特殊动力作用在海洋生物中的研究进展   总被引：2，自引：1，他引：1  

钱周兴  方一峰 《海洋学研究》2005,23(3):30-35

由摄食而引起的特殊动力作用(SDA)使动物在处理和转化食物时需要额外消耗能量。阐述了SDA的含义及其研究参数,讨论了目前国内外对SDA研究的主要途径及不同的研究重点,探讨了影响SDA耗能的主要因素,指出了SDA与动物生长之间的关系。从两方面的研究角度考虑,展望了研究SDA的前景和意义。  相似文献   

Speeding Up the Analytical Workflow for Coltan Fingerprinting by an Integrated Mineral Liberation Analysis/LA‐ICP‐MS Approach     

Hans‐Eike Gäbler  Frank Melcher  Torsten Graupner  Andreas Bahr  Maria A. Sitnikova  Friedhelm Henjes‐Kunst  Thomas Oberthür  Helene Brätz  Axel Gerdes 《Geostandards and Geoanalytical Research》2011,35(4):431-448

Coltan (the African trade name for columbite‐tantalite, a tantalum ore) is one of several raw materials that finance the civil wars in the eastern provinces of the Democratic Republic of the Congo. To improve the transparency along the tantalum trade chain, a ‘certificate of origin’ for so‐called ‘conflict minerals’ has been recommended by the United Nations. Accordingly, the German Federal Institute for Geosciences and Natural Resources (BGR) has developed an analytical fingerprint procedure for coltan. Mineral formation age, modal mineralogy and chemical composition are important fingerprint parameters. The original workflow to obtain these parameters was streamlined and is now based on mineral liberation analysis and LA‐ICP‐MS. The use of an ICP‐MS instrument with a detector system covering an extended linear dynamic range and the application of an internal standard‐independent calibration strategy allowed data for major and trace element determination and mineral formation age estimates to be obtained simultaneously. The analytical results of this new approach were compared with analytical techniques of the original workflow and showed excellent agreement in terms of mineralogical and chemical characterisation and mineral formation age of coltan samples. Within a test, samples of different origin were allocated correctly and simple, binary mixtures were also identified successfully.  相似文献   

Silicifications pédogénétiques dans les dépôts hamadiens du piémont de Boudenib (Maroc)     

Médard Thiry  Mohamed Ben Brahim 《Geodinamica Acta》2013,26(4):237-251

Résumé

— Le système de piémont atlasique du Sud marocain, d’âge tertiaire, est constitué dans le secteur de Boudenib de deux unités distinctes. La llamada de Boudenib forme l’unité inférieure et se caractérise par d’importants encroûtements carbonatés, riches en dolomite et attapulgite. L’unité supérieure de la llamada du Cuir marque une reprise de l’érosion et le dépôt de matériaux relativement peu altérés.

Des silicifications affectent les différents faciès de l’unité inférieure, ainsi que les grès crétacés sous-jacents, et jalonnent une surface d’érosion intra-fonnationnelle. Ces silicifications sont précoces, puisque remaniées dans les dépôts ultérieurs. Les illuviations d’opale et les accumulations gramdaires intercalées entre les concrétionnements successifs de silice attestent d’environnements pédologiques. La silicification plus forte vers la partie supérieure des coupes, ainsi que l’association fréquente des faciés silicifiés avec des niveaux hioturhés et altérés sont également à rapporter à des dispositions pédologiques. Ce sont des silcréles pédogénétiques.

L’étude micrographique montre que la silicification procède par épigénie des argiles et des carbonates, ainsi que par des cristallisations dans les vides. C’est à partir des vides existants (fentes, bioturbations et porosité intergranulaire) que se développe la silicification, montrant ainsi le rôle primordial des circulations. En particulier, l’épigénie des carbonates par la silice semble limitée par la diffusion de la silice à partir des vides, où le renouvellement des solutions est assuré. Les séquences de cristallisation des différentes formes de silice (allant de l’opale vers les quartz automorphes) peuvent être interprétées en terme d’évolution du milieu au cours de la silicification. Au fur et à mesure que des dépôts de silice se font sur les parois des vides, les solutions nourricières sont isolées de la roche encaissante, elles se chargent alors moins en cations étrangers, et la cristallisation de plus grands cristaux peut intervenir.

Les silicifications se développent pendant une période de stabilité tectonique et s’installent dans un paysage de glacis et sous des climats chauds à saisons alternées. Leur reconnaissance à l’échelle régionale peut constituer un repère lithostratigraphique précieux.  相似文献   

Ionic surfactants adsorption on heterogeneous surfacesAdsorption de tensioactifs ioniques sur les surfaces hétérogènes     

Jean-Maurice Cases  Jerzy Mielczarski  Ella Mielczarska  Laurent J. Michot  Frédéric Villiéras  Fabien Thomas 《Comptes Rendus Geoscience》2002,334(9):675-688

The adsorption of surfactants from aqueous solution is a phenomenon of major importance in applications ranging from ore flotation and paint technology to enhanced oil recovery. As this paper will illustrate, the process is very complex and of high scientific interest; its results can be extended to the retention of organic compounds (humic and fulvic acids, pollutants...) on solids in the biosphere. For a good understanding of the mechanisms involved in surfactants adsorption at the hydrophilic solid–aqueous solution interface, thermodynamic models have to take into account: (i) the physical chemistry of the surfactant in aqueous solution for choosing the appropriate reference phase, (ii) the surface heterogeneity of the adsorbing solid, (iii) the intensity of normal adsorbate–adsorbent bonds responsible for adsorption, (iv) the intensity of lateral bonds that favour the formation of surface aggregates through cooperative process and finally, (v) suitable theoretical models to describe adsorption phenomena. Once this has been achieved, two systems can be discussed: systems characterised by strong normal adsorbate–adsorbent bonds, currently used in ore flotation, which lead, in the case of heterogeneous surfaces, to the formation of lamellar aggregates at monolayer concentration and bilayer formation for higher concentrations. Systems characterised by weak normal adsorbate–adsorbent bonds, currently used in enhanced oil recovery and hydrocarbon (bio)remediation, which correspond to: (i) formation of globular micelles at the solid surface near the CMC when the temperature is higher than the Krafft point, (ii) formation of bilayered lamellar aggregates in the opposite case, (iii) three-dimensional condensation on substrate (T<T_Krafft) if the ionic surfactant interacts with cations in the bulk. To cite this article: J.-M. Cases et al., C. R. Geoscience 334 (2002) 675–688.  相似文献   

Signification des ferruginisations des formations néoprotérozoı̈ques du Nord-Burkina Faso (Afrique de l'Ouest)Meaning of ironstones in the sedimentary Neoproterozoic formations of the northern Burkina Faso (western Africa)     

Alain Blot 《Comptes Rendus Geoscience》2002,334(12):909-915

There are many small ferruginous outcrops of different facies, often breccia-like, in the Neoproterozoic sedimentary formations in northern Burkina. These outcrops are made up of goethite and quartz, and are often along with high grades of various elements. It could be a question of gossans. Their large distribution in this part of the Taoudéni Basin offers it prospects as a province geochemically rich in Cu, Pb, Zn, Mo, As, Cd, Co... This basin would be a geochemical bin for ancient formations, which would have been evacuated before the Neoproterozoic. The ironstones would be the mark of further concentrations. To cite this article: A. Blot, C. R. Geoscience 334 (2002) 909–915.  相似文献   

Growth, feeding, production, and consumption in 0-group bib (Trisopterus luscus L.) and whiting (Merlangius merlangus L.) in a shallow coastal area of the south-west Netherlands     

Hamerlynck  Olivier; Hostens  Kris 《ICES Journal of Marine Science》1993,50(1):81-91

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饵料种类和摄食水平对中国对虾蜕皮的影响   总被引：8，自引：2，他引：8  

黄国强  董双林  王芳  马甡 《中国海洋大学学报(自然科学版)》2004,34(6):942-948

采用鱼肉、虾肉、蛤肉、沙蚕、配合饲料和以上 5种饵料的等干重混合物投喂体重为 ( 1.5 3 0± 0 .0 47) g的中国对虾 3 0d ,并对体重分别为 ( 2 .988± 0 .2 0 0 )g ,( 7.960± 0 .45 0 ) g ,( 14 .177± 0 .868) g ,( 19.0 12± 1.413 )g 4个规格的中国对虾采用配合饲料分别按每天体重 0 % ,0 .5 % ,1.0 % ,1.5 %和过量 5个摄食水平进行投喂 2 8d ,对中国对虾的蜕皮进行了研究。实验结果证明 ,饵料种类对中国对虾的蜕皮次数 (MT)、蜕皮量、蜕皮能占摄食能的比例及每次蜕皮的体重增长都有显著影响。实验期间中国对虾的蜕皮次数范围为 2 .3 1～ 3 .98次 ,蜕皮能占摄食能的比例为 1.16%～ 2 .72 % ,每次蜕皮的体重增长为 0 .14 1～ 0 .488g。不同摄食水平对中国对虾的蜕皮能占摄食能的比例及每次蜕皮的体重增长都有显著影响 ,前者随摄食水平的提高而下降 ,后者随摄食水平的提高而增加。摄食水平对 ( 2 .988± 0 .2 0 0 ) g的对虾的蜕皮次数 (MT)和蜕皮的干重、氮含量、能量的影响较大 ,而对其余 3个规格的对虾影响较小。摄食水平对对虾每次蜕皮的干重、氮含量、能量及单位体重每次蜕皮的干重、氮含量、能量的影响仅表现为饥饿或较低摄食水平与其它摄食水平差异显著 ,而更高的摄食水平对它们没有显著影响。  相似文献   

The rise of trees and their effects on Paleozoic atmospheric CO₂ and O₂     

Robert A. Berner 《Comptes Rendus Geoscience》2003,335(16):1173-1177

The rise of large vascular plants during the mid-Paleozoic brought about a major increase in the rates of weathering of silicate minerals that induced a drop in the level of atmospheric CO₂ and contributed, via the atmospheric greenhouse effect, to global cooling and the initiation of the most long lived and a really extensive glaciation of the past 550 million years. Sedimentary burial of the microbiologically resistant remains of the plants resulted during the Permo-Carboniferous in both further lowering of CO₂ and in elevation of atmospheric O₂. Evidence of changes in CO₂ and O₂ are provided by mathematical models, studies of paleosols, fossil plants, fossil insects, and the effects of modern plants on silicate weathering, and by laboratory studies of the effects of changes in O₂ on plants and insects. To cite this article: R.A. Berner, C. R. Geoscience 335 (2003).  相似文献   

Structure et caractérisation des matériaux utilisés dans la construction d'une mosaı̈que romaine de la cité de Volubilis (Maroc)     

Abdelilah Dekayir  Marc Amouric  Juan Olives  Claude Parron  Abdelilah Nadiri  Abdelkader Chergui  M.Abdeljalil El Hajraoui 《Comptes Rendus Geoscience》2004,336(12):1061-1070

In Volubilis, Roman mosaics are very beautiful and reveal, from the bottom to the surface, three layers: (i) ‘hedgehog’ layer, (ii) coarse grain mortar layer (rudus + nucleus) and (iii) tesselatum. Mineralogical analysis of coarse grain mortar sampled in Flavius Germanus mosaic shows that it consisted of quartz and calcite, with some feldspar and probably mica and dolomite. Fine-grained mortar in tesselatum is made from a mixture of calcite and quartz only. Limestone tesserae (white, pink and brown) show petrographic facies that change from micritic to oolithic limestone. Conversely, black and brick red tesserae are respectively made of marble, red sandstone and from fire clay. Other colours as yellow, blue, green and grey are obtained from artificial glass with different chemical compositions. To cite this article: A. Dekayir et al., C. R. Geoscience 336 (2004).  相似文献   

CFG桩复合地基现场试验及有限元模拟分析   总被引：5，自引：0，他引：5  

黄生根 《岩土力学》2008,29(5):1275-1279

在厚褥垫状态或路堤荷载作用下复合地基的破坏主要取决于桩-褥垫体系的作用,复合地基中单桩的承载力远未发挥出来。由有限元计算结果得出以下规律：(1) 随着褥垫厚度增加,桩土应力比减小;褥垫厚度超过300 mm后,褥垫厚度的影响急剧减小;褥垫厚度超过500 mm后,褥垫厚度的影响继续减小。(2) 褥垫厚度较薄时（ 100 mm）,褥垫模量对桩土应力比影响很大;褥垫厚度超过300 mm时,褥垫模量对桩土应力比的影响减小;褥垫厚度达到500 mm后,褥垫模量对桩土应力比影响很小。(3) 承载板刚度小于6.25 MN•m2时,桩土应力比随刚度增大;承载板刚度大于6.25 MN•m2时,刚度对桩土应力比的影响很小。  相似文献