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251.
The resolution of ocean reanalysis datasets is generally low because of the limited resolution of their associated numerical models. Low-resolution ocean reanal... 相似文献
252.
253.
A constrained LAMBDA method for GPS attitude determination 总被引:4,自引:0,他引:4
An improved method to obtain fixed integer ambiguity in GPS attitude determination is presented. Known conditions are utilized
as constraints to acquire attitude information when the float solution and its variance–covariance matrix are not accurate
enough. The searching ellipsoidal region is first expanded to compensate for errors caused by the inaccurate float solution.
Then the constraints are used to shrink the region to a proper size, which maintains the true integer ambiguity. Experimental
results demonstrate that this scheme gives a fast search time and a higher success rate in determining the fixed integer ambiguity
than the unconstrained method. The accuracy of attitude angles is also improved.
相似文献
Bo WangEmail: |
254.
Sulfide and iron control on mercury speciation in anoxic estuarine sediment slurries 总被引:2,自引:0,他引:2
Seunghee Han Anna Obraztsova Patrizia Pretto Dimitri D. Deheyn Joris Gieskes Bradley M. Tebo 《Marine Chemistry》2008,111(3-4):214-220
In order to understand the role of sulfate and Fe(III) reduction processes in the net production of monomethylmercury (MMHg), we amended anoxic sediment slurries collected from the Venice Lagoon, Italy, with inorganic Hg and either potential electron acceptors or metabolic byproducts of sulfate and Fe(III) reduction processes, gradually changing their concentrations. Addition of sulfide (final concentration: 0.2–6.3 mM) resulted in an exponential decrease in the sulfate reduction rate and MMHg concentration with increasing concentrations of sulfide. Based on this result, we argue that the concentration of dissolved sulfide is a critical factor controlling the sulfate reduction rate, and in turn, the net MMHg production at steady state. Addition of either Fe(II) (added concentration: 0–6.1 mM) or Fe(III) (added concentration: 0–3.5 mM) resulted in similar trends in the MMHg concentration, an increase with low levels of Fe additions and a subsequent decrease with high levels of Fe additions. The limited availability of dissolved Hg, associated with sulfide removal by precipitation of FeS, appears to inhibit the net MMHg production in high levels of Fe additions. There was a noticeable reduction in the net MMHg production in Fe(III)-amended slurries as compared to Fe(II)-amended ones, which could be caused by a decrease in the sulfate reduction rate. This agrees with the results of Hg methylation assays using the enrichment cultures of anaerobic bacteria: whereas the enrichment cultures of sulfate reducers showed significant production of MMHg (4.6% of amended Hg), those of Fe(III), Mn(IV), and nitrate reducers showed no production of MMHg. It appears that enhanced Fe(III)-reduction activities suppress the formation of MMHg in high sulfate estuarine sediments. 相似文献
255.
Kosuke Mori Takeshi Matsuno Tomoharu Senjyu Naoki Hirose In-Seong Han 《Journal of Oceanography》2009,65(3):301-310
Temporal variations in temperature and salinity observed in 2004 were investigated on a short time scale in the Tsushima Strait.
The data were obtained by long-term in situ measurements at Mitsushima and Futaoi Island using an instrument equipped with
a piston-type wiper to avoid biofouling. In addition, the temperature and salinity values of the surface layer obtained by
a commercial ferryboat between Hakata and Busan were used to investigate their spatiotemporal variations. Temperature and
salinity variations with a time scale of several days had a negative correlation in the summer. This evidence suggests that
a warm and less saline water mass, which is considered to be mainly the Changjiang Diluted Water (CDW), flowed intermittently
through the Tsushima Strait in summer. In late July 2004, a large low-salinity water mass was detected in the Tsushima Strait.
At that time, the freshwater transport through the Tsushima Strait transiently reached about 12 × 104 m3s−1, which is estimated from observed acoustic Doppler current profiler (ADCP) data along a ferryboat line and inferred salinity
profiles. This estimated value is more than double the maximum of the climatological monthly mean of the Changjiang discharge.
Furthermore, salinity and surface current data obtained by high frequency ocean radar (HF radar) indicate that water properties
at Mitsushima may occasionally represent part of the water flowing through the western channel via a countercurrent, although
Mitsushima is geographically located in the eastern channel. 相似文献
256.
???????????????????????????????????Kalman????????????????????????????????????????????????????????????в????? 相似文献
257.
258.
淹没不整合型层序——一种特殊的加深淹没 总被引:1,自引:0,他引:1
淹没不整合型层序以其凝缩层直接覆盖于层序界面上,即凝缩层+高水位体系域层序类型为特征,以不含有任何暴露证据而区别于层序地层学定义的Ⅰ型和Ⅱ型层序界面,成为碳酸盐地层层序中的一种特殊类型的三级旋回层序界面。以淹没不整合型层序的特征描述、鉴别方法和实例分析阐述了淹没不整合是一种旋回层序的特殊类型即加深淹没型层序界面。这种淹没不整合型层序在油气运移方面起着重要作用。 相似文献
259.
本文提出了一种基于冷冻脱盐的海水双级冷冻预淡化系统。该系统利用蒸发结晶器对海水进行冷冻,并通过振动分离与洗涤实现冰晶与卤水的分离,以此实现海水的初步脱盐,可作为反渗透淡化的预处理系统。同时,海水冷冻淡化过程中消耗的冷量可重新回收用于空调制冷,淡化成本得以有效降低。本文建立了海水双级冷冻预淡化系统的数学模型,获得了试验系统的关键设计参数,以此搭建了试验平台并完成了试验测试,并对海水双级冷冻预淡化系统进行了经济性分析。试验结果表明:经过海水冷冻预淡化系统,预淡化海水产量可维持在21~27 L/h之间;预淡化海水盐度可从35降低到约11;预淡化过程可回收总冷量7.91 kW;反渗透淡化总成本可降低约33%。 相似文献
260.