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1.
ZOOPLANKTON COMMUNITY STRUCTURE OF THE SEA SURFACE MICROLAYER NEAR NUCLEAR POWER PLANTS AND MARINE FISH CULTURE ZONES IN DAYA BAY 总被引：1，自引：0，他引：1
ＩＮＴＲＯＤＵＣＴＩＯＮＴｈｅｓｅａｓｕｒｆａｃｅｍｉｃｒｏｌａｙｅｒ (ＳＭ)ｗｉｔｈｓｐｅｃｉａｌｐｈｙｓｉｃａｌ,ｃｈｅｍｉｃａｌａｎｄｂｉｏｌｏｇｉｃａｌｐｒｏｐｅｒｔｉｅｓ,ｈａｄｂｅｅｎｗｅｌｌｄｅｓｃｒｉｂｅｄａｓａｓｉｔｅｏｆｉｎｔｅｎｓｉｖｅａｃｃｕｍｕｌａｔｉｏｎｏｆｄｉｓｓｏｌｖｅｄａｎｄｐａｒｔｉｃｕｌａｔｅｏｒｇａｎｉｃｍａｔ ｔｅｒｉｎｖｏｌｖｉｎｇｐｈｙｔｏｐｌａｎｋｔｏｎａｎｄｂａｃｔｅｒｉａ (Ｈａｒｄｙ,1 982 ) .Ｔｈｉｓｅｎｖｉｒｏｎｍｅｎｔｈａｓｇｒｅａｔｉｍｐｏｒ… 相似文献
2.
ＩＮＴＲＯＤＵＣＴＩＯＮＪｏｈａｎｎｅｓ (1 965)ｆｉｒｓｔｓｈｏｗｅｄｔｈｅｉｍｐｏｒｔａｎｃｅｏｆｐｒｏｔｏｚｏａａｓｒｅｍｉｎｅｒａｌｉｚｅｒｓｉｎｍａｒｉｎｅｅｎｖｉｒｏｎｍｅｎｔｓ.Ｔｈｅｓｉｇｎｉｆｉｃａｎｃｅｏｆｐｒｏｔｏｚｏａｉｎｔｈｅｆｒｅｓｈｗａｔｅｒｆｏｏｄｗｅｂｈａｓｂｅｅｎｋｎｏｗｎｆｏｒｔｈｅｐａｓｔ2 0ｙｅａｒｓ.Ｐｒｏｔｏｚｏａｉｓａｍａｉｎｐｒｅｄａｔｏｒｏｆｐｌａｎｋｔｏｎｉｃｂａｃｔｅｒｉａａｎｄｐｈｙｔｏｐｌａｎｋｔｏｎ ,ａｎｄａｌｓｏａｆｏｏｄｓｏｕｒｃｅｏ… 相似文献
3.
1 INTRODUCTIONRecently ,thepollutionoftracemetalinseawaterhasbecomeincreasinglyevident.Researchershavefo cusedattentiontotracemetalpresentinvariousexistenceforms ,especiallyorganiccomplexingphases.Theexistencestatesandtransportmechanismofbaytracemetalswerethesubjectofstudybysomere searchers(Gu ,1 991 ;Florence ,1 998;Guo ,1 998;Wells,1 991 ,1 998a ,b ;Wellsetal.,1 998) .Whetherinfreshwaterorseawater,colloidsareclearlydominantfactorsaffectingtheexistencestatesandtransportmechanismoftrac… 相似文献
4.
CHARACTERISTICS OF THE OXYGEN REDUCTIONIN ATMOSPHERIC CORROSION 总被引：1，自引：0，他引：1
ImODUcrlONArnaorandnowincreasinglyimPoftantprobleminthemanyyearsinvestigationsofabosphericcormsionofmetaIsandalloyisthatthecormsionrmctionunderathineleCtrolytelayerchangessigwhcanhywithdrying.Tornashov(l966)reportedthatthecorm-sionrateisinfluentalbytheelamlytelayerthwhnessandiscontrolledbythedtheion-lndtingcurrentofoxygenreduCtionreig.l)whentheel~lytefilmisthickerthanthediffUSionlayerthickness.ThereforetherateisnotaffededbytheelCCtrolyteFilmthwh-nessforthecaseofaverythickFilm,e.g.regionI… 相似文献
5.
Surface water can be divided into three layers from top downward: surface microlayer (SML, thickness≤50 μm), subsurface layer (SSL, ≈25 cm) and surface layer (SL, 1–5m), among which the SML plays an important role on sea-air interaction because of its unique physical-chemical property. Carbon dioxide system including DIC (dissolved inorganic carbon), Alk (alkalinity), pH and pCO2 (partial pressure of CO2) in multilayered waters of the Yellow Sea was studied for the first time in March and May 2005. The results show that: DIC and Alk are obviously enriched in SML. The contents of DIC, Alk and pCO2 become lower in turn from SML, SSL to SL, higher in March and lower in May, whereas for pH it was opposite. The relationship between DIC and Alk is clearly positive, but negative between pH and pCO2. Meanwhile, pCO2 and temperature/salinity is also in positive relation, pCO2 decreases with latitude increase. DIC and Alk show a similar variation trend with the maximum at 02:00–03:00, but pH and pCO2 show an opposite pattern. In addition, the distribution patterns are similar to each other in the three layers. The Yellow Sea is shown to be a sink of atmospheric CO2 in spring by two methods: (1) comparing pCO2 in seawater and atmosphere; (2) turning direction of “pH-depth” curve. Calculation on the base of pCO2 data in SML in four models shows that carbon flux in spring in the area was about -6.96×106 t C. 相似文献
6.
7.
Carbon dioxide partial pressure and carbon fluxes of air-water interface in Taihu Lake, China 总被引：2，自引：0，他引：2
1 INTRODUCTION Carbon dioxide (CO2) is principal greenhouse gas. Its air-water exchange is important in terrestrial ecosystems for climate change (Frankignoulle et al., 1998; Schimel et al., 2001). The direction of CO2 gas movement depends on the CO2 concentration gradient between air and surface water. The amount of CO2 exchange is related to the gas exchange coefficient, k. All lakes, with their small area but large atmospheric CO2 flux are important to under-stand the CO2 fluxes … 相似文献
8.
Glass-plate sampling during 1988- 1999 in Daya Bay and suitable corresponding analytical methods were used for the measurement of dissolved trace metals, dissolved organic carbon, biological oxygen demand, chemical oxygen demand, salinity of the sea surface mierolayer and subsurface water. Apparent enrichment mechanism and diurnal variation have been revealed for dissolved trace metals in the microlayer in Daya Bay. The more dissolved organic matter was enriched in the sea surface microlayer, the more dissolved trace metals were enriched in the layer. The organic matter played an important role in the enrichment process. The diurnal variations of dissolved trace metals showed that their concentration was apparently inversely related to the tide activity that the concentration was low during rising tide, but high during falling tide. The behavior of dissolved trace metals expressed by the diurnal variation was clearly opposite to that of salinity. 相似文献
9.
Distributions of inorganic nutrients in the bohai sea of china 总被引：2，自引：0，他引：2
LI Zhengyan * BAI Jie SHI Jinhui GAO Huiwang College of Environmental Science Engineering Ocean University of China Qingdao P..R.China 《中国海洋大学学报(英文版)》2003,2(1):112-116
1 Introduction TheBohaiSeaislocatedinthenorthernChinawithlongitudesofbetween 117°38′Eand 12 2°31′Eandlat itudesofbetween 37°0 8′Nand 4 1°0 2′N .Itisashal lowseawithanaveragewaterdepthof 18m (LiuandZhang ,2 0 0 0 ) .Severalbigrivers ,suchastheLiaoheRiver,theHaiheRiverandtheYellowRiver ,findtheirwaysintotheBohaiSeaandtransportlargeamountofnutrientsandsuspendedmattersfromthecontinentintothesea (Zhangetal.,1994 ;Zhang ,1996 ) .Duringthelasttwodecades ,marineenviron mentintheBohai… 相似文献
10.
Survival, growth and immune response of the scallop, Chlamys farreri, cultured in lantern nets at five different depths (2, 5, 10, 15, and 20 m below the sea surface) were studied in Haizhou
Bay during the hot season (summer and autumn) of 2007. Survival and growth rates were quantified bimonthly. Immune activities
in hemolymph (superoxide dismutase (SOD) and acid phosphatase (ACP)) were measured to evaluate the health of scallops at the
end of the study. Environmental parameters at the five depths were also monitored during the experiment. Mortalities mainly
occurred during summer. Survival of scallops suspended at 15 m (78.0%) and 20 m (86.7%) was significantly higher than at 2
m (62.9%), 5 m (60.8%) or 10 m (66.8%) at the end of the study. Mean shell height grew significantly faster at 10 m (205.0
μm/d) and 20 m (236.9 μm/d) than at 2, 5 or 15 m in summer (July 9 to September 1); however, shell growth rate at 20 m was
significantly lower than at the other four depths in autumn (September 2 to November 6). In contrast to summer, scallops at
5 m grew faster (262.9 μm/d) during autumn. The growth of soft tissue at different depths showed a similar trend to the shell.
Growth rates of shell height and soft tissue were faster in autumn than in summer, with the exception of shell height at 20
m. SOD activity of scallops increased with depth, and ACP activity was significantly higher at 15 and 20 m than at other depths,
which suggests that scallops were healthier near the bottom. Factors explaining the depth-related mortality and growth of
scallops are also discussed. We conclude that the mass mortality of scallop, C. farreri, during summer can be prevented by moving the culture area to deeper water and yield can be maximized by suspending the scallops
in deep water during summer and then transferring them to shallow water in autumn. 相似文献
11.
Distribution of microbial populations and their relationship with environmental variables in the North Yellow Sea, China 总被引：1，自引：0，他引：1
Xiaoge Bai Min Wang Yantao Liang Zhifeng Zhang Fang Wang Xuejiao Jiang 《中国海洋大学学报(英文版)》2012,11(1):75-85
In order to understand the large-scale spatial distribution characteristics of picoplankton,nanophytoplankton and virio-plankton and their relationship with environmental variables in coastal and offshore waters,flow cytometry(FCM) was used to ana-lyze microbial abundance of samples collected in summer from four depths at 36 stations in the North Yellow Sea(NYS).The data revealed spatial heterogeneity in microbial populations in the offshore and near-shore waters of the NYS during the summer.For the surface layer,picoeukaryotes were abundant in the near-shore waters,Synechococcus was abundant in the offshore areas,and bacte-rial and viral abundances were high in the near-shore waters around the Liaodong peninsula.In the near-shore waters,no significant vertical variation of picophytoplankton(0.2-2μm) abundance was found.However,the nanophytoplankton abundance was higher in the upper layers(from the surface to 10 m depth) than in the bottom layer.For the offshore waters,both pico-and nanophytoplankton(2-20μm) abundance decreased sharply with depth in the North Yellow Sea Cold Water Mass(NYSCWM).But,for the vertical dis-tribution of virus and bacteria abundance,no significant variation was observed in both near-shore and offshore waters.Autotrophic microbes were more sensitive to environmental change than heterotrophic microbes and viruses.Viruses showed a positive correla-tion with bacterial abundance,suggesting that the bacteriophage might be prominent for virioplankton(about 0.45μm) in summer in the NYS and that viral abundance might play an important role in microbial loop functions. 相似文献
12.
1 INTRODUCTION Bioavailability to the biota and the biogeo-chemistry of trace metals in marine environment areaffected by their chemical speciation in the naturalsystem (Bruland et al., 1991; Van den Berg andDonat, 1992; Wells et al., 1998). Therefore, thesetwo parameters, the ligands concentrations andconditional stability constants, are important todetermine the complexing capacity. Sea surface microlayer (SML), the thin interfa-cial boundary between ocean and atmosphere, playsan imp… 相似文献
13.
A cruise was undertaken from 3rd to 8th November 2004 in Changjiang （Yangtze） River Estuary and its adjacent waters to investigate the spatial biomass distribution and size composition of phytoplankton. Chlorophyll-a （Chl-a） concentration ranged 0.42-1.17 μg L^-1 and 0.41-10.43 μg L^-1 inside and outside the river mouth, with the mean value 0.73 μg L^-1 and 1.86 μg L^-1, respectively. Compared with the Chl-a concentration in summer of 2004, the mean value was much lower inside, and a little higher outside the river mouth. The maximal Chl-a was 10.43 μg L^-1 at station 18 （122.67°E, 31.25°N）, and the region of high Chl-a concentration was observed in the central survey area between 122.5°E and 123.0°E. In the stations located east of 122.5°E, Chl-a concentration was generally high in the upper layers above 5 m due to water stratification. In the survey area, the average Chl-a in sizes of 〉20 μm and 〈20 μm was 0.28 μg L^-1 and 1.40 μg L^-1, respectively. High Chl-a concentration of 〈20 μm size-fraction indicated that the nanophytoplankton and picophytoplankton contributed the most to the biomass of phytoplankton. Skeletonema costatum, Prorocentrum micans and Scrippsiella trochoidea were the dominant species in surface water. The spatial distribution of cell abundance of phytoplankton was patchy and did not agree well with that of Chl-a, as the cell abundance could not distinguish the differences in shape and size of phytoplankton cells. Nitrate and silicate behaved conservatively, but the former could probably be the limitation factor to algal biomass at offshore stations. The distribution of phosphate scattered considerably, and its relation to the phytoplankton biomass was complicated. 相似文献
14.
The ultrastructure of hemocytes ofPenaeus vannamei was examined by transmission electron microscope. Three types of hemocytes were identified: hyaline cell, small-granule cell
and large-granule cell. Hyaline cells are the smallest of the hemocytes, lack electron-dense granules, have average size of
11.11 μm (SE±0.50,n=10)×6.96μm (SE±0.55,n=10), comprise 25.8% (SE±2.87,n=4×10) of the hemocytes; small granule cells are the most abundant type of hemocytes, comprise 58.1% (SE±3.40,n=4×10) of the hemocytes, contain small electron—dense granules, have average size of 10.78 μm (SE±0.60,n=10)×8.63 μm (SE±0.44,n=10); and large-granule cells comprise 16.1% (SE±2.55,n=4×10) of the hemocytes, are filled with large electron dense granules, have average size of 12.51 μm (SE±0.63,n=10)×8.99μm (SE±0.71,n=10).
This research was supported by the National Climbing Project B, PDB6-6-3.
Contribution No. 3448 from the Institute of Oceanology, Chinese Academy of Sciences. 相似文献
15.
Distribution, variation and impact factors of biomass of bacterioplankton from April to May 1999 in Bohai Sea were studied in DAPI method with epifluorescence microscopy. The biomass in surface waters showed a small day-night variation, varying from 0.13 to 2.51μg/dm^3 with an average of 0.84μg/dm^3. The biomass in bottom waters showed, however, a large variation, changing from 0.15 to 4.18μg/dm^3 with an average of 1.36μg/dm^3. The peak values occurred at 5 and 11 a.m. The bottom water biomass showed a significant correlation with particulate organic carbon （r=0.639, P〈0.05）. Heterotrophic bacterioplankton biomass was high in nearshore waters and low in offshore areas with a high biomass zone around Huanghe （Yellow） River mouth, showing the same distribution of nutrients. In vertical distribution, heterotrophic bacteria biomass in bottom waters was higher than that in surface water. 相似文献
16.
Preliminary studies on microzooplankton grazing were conducted with dilution method in Jiaozhou Bay from summer 1998 to spring
1999. Four experiments were carried out at St. 5 located at the center of Jiaozhou Bay. Chlorophyll a concentrations were
consistently dominated by netphytoplankton (net-, >20μm), except during the autumn 1998 cruise, when they were dominated by
nanophytoplankton(nano-, 2–20μm). The contribution of picophytoplankton (pico-, <2μm) to total chlorophyll a concentrations
(<200μm) varied considerably between cruises. Instantaneous growth coefficients(u) of phytoplankton varied from 0.098 to 1.947d−1, with mean value of 0.902d−1. Instantaneous coefficients(g) of microzooplankton grazing on phytoplankton ranged from 0.066 to 0.567d−1, mean value of 0.265d−1, which was equivalent to daily lose of 21.9% of the initial standing stock and 58.1% of the daily potential production.
Project No KZCX3-SW-214 supported by Chinese Academy of Sciences. 相似文献
17.
Persistent organochlorine residues in sediments of Hong Kong Victoria Harbour and Xiamen Western Bay 总被引：2，自引：0，他引：2
INTRODUCTIONOrganochiorine(OC)compounds,suchaspolych1orinatalbiphenyIsrpCBs),hexachlorocycohexane(HCH)andDDThaveentetalmarineenvirorimentSthI0ughatmospherictransport,estuarinerunofTcoastalwaterdischarge,andsoon.InspiteoftheastriCtion0rbanonOCsusageinmostcountriesformanyyears,OCnsiduescanstillbefoundatconsiderableleveIsinvari0usmarineaservotrisuchasseaWhtef,maforor-ganismandtaltrit.ooinrnarineenvirOrimenthavedrawnmuchattenti0ntheuse0ftheirubiquity,persistenceandt0xidty.Marinesedtri… 相似文献
18.
LIU Jiying WEN Jiahong WANG Yafeng WANG Weili Beata M CATHSO Kenneth CJEZEK 《中国地理科学(英文版)》2007,17(2):160-165
Dome A, the highest dome of East Antarctic Ice Sheet, is being an area focused by international Antarctic community after Chinese Antarctic Expedition finally reached there in 2005, and with the ongoing International Polar Year (IPY) during August 2007. In this paper two data processing methods are used together to generate two 100-m cell size digital elevation models (DEMs) of the Dome A region (Dome A-DEM) by using Cokriging method to interpolate the ICESat GLAS data, with Ihde-DEM as a constraint. It provides fundamental data to glaciological and geophysical investigation in this area. The Dome A-DEM was applied to determining the ice-sheet surface elevations and coordinates of the south and north summits, defining boundaries of basins and ice flowlines, deducing subglacial topography, and mapping surface slope and aspect in Dome A region. The DEM shows there are two (north and south) summits in Dome A region. The coordinate and the surface elevation of the highest point (the north summit) are 80°21′29.86″S, 77°21′50.29″E and 4092.71±1.43m, respectively. The ice thickness and sub-ice bedrock elevation at north summit are 2420m and 1672m, respectively. Dome A region contains four drainage basins that meet together near the south summit. Ice flowlines, slope and aspect in detail are also derived using the DEM. 相似文献
19.
WANG Yangang HU Xiaozhong LONG Hongan SONG Weibo 《中国海洋大学学报(英文版)》2007,6(4):387-392
The living morphology and infraciliature of a marine ciliate, Cardiostomatella vermiformis isolated from a sand beach of the Jiaozhou Bay near Qingdao, China, were investigated by live observation, protargol and silver carbonate impregnation methods. Both the morphological and morphometric data largely agree with former records. Based on the data obtained, an improved diagnosis for Cardiostomatella vermiformis is supplied: Large marine Cardiostomatella with cylindrical body shape and several prolonged caudal cilia; cells in vivo about (90–500) μm×(30–120) μm; macronucleus beaded; single contractile vacuole caudally positioned; buccal apparatus conspicuously small, genus typical; three to six postoral kineties; 96-130 somatic kineties. This species is recorded for the first time in China. 相似文献
20.
Feeding of freshwater cyclopoid copepodAcanthocyclops robustus on zooplankton was examined by a senes of feeding experiments during August–September of 1993. Study results showedA. robustus can capture and eat all type items provided from the Stary Haklovsky fishpond, a shallow eutrophic water body near Budějovice
City, Czech Republic. Selection by the predator was determined largely by prey body-size and density, but was also affected
by prey types. Variable but significant changes in feeding rates were found in various size distribution and concentration
of prey types. Percentages of small (80–235μm) and large (445–610μm) prey consumed were 42.47 and 3.85%, respectively. Starvation
did not cause statistically significant difference. The feeding onCeriodaphnia quadrangula showed significant difference between large and small prey. Feeding rate increased with increasing prey concentration. 相似文献