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International Journal of Sediment Research 2011年第1期26卷 1-14页

The suspended sediment flux field in the Yellow and East China Seas(YECS) displays its seasonal variability.A new method is introduced in this paper to obtain the flux field via retrieval of ocean color remote sensing data,statistical analysis of historical suspended sediment concentration data,and numerical simulation of three-dimensional(3D) flow *** components of the sediment flux field include(i) surface suspended sediment concentration inverted from ocean color remote sensing data;(ii) vertical distribution of suspended sediment concentration obtained by statistical analysis of historical observation data;and(iii) 3D flow field modeled by a numerical *** the improved method,the 3D suspended sediment flux field in the YECS has been *** comparison with the suspended sediment flux field solely based on the numerical simulation of a suspended sediment transport model,the suspended sediment flux field obtained by the improved method is found to be more *** 3D suspended sediment flux field from ocean colour remote sensing and in situ observation are more closer to the ***,by quantitatively analyzing the newly obtained suspended sediment flux field,the quantity of sediment erosion and deposition within the different regions can be *** sediment exchange between the Yellow Sea and the East China Sea can be *** mechanism of suspended sediment transport in the YECS can be better *** particular,it is suggested that the long-term transport of suspended sediment is controlled mainly by the circulation pattern,especially the current in winter.

关键词： Suspended sediment flux field Seasonal variability Yellow and East China Seas Regression equation Numerical simulation

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山东青岛中德生态园绿色公元被动房项目

建筑实践 2024年第3期 160-167页

作者： qingdao Public Architectural Design institute Co., Ltd. 青岛市公用建筑设计研究院有限公司

中德生态园被动房推广住宅示范小区—“绿色公元”,定位成为中国被动房居住建筑大面积推广的典型示范。项目位于青岛市中德生态园C-2-06地块,为居住类项目,包含别墅及多层洋房等多类产品,同时配建社区服务中心及配套商业服务网点。总建...

中德生态园被动房推广住宅示范小区—“绿色公元”,定位成为中国被动房居住建筑大面积推广的典型示范。项目位于青岛市中德生态园C-2-06地块,为居住类项目,包含别墅及多层洋房等多类产品,同时配建社区服务中心及配套商业服务网点。总建筑面积70,226.28 m2,其中地上建筑面积4.,937.4.m2。项目于2019年10月完工交付。

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中国科学院青岛生物能源与过程研究所2023年度“十大工作进展”

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高科技与产业化 2024年第9期30卷 20-23页

作者： qingdao institute of Bioenergy and Process, Chinese Academy of Sciences 中国科学院青岛生物能源与过程研究所

2023年,中国科学院青岛生物能源与过程研究所驰骋奋发、勇毅前行,紧紧围绕“四个率先”和“两加快一努力”的目标要求,进一步强化国家战略科技力量主力军使命担当,共同绘就了研究所繁荣发展的辉煌历程,各项事业取得可喜进展。

关键词：中国科学院生物能源工作进展使命担当研究所主力军辉煌历程青岛

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CALLI ASTER QUADRISPINUS, A NEW SPECIES OF THE FAMILY GONIASTERIDAE (ASTEROIDEA) FROM SOUTHERN CHINA

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海洋与湖沼 1989年第1期 26-27页

作者： Liao Yulin(institute of oceanology, Academia Sintca, qingdao)

Among the sea-stars collected by the institute of oceanology, Academia Sinica, there was a single very large and handsome specimen representing a new species of the genus Calliaster Gray. The following is a descriptio... 详细信息

关键词： ASTEROIDEA CALLI ASTER QUADRISPINUS FROM SOUTHERN CHINA A NEW SPECIES OF THE FAMILY GONIASTERIDAE

STUDIES ON. PHYSICAL SCIENCES. OF THE OCEANS AND SEAS IN CHINA, 1979-1982

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Chinese Journal of oceanology and Limnology 1984年第2期2卷 243-268页

作者： Mao Hanli (institute of oceanology, Academia Sinica, qingdao) institute of oceanology Academia Sinica Qingdao

In 1979—1982, considerable research works on physical sciences of the oceans were done by Chinese scientists and some fruitful results were achieved. In the following, a brief account is given of the achievements in the studies of currents and circulation, hydrographic characteristics and watermasses, tides and sea level, surface waves, storm surges, air-sea interaction, numerical modelling, estuarine and coastal research, marine chemistry, marine acoustics and marine optics.

关键词： OF THE OCEANS AND SEAS IN CHINA PHYSICAL SCIENCES STUDIES ON

MAJOR FEATURES OF WARM AND COLD EDDIES SOUTH OF THE NANSEI ISLANDS

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Chinese Journal of oceanology and Limnology 1983年第3期1卷 248-257页

作者： Guan Bingxian (institute of oceanology, Academia Sinica, qingdao) 1. institute of oceanology Academia Sinica Qingdao

As regards the eddies occurring in the origination region of the Kuroshio (west of 130° E), the earliest informations were reported by R. Shigematsu (1932) and K. Koenuma (1936) respectively. From the data observed in the twenties, they pointed out that there was a warm eddy located to the right side of the Kuroshio in the Luzon Strait. Using the data obtained from the fourties through the sixties, Nitani further convinced the existence of the warm eddy. During the latest two decades, observations of the area south of the Nansei Islands on board of R/V Chofu Maru (1965, ’66, ’67) and Hakuho Maru (1974. ’75) also revealed the existence of warm and cold eddies, but few works on 'eddies' are reported, so far as we know.

关键词： MAJOR FEATURES OF WARM AND COLD EDDIES SOUTH OF THE NANSEI ISLANDS

Improvement of the SLP simulation in the coupled AGCM-ocean surface wave model

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Chinese Science Bulletin 2005年第20期50卷 2397-2400页

作者： YU Weidong1, 2, 3, LI Zhaoxin4.& YUAN Yeli3 1. institute of oceanology, Chinese Academy of Sciences, qingdao 2.6071, China 2. Graduate School of Chinese Academy of Sciences, Beijing 10004., China 3. Laboratory of Marine Science and Numerical Modeling, First institute of Oceanography, State Oceanic Administration, {4. 266061, China 4. LMD/CNRS, Univ. Paris 6, Paris, France institute of oceanology Chinese Academy of Sciences Qingdao 266071 China Graduate School of Chinese Academy of Sciences Beijing 100049 China Laboratory of Marine Science and Numerical Modeling First Institute of Oceanography State Oceanic Administration Qingdao 266061 China LMD/CNRS Univ. Paris 6 Paris France

The coupled atmosphere-ocean general circulation models (CGCM) are nowbecoming the indispensable tools for the climate study. However, most models still suffer fromunrealistic simulations. One problem is the troublesome climate drift. It may come from someunresolved aspects. One possibility is the poor air-sea surface flux description now adopted inCGCM. The commonly used solution for this problem is the so-called flux correction. To deal with it,Hasslemann proposed an alternative solution of prospect. That is to incorporate the ocean surfacewave model into this coupled GCM system so as to establish a coupled atmosphere-wave-ocean *** necessity is clearly seen from the recent field experiment that air-sea momentum flux dependsstrongly on the sea state. So the explicit calculation of the air-sea flux with the aid of the oceansurface wave model is highly desired. Theoretical progress has provided feasibility to such ideaand experiments have been conducted. Recent work also reveals that coupling ocean surface wave modelwith oceanic general circulation model can result in much better reproduction of the upper oceanthermal structure. This further strengthens our belief in the final realization of the coupledatmosphere-wave-ocean modeling system.

关键词：大气海洋循环模式气象学 SLP模拟

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Isotopic feature and uranium dating of the volcanic rocks in the Okinawa Trough

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中国科学：地球科学英文版 2006年第4期49卷 375-383页

作者： HUANG Peng1,2, LI Anchun1, HU Ningjing2,3, FU Yongtao1& MA Zhibang4.1. institute of oceanology, Chinese Academy of Sciences, qingdao 2.6071, China 2. Graduate School of the Chinese Academy of Sciences, Beijing 100039, China 3. institute of Soil Science, Chinese Academy of Sciences, Nanjing 210008, China 4. institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China 1. institute of oceanology Chinese Academy of Sciences Qingdao 266071 China 2. Graduate School of the Chinese Academy of Sciences Beijing 100039 China 3. institute of Soil Science Chinese Academy of Sciences Nanjing 210008 China 4. institute of Geology and Geophysics Chinese Academy of Sciences Beijing 100029 China

Volcanic rocks from the northern and middle Okinawa Trough were dated by ura- nium-series dating method. Differential fractions using magnetic procedure were designed to separate samples. New report on the ages and isotopic data of rocks in the northern trough (especially black pumice) was discussed. Based on the uranium dates and Sr-Nd isotopic ratio, magmatic evolution process of the Okinawa Trough was noted. Firstly, there have been wide silicic volcanic activities in the Okinawa Trough from late Pleistocene to present, and the volcanic rocks can be divided into three subgroups. Secondly, magma generally came from PREMA source area under the Okinawa Trough. Magmatic evolution in the northern trough was similar to the middle, but different to the south. Finally, volcanic activities indicated that opening of the southern Okinawa Trough did not happen due to the collision between Luson Arc and Eurasian Plate until the early Pleistocene.

关键词： Okinawa Trough, black pumice, uranium-series dating, Sr-Nd isotopic ratio, magmatic evolution.

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SOME GEOCHEMICAL PATTERNS OF SHELF SEDIMENTS OF THE CHINA SEAS

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Journal of oceanology and Limnology 1985年第2期3卷 200-211页

作者： Zhao Yiyang (institute of oceanology, Academia Sinica, qingdao) 1. institute of oceanology Academia Sinica Qingdao

Geochemical patterns of shelf sediments of China Seas are discussed in the following order: 1) the grain-size control of elements, 2) zonal distribution of elements along the coast, 3) estuarine enrichment of elements, 4. correlation of elements, 5) philo-detrital property of elements, 6) philo-continental property of elements, 7) rapid accumulation rate of elements. Statistics show that the abundance of indicator elements in shelf sediments is relatively close to that in terrestrial rocks and continental crust, and the abundance distribution pattern of elements in shelf sediments is similar to that in continental crust.

关键词： SOME GEOCHEMICAL PATTERNS OF SHELF SEDIMENTS OF THE CHINA SEAS

UPWELLING AND SEDIMENTATION DYNAMICS I. THE ROLE OF UPWELLING IN SEDIMENTATION IN THE HUANGHAI SEA AND EAST CHINA SEA-A DESCRIPTION OF GENERAL FEATURES

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Chinese Journal of oceanology and Limnology 1984年第1期2卷 12-19页

作者： Hu Dunxin (institute of oceanology, Academia Sinica, qingdao) institute of oceanology Academia Sinica Qingdao China

It is found that the mud distributions in the Huanghai Sea and East China Sea are extremely identical with the upwelling’s in terms of locality and extent. The process of the mud formation is examined. It is concluded that vertical circulation i.e. upwelling plays a determinant role in the: process and furthermore, it is inferred that wherever upwelling occurs on continental shelf, mud should be formed and, conversely, wherever downwelling takes place, mud should not exist, for which coarse: sediment should substitute.

关键词： THE ROLE OF UPWELLING IN SEDIMENTATION IN THE HUANGHAI SEA AND EAST CHINA SEA-A DESCRIPTION OF GENERAL FEATURES UPWELLING AND SEDIMENTATION DYNAMICS I 口口 EAST SEA