共查询到19条相似文献，搜索用时 125 毫秒
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方斑东风螺性畸变现象的解剖学和组织学研究 总被引：1，自引：0，他引：1
以解剖学和组织学方法研究了方斑东风螺未成熟和成熟的正常雌、雄个体以及性畸变个体的生殖系统结构.性畸变个体除具有正常的雌性器官外,还有输精管或阴茎.在正常雄性输精管的个体发育过程中再现了系统发育的过程,而且在性畸变个体输精管的形成过程和发育过程中组织学结构特征的变化与正常雄性输精管的个体发育过程的相似.性畸变雌体的性腺发育受阻.目前,性畸变现象仅存在于成熟个体,但这并不表明未成熟个体中不会发生性畸变现象.具有较高食用价值的方斑东风螺因有机锡污染可能会对人类健康不利,应引起人们的关注. 相似文献
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海洋防腐工程中受阴极保护金属构筑物表面的电位电流分布常常是不均匀的,而金属表面的电位电流只有在一定范围内才能使构筑物受到有效和适当的保护.尤其是复杂而庞大的海洋钢结构物(如滨海电厂钛管凝汽器)阴极保护系统的设计和监测较复杂,此阴极保护下电化学场的计算,对评价阴极保护效果,优化阴极保护设计有重要意义.采用电化学场中的拉普拉斯(Laplace)方程,使用四节点四面体和合适的形状函数对水室表层和复杂结构体系周围场域进行离散.用有限元计算法,通过对各单元的分布和整个求解区域的总和,建立了两种不同金属组成复杂结构体系的三维有限元数学模型. 相似文献
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基于自旋-轨道-晶格Hamilton量,应用团簇自洽场方法,研究了双层钙钛矿结构材料K3Cu2F7基态的晶格、磁及轨道结构,发现近孤立的双层的对称破缺和Jahn-Teller晶格畸变使得Cu2+离子在每层内交替占据 z2-x2〉/ z2-y2〉轨道,进而导致双层的层间表现为强的反铁磁耦合,层内为弱的铁磁耦合.强反铁磁耦合导致层间 相似文献
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采用基于密度泛函理论的广义梯度近似(GGA),对不同尺寸(N=2—11)的单层正三角锯齿型石墨烯量子点(Z N -GNDs)的结构进行优化,得到与实验数据较好符合的晶格常数,进一步计算得到不同尺寸下体系的自旋多重度、磁矩、电子态密度以及自旋电子密度.结果表明:所有体系都呈现金属性,在尺寸较小的体系中量子尺寸效应对电子结构的影响比较明显;与单层石墨烯片一样,sp2杂化作用和非键态电子在量子点中仍起到非常重要的作用;费米能级上有自旋向上的电子分布,体系的自旋多重度 相似文献
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福建沿岸上升流数值研究Ⅱ.台湾海峡上升流的三维数值模拟 总被引：2，自引：0，他引：2
用有限差分法结合新sine-σ坐标变换和三次样条函数性质,建立了适用于台湾海峡上升流计算的三维数值模型.为考察海峡内潮、风、北上的海峡暖流和地形等因子对上升流形成的影响,设计了多种实验方案.结果表明,潮的非线性效应对海峡内上升流的形成有相当重要的影响.潮流和海峡暖流的存在是台湾浅滩上升流形成的主要原因,也是非季风期福建沿岸上升流形成之主因.西南季风盛行期,福建沿岸上升流得以加强,范围扩大,台湾浅滩上升流中心位置南移;东北季风期,福建沿岸上升流在上、中层基本消失,但海坛岛和东山岛近岸下层仍有上升运动存在,台湾浅滩上升流出现范围向北扩展.由于东北风的连续吹刮,台湾西岸亦出现了范围较窄的上升流迹象.计算还表明,海峡内各上升流有明显的季节性和区域性差异.风对海峡内上升流的中、上层结构起主导作用,而潮和海峡暖流则对中、下层上升流的形成起支配作用,因而导致上升流垂向结构的上下异性. 相似文献
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比例边界有限元法(SBFEM)是一种半解析的数值方法,比完全数值方法具有更高的精度,该方法结合了有限元和边界元的优点,采用相对少的剖分单元就可以得到较高精度的模拟结果。通过改变有限子域内部比例中心的位置,使这种方法可以应用到多种形式浮体在波浪作用下的水动力特性的计算中。同时还给出了各种形式浮体的波浪力及反射、透射系数的数值结果,并与边界元方法(BEM)计算结果和特征函数展开方法得到解析解进行了比较,均吻合良好。研究表明比例边界有限元不仅可以计算矩形的浮体结构,而且对于多种结构形式的浮体都可以计算,这为多种结构形式浮体的水动力分析提供了一个可行的方法。 相似文献
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利用强流脉冲电子束(high-current pulsed electron beam,HCPEB)技术对多晶纯Ni进行了辐照处理,采用透射电子显微镜详细分析了辐照诱发的缺陷结构.HCPEB辐照后,纯镍表层积聚了幅值极大的残余应力,沿{111}晶面形成了稠密的位错墙及孪晶结构,另外还形成了大量的包括位错圈、堆垛层错四面体(SFT)及孔洞在内的空位簇缺陷.SFT缺陷的数量远高于其他空位簇缺陷,其周围区域位错密度很低.孔洞缺陷主要出现在SFT密集区域.HCPEB瞬间的加热和冷却诱发的幅值极大的应力和极高的应变 相似文献
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针对海洋环境中的半潜式平台多方面不确定性,基于半潜式平台结构整体强度分析方法,考虑多种波浪荷载作用的结构响应,采用非线性逐步垮塌分析方法,研究平台在不同控制工况下的极限承载力模型,建立相应的功能函数.根据结构体系可靠度理论和失效模式之间的关系,采用串联体系的可靠度计算方法.最后,对一座具体半潜式平台在100年重现期波浪荷载作用下进行了体系可靠性计算.计算结果表明平台整体可靠度水平由波浪引起的主要结构响应形式决定.通过计算,验证可靠度计算方法具有高效性和可行性,可以为大型深水浮式平台结构的设计、维护和评估提供理论依据. 相似文献
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提出直接由MATLAB读入光纤端面图实现复杂结构光子晶体光纤(PCF)模型的快速建立,并综合平面波法(PWM)和频域有限差分(FDFD)法,模拟分析带隙型光子晶体光纤(PBG-PCF)的带隙和模场分布.利用PWM计算得到了在PBG-PCF中传输的光波频率及模式有效折射率范围;基于FDFD法在给定波长及模式有效折射率范围情况下,模拟得到了PBG-PCF中可能存在的模场分布及其他特性.以市售的PBG-PCF为例,验证了数值模拟的正确性,随后系统地分析了结构参数(晶格结构、"原子"占有率、背景材料折射率及"原子 相似文献
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海水中的氦同位素能对海底热液活动进行有效示踪。本文对在西南印度洋49°~56°E洋脊段采集的5条CTD拖曳剖面共14件深水样品进行了氦氖同位素分析。通过分析水体中存在的氦同位素异常,探讨调查区热液异常的特征和热液羽状流的分布。分析表明,5条CTD剖面均存在δ3He异常,其中CTD7-2(位置:37.927°S、49.412°E,水深2 140m,离底高度100m)的δ3He值最大,达到49.2%。根据δ3He分布特征,认为调查区内存在至少6处热液羽状流,其中37.927°S、49.412°E以西数千米范围内可能存在海底热液喷口。 相似文献
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电沉积促进珊瑚生长和岸礁修复技术是国际上常采用的生态修复方法,但电沉积技术中电流条件与沉积晶体之间的关系却鲜有研究,关于其形成的电沉积物的晶体结构的报道更是少有。本文探索了在不同电流密度的条件下海水形成碳酸钙晶体的特点,并与珊瑚骨骼晶体进行了对比。本实验设置了300、600、900和1200 m A/m2四组电流密度,在海水中进行5 d电沉积反应,实验后称量了阴极上形成的电沉积物质量,用扫描电子显微镜和X-射线衍射分析了电沉积物中晶体特点并与珊瑚骨骼进行了比较。结果发现,随着电流密度增大,电沉积物质量增加,电流密度为600 m A/m2条件下电沉积物形成的速率与南海的滨珊瑚的生长速率相当。在各个电流密度梯度条件下形成的晶体均与珊瑚骨骼的晶体结构相似。较低电流密度下电沉积物中碳酸钙比例较高。其中,在电流密度为600 m A/m2的条件下,形成的沉积物碳酸钙文石比例最高,和珊瑚骨骼晶体最为接近。本研究为促珊瑚生长的电沉积技术提供了基础数据和理论。 相似文献
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The results of a joint analysis of the synchronous-profile ensemble of density and current velocity measured using the autonomous moored Aqualog profiler at the Gelendzhik experimental site of the Shirshov Institute of Oceanology in 2013–2015 are presented. The distribution of probability density of current velocity by directions reveals the presence of two well-pronounced maxima in the southeastern and northwestern sectors at all depths of measurements, which confirms the bimodal direction of the currents in the study site. We consider in detail the vertical structure of the density stratification and the current velocity corresponding to the modes determined from the maximum of the probability density distribution of the current velocity by directions. The averaged profiles of the kinetic, potential, and total energies are given. The results of isopycnic averaging over the entire ensemble of profiles indicate that possible self-similarity exists in the dependence of the vertical distribution of density and kinetic energy. 相似文献
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In this article we explored the crystal structure of a few pearls and shellfish's shell of fresh water and sea water, and found that pearls and nacreous layer (perhaps and prismatic layer) of shells are all the same: CaCO3, orthorhombic system, aragonite structure and the value of lattice spacings are almost identical. This shows that the pearls of fresh water and sea water are all the same in nature. 相似文献
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E. M. Prasolov I. V. Tokarev G. D. Ginsburg V. A. Soloviev G. M. Eltsova 《Geo-Marine Letters》1999,19(1-2):84-88
He, Ar, Ne contents and 3He/4He, 4He/20Ne, and 40Ar/36Ar ratios in gas-hydrate bearing sea-floor sediments of the Håkon Mosby Mud Volcano show that Ne, Ar, and part of He are atmospheric. Nonatmospheric, deep He (3He/4He=0.9???10-8) is present in all samples. Helium isotopic composition suggests that its origin is uniform, crustal (radiogenic) and, probably, connected with mud volcano gases. Apparently deep helium is residual gas that remains in isolated volumes after hydrate formation. Measured helium content in hydrate gases is very low: 0.5–10?ppm. but in one particular sample it is very high: 7080?ppm. 相似文献
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Naoto Takahata Yuji Sano Keika Horiguchi Kotaro Shirai Toshitaka Gamo 《Journal of Oceanography》2008,64(2):293-301
We have collected fifty-five seawater samples at seven stations at various depths in the Yamato and Japan Basins of the Japan
Sea and measured their helium isotopic ratios. The 3He/4He ratios vary from 0.997 Ratm to 1.085 Ratm where Ratm is the atmospheric ratio. The maximum 3He excesses about 8%, are observed at mid-depth (1000 m), and these values are significantly lower than those observed in
deep Pacific waters. This implies that mantle-derived helium in deep Pacific water cannot enter the Japan Sea since it is
an almost landlocked marginal sea. The observed 8% excess 3He may be attributable to the decay product of tritium. Slightly higher 3He/4He ratios in the Bottom Water were observed in the Yamato Basin than in the Japan Basin. The ventilation ages of seawater
shallower than 1000 m are calculated as about 5 to 20 years, which is consistent with the CFC ages reported in the literature.
There is a positive correlation between the apparent oxygen utilization and 3H-3He ages. The estimated oxygen utilization rate from the correlation in a layer between 500 m and 1000 m is about 3 μmol/kg/yr, which is similar to that in the eastern subtropical North Atlantic. 相似文献
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Helium, neon and argon isotope compositions of fluid inclusions have been measured in massive sulfide samples from the Jade hydrothermal field in the central Okinawa Trough. Fluid-inclusion 3He/4He ratios are between 6.2 and 10. l times the air value (Ra), and with a mean of 7.8Ra, which are consistent with the mid-ocean ridge basalt values [3He/^4He≈(6Ra- 11Ra)]. Values for ^20Ne/^22Ne are from 10.7 to 11.3, which are significantly higher than the atmospheric ratio (9.8). And the fluid-inclusion ^40Ar/^36Ar ratios range from 287 to 334, which are close to the atmosperic values (295.5). These results indicate that the noble gases of trapped hydrothermal fluids in massive sulfides are a mixture of mantle- and seawater-derived components, and the helium of fluid inclusions is mainly from mantle, the nelium and argon isotope compositions are mainly from seawater. 相似文献
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The 110+, 11(-1)+and 11(-2)+ states of the helium atom in the magnetic field regime between 0 and 100 a.u. are studied using a full configuration-interaction (CI) approach. The total energies, derivatives of the total energy with respect to the magnetic field and ionisation energies are calculated with Hylleraas-like functions in spherical coordinates in low to intermediate fields and Hylleraas--Gaussian functions in cylindrical coordinates in intermediate to high fields, respectively. In intermediate fields, the total energies and ionisation energies are determined in terms of Hermite interpolation, based on the results obtained with the two above-mentioned basis functions. Calculations show that the current method can produce lower total energies and larger ionisation energies, and make the two ionisation energy curves obtained with the two above-mentioned basis functions join smoothly in intermediate fields. Comparisons are also made with previous works. 相似文献