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海洋磁异常的解释已经对海洋地质学和海洋古地磁学的发展起了相当大的推动作用。已有多种方法可用于海洋磁异常的解释。在这些方法中将观测到的磁场同模型计算后所得到的磁场相对比是一种传统的异常解释方法。不过在此种方法中的模型计算多半都具有不同程度的假设前提,因而使其只具有一定的适应性。本文给出一种并无 相似文献
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海缆在长久的电力信息输送过程中,损坏故障等突发事故经常发生,研究海缆在地磁背景下环境周围产生磁异常扰动信号,确定海底海缆轨迹和埋设深度,能够在突发状况之后迅速针对该区域内的海缆进行定位,及时对海缆进行维修。基于微元磁偶极子有限元仿真建立海缆磁场模型,探究了检测距离(DCPA)、海缆长度(L)、背景磁场对海缆磁异常特性的影响规律。通过研究可知:DCPADCPA>L时衰减指数约为–2.8,DCPA>3L时衰减指数约为–3;DCPA固定时,海缆磁异常随长度明显增加到一定程度会趋向稳定,信号发生畸变;背景磁场分量改变不仅可能改变海缆磁异常信号的强度,还可能改变其信号波形特征。 相似文献
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南海北部磁场特征及其构造意义 总被引:1,自引:0,他引:1
根据南海北部的地磁场数据及其化极异常特征,该区由北向南可分为复杂异常区、高磁异常区、陆坡磁异常平静区(磁静区)和海盆磁条带区四大构造特征区.其中,磁静区可为内磁静区1、内磁静区2和外磁静区三部分.该区磁性基底反演结果表明,外磁静区磁性基底深度为6-7km,介于内磁静区(8-10km)和海盆区(4-5km)之间,可能是前新生代残留古洋壳.外磁静区和下地壳高速层相对应,指示其可能是在裂前或裂间由底侵作用形成的.陆架坡折带附近的F2断裂是内磁静区的北侧边界,指示了南海北部陆壳向过渡壳的转变分界;位于下陆坡与海盆的交界处的F4断裂为外磁静区的南侧边界,F3断裂可能指示了洋陆分界线的位置. 相似文献
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以海底未爆弹作为待测目标物,对其建立了偶极子磁异常探测模型,应用正交基检测算法 (Orthogonal Basis Functions,OBFs)对获取的磁信号进行弱磁信号提取。结合 GPS 经纬度信息,提出处理海底磁异常数据的数据融合过程,然后创建地磁图来定位可疑的未爆弹(Unexploded Ordnance,UXO)。通过仿真对算法处理流程进行分析。首先,利用有限元模拟方法对未爆弹在地磁背景下所产生的磁异常进行建模,然后模拟实际当中的空间采样过程,得到观测区采样信号图。通过插值的方法进行磁场的重构,最后获取异常源的位置信息。在未爆弹实际探测中,原始磁异常信号信噪比为 14.34 dB。对原始磁异常数据进行滤波、正交基算法检测,信噪比为 20.04 dB,显著提高了 5.7 dB。最终利用地磁图确定可能存在的未爆弹的经纬度位置。结果显示目标探测准确率达到 100%,虚警率为 0。该研究验证了磁异常探测在浅海掩埋未爆弹探测和定位的准确性和可靠性。 相似文献
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In this paper, by the transparent-component-decimation (TCD) method we obtain three kinds of new basic-components (BCs) through simplifying and decomposing the BCs of three-component Thue--Morse (3CTM) sequence. Based on these new BCs we propose a type of basic-structural-units (BSUs) and investigate the optical transmission of the one-dimensional (1D) superlattices composed of these BSUs. It is found that if the substrates of the 1D BSU superlattices are certain, the optical transmission at the central wavelength (CW) will be determined completely by the number and the type of BSUs and has nothing to do with the marshalling sequence. In particular, if the substrates are identical, the numbers of different types of BSUs are all the same and the middle two elements of BSUs constitute a cycle, then no matter whether the system is periodic, or quasiperiodic, or aperiodic, or unordered, or even random, it will be transparent at the CW. The conclusion is confirmed by the numerical results. Similar to the even layers of neighbourhood identical elements in TCD method, such a kind of optical BSU subsystem can also be decimated from the chain in the process of transmission investigation. There would be a potential application in the designing of some interesting optical devices. 相似文献
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调光生态膜光学性能研究 总被引:5,自引:2,他引:3
为提高光合作用效率,促进农作物早熟、增产,根据叶绿素进行光合作用所需的吸收谱,采用新型有机共轭分子化合物按一定比例分散到聚烯烃化合物中,可产生与叶绿素吸收谱匹配的荧光谱,从而实现对太阳光谱中不同波段光的红移。对调光膜进行光学性能研究。结果表明:直射光透光率略低于普通膜,而散射光的透光率大于普通膜;红橙光波段调光度较高,蓝紫光波段的调光度较低;光学稳定性早期衰减较大,但逐渐趋于平稳。 相似文献
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Busygin V. P. Krasnokutskaya L. D. Kuzmina I. Yu. 《Izvestiya Atmospheric and Oceanic Physics》2019,55(5):453-461
Izvestiya, Atmospheric and Oceanic Physics - Mathematical models are developed and simulations are performed of the transport of short optical impulses through the cloud layer into space. The... 相似文献
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An attempt to the approximate figures of seasonal distribution of solar energy reached to and penetrated in the water of the
oceans, as a preliminary step to the estimation of primary production in the oceans from the optical point, was performed
in the Indian Ocean, North Pacific Ocean and Antarctic Ocean on the same lines in the part III. In consequence, the total
amount of solar energy for the year in each depth showed marked differences in each zone of the oceans as illustrated in Fig.
5. By way of example, it could be said that underwater solar energy already came to 33.4 Kg·cal/cm2·year in 10 m deep in the equator of Indian Ocean and was 54% of that, in the Kuroshio region of the North Pacific Ocean,
44% in the Sub-Antarctic zone, 13% in the Antarctic zone and 6% in the Antarctic Convergence zone, respectively.
Besides, on the assumption that a lower limit of the photic zone is marked by the depth here underwater surface solar energy
is reduced to 1% or 5g·cal/cm2·day, the ratio of the total photic zone for the year in unit area of sea surface was approximately 100∶80∶60∶25 or 100∶75∶50∶20
in the equator of the Indian Ocean, Kuroshio region, Sub-Antarctic zone, and Antarctic and Antarctic Convergence zones, respectively. 相似文献