《海洋学报》(英文版)第8卷(1989年)总目录

Marlne Hydrology11······.-··一,···……A hvbrid model for numerical wave forecasting and its implementarion一IThe w 1 nd wave model 甲en sheogehang(S,e.甲e,)(文圣常),Zhang Daeuo(张大错),che。召。人ai(陈波海) and Guo Peifa六g(郭佩芳)l一15··················……Parame全ers 1 n wind·wave frequeneys阵etra and their bearings ons详etrum forms and growth 邵en she,了ehang(s.e尸en丫文二、,艺内a,,尸。a〔、uo(张大错),‘uo pei心n矛(郭佩芳) and Chen Bohai(陈波海)王41····…     

《海洋学报》(英文版)第10卷(1991年)总目次

Marine Hydrology一l·····……E,t imation of wat,r vol叹爪,tran3port3 throu‘h main stra!ts ort、”Eagt Cl‘inas“a Zhao刀。ore。(赵保仁)and Fa,夕‘”OhO”夕(方国洪)1一15······……T卜户e二f Oc七of intolnal tid,5 on thev,rt!cal structur,of tidal culront in tho North Huaugha!Sea Zhao Jon。人e”夕(赵浚仁),‘eog夕hfj‘。。夕(耿世江),Son万001￡a”,(刹、洪亮)and Zhaog 2111(于长自历)1一37······……Surfaeod呈弓tribution of alkalinity ands,eeifie alkalinit犷and thoir apPlieation to…     

In situ determination on food consumption and ecological conversion efficiency of a marine fish species, Hyporhamphus sajori

The food consumption and ecological conversion efficiency of a species marine pelagic andsmall size fish, Hyporhamphus sajori, were determined by using in situ stomach content method presented by Eggers. The results showed that: (1) the fish was taken in food all day, so empty-stomach rate was very low, taking up about 4.5% of the total determined fish number. However, the fish still has significant daily feeding rhythm. A feeding peak was found 0:00 o'clock at night, but feeding level was always high in the daytime; (2) relationship between instantaneous food content in stomach and corresponding time could be described as S_t = a ·e ~(-b ·t). There was not significant difference of instantaneous gastric evacuation rate between two determinations, with average value being 0.13 × 10~(-2)g/ (g·d) (wet weight); (3) the daily food consumption tended to change in irregular waving form, with average value being (10.16×l0~(-2)±1.19×l0~(-2) g/ (g·d) (wet weight) or (55.56 × 10~(-2) ±6.51 × 10~(-2) kJ/     

ACTA OCEANOLOGICA SINICA Subject index to Vol. 12, 1993

Marine Hydrologyl············……Fronts and transport of suspended matter zn the Ha叩见hou浅y Su Jiza,(苏纪兰),Wa,9 Ka、那ha,(王康塔)andL,Ya。(李炎)1,············……Hydrographie features of the plume front in the Hangzhou翔y 环几王n君Ka,gsha二(王康塔)and Su了ttan(苏纪兰)2,1··········,··…Residual eurrents in plume front zone of the Hangzhou枷yche,w‘i(陈伟),月“angD‘户(黄大吉)andya,92人a阅Ing(杨昭庆)39··,·········……Suspended sediment tra…     

海洋预报第3卷(1986年)总目录

研究 与探讨 期 页东海及外缘海域表层海水温度场的分析和预报…………………………·、、……、、·、…、杜碧兰、袁小军(l——l)太平洋低纬地区垂直环流圈与海温的季节变化…………………………………………………··赵黔源(l—10)相似理沦在海洋上混合层深度预报中的应用………………、…………………·、……·。、··、··、…·姜景忠(l—18);海洋加热场对副高西伸影响的分析………………………………………………………………李月洪(1—27)夏季风撤退前后低纬高低空环流及高空温度与散度场的变化特征……·、。…·。··。··,…     

《海洋学报》(英文版)第11卷(1992年)总目次

Marine HydrologyCross thermoel!nem盆x!ng effeet due tot!de in the shallow seayan夕D亡aoro:夕(杨殿荣),Z入00 Dejfa。(周德坚)and Zhan夕Yulfn(张玉林)LAGFD一WAM numeriealapplleationwave model一1 .Charaeter!sties笼nlaid seheme and!tsY“ao Yelf(袁业立)(孙乐涛)Hoa Fen夕(华锋),Pao Ze”夕d‘(潘增弟)ands“”Letao2一157......……2一叉了9…‘”””“2一13口·…,,-…3一3生7.·....……3一33卜··.·.……3一343.·..……”3一367··..·.……3一375··....……4一471·.……。…The study on the numer!eal …     

《海洋学报》《英文版)第9卷(1990年)总目录

l一l。”。.。。。。。。。。.。。“。。。。”1一13二。二。二。二。二。。.。。.。。.。1一25二。二。二。二。……。.。。二1一37”。。”一。..~,”.。..。”The equil一br一um ra昭e of wind wavef佗queney sPeetrum尸en Shen即加n了(s.C.分e,)(文圣常),Zhan了Dacuo(张大错),Ch,n .ohai(陈波海)an口Guo pei为心(郭佩芳)Combi此d refraetion andd一f企ra‘一on models for sea waves over eomPlieatedtopograPhy and with eurrents in shallow waterYin Baoshu(尹宝树)and Jiang Deeai(蒋德才)Seasonal respol朽七5 of monthl y…     

The study of fluorescence characteristics and biochemical composition of a marine diatom Thalassiosira pseudonana 3H in light and dark cycles-Ⅱ. The effects of light

The effects of light on the fluorescence characteristics and biochemical composition of a marine diatom Tha-lassiosira pseudonana in light and dark cycles were investigated with semi-continuous culture. The results indicate that, with the increase of growing light intensity, DCMU enhanced fluorescence yield (Fd/Chl), enhanced fluorescence ratio (Fd/F) , cellular carbohydrate content. carbohydrate/chlorophyll a and carbohydrate/protein ratio increased , but the fluorescence yield and cellular chlorophyll a content decreased; The protein content declined with the increase of light intensity in the range of 10- 100 μmol/ (m2·s) and increased at higher than 100 μmol/ (m2·s). Sampling time during the day had great effect on the relationships between growing light intensity and cellular chlorophyll a , carbohydrate content , carbohydrate/chlorophyll a and carbohydrate/protein ratio.     

Measurement of the current and spectral analysis on the continental shelf in the East China Sea

Direct measurements of current velocity and water temperature were undertaken at the mooring Sta. M (125°29.38' N, 31°49.70' E) on the continental shelf area in the East China Sea in June 1999 by R/V Xiangyanghong 14. The relationship between various time series of oceanic fluctuations is calculated by spectral analysis. The major results are as follows: (1) an average (u,v) of (6.9,-3.0 cm/s) at the 30 m depth is obtained during the 9-day observation, and that at the 45 m depth is (3.7,-1.1 cm/s), i. e., the mean flows are southeastward at both the 30 and 45 m depths;the currents become stronger gradually during the observation period; this may be mainly attributed to the transition of the tidal currents from neap to spring; (2)semidiurnal fluctuation is the most dominant in the current fluctuations, and rotates mainly clockwise; in the next place, there is also diurnal fluctuation;the local inertial period is close to the period of diurnal fluctuation, and an inertial motion is clockwise; thus, loca     

ACTA OCEANOLOGICA SINICA Subject index to Vol.9,1990

Marine Hydrologyl·····,·····,·····,·········……The equilibrium range of wind wave frequency spectrum wi砚5‘,绍‘扒夕(5.‘.”h沙)(文圣常),z加爪夕建灿。妇(张大错),〔〕饭,及汤面(陈波海)耐G翻尹如尹翻夕 (郭佩芳)13·,,···················,·····,·…伪mbined refraetion andd‘ffraetion models for sea wa低over comPlieated toPograPhy andw亘th eur- te月ts jn shallow water 玩及侧昭尹如(尹宝树)耐J如吩八”翻(蒋德才)25-···.--····-·····-·····…     

海洋与湖沼 1979年 (第10卷) 总目录

乎稳正态过程反正弦定律在海浪谱估计中的应用‘,,:,…:,:,,。,:,:一,,::”,,,·,‘···……余宙文、蓝昌华(l)莱州湾西岸晚第四纪海相地层及其沉积环境的初步研究叭..凡··········..~·……,·…‘····……王绍鸿(9--)户国双星藻科植物研究仁峥”,,..、...尸,.’.,,’”t’.’,”·二,…,·,·,’·,..·..···~·一:二··……,饶钦止、胡鸿钧(24)温度对条斑紫菜丝状体生长发育的影响····……任国忠、崔广法;费修埂、曾呈奎、李楚朴、刘清晨(28)不同氮肥对条斑紫菜丝状体生长发育的影响::,,:,,,,,::,:、,…:,,二:,…     

海洋技术1989年1—4期总目录

单点锚定绷紧型千米潜标系统的设计和计算····一:气:·_·:·:……,二,’’‘·‘··…i.…宋铭航(1一力深海潜标系留系统的设计...·....……;......·……狱..’.···...一:····……,,,’·…王明午(1一”‘千米声学应答释放器释放动力计算…’…,’、‘·:’’···……,:’,二…·,’’······……i..…仲伟彬(1一16入-zGYI一1型灯光信标机简介·……:!’······……军···……,’’·,’’·············……郭焕章(1一23)-千米潜标系统的海上试验·····,············……少…,…     

THE DIAGNOSTIC CALCULATION OF EQUATORIAL FLOWS IN THE EASTERN PART OF THE WESTERN PACIFIC OCEAN

On the basis of observational data of the eastern part of the West Pacific Ocean, a diagnostic calculation of equatorial flow for this region is performed by using the authors' model equations and computing scheme and methods. For the first cruise (January 3-March 4, 1979), the results show: (i) The primary driving force of the equatorial surface flows comes from the prevailing northeasterly wind field, with an average uniform wind speed Vw = 6.3 m/s. The steady westward wind produces divergent westward flows in the surface layers, causing an upwelling near the equator. The importance of the steady wind stress in the upper layer (120 m) decreases with depth and becomes insignificant at the level of z = 75 m or z = 100 m, (ii) The equatorial undercurrent is a strong eastward and equator-ward flow, with its eastward component of undercurrent larger than its meridional component. The core of the undercurrent is at the thermocline, and its maximum velocity is 88-90 cm/s at the level of z=200 m. The deeper f     

海洋湖沼通报1991年1—4期(总47—50期) 总目录

第1期南海东北部台风潮的数值后报及极值增水估计·,·············……丁文兰方国洪李春雁(1)滨海潜水含水层稳定流模型及其应用···················································……邱汉学(10)青岛唠山碱性花岗岩的元素地球化学研究··················……韩宗珠倪帮发赵广涛等(16)海水中氨基酸对Cu(l)—蒙脱石、5102之间离子交换的影响 ...............................................................·········……王修林刘莲生张…     

China Ocean Engineering Contents of Volume 17, 2003

N世nberlG找灿PDec训咖l晒翻吨目】如,月万址叮P油ttemRec理州位价ModelforLeCtoty伴吻山址.公曲谊O找过目砚P肠d勿m‘ 叭NC儿l几~阴切g(王建明),‘月E刀夕汉〕沙,(陈守煌),Fu。双UI夸tao(伏广涛) andHou扮。之卜动翻g(侯召成)···································································4·,···················……(I)Rd加叹舫ty旧泊,刃即均旧习】》目幼for Ve叮U招eF】.的飞St门d.花 2“4四‘夕切功侧乙(张淑华)山以凡口伏…     

Study on halotolerance of phyllosoma larva of Chinese spiny lobster (Panulirus stimpsoni Holthuis)

INTRODUcrIONAs a quality seaha, lobster has a greater market demand or higher demand than supply. Inrecent years the natural resource of lobster is decreasing day by day due to overfishing oPera-tions. Conequently, an attention has been increasingly drawn to the development of artificialbreeding in lObster and seedstock preduction. From the l970s to the l980s the culture of lobsterlarva started but with very slow pngress. Inoue et al. (l978), Yamakawa et al. (1989), Kitta-ka and Kimura(l…     

Chemistry of marine resources——ⅩⅥ. A new potassium reagent and its enrichment behaviour for potassium ion in seawater

This paper first presents a new potassium reagent and efficient enrichment agent for direct recovery of potassium from seawater,i.e.,1,2,4,5-tetrahydroxybenzen -O,O'',O",O''"-tetraacetic acid (TTAH₄).The synthetic method of TTAH₄,its enrichment behaviour for potassium ion in low concentration solution and seawater,and the chemical structure of its corresponding potassium salt have been investigated.A mechanism which caused the uptake of potassium ion is suggested.Elementary analysis and IR-spectrum determination of the potassium salt proved correct evidence for a polynuclear complex,i.e., (TTAH₃K)_n.Thus,the mechanism which caused the uptake of potassium ion may be interpreted in terms of the formation of polynuclear chains as a continual sandwich type coordination complex.     

Rifting characteristics of eastern subbasin of South China Sea and its spreading pattern

With processing and interpretation of 25 000 km full-coverage multibeam swath data fromthe eastern South China Sea, it is found that NE-trending and NW-trending linear morphological features such as scarps, horsts and grabens, govern the central part (14°- 17° N) of eastern subbasin. Compared with reflection seismic profiles, these NE-trending linear morpho-structures are considered to be the representation of basement structures on seabed and can be divided into three linear structural zones. The trend of the central zone is NE45°-50° occurring around extinct spreading center, the trend of the second zone is NE70° - 78° on both sides of the central one and the trend of the third zone is about NE60° just on the north of the second one. These three NE-trending linear zones are formed in late-stage NW - SE-trending seafloor spreading of the eastern subbasin along NW-trending linear faults, and respectively correspond to three spreading episodes: 17.0- 19.0 Ma (5d-5e), 19.0 - 21.0 Ma (5e-6a) and 21.0     

Study on the upwelling along the east coast of Guangdong

-There is a wind-caused upwelling along the east coast of Guangdong in summer. Its central position is above the depth of 20 m, and its annual variation is quite large. In August 1982, the velocity of the upwelling was 1.2 ×10-3 cm/s, the vertical flux of active phophate, 1.5m mol/(m2·d); and the primary productivity, 1558 mg/(m2·d), in the area outside the bay of Jieshi. Inside the up-welling facing the shore, a phenomenon of lacking oxygen existed at the sea bottom above 5 m depth. In the area outside the upwelling center, there was a phenomenon of upward water temperature inversion. The physical and chemical characteristics in the area of the upwelling are as follows: temperature, 22.13℃; salinity, 34.19, dissolved oxygen, 3.72 ml/1; oxygen saturation degree, 74.6%; pH value, 8.14; and active phosphate, 1.10 m mol/m3.     

海洋技术1990年1—4期总目录

渤海BZ一34油田海底管线敷设中的水声定位技术························……李占师(1一1) “鱼鹰”号载人潜器打捞机械手的研制······~···············……向忠祥茅及愚(l一12)CTD剖面仪现场定标和误差分析····,··4·····················,···……刘雪堂林红军(1一18)近岸浅水破碎波能谱近似计算····································……陶尧森郭志兵(1一25)蒸汽压差法浓差能开发···············,···…