• Journal of the korean society of oceanography
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• 제39권1호
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• pp.57-71
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• 2004

Based on the data obtained under the China-Korea joint project (1997-2001) and historic observations, the distribution, transportation and sedimentation of sediment in the southern Yellow Sea (SYS) are discussed, and the controversial formation mechanism of muddy sediments is also explored. The sediment transport trend analysis indicates that the net transport direction of sediment in the central SYS (a fine-grained sediment deposited area) points to $123.4^{\circ}E,\;35.1^{\circ}N$, which is a possible sedimentation center in the central SYS. The sediment transport pattern is verified by the distribution of total suspended matter (TSM) concentration and ${\delta}^{13}C$ values of particulate organic carbon (POC), the latter indicates that the bottom water plays a more important role than the surface water in transporting the terrigenous material to the central deep-water area of the SYS, and the Yellow Sea circulation is an important control factor for the sediment transport pattern in the SYS. The carbon isotope signals of organic matter in sediments indicate that the Shandong subaqueous delta has high sedimentation rate and the deposited sediments originate mainly from the modern Yellow River. The terrigenous sediments in deep-water area of the SYS originate mainly from the old Yellow River and the modern Yellow River, and only a small portion originates from the modern Yangtze River. The analytical results of TSM and stable carbon isotopes are further confirmed by another independent tracer of sediment source, polycyclic aromatic hydrocarbons (PAHs). Five light mineral provinces in the SYS can be identified and they indicate inhomogeneity in sources and sedimentary environment. The modern shelf sedimentary processes in the SYS are controlled by shelf dynamic factors. The muddy depositional systems are produced in the shelf low-energy environments, which are controlled by some meso-scale cyclonic eddies (cold eddies) in the central SYS and the area southwest of the Cheju Island. On the contrary, an anticyclonic muddy depositional system (warm eddy sediment) appears in the southeast of the SYS (the area northwest of the Cheju Island). In this study, we give the cyclonic and anticyclonic eddy sedimentation patterns.

• 한국문헌정보학회지
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• 제29권
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• pp.345-382
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• 1995

The type printing of first Ch'ing dynasty term in China is worthy to be studied because the type printing during that period included metal type, wood type, and clay type as well as the development phase was similar to Chosun dynasty culturally and technologically. This paper studied typography during the first Ch'ing dynasty term, including Shunzhi(1662-1722), Yongaheng(1723-1735), Qianlong(1736-1795), Jiaqing(1796­1820) period. The main results of the study is as follows. 1. The main body of type printing was bookstore, lecture-hall, and individual as well as the royal court that is the central government. 2. The content of type edition covers classics, history, philosophy, and literary works. Specifically, even though Wuyingdienjuzhenban series is excluded, the content includs study of the classics, class of the history, class of the philosophy, literature works that include collection works and novel and government official bulletin. 3. The printing technique of bronze type was very popular In Beijing. Jiangsu, and Taiwan. It's scale and production technique was more elaborate than in Ming dynasty. 4. Wood type was very popular in Beijing, Jiangsu, Zhejiang, Anhui, Sichuan, and Fujian. In addition to wood type, chinese ware type was applied to book printing in Shandong. However, most of them were wood type and they were used after Qianlong period. 5. The production technique of type was skilled enough to present the fine view of a style of type. The typesetting technique was improved as much as woodblock printing. With regard to the making technology of Chinese ink, the light and darkness of chinese ink was not even sometimes. But, the technology was improved significantly when comparing with the failure experience of printing that chinese ink was not developed in early type invention. 6. In case that the book was printed in bookstore with the intention of profit and the number of book was large, the proofreading attitude was rough. However, overally, it was made correction carefully applying the various methods of proofreading. 7. The support of government made a great contribution in the area of all printing technology, including production, typesetting, and brushing of type.

• 대한지역사회영양학회지
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• 제22권1호
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• pp.63-73
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• 2017

Objectives: This study was conducted to survey the related factors of metabolic syndrome of Chinese workers aged 20 years and above. Methods: The study was conducted at three locations in Shandong, China, currently working and took the physical examination (PE) within one year in the area as target participants. Personal characteristics, physical and biochemical results based on the PE, lifestyle habits, and food intake of the participants were used to analyze the relationship with metabolic syndrome. Results: Results showed that overall, thirty-one subjects (22.5%) had metabolic syndrome, twenty males (32.7%) and eleven females (14.2%). Metabolic syndrome was related to age, gender, educational level and occupational type with more risk in male (P < 0.05), people of older age (P < 0.001), low educational level (P < 0.05) and non-office workers (P < 0.01). According to the life style scores, lifestyle evaluation showed specifically alcohol consumption and smoking (P < 0.001) and stress management (P < 0.05) as important factors that were associated with the metabolic syndrome. High calorie (P < 0.01) and carbohydrate (P < 0.01) intakes were observed on male participants with metabolic syndrome in comparison to the non-metabolic syndrome but no significant difference on female participants. Conclusions: This results of this study can be used as significant supporting data to prevent and control metabolic syndrome in Chinese workers.

• 한국제4기학회지
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• 제16권1호
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• pp.1-16
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• 2002

황해 중앙부 해역에 분포하는 니토대의 공급지와 퇴적작용을 파악할 목적으로 이곳 니질 퇴적물에서 채취한 4개의 시료에서 분석한 화학조성과 기존의 황하, 양자강 및 한반도의 금강 퇴적물 등의 지화학적 자료와 비교하고 퇴적률을 추정하였다. 연구지역 표층 퇴적상의 분포는 사질 퇴적상이 분포하는 동쪽지역, 니토대가 분포하는 서쪽지역, 중앙부지역에 남북방향의 대상분포를 보이는 혼합 퇴적상으로 구분된다. 퇴적물내 탄산염 함량은 2.B~10.5%의 범위를 보이고 사질 퇴적물이 분포하는 동쪽보다 니질 퇴적물이 분포하는 서쪽으로 갈수록 점차 증가하는 경향을 보인다 Pb-210 동위원소를 이용한 연구지역 니질 퇴적물의 퇴적률은 0.21~0.68cm/yr 혹은 0.176~0.714 g/$\textrm{cm}^2$.yr의 범위를 보였다. 황하와 가까운 산둥반도 동쪽 정점 CY96010에서 퇴적률은 0.68cm/yr 혹은 0.714g/$\textrm{cm}^2$. yr의 높은 값을 보이고, 황해 중앙부 해역 정점 CY96008과 CY96002에서 퇴적률은 0.21~0.23cm/yr혹은 0.176~0.220g/$\textrm{cm}^2$. yr로 낮은 값을 보여 황하기원 퇴적물이 황해 중앙부 해역까지 이동되어 퇴적되고 있음을 의미한다. 황해 중앙부 해역 니질 퇴적물의 화학조성 중 Ca, Na, Sr, Ho, La, Tb 및 Ta원소함량과 Ca/Ti비는 양자강 퇴적물보다는 높고, 황하보다는 낮거나 이와 비슷한 함량 변화 경향을 보였고, Fe, Ti, Ni, Co, Cr, Cu, Pb, Sc, Ce, Nd, Sm, Eu, Gd 및 Dy 원소함량은 황하 퇴적물 보다는 높고, 양자강보다는 낮으나 이와 비슷한 함량변화를 보였다. 반면, Mn, K 및 Sr 원소는 금강과 황해 동쪽의 퇴적물보다는 낮으나 이와 비슷한 함유량을 보였고, Zn, Rb, Cd, U, Cs 및 Li 원소는 비교지역 보다 높은 함량치를 보였다. 따라서 황해 중앙부 해역에 분포하는 니질 퇴적물의 공급지는 황하 및 고황하기원 물질이고, 이외에 양자강과 금강으로부터 공급된 물질과 황해 난류수에 의해 운반된 생물기원 물질의 영향도 다소 있는 것으로 해석된다.