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1.
魏雅娜  杨世平 《海洋学报》2010,32(10):7298-7305
利用半经典再散射模型研究了激光强度在一定范围内时分子核间距对非时序双电离过程的影响.分别计算了非时序双电离率、两电子的电离能、两电子的动量相关、Coulomb和激光场的复合势随分子核间距的变化关系.研究表明,分子核间距在1.0—6.0 a.u.范围内时,非时序双电离率和两电子动量和为零的双电离事件数随着分子核间距的增大而增大.当分子核间距继续增大(大于6.0 a.u.)时,非时序双电离率和两电子动量和为零的双电离事件数却减小.  相似文献   

2.
宋婷婷  何捷  林理彬  陈军 《海洋学报》2010,32(9):6480-6486
本文利用第一性原理方法研究了金红石相和单斜相VO2晶体的电子结构和热力学性质.在计算中采用局域密度近似结合Hubbard U模型(LDA+U)描述电子的局域强关联效应,同时也利用微扰密度泛函方法计算了两种相结构的声子谱.计算结果表明V原子3d电子轨道中x2-y2轨道能级分裂决定了VO2晶体在不同相结构下的金属和绝缘体特性.零温状态方程计算揭示了在68 GPa时可以发生从单斜结构  相似文献   

3.
吴小霞  王乾恩  王福合  周云松 《海洋学报》2010,32(10):7278-7284
基于密度泛函理论,在广义梯度近似下研究了Cl在γ-TiAl(111)表面的吸附.计算结果表明:γ-TiAl(111)表面的面心立方位置(fcc)和六角密排位置(hcp)为Cl吸附的稳定位置,当覆盖度Θ小于一个单层(ML)时,Cl原子倾向于吸附在γ-TiAl(111)表面近邻为多Ti的位置.电子结构分析发现,Cl原子同表面金属原子形成较强的离子键,并且成键具有一定的方向性.当Cl原子和O原子共同在γ-TiAl(111)表面吸附时,二者都趋  相似文献   

4.
蛟龙号载人潜水器在位于雅普海沟北部6 745 m深处的底栖沉积环境中采集到两只石鳖样本,这是石鳖物种分布于此的新记录。形态学和DNA分子标记均支持两只石鳖为鳞侧石鳖属(Leptochiton)同一物种。该种在形态上与L.vanbelleiL.deforgesi接近;在系统发生方面,与L.vanbellei,L.deforgesiL.boucheti的亲缘关系密切。这是截至目前世界石鳖分布报道的第三深度记录。  相似文献   

5.
提出了一种介质加载折叠波导慢波结构,给出了该结构中存在电子注时慢波互作用的热色散方程,在介电常数εr=1的特殊情况下该方程即简化为普通折叠波导的小信号工作方程.在给定慢波结构尺寸的基础上,分析比较了介质加载对放大器小信号增益特性的影响,结果表明:"弱加载"(介质厚度d/a<0.1)时,无需重新设计慢波结构的参数,只需适当调整工作电压和电流就可以满足原有设计要求,而且和未加载时相比增益特性更为平坦,降低的电子注阻抗也有利于电子效率的提高.考虑到  相似文献   

6.
利用常规高空资料、地面加密自动站、双偏振多普勒天气雷达、微波辐射计与ERA5再分析数据等多源资料,分析了2021年2月下旬黄河中下游两次暴雪过程的相态演变及形成机理。结果表明:两次过程的大尺度影响系统基本一致,只是影响系统的强度和位置不同导致两次过程存在些许差异。两次过程均存在相态转换,过程Ⅰ中存在相态逆转(由雨转雪再转雨),而过程Ⅱ中只存在雨转雪的转换。在太行山以西的山区,当地面2 m气温低于0.5 ℃时,降水相态以雪为主,在0.5~1 ℃之间时,多为雪或雨夹雪并存;在平原地区,当2 m气温为1~2 ℃时,降水相态为雨或雨夹雪,在0~1 ℃之间时,则为雪与雨夹雪并存,低于0 ℃时,降水相态为雪。在降雨阶段,双偏振雷达产品相关系数(CC)值约在0.98以下,差分反射率(ZDR)在0.6 dB以上,差分传播相移率(KDP)值约在0.2 (°)·km-1以上;在降雪阶段,CC值在0.98~0.99之间,ZDR值在0.2~0.8 dB之间,KDP 值约在0.2 (°)·km-1以下;但在降水相态由雨转雨夹雪时,ZDRCCKDP 值没有明显变化。  相似文献   

7.
李悦科  张桂明  高云峰 《海洋学报》2010,32(9):6178-6184
研究了含Kerr介质高Q腔内单个二能级原子与双模二项式光场发生双光子共振相互作用系统的腔场谱,给出了Kerr效应与量子干涉项ΔS(ω)关系的数值计算结果,讨论了Kerr效应对二项式腔场谱量子干涉的影响.结果表明:若初始时刻原子处于激发态而双模光场处于二项式态,随Kerr效应的增强,致使量子干涉项引起谱线强度的改变量呈现出"不规则的周期性衰减振荡"特性,震荡幅度与两模光场的频差密切相关.在Kerr系数χ<g(g为光场与原子的耦合常数)时,Kerr效应对干涉项的影响比  相似文献   

8.
本研究从实验室保藏的节旋藻(Arthrospira)藻种出发, 挑取形态不同的单藻丝体进行纯化培养,采用6 种方法进行全基因组DNA 提取的比较研究, 而后以16S rRNA-ITS 区基因作为分子标记对藻株进行相关序列测定和分子系统进化分析。结果表明, 冻融CTAB 法能够提取出包含染色体外DNA 在内的节旋藻全基因组, 高质量样品可以满足分子生物学实验要求; 分子系统研究表明, 纯化藻株皆为钝顶节旋藻, 节旋藻与螺旋藻在分子鉴定中属间差异明显。  相似文献   

9.
受限于海洋动力条件的复杂性,基于陆架泥质沉积重建的古气候或古环境一直存在争议。为此,本文在北黄海地区沿沉积物输运路径采集3根柱样,通过沉积物粒度及其端元组分和基于器测数据的东亚冬季风指数和黄海暖流强度,分析了不同泥区沉积物粒度端元组分对冬季风暴和黄海暖流变化的响应机理和强度,揭示了上述变化在不同区域产生的沉积效应。结果表明,近百年以来黄河远端泥北支的沉积物组分变化受到了自然因素和人类活动的共同影响。1980年以后,人类活动对黄河沉积物入海通量及其组成的影响开始增强,并掩盖了自然演化信息。而1980年以前,不同泥区的不同端元组分对冬季风暴和黄海暖流的响应机理和强度存在差异,具有显著的区域沉积效应:粗端元组分受冬季风暴强度变化主导,能够反映山东半岛北岸跨锋面物质输运强度的变化;细端元组分受到黄海暖流强度变化主导,反映沉积物从北黄海西部泥区到辽东半岛东岸泥区的输运过程。上述结论说明,虽然粒度是表征古气候和古环境变化的重要标志物,但应根据不同泥区沉积物来源和沉积动力环境的特点,谨慎选择敏感端元组分,正确地使用粒度指标。  相似文献   

10.
钟春良  耿魁伟  姚若河 《海洋学报》2010,32(9):6538-6544
通过异质结界面分析与 AMPS 模拟计算研究了 a-Si:H/c-Si 异质结太阳电池在低温工作、a-Si:H 层低掺杂、高价带补偿以及高界面态时光态 J-V 曲线出现 S-Shape 现象的物理过程,总结了 S-Shape 现象的物理原因.分析结果表明,当空穴输运受到界面势垒的限制时,空穴在 c-Si 界面附近聚集,能带重新分配,c-Si 耗尽区的电场减小,更多的电子从 c-Si 准中性区反转至 c-Si 界面及耗尽区与空穴复合,复合速率显著增大,光电流的损失显著增大,光态 J-V<  相似文献   

11.
BacterialkineticsandenvironmentalcapacityinheWesternXiamenHarbour¥YeDezan;NiChunzhi;ZhouZongcheng;YaoRuimei;ZengHuoshui;LinYa...  相似文献   

12.
黄雯  王巍巍  加攀星  姜天华 《海洋工程》2022,40(3):69-74,92
跨海大桥桥墩基础施工若采用双壁钢围堰,则在其外壁进行开孔可有效减小波浪力,有利于降低钢围堰的制作造价和提高基础施工的安全性。以某跨海大桥基础施工采用的双壁圆形钢吊箱围堰为研究对象,引入波浪力折减系数Kd对消波效果进行评价,采用数值方法着重分析波浪参数和围堰自身结构设计参数对消波效果的影响规律。结果表明:Kd随波陡增大呈先快后缓的增大趋势,波陡超过0.032后,消波效果基本不再变化;随着相对水深的增大,Kd呈先减小后增大并趋缓的规律,在相对水深d/L约为0.455时取得最小值;Kd随开孔率的增大呈线性减小,开孔率越大,消波效果越好。随着双壁间距s的增大,Kd总体上呈减小趋势,且减小速率先快后慢;双壁间距较小时,开孔的消波作用较弱。开孔率和双壁间距两种因素间存在耦合作用,两者越大,其耦合作用也越强。围堰设计中可适当增大开孔率并选取合适的双壁间距以得到最佳消波效果。  相似文献   

13.
The influence of macronitrogen (NO - 3 and NH + 4 ) addition with Ulva pertusa on dissolved inorganic carbon system in seawater was studied. The results indicate that p(CO 2 ) and HCO 3 concentration decrease significantly, while pH and CO 2- 3 concentration increase significantly. When the concentration of NO 3 was less than 71 μmol/dm 3 or NH + 4 was less than 49.7 μmol/dm 3 , dissolved inorganic carbon (DIC) absorption rates by Ulva pertusa generally increased with the increasing of nitrogen concentration. The DIC decreased 151 μmol/dm 3 with the addition of 71 μmol/dm 3 NO 3 and decreased 232 μmol/dm 3 with the addition of 49.7 μmol/dm 3 NH + 4 after the experiment compared with DIC measured without nitrogen addition. A significant negative-correlation was found between c(DIC) and growth rate (μ) of Ulva pertusa (r = -0.91, P <0.000 1, n=11). NH + 4 had more influence on the species of inorganic carbon system than NO 3 .  相似文献   

14.
日本真海带对硒的积累和生物转化   总被引:4,自引:0,他引:4  
在海水中添加亚硒酸盐(Na2SeO3)及不同浓度的氮磷营养盐(NaNO3+NaHO2PO4),研究海带对硒的积累,通过分离测定海带富硒前后各生化组分的含硒量来探讨硒的生物转化问题.结果表明天然海带含硒量(鲜重)为0.451~0.596μg/g,海带富硒最佳的Na2SeO3浓度为200mg/dm3,培养56h后的富硒倍率约为50.在天然海带中,硒主要以有机态存在,有机硒占总硒含量的86.22%;在含有200mg/dm3NaO2SeO3的海水中培养56h后测得海带的总硒为24.481μg/g,其中有机硒含量为16.703μg/g,无机硒为4.714μg/g;在添加氮磷营养盐的含硒海水中,海带的富硒能力得到进一步的提高,在适宜的氮磷条件下(150mg/dm3NaNO3和25mg/dm3NaHO2PO4)总硒含量达到33.649μg/g,而无机硒含量基本不变,为4.497μg/g,因此提高部分转化为有机硒,有机硒含量达到24.678μg/g.这说明海带具有通过自身代谢将无机硒转化为有机硒的较强的能力.  相似文献   

15.
Numerical prediction of performance of submerged breakwaters   总被引:1,自引:0,他引:1  
The results of a numerical model study on the transmission characteristics of a submerged breakwater are presented. Study aimed to determine the effect of depth of submergence, crest width, initial wave conditions and material properties on the transmission characteristics of the submerged breakwater. The results highlight the optimum crest width of the breakwater and optimum clear spacing between two breakwaters. A submerged permeable breakwater with ds/d=0.5, p=0.3 and f=1.0, reduces the transmission coefficient by about 10% than the impermeable breakwater. The results indicates an optimum width ratio of B/d=0.75 for achieving minimum transmission. By restricting the effective width ratio of the series of breakwaters to 0.75, studies were conducted to determine the effect of clear spacing between breakwaters on transmission coefficient, suggesting an optimum clear spacing of w/b=2.00 to obtain Kt below 0.6.  相似文献   

16.
The experimental results have so far shown that when a wave breaks on a vertical wall with an almost vertical front face at the instant of impact that is called perfect breaking or perfect impact, the greatest impact forces are produced on the wall. Therefore, the configuration of breaking waves is important in the design considerations of coastal structures. The present study is concerned with determining the geometrical properties of oscillatory waves that break perfectly on the vertical wall of composite-type breakwaters. The laboratory tests for perfect breaking waves on composite breakwaters are conducted with base slopes of 1/2, 1/4 and 1/6, and with berm widths of 0.00, 0.10, 0.20, 0.30 and 0.40 m. The shape and the dimensions of waves at the instant of perfect breaking on the wall are determined using a video camera. The experimental results for the geometrical properties of the breakers are presented non-dimensionally. Within the range of present experimental conditions, it is found that the dimensionless breaker crest height, hb/dw, and dimensionless breaker height, Hb/dw, decrease; and, dimensionless breaker depth, dw/H0, increases with increasing relative berm width, B/D. The breaker height index, Hb/H0, is almost unaffected by B/D. The deep-water wave steepness and the base slope of the breakwater do not seem to influence the geometrical properties of the breakers at wall systematically.  相似文献   

17.
过氧化氢(H2O2)等活性氧(ROS)物质因具有绿色高效的特点,在废水处理、杀菌消毒等领域受到研究者广泛关注。利用电催化生成H2O2是一种实时提供活性氧物质的有用方法。然而,目前报道的大多数高性能催化材料都是粉体形式,不便于在实际场景中的应用。因此,制备可直接应用的电极材料显得尤为重要。本研究利用喷涂-热解的制备方法,制备了高活性氧催化活性的氧化炭黑(O−CB)/多孔碳毡电极,通过聚四氟乙烯(PTFE)的修饰优化电极表面的氧气传质,成功制备氧掺杂碳气体扩散电极。研究结果表明,O−CB/PTFE-5 wt%电极具有最高的催化性能,其合成H2O2的速率达27.19 mg·L-1(mg catalyst)-1·cm-1·h-1。海洋典型污损微生物假单胞菌(Pseudomonas sp.)的抗菌实验表明,该电极电催化作用60 min产生的活性氧对Pseudomonas sp.的杀菌率可达到97.69%,作用120 min的杀菌率可达到99.99%。  相似文献   

18.
The wave transmission, reflection and energy dissipation characteristics of ‘’-type breakwaters were studied using physical models. Regular and random waves in a wide range of wave heights and periods and a constant water depth were used. Five different depths of immersion (two emerged, one surface flushing and two submerged conditions) of this breakwater were selected. The coefficient of transmission, Kt, and coefficient of reflection, Kr, were obtained from the measurements, and the coefficient of energy loss, Kl was calculated using the law of balance of energy. It was found that the wave transmission is significantly reduced with increased relative water depth, d/L, whether the vertical barrier of the breakwater is surface piercing or submerged, where ‘d’ is the water depth and ‘L’ is the wave length. The wave reflection decreases and energy loss increases with increased wave steepness, especially when the top tip of the vertical barrier of this breakwater is kept at still water level (SWL). For any incident wave climate (moderate or storm waves), the wave transmission consistently decreases and the reflection increases with increased relative depth of immersion, Δ/d from −0.142 to 0.142. Kt values less than 0.3 can be easily obtained for the case of Δ/d=+0.071 and 0.142, where Δ is the height of exposure (+ve) or depth of immersion (−ve) of the top tip of the vertical barrier. This breakwater is capable of dissipating wave energy to an extent of 50–80%. The overall performance of this breakwater was found to be better in the random wave fields than in the regular waves. A comparison of the hydrodynamic performance of ‘’-type and ‘T’-type shows that ‘T’-type breakwater is better than ‘’-type by about 20–30% under identical conditions.  相似文献   

19.
中国沿海不同地区泥蚶(Tegillarca granosa)的遗传多样性分析   总被引:1,自引:0,他引:1  
以采自海南海口、广西防城港、广西北海、广东湛江、福建漳州、山东荣成、山东威海7个地理群体62个泥蚶个体为材料,获取592bp线粒体COI基因片段序列,并进行遗传多样性及分化分析。多态性遗传参数统计显示:62个个体共检测出103个多态性位点,定义了26个单倍型;总群体单倍型多样性指数为0.834,核苷酸多样性指数为0.01665,平均核苷酸差异数为9.85772。7个群体均显示出较丰富的遗传多样性,群体内遗传距离及群体内遗传多样性参数显示中国沿海泥蚶遗传多样性由北向南呈升高趋势,而群体内遗传分化系数也呈现升高的趋势。基于26个单倍型COI序列构建的NJ树和UPGMA树以及基于群体间遗传距离构建的UPGMA树显示,荣成群体和威海群体亲缘关系较近,聚成一小支,而后与漳州群体相聚,然而南方类群并没有聚为独立的一支。  相似文献   

20.
A nonlinear theory for the generation of the Ulleung Warm Eddy (UWE) is proposed. Using the nonlinear reduced gravity (shallow water) equations, it is shown analytically that the eddy is established in order to balance the northward momentum flux (i.e., the flow force) exerted by the separating western boundary current (WBC). In this scenario, the presence of β produces a southward (eddy) force balancing the northward momentum flux imparted by the separating East Korean Warm Current (EKWC).It is found that, for a high Rossby number EKWC (i.e., highly nonlinear current), the eddy radius is roughly 2Rd/ε1/6 (here εβRd/f0, where Rd is the Rossby radius), implying that the UWE has a scale larger than that of most eddies (Rd). This solution suggests that, in contrast to the familiar idea attributing the formation of eddies to instabilities (i.e., the breakdown of a known steady solution), the UWE is an integral part of the steady stable solution. The solution also suggests that a weak WBC does not produce an eddy (due to the absence of nonlinearity).A reduced gravity numerical model is used to further analyze the relationship between β, nonlinearity and the eddy formation. First, we show that a high Rossby number WBC which is forced to separate from the wall on an f plane does not produce an eddy near the separation. To balance the northward momentum force imparted by the nonlinear boundary current, the f plane system moves constantly offshore, producing a southward Coriolis force. We then show that, as β is introduced to the problem, an anticyclonic eddy is formed. The numerical balance of forces shows that, as suggested by the analytical reasoning, the southward force produced by the eddy balances the northward flow force imparted by the boundary current. We also found that the observed eddy scale in the Japan/East Sea agrees with the analytical estimate for a nonlinear current.  相似文献   

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