影响鸢乌贼手钓上钩率的因子探讨

根据印度洋西北部鸢乌贼（Sym plectoteuthis oualaniensis）作业渔场的现场调查数据．分析了作业水深、作业时段、摄食等级和月相等因子对手钓上钩率的影响。统计表明．晚上、午夜和凌晨3个不同时段和不同作业水深对手钓上钩率均有显著性影响。3个时段中，其摄食等级呈先低后高再低的现象。午夜和凌展，上钩率的变化趋势与摄食等级的变化趋势呈显著的负相关。在月相的影响下．离朔日三四天之前，手钓产量呈上升趋势；离望日五六天之前。手钓产量呈明显的下降趋势。     

脉冲星的射电发射

脉冲星的射电辐射与其他天体物理辐射源有很大的不同，因为它们有着极高的亮温度和高度的线或圆偏振。极高的亮温度意味着起作用的发射机制一定是相干的。至今尚无对这种辐射普遍接受的模型。本文讨论了关于脉冲星的射电辐射产生和传播研究中的新进展。     

怎样做好土地整理项目规划设计变更工作

土地整理项目规划设计变更是指在施工过程中,由于施工现场条件改变、工程使用意图变化等客观原因,对原规划设计局部工程进行修改,或增加或减少某些分项工程的施工任务.     

工业用地转让亟待规范

存在问题 在城市化进程发展过程中,许多建成区的工业用途的房地产由于规划调整、环境影响、债务纠纷等原因,被搬迁、被兼并、被变卖、被裁定,其土地使用权随之进入土地市场转让交易,一些房地产开发企业和自然人也参与其中,他们有的是通过司法裁定获得,有的是通过中介市场淘得,也有的是双方协议转让取得.于是,一个国有土地使用权转让管理中的棘手问题出现了,那就是,作为没有工业用地经营资格,不具备工业生产基本能力的房地产开发企业和自然人,能否买受工业用地?     

海浪非线性性的实验研究——Ⅰ.波面高度分布的非正态性

本文介绍海浪非线性性实验研究的第一部分。利用实验室测得的在各种背景下具有不同非线性强度的风浪波面记录,通过波面统计分析,并与非线性波面理论分布比较,揭示了海浪非线性性的外观特征及其随风速、风区等的变化规律。     

Mantle processes during ocean formation：Petrologic records in peridotites from the Alpine－Apennine ophiolites

Mantle peridotites were early exposed at the sea-floor of the Jurassic Tethys derived from the subcontinental mantle of the Europe-Adria system. During continental rifting and oceanic spreading, these lithospheric peri-dotites were percolated via diffuse reactive porous flowby melt fractions produced by near-fractional melting of the upwelling asthenosphere. Ascending melts inter-acted with the lower lithosphere, dissolving pyroxenes and precipitating olivine, and crystallized at shallower levels in the mantle column causing melt impregnation.Subsequent focused porous flow formed replacive dunitechannels, cutting the impregnated oeridotites, which were conduits for upward migration of MORB-type liq-uids. Melt migration produced depletionlrefertilization and significant heating of the percolatedlimpregnated mantle, i.e the thermochemical erosion of the litho-sphere. Impregnated and thermally modified lithos-pheric mantle was cooled by conductive heat loss dur-ing progressive lithosphere thinning and was intrudeaby MORB magmas, which formed Mg-rich and Fe-richgabbroic dykes and bodies. Alpine-Apennine ophiolitic peridotites record the deep-seated migration of melts which changed their compositions and dynamics during the rift evolution. The thermochemical erosion of the lithospheric mantle by the ascending asthenospheric melts, which induces significant compositional and rhe-ological changes in the lower lithosphere, is a major process in the evolution of the continent-ocean transi-tion towards a slow spreading oceanic system.