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81.
基于2018年8月至2019年5月布放在北极随海冰漂流的自动气象站和温度链浮标获取的观测数据,分析了北极高纬度区域的大气特征和海冰生消过程。根据海冰的漂移轨迹分为两个阶段分析,第1阶段,海冰主要向东南漂移;第2阶段,海冰主要向东北漂移。第1阶段观测的平均气温和平均相对湿度分别为–6.6℃和93%,第2阶段观测的平均气温和平均相对湿度分别为–29.3℃和76%,第2阶段平均气压高于第1阶段。海冰的漂移轨迹主要受到波弗特高压外围气流的影响。利用自动气象站漂移轨迹计算得到海冰漂移速度,与美国国家冰雪数据中心海冰漂移速度比较显示,两者纬向速度更为接近。海冰在第1阶段以融化为主,海冰厚度略有减小,8月份海冰生长率为–0.11 cm/d;海冰的生长过程主要发生在第2阶段,1–3月生长率均超过0.9 cm/d,2019年3月海冰生长最快,平均生长率为1.3 cm/d,海冰的增长一直持续至观测结束。 相似文献
82.
Mélina C.Z. Laurent Olivier Gros Jean-Pierre Brulport Françoise Gaill Nadine Le Bris 《Marine environmental research》2009,67(2):83-88
Large organic falls to the benthic environment, such as dead wood or whale bones, harbour organisms relying on sulfide-oxidizing symbionts. Nothing is known however, concerning sulfide enrichment at the wood surface and its relation to wood colonization by sulfide-oxidizing symbiotic organisms.In this study we combined in situ hydrogen sulfide and pH measurements on sunken wood, with associated fauna microscopy analyses in a tropical mangrove swamp. This shallow environment is known to harbour thiotrophic symbioses and is also abundantly supplied with sunken wood. A significant sulfide enrichment at the wood surface was revealed. A 72 h sequence of measurements emphasized the wide fluctuation of sulfide levels (0.1–>100 μM) over time with both a tidal influence and rapid fluctuations. Protozoans observed on the wood surface were similar to Zoothamnium niveum and to vorticellids. Our SEM observations revealed their association with ectosymbiotic bacteria, which are likely to be sulfide-oxidizers. These results support the idea that sunken wood surfaces constitute an environment suitable for sulfide-oxidizing symbioses. 相似文献
83.
In this paper AlGaInP light emitting diodes with different types of electrodes: Au/Zn/Au-ITO Au/Ti-ITO Au/Ge/Ni-ITO and Au-ITO are fabricated. The photoelectricity properties of those LEDs are studied. The results show that the Au/Zn/Au electrode greatly improves the performance of LEDs compared with the other electrodes. Because the Au/Zn/Au electrode not only forms a good Ohmic contact with indium tin oxide (ITO), but also reduces the specific contact resistances between ITO and GaP, which are 1.273×10-6 Ω · cm2 and 1.743×10-3 Ω ·cm2 between Au/Zn/Au-ITO and ITO-GaP respectively. Furthermore, the textured Zn/Au-ITO/Zn electrode is designed to improve the performances of LEDs, reduce the forward-voltage of the LED from 1.93 to 1.88 V, and increase the luminous intensity of the LEDs from 126 to 134 mcd when driven at 20 mA. 相似文献
84.
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86.
N. P. Bulgakov S. N. Bulgakov V. N. Davydova A. Z. Martinez 《Physical Oceanography》1999,10(2):107-121
On the basis of the data ofin situ measurements of the velocities of currents and basic hydrophysical parameters (such as temperature and salinity) carried
out during Cruise 41 of the R/VAkademik Vernadsky, we analyze the structure of the North Brazil Current near the continental slope and in the equatorial abyssal part of the
ocean in winter, establish the regularities of changes in the current velocity with depth, and compare the structures of the
North Brazil and Guiana Currents.
Translated by Peter V. Malyshev and Dmitry V. Malyshev 相似文献
87.
DGPS(DifferentialGlobalPositioningSystem)测量技术即差分定位技术,包括实时差分和后处理差分定位技术,正在远海和近海测量中得到广泛应用。后处理差分定位与微波定位及GPS实时差分定位相比,具有作用距离远,不受基准台与船台之问的障碍物影响以及减少基准台等优点。对于近海大比例尺(大于1:1万)测量,可采用实时差分定位的方法,而小于1:1万中小比例尺海底地形图测绘及海上其他工程测量,采用后处理差分定位,既能满足精度要求,又能提高工作效率。本文主要介绍利用DGPS后处理定位方法,在测绘广西沿海1:5万海底地形图中的应用情况。 相似文献
88.
D. J. Fan R. D. Neuser X. G. Sun Z. S. Yang Z. G. Guo S. K. Zhai 《Geo-Marine Letters》2008,28(1):7-14
Estuaries are elementary geochemical fronts where river water and seawater mix. Within this mixing zone, iron and other non-conservative
elements can undergo complex reactions to form new solid phases. In order to understand authigenic iron oxide formation in
the Yangtze River Estuary, two onsite water-mixing sets of experiments were conducted, one by mixing variable amounts of unfiltered
Yangtze River water with filtered East China Sea water of different salinity (set 1), the other by mixing variable amounts
of filtered Yangtze River water with filtered East China Sea water of different salinity (set 2). In set 2, the minerals newly
formed in the course of mixing were investigated by means of a scanning electron microscope fitted with an energy-dispersive
X-ray analytical system. It was found that ferrihydrite and lepidocrocite were formed in these mixing experiments, coexisting
in nearly equal amounts. These iron oxides appear as aggregated particles with a large grain-size range of several microns
to more than 100 μm. The electrolytic properties of seawater played an important role in the formation of these authigenic
iron oxides. Kaolinite and organic aggregates were also found in the experimentally mixed pre-filtered waters. Amounts of
newly formed suspended matter (set 2) were one to three orders of magnitude lower than those of total suspended matter (TSM)
(set 1). This implies that newly formed minerals represent only a very small proportion of TSM in the estuarine mixing zone
of the Yangtze River. 相似文献
89.
It is a good test for a numerical model to simulate progressive waves propagating over a submerged bar with a relatively high ratio of slopes. In this paper, the combined IB–VOF model is used to predict nonlinear dispersive waves propagating over a submerged bar with both slopes of 1:2. The predicted free surface elevations are compared with the experimental data and numerical results presented by other researchers. The comparison shows that the IB–VOF model is able to provide satisfactory wave profiles in the shallow water with strong nonlinear effects and in the wave transmitted region with strong wave dispersion in particular. Moreover, the wave evolution behind the submerged bar is described in detail, including the spatial wave profile modulation, spectral analysis of the time-series waves, flow velocity and pressure fields, and kinetic energy distribution. The effect of fluid viscosity on the numerical simulations is also studied, and it is found that the effect on the wave evolution considered in this paper is not significant. Finally, the hydrodynamic force acting on the bar is calculated using the IB–VOF model. 相似文献
90.
J. O. Z. Abuodha 《Marine Georesources & Geotechnology》2013,31(3):199-207
This article addresses both environmental and socioeconomic issues concerned with the development or operation of the envisaged titanium mining project in Kwale District of Kenya. TIOMIN Resources Inc., of Canada, through its wholly owned Kenyan subsidiary, Kenya Titanium Minerals Ltd., is proposing to develop a titanium sands mine and mineral processing plants which will produce high grades of heavy minerals including rutile, ilmenite, and zircon. In addition, TIOMIN has proposed to develop a ship loading facility at Shimoni, a significant marine habitat in Kenya. When properly designed and implemented, an Environmental Impact Assessment (EIA) is a powerful tool for ensuring that environmental issues are given due consideration during project design, allowing the benefits of the project to be maximized, while reducing the environmental and social costs of development. In Kenya, the EIA has to be conducted according to the requirements of the Kenya Environmental Management and Co-ordination Act (2000) and in compliance with World Bank standards. An EIA document submitted to the enforcement authority, National Environmental Management Authority (NEMA), enables the issuing of an Environmental Impact Assessment License and a Mining License. A number of exploration studies have been undertaken and several sites have been identified for the extraction of titanium minerals and zircon. Many have expressed concern that environmental matters should be considered before a decision about titanium mining is undertaken. Toxic chemicals used in heavy mineral separation processes and disturbance or redistribution of sediment could spell a disaster for the coastal waters. The Wasini channel is home to world class coral reefs, humpback and spotted dolphins, and marine turtles. Another contentious issue is that of radioactivity associated with the minerals zircon and monazite. The coastal zone is a crucial part of the economy, as it supplies a living for a large number of people along the coast. It is envisaged that involuntary resettlement without adequate compensation and viable alternative sites may result in serious socioeconomic consequences. 相似文献