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利用美国甚长基线阵,在5GHz和8GHz波段观测致密对称源(CSO)OQ208,由获得的总流量图均显示OQ208是由2个主要的射电结构组成。5GHz波段在该源西南(SW)部分和东北(NE)部分都探测到2个子源。8GHz波段在该源(SW)部分探测到2个子源,而在(NE)部分探测到3个子源。在5GHz波段,根据子源A和D自1993年到2001年间的5个时段VLBI观测成图结果,拟合出它们的分离速度为0.037±0.006mas/a(年)。在8GHz波段,根据1994年到2002年间的9个时段观测数据,获得子源A和C的分离速度为0.046±0.009mas/a。 相似文献
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A Three-Dimensional Global Model Study of Carbonyl Sulfide in the Troposphere and the Lower Stratosphere 总被引：4，自引：0，他引：4
Erik Kjellström 《Journal of Atmospheric Chemistry》1998,29(2):151-177
Global distributions of carbonyl sulfide and carbon disulfide have been calculated with a three-dimensional global model of the atmospheric general circulation (ECHAM). The model calculates a global sink strength for carbonyl sulfide of 0.3 Tg S yr-1, with vegetation uptake being the largest sink. With this sink strength, the sources have to be close to the lower limit of the present estimate in the literature. The calculated mixing ratios are higher in the Southern Hemisphere than in the Northern Hemisphere. This interhemispheric gradient is the opposite of what is observed demonstrating that the present knowledge of the distribution of sinks and sources is not fully adequate. The model calculations support the idea that the open oceans could act as a net sink of carbonyl sulfide. The calculated stratospheric photolysis of carbonyl sulfide constitutes about 4% of the total sink of carbonyl sulfide. A stratospheric production of sulfate from carbonyl sulfide of 0.013 Tg S yr-1 is obtained, which is 3 to 12 times less than what is needed to maintain the stratospheric sulfate aerosol layer. Although these results are associated with uncertainties, due to the low upper boundary and coarse vertical resolution of the model, they support recent findings of a low stratospheric production of sulfate from carbonyl sulfide. Instead, sulfur dioxide transported from the troposphere is calculated to be the most important precursor for the stratospheric sulfate aerosol layer. 相似文献
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N. Mihalopoulos J. P. Putaud B. C. Nguyen S. Belviso 《Journal of Atmospheric Chemistry》1991,13(1):73-82
Measurements of the concentrations of carbonyl sulfide (COS) in the marine atmosphere were made over a period of two years in the southern Indian Ocean (Amsterdam Island, 37°50 S–77°31 E; March 1987–February 1988 and April 1989–February 1990). The mean atmospheric COS concentration for the whole period was 475±48 pptv (n=544). Atmospheric COS concentrations show no significant seasonal variation with a summer to winter ratio of 1.05. Taking into account the observed variability of the atmospheric COS concentration (10%), a value of 1.4 yr is estimated as a lower limit for the atmospheric COS lifetime. A comparison of the COS data at Amsterdam Island with those obtained in the Southern Hemisphere in the past 12 yr does not reveal any significant trend in the tropospheric background COS mixing ratio. 相似文献
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地形校正可以减小地形起伏对地物光谱的影响,提高计算机分类在山区的精度。设计了针对全球土地覆盖分类的Landsat TM/ETM+数据地形校正方法 SCOS(Smoothed COS余弦),首先对地形的坡度角进行抹平处理,很大程度上削弱了地表非朗伯性对地形校正的影响,然后利用简单有效的余弦校正去除地形效应。该方法与其他常用地形校正算法的对比分析是通过对全球不同区域、不同地表覆盖的有代表性的6景Landsat TM/ETM+数据的试验,采用统计分析与目视判读的方式,从过度校正和类内均一性两个方面进行的。结果表明,该方法在目视效果和统计结果上优于常规方法,并且更加简单有效,无需复杂的大气参数及传感器参数,满足全球地表覆盖分类对地形校正的需求。 相似文献
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本研究应用具有不同电荷性的褐藻寡糖(ADO)和壳寡糖(COS)处理大麦种子,探索在相同条件下不同浓度的海洋寡糖对大麦幼苗生长情况及生理特性的影响。生长指标包括苗长、根长、苗重及根重,以及对大麦种子淀粉酶活力和叶绿素含量的影响。试验结果表明:当ADO和COS处理浓度分别为0.5%和0.025%时,大麦的各项生长指标、种子淀粉酶活力及叶绿素含量均达到最大值,与对照组相比显著增加(P<0.05)。2种海洋寡糖均是具有独特生理活性的分子片段,分子量大小相近,但基于2种寡糖分子结构的不同,造成在对大麦的促生长方面存在差异性,为以后2种海洋寡糖的合理开发利用提供了参考。 相似文献
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B. C. Nguyen N. Mihalopoulos J. P. Putaud B. Bonsang 《Journal of Atmospheric Chemistry》1995,22(1-2):55-65
Carbonyl sulfide emissions from biomass burning have been studied during field experiments conducted both in an African savanna area (Ivory Coast) and rice fields, central highland pine forest and savanna areas in Viet-Nam. During these experiments CO2, CO and C2H2 or CH4 have also been also monitored. COS values range from 0.6 ppbv outside the fires to 73 ppbv in the plumes. Significant correlations have been observed between concentrations of COS and CO (R
2=0.92,n=25) and COS and C2H2 (R
2=0.79,n=26) indicating a COS production during the smoldering combustion. COS/CO2 emission factors (COS/CO2) during field experiments ranged from 1.2 to 61×10–6 (11.4×10–6 mean value). COS emission by biomass burning was estimated to be up to 0.05 Tg S/yr in tropics and up to 0.07 Tg S/yr on a global basis, contributing thus about 10% to the global COS flux. Based on the S/C ratio measured in the dry plant biomass and the COS/CO2 emission factor, COS can account for only about 7% of the sulfur emitted in the atmosphere by biomass burning. 相似文献
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本研究测定了壳寡糖对海南热带糙海参(Holothuria scabra)体腔液和体壁组织中免疫相关因子,酸性磷酸酶(ACP)、碱性磷酸酶(AKP)、溶菌酶(LSZ)和溶血素活性的影响。结果表明,投喂0.5%壳寡糖对糙海参体腔液中AKP、ACP、LSZ和溶血素活性均有明显增强作用(P0.05),其中对ACP和LSZ活力有极显著的影响(P0.01),且投喂6 d内活性均持续增强;0.5%壳寡糖对体壁组织匀浆液中AKP、ACP活性明显增强(P0.05),但随着时间延长,对体壁组织中LSZ和溶血素作用不明显。壳寡糖可以提高海南热带糙海参(Holothuria scabra)的非特异性免疫力。 相似文献
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Jonny Hesthammer Aristofanis Stefatos Mikhail Boulaenko Alexander Vereshagin Peter Gelting Torolf Wedberg Gregor Maxwell 《Marine and Petroleum Geology》2010
The use of the controlled source electromagnetic (CSEM) method as a risk reduction tool in marine hydrocarbon exploration is gaining increased acceptance in the oil industry. This is related to the ability to map resistivity contrasts in the sub-surface and thus aid the detection of hydrocarbons which are typically more resistive than surrounding rocks. Whereas acoustic (seismic) energy allows for mapping sub-surface structures that may contain hydrocarbons, electromagnetic (EM) energy can often say something about the fluids contained within the structures. Numerous successful CSEM case stories have been published over the past several years. However, there are also quite a few stories about “failure”-cases, although not well documented in the literature. Such “failure”-cases may reflect the lack of understanding of the CSEM technology and how CSEM data can act as a value driver. In order to understand this, it is necessary to handle uncertainties and decisions associated with the technology, These include geological uncertainties, noise models, survey designs, forward modelling parameters, inversion/migration parameters and pre-processing of real data. A proper handling of these uncertainties and decisions will aid in defining and constraining the chance of geologic success and geologic-success-case net present value for prospects prior to drilling wells. As such, the CSEM technology has a significant potential to increase exploration efficiency, if applied correctly. 相似文献
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