Interspecies differences in heavy metal detoxication in oysters     

S.G. George  B.J. Pirie  J.M. Frazier  J.D. Thomson 《Marine environmental research》1984,14(1-4)

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Unevenly compressed flexural-gravitity waves     

A. E. Bukatov  A. M. Goncharov 《Physical Oceanography》1990,1(5):363-368

Free flexural-gravity waves unevenly compressed in an ice-covered basin have been studied using a linear formulation. The conditions were specified allowing determination of the bounds of the angular area of wave disturbances and of the oscillation frequency intervals due to compression. The paper considers the distribution of the wave characteristics over frequency depending on compressive stresses and the direction of wave propagation.Translated by Vladimir A. Puchkin.  相似文献   

Sea surface temperature and zooplankton, North Sea, 1948 to 1983   总被引：2，自引：0，他引：2  

Colebrook  J. M. 《ICES Journal of Marine Science》1985,42(2):179-185

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The Winter Distribution of Silicate in Southampton Water     

Banoub  M. W.; Burton  J. D. 《ICES Journal of Marine Science》1968,32(2):201-208

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On the nature of the calcareous substrate of a ferromanganese crust from the Vityaz Fracture Zone, Central Indian Ridge: inferences on paleoceanography     

M. Guptha  Ranadip Banerjee  Lina Mergulhao 《Geo-Marine Letters》2002,22(1):12-18

A 15-cm-thick carbonate substrate encrusted with ferromanganese oxides from the Vityaz Fracture Zone, Central Indian Ridge was analyzed to reconstruct the paleoceanography of the region. Based on the calcareous nannoplankton assemblage, an early Pliocene age has been assigned to the calcareous substrate. Among the nannoplankton, discoasters outnumber coccoliths and show signs of dissolution. The presence of certain species of benthic Foraminifera such as Uvigerina, Lenticulina, Bulimina and Bolivina, indicates the infringement of the oxygen minimum zone during the deposition of the carbonates. The occurrence of a Reticulofenestra pseudoumbilica zone of early Pliocene age suggests a change in depositional conditions coinciding with the time of formation of the large depositional hiatuses documented in sediment cores from adjacent basins of the western Indian Ocean. These hiatuses resulted from the prevalence of intermediate subsurface currents such as the Somali Current or the Western Boundary Current.  相似文献   

Subaerially exposed Late-Quaternary basinal shelf of the inner Mersin Bay,Eastern Mediterranean: Paleoenvironmental evidence     

M. Ergin 《Geo-Marine Letters》1996,16(2):95-100

High-resolution seismic profiles and petrographic data from surface and subsurface sediment samples from Mersin Bay, together with lithologic data from boreholes, were used to determine the origin and distribution of the pre- or early-Holocene unconformities in Mersin Bay (eastern Mediterranean). Reflectors corresponding to unconformities separate the younger, unconsolidated, marine transgressive sediments (Holocene) from the underlying, relatively coarser, consolidated sediments (Plio-Pleistocene). These unconformities correspond mainly to the erosional and subaerially deposited or later subaerially weathered land surfaces. These unconformities are probably related to the latest Pleistocene or earliest Holocene sea-level low stands.  相似文献   

On the 75th anniversary of the Department of Atmospheric Physics of St. Petersburg State University     

G. S. Golitsyn  Yu. M. Timofeev 《Izvestiya Atmospheric and Oceanic Physics》2007,43(4):397-398

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An improved specific interaction model for seawater at 25°C and 1 atmosphere total pressure     

M. Whitfield 《Marine Chemistry》1975,3(3):197-213

Equations recently developed by Pitzer are applied to a seawater model on the assumption that only interactions between ions of opposite charge sign are significant. This model is shown to give good agreement with available experimental data for the osmotic coefficient and for the mean-ion activity coefficients of the major electrolyte components. The results are compared with the predictions of the ion-association model and with a number of models using the concept of specific ionic interaction. The relative merits of the various models are discussed. Pitzer's original equations are modified to enable the calculation of conventional single-ion activity coefficients. These values are compared with those obtained on the basis of alternative conventions and an encouraging measure of agreement is observed. It is concluded that the new model introduces a fluency into the specific interaction approach that should greatly facilitate the incorporation of trace components into future models.  相似文献   

Remote determination of momentum-flux profiles in the lower atmospheric boundary layer     

R. D. Kouznetsov  V. F. Kramar  M. A. Kallistratova 《Izvestiya Atmospheric and Oceanic Physics》2006,42(6):696-703

An acoustic locator—a sodar—is a unique instrument for getting the objective characteristics of the current state of the atmospheric boundary layer (ABL) owing to a combination of such properties as remoteness, mobility, resolution, and information content. This study demonstrates the capabilities of a sodar to obtain data on the second moments of the field of wind-velocity fluctuations, in particular, the profiles of momentum flux in the lower ABL, which are very important in practical applications. A corresponding method is described, and the results of its experimental verification and some examples of its application under the conditions of different ABL stratification are presented.  相似文献   

On the collapse of a vertical packet of mixed patches. Laboratory and field studies     

A. M. Kudin  A. N. Lozhkin  A. V. Kholoptsev 《Physical Oceanography》1992,3(5):343-348

Visualization of a collapsing vertical packet of patches in a laboratory experiment and the results of acoustical sounding under field conditions allowed us to discriminate the stage of its evolution which was previously unknown. It is defined by the variations of the horizontal dimensions of patches and their effective scattering surface with a period ofT=150–250/N, whereN is the Brunt-Väisälä frequency. The horizontal dimensions of patches can reach 40% of their final dimensions at the evolution stage discriminated.Translated by Mikhail M. Trufanov.  相似文献