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笔者分析、鉴定了100多个南海表层沉积样品中的大量放射虫标本,本文仅报道其中的1个新属和12个新种,作为我们对南海沉积物中放射虫的系列研究之一。 本文是我们对南海沉积物中放射虫的系列研究之一,现仅报道1新属12新种。新种的模式标本均保存于中国科学院南海海洋研究所。 相似文献
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本文报道了以芦笋皮替代酒糟、糖泥养殖尼罗罗非鱼的试验。结果是:其饲料系数基本相同,而且无发现鱼病,说明芦笋皮作为尼罗罗非鱼饲料填充物可行又具防病效果。 相似文献
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渤海是我国主要的海洋渔场之一,许多重要的鱼、虾类,如对虾等在此产卵、育幼、索饵。因此,研究作为饵料基础的环节动物多毛类的种类组成和数量分布,对渤海水产资源开发和经济动物的增、养殖都是有益的,并能为海洋环境硏究提供科学依据。关于渤海多毛类,前人已有很多报道。Fauvel(1933)报道了52种采自天津附近的多毛类,高哲生等(1959)也报道了渤海的一些多毛类,特别是吴宝铃和乌沙科夫(1963a,1963b)对渤海和黄海的多毛类进行过许多研究。最近,杨德渐和孙瑞平(1988)也报道了渤海的58种多毛类,但上述研究多限于区系分类方面的内容。本文主要根据1982年6月至1983年11月作者对渤海101个站(图1)底栖动物调查所获得的多毛类资料,对渤海多毛类的组成和数量分布进行探讨。 相似文献
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Joan D. Willey 《Marine Chemistry》1975,3(3):227-240
Dissolved alumina can coprecipitate with dissolved silica from seawater enriched with both compounds. This coprecipitation is almost complete within 1h and maintains the concentration of dissolved alumina near naturally occurring oceanic concentrations, well below the alumina concentration of 0.50 ppm A1 found to be stable in filtered Sargasso seawater at 2°C. Only 0.5 ppm Si is necessary to initiate this coprecipitation, which indicates that the concentrations of dissolved alumina that occur in seawater and in interstitial water are a function of the concentration of dissolved silica as well as of the alumina solubility.Dissolved alumina is also quickly removed by solid amorphous silica from solutions of seawater enriched in dissolved alumina and also by several marine sediments in contact with the solution. This process may be an important factor in authigenic mineral formation in marine sediments. 相似文献
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Joan D. Willey 《Marine Chemistry》1977,5(3):267-290
Dissolved silica can coprecipitate with zinc from seawater or distilled water that has been enriched with both elements. More than 2 ppm Si are necessary for the reaction to begin. The coprecipitation shows pH dependence. The addition of pulverized illite or natural sediment as suspended particulate material does not enhance the reaction in seawater. The organic material present in the nearshore seawater samples decreases the rate and extent of reaction, as indicated by comparisons of results of experiments using natural seawater with results obtained using UV-irradiated seawater. In unbuffered distilled water the reaction must compete with hydrolysis of zinc; however, reaction does occur, which indicates that the seawater matrix is not essential for the reaction. The coprecipitation can limit the concentration of zinc in seawater to less than the solubility concentration assumed for ZnCO3 or Zn(OH)2. The results suggest that a zinc silicate can precipitate directly from seawater or interstitial water as an authigenic mineral. 相似文献
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Studies on migration pathways remain qualitative, albeit extensive quantification of migration forcing. In this study, hydrocarbon carriers are defined as carrier units and their corresponding carrier beds for the Third Member of Eocene Shahejie Formation in the Dongying Depression, Bohai Bay Basin, eastern China, on the basis of their lithofacies and physical properties, spatial relationships, and data availability; secondary migration conduits are then quantified. A carrier unit is defined as a stratigraphic unit that contains microscopically porous and permeable carrier beds and is covered by regional seals. The carrier beds are macroscopically and physically connected to each other within a carrier unit and are hydrodynamically connected during secondary migration. A method of quantifying sandstone carrier units using common physical properties is developed. First, a carrier unit containing potential carrier beds is identified on the basis of lithofacies and their lateral changes. Second, physical connectivity of sandstone carrier beds is assessed on the basis of percolation theory. Third, the hydrodynamic connectivity of a sandstone carrier unit is analyzed using effective parameters that may reflect the hydraulic circulation in the carrier unit. Last, the conductivity of a sandstone carrier bed is quantitatively characterized using appropriate physical property parameters. The results for sandstone carrier units in the Third Member of the Shahejie Formation are used in numerical models addressing Pleistocene secondary migration. The model results explain the discovered accumulation and hydrocarbon shows well; and the model predictions on exploration targets have been confirmed by drilling. 相似文献
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《Marine Chemistry》2001,74(1):15-28
In this paper, an intercomparison of methods for the determination of 234Th in seawater is discussed. Samples were collected either from a shore-based 600 m water source, or from standard bottle casts in deep waters off Hawaii and the Southern Ocean. We compared large-volume techniques, which rely upon Mn cartridges for the collection of dissolved 234Th and its detection via gamma counting (>200-l samples), with small volume methods that employed either direct beta counting, or beta counting after radiochemical purification (2–20-l samples). Unique to this study is the presentation of small volume (2 and 5 l) 234Th methods. This new technique is an adaptation of 20-l methods that are based on the coprecipitation of thorium with Mn oxides followed by direct beta counting of the precipitate. The small volume Mn coprecipitation methods were found to be superior to other methods due to ease of sample collection, processing and low overall analytical uncertainties. 相似文献
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LIU Sumei ZHAO Yingfei REN Jingling ZHANG Jing SUN San JIN Jie ZHANG Guiling 《海洋学报(英文版)》2010,29(1):42-51
Phosphorus (P) is an essential nutrient utilized by all organisms for energy transport and growth.
Both the conventional molybdenum-blue method and the magnesium-induced coprecipitation
(MAGIC) procedures were applied for the measurement of dissolved inorganic phosphorus (DIP)
and total dissolved phosphorus (TDP) in more than 840 water samples collected between 2003 and
2005, including seawater (the Huanghai Sea, the East China Sea, and the northern South China
Sea), water from rivers and estuaries (the Changjiang, the Huanghe, and the major rivers emptying
into the Jiaozhou Bay), groundwater (in the drainage basin surrounding the Jiaozhou Bay), rain-
water, and aquaculture water samples. The MAGIC method allows the investigation of phosphorus
distributions and cycling for systems in which DIP is below the detection limits of conventional
methods. Comparison between the two methods demonstrated that the concentrations obtained
with both methods were signiˉcantly correlated. The di?erences of DIP and TDP concentrations
measured with the two methods were higher when the concentrations of DIP and TDP were lower,
implying the lower reproducibility at low concentrations. The concentration di?erences increase
with the increase in the proportion of DOP in TDP, which indicates that the discrepancy of DIP
concentrations measured with the two methods increases when the DOP concentration is high. The
discrepancies indicated that the composition of P compounds di?ers depending on sample sources
and water type; it would be useful to infer the presence of di?erent phosphorus compound pools
from di?erences between the two methods. This study indicates the potential presence of a pool
of alkaline-labile compounds for samples from rainwater and rivers and estuaries surrounding the
Jiaozhou Bay; the potential presence of acid-labile compounds that were adsorbed by Mg(OH)2 for
samples from the Changjiang Estuary, Huanghai Sea, East China Sea, and groundwater; the po-
tential presence of a substantial pool of acid-labile compounds that were not adsorbed by Mg(OH)2
for samples from the Huanghe Estuary, aquaculture water, the East China Sea algal bloom water,
and the northern South China Sea. 相似文献
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Marine surficial sediments, intertidal molluscs and reed leaves collected in the Bay of Follonica are slightly contaminated by Pb, Ni, Zn and Fe. The main pollution sources are the waste water and the atmospheric emission of industrial plants. Probably, the weathering of the pyrite deposits along the eastern coast of Elba Island and adsorption and coprecipitation with hydrous Fe-Mn oxides increase the trace metal concentrations in sediments from the Piombino Channel. Mussels and limpets are contaminated by Hg because of the higher background level of the northern Tyrrhenian Sea. 相似文献
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Yoshimasa Toyota Shiro Okabe Satoru Kanamori Yasushi Kitano 《Journal of Oceanography》1983,38(6):357-361
A simple and rapid coprecipitation method for the determination of several trace metals in seawater is presented. These metals are coprecipitated with lanthanum hydroxide, the precipitate is dissolved, and then the metals are determined by atomic absorption spectrometry. Lanthanum hydroxide was chosen as a coprecipitant for the following reasons, (a) lanthanum hydroxide has a sufficiently low solubility and forms an easily filterable flocculate at about 80C, and (b) lanthanum has an absorption wavelength that is sufficiently separated from those of the other elements to be analysed, i.e., Mn, Fe, Ni, Cu and Zn. Experimental results show that these metals are coprecipitated by the present method with excellent recoveries. 相似文献
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Determination of total chromium on two profiles and chromium III on four samples of equatorial Pacific Ocean water have been carried out using coprecipitation of chromium from sea water with hydrous iron oxides, followed by ion-exchange separation and isotope dilution mass spectrometry. Results for two Pacific profiles show increasing total chromium concentration from surface to 250 m. The Cr concentration appears to be different below 1,000 m, with nearly homogeneous concentrations for the first profile and regularly increasing Cr concentrations from 0.330 to 0.550 μg/l at 3,900 m for the second one. Results for Cr(III) show that trivalent species are dominant in these samples. 相似文献
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《Marine Chemistry》1986,18(1):49-57
This work presents analytical evidence supporting the proposition that Pu(V) is the sole or predominant form of oxidized plutonium in natural waters. Two independent methods, the selective adsorption of Pu(VI) by silica gel, and the somewhat less selective coprecipitation of Pu(V) with calcium carbonate, were developed to separate Pu(V) from Pu(VI). Measurements of ambient plutonium in several natural waters by these methods found only Pu(V). In laboratory tracer studies, Pu(VI) was shown to be highly unstable in dilute bicarbonate solution and in Lake Michigan water, reducing in first-order fashion to Pu(V). 相似文献