonies/g$ 으로 가장 많이 분리(分離)되었다. 4. 토양(土壤) 산도별(酸度別) 균주(菌株) 분포(分布)에서는 pH 7.5 에서 $1.05{\times}10^6\;colonies/g$ 으로 가장 많은 분포(分布)를 보였다. 5. 분리(分離)한 균주(菌株)를 균총색(菌叢色)으로 분류(分類)한 결과(結果)는 회색계통(灰色系統)이 60%, 백색계통(白色系統)이 26% 를 차지하였다.

• 아시안잔디학회지
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• 제6권2호
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• pp.113-119
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• 1992

전국 70개 골프 코스의 토양통을 정밀토양토에서 판독하여 토양특성을 해석한 결과, 골프장의 토양통 수는 17개이고 대토양군(구분류)은 6매, 대군(신분류)은 8개였다. 대토양군은 적황색토에 50%의 골프코스가 분포하고 암쇄토에는 44%가 분포되었다. 대군은 Dystrochrepts에 74% Eutrochrepts에 8.6% Hapludults에 7.1%가 분포되었다. 주요 토양통은 오산(27.1%), 삼각(18.6%), 예산(11.4%) 송산(8.6%), 대구(7.1%)의 순이었다. 골프장 토양통 17개의 간략한 설명과 5매 주요 토양통과, 주요 대토양군과 대군에 대한 상세한 설명을 제시하여 골프 코스 관리에 참고토록 하였다.

• 한국대기환경학회지
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• 제12권2호
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• pp.167-177
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• 1996

To investigate the source-receptor relationships aerosol model has been used to simulate the distribution behavior of the yellow sand. Data for meteorological fields were obtained by Meso-scale Analysis and Prediction Model System/Seoul National University (MAPMS/SNU) for five days (10-14 April 1988). To obtain the distributions of concentration of yellow sand,the aerosol model has been modified to allow quantifications of relative concentration distributions of yellow sand. Source regions of yellow sand were delineated by soil maps of China and emission rate as a function of wind stress(Westphal et al., 1987). Using 3-dimensional wind fields the backward trajectories from 3 receptor grids at the layer of .sigma. =0.95, 0.9, 0.85, 0.8 were calculated. In order to facilitate quantitative assessment of source-receptor relationships, it was assumed that the perturbations in along-trajectory and cross-trajectory proceed linearly with time, in accord with Gaussian distribution characteristics. On the basis of this assumption, the probability fields were calculated from every grid point with source strength 1. Using these probability fields and emission retes, the potential contributions of upstream sources along the trajectories were estimated. The results of this study indicate that the application of trajectory modeling is useful in investigating the quantitative relationship between source and receptor regions.

• 한국산림과학회지
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• 제47권1호
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• pp.52-61
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• 1980

본(本) 연구(硏究)는 한국삼림토양(韓國森林土壤)의 특성(特性)을 비악(把握)하여 그 합리적(合理的) 이용(利用) 및 관리방법(管理方法)을 제공하기 위하여 실시되었다. 현재(現在)까지 조사발표(調査發表)된 토양(土壤)의 종류(種類)는 178개(個) 토양통(土壤統)으로 그중 64개(個) 토양통(土壤統)이 삼림토양(森林土壤)이다. 삼림토양(森林土壤)은 그 풍화모재(風化母材)의 종류(種類)에 따라 산악잔적토(山岳殘積土), 구릉잔적토(丘陵殘積土), 곡간붕적토(谷間崩積土), 충적토(沖積土) 및 화산회토(火山灰土)로 구분(區分)하여 분석(分析)하였다. 본(本) 논문(論文)에서는 토양(土壤)의 분류학적(分類學的) 특성(特性)과 모암(母岩), 토성(土性) 및 배수상태(排水狀態)를 다루고 있다. 기타 물리적(物理的), 화학적(化學的) 특성(特性)은 다음 논문(論文)에서 서술될 예정이다. 분류(分類)된 한국삼림토양(韓國森林土壤)의 특징(特徵)은 다음과 같다. 1. 산악잔적토(山岳殘積土)(29개통(個統))는 대부분(大部分) Lithosols로서 토양단면(土壤斷面)의 층위분화(層位分化)가 발달(發達)하지 못하였고 토성(土性)은 석력(石礫)이 있는 양토(壤土)가 가장 많고 점질(粘質)로 갈수록 토양통수(土壤統數)가 감소하며 배수상태(排水狀態)는 과도(過度)하다. 2. 구릉잔적토(丘陵殘積土)(19개통(個統))는 대부분(大部分) Red-yellow Podzolic Soils로서 단면(斷面)이 잘 발달(發達)되어 있고 토성(土性)은 주 로 양토(壤土)와 식토(埴土)로 되어 있으며 토양배수(土壤排水)는 양호(良好)하다. 3. 곡간붕적토(谷間崩積土)(13개통(個統))는 주로 Regosols로서 단면발달(斷面發達)이 미약하나 일부 층위분화(層位分化)가 이루어진 Red-Yellow Podzolic Soils와 Acid Brown Forst Soils 가 있다. 토성(土性)은 다양(多樣)하나 조립질(粗粒質)인 경향(傾向)이 있고 배수(排水)는 양호(良好)하다. 4. 각종모암(各種母岩)의 풍화산물(風化産物)의 토성(土性)을 보면 다음과 같다. 1) 조립질토성(粗粒質土性)을 생산(生産)하는 모암(母岩)들로는 유문암(流紋岩), 화강편마암(花崗片麻巖), 편암(片岩), 혈암(頁岩), 사암(砂岩), 역암(礫岩) 등(等)이 있다. 2) 미립질토성(微拉質土性)을 생산(生産)하는 모암(母岩)들로는 석회암(石灰岩), 현무암(玄武岩), 반려(斑糲岩) 및 안산반암(安山斑岩)이 있다. 3) 여러가지 토성(土性)을 다양(多樣)하게 생산(生産)하는 모암(母岩)으로는 화강암(花崗岩)이 있다.

• 한국환경복원기술학회지
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• 제12권5호
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• pp.110-120
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• 2009

The hipped roof on the research building, which was constructed 51.9m above sea level on a hillock by Korea National University of Education in June 1999, is composed of four inclined planes which are 12m in breadth, 8m in length and have a 30 degree gradient. For the roof vegetation, the yellow earth collected from around the building was laid on top. It was designed to supply the soil on the slope with water for a considerable period by making rainfall pool at the edges. In order to prevent the soil on the slope from being swept away, 31 sorts of grass seeds were imported from Germany and sown in the soil. At the present day, 10 years after the seeds began to sprout and inhabit the settled slope, 30 individual plant species were identified in the period between April 2008 and March 2009. Out of 31 species were seeded on the slanted, soiled roof, only 8 were still alive. It was confirmed that the Artemisia Princeps var, Chrysantheum, Prunella Vulgaris and Lespedeza Cuneata have been the major species inhabiting the east, west, south and north inclined planes respectively. The Phragmites Communis was inhabiting the edge of the roof where the water supply was adequate, while the Dianthus Barbatus was primarily inhabiting the south-east side of the roof. As a whole, 26 identifiable plants and 4 unidentified plants were observed on the inclined planes of the hipped roof. In consideration of the plant distribution on the slope, it was confirmed that the selection of seeds may have had an effect on the slope vegetation. As for the yellow earth laid on the roof, it was discovered that about 2~3cm thickness around the ridge was swept away, but the rest of the slope was in relatively good condition. Accordingly, it has been proven that vegetations can be applied to hipped roofs by using ordinary plants without any special structural measures.