山东省海洋空间开发保护现状、问题及对策          下载免费PDF全文

陈斌  徐永臣  徐承芬  王琰  牟秀娟 《海洋开发与管理》2021,38(3):3-8

海洋是国民经济发展和社会进步的重要空间载体,海洋国土空间开发与保护对于实现可持续的经济增长、改善全球气候环境和提升人民生活福祉具有重大战略意义。山东省海域使用类型基本齐全,但开发利用结构规模不均衡,渔业用海比重较大,不合理的开发利用给海岸带和近海生态环境带来巨大威胁,严重制约了海洋经济的健康发展。文章根据山东省海域使用调查数据,综合分析了山东省海洋空间使用现状的特点以及存在的自然岸线保有压力增大、海洋空间开发利用科学性不足、近岸海域生态系统及服务功能受损较重、海洋污染造成的环境风险不容忽视、现代海洋产业体系不够完善、陆海统筹机制不健全等主要问题,在此基础上,从海洋空间资源、陆海统筹污染防治体系、现代海洋产业体系等角度提出了优化山东省海洋国土空间开发保护的相关对策建议。  相似文献   

Soft X—ray Properties of Ultraluminous IRAS Galaxies     

Yiao－YangXia  Th.Boller 《中国天文和天体物理学报》2001,1(3):221-223

We report on the results of cross-correlation of a sample of 903 Utraluminous IRAS galaxies (ULIRGs) with the ROSAT-All Sky Survey Bright Source Catalogue and the ROSAT archived pointing observations. The sample of ULIRGs has been compiled from the recently released PSCz redshift survey. In total,35 ULIRGs are securely detected by the ROSAT All-Sky Survey and pointing observations, five of which are blazars. The statistical properties of these sources in the soft X-ray band are determined and compared with their properties on other wavebands. We find that the ratio of the soft X-ray to the far-infrared flux spans about five orders of magnitude and reaches values of about unity. This ratio is a good indicator of the main energy source of ULIRGs. Those with soft X-ray to far-infrared flux exceeding 0.01 are probably powered by accretion onto central supermassive black holes while those with ratios smaller than 0.001 are probably powered by starbursts or other heating processes, or are Compton thick sources. Some ULIRGs have energy contributions from both. This ratio is low for most ULIRGs and hyperluminous infrared galaxies, which explains their low detection rate by ROSAT and ASCA.We also find that some ULIRGs have a similar soft X-ray luminosity vs. temperature relation to that for groups of galaxies and elliptical galaxies,suggesting a common origin of these systems. Our study also reveals a tight correlation between the hardness ratio and the soft X-ray luminosity for Seyfert 1s/QSOs.  相似文献   

Numerical Simulation of Changes in Tropical Cyclone Intensity Using a Coupled Air-Sea Model   总被引：1，自引：0，他引：1  

DUAN Yihong  WU Rongsheng  YU Runling  LIANG Xudong 《Acta Meteorologica Sinica》2013,27(5):658-672

A coupled air-sea model for tropical cyclones （TCs） is constructed by coupling the Pennsylvania State University/National Center for Atmospheric Research mesoscale model （MM5） with the Princeton Ocean Model.Four numerical simulations of tropical cyclone development have been conducted using different configurations of the coupled model on the f-plane.When coupled processes are excluded,a weak initial vortex spins up into a mature symmetric TC that strongly resembles those observed and simulated in prior research.The coupled model reproduces the reduction in sea temperature induced by the TC reasonably well,as well as changes in the minimum central pressure of the TC that result from negative atmosphere-ocean feedbacks.Asymmetric structures are successfully simulated under conditions of uniform environmental flow.The coupled ocean-atmosphere model is suitable for simulating air-sea interactions under TC conditions.The effects of the ocean on the track of the TC and changes in its intensity under uniform environmental flow are also investigated.TC intensity responds nonlinearly to sea surface temperature （SST）.The TC intensification rate becomes smaller once the SST exceeds a certain threshold.Oceanic stratification also influences TC intensity,with stronger stratification responsible for a larger decrease in intensity.The value of oceanic enthalpy is small when the ocean is weakly stratified and large when the ocean is strongly stratified,demonstrating that the oceanic influence on TC intensity results not only from SST distributions but also from stratification.Air-sea interaction has only a slight influence on TC movement in this model.  相似文献   

印度洋构造过程重建与成矿模式：西南印度洋洋中脊的启示EI北大核心CSCD     

李三忠  索艳慧  刘鑫  赵淑娟  余珊  戴黎明  许立青  张臻  刘为勇  李怀明 《大地构造与成矿学》2015,(1):30-43

印度洋经历过复杂的构造演化,其中3次重大的三联点和洋中脊跃迁、板块重组对印度洋现今构造格局的形成具有重要影响。本文基于Gplates板块重建技术和古水深数据,并融合前人热点和年代学研究结果,重点探讨了120 Ma、90 Ma、84 Ma、65 Ma、40 Ma、24 Ma和15 Ma发生在印度洋的重大构造事件,讨论了这些构造事件在西南印度洋超慢速扩张脊构造特征上的关联,探讨了西南印度洋不同演化阶段的两种海底热液成矿模式,即早期热点-洋中脊相互作用相关的热点成矿模式和后期海洋核杂岩相关的湿点成矿模式。  相似文献   

副热带高压气候动力学研究回顾   总被引：1，自引：0，他引：1  

刘屹岷  姜继兰  何编 《气象科学》2020,40(5):585-595

基于早期副热带高压气候动力学的研究,本文重点介绍了近10 a在南亚高压和西太平洋副热带高压形成和变异机理方面的动力学研究,包括南亚高压的建立和维持机理、副热带高压的季节变化、年际—年代际变化和未来预估,最后讨论了需要进一步深入研究的方面。  相似文献   

一次东北冷涡背景下MCS过程多尺度能量相互作用研究          下载免费PDF全文

沈新勇  张弛  肖云清  沙莎  王林  李小凡 《大气科学学报》2020,43(3):447-457

采用WRF模式对东北冷涡背景下MCS过程进行模拟,利用Barnes滤波将模式数据分解为3个尺度,分别代入相应的能量方程中进行计算,从能量角度研究MCS发展过程,多尺度系统能量相互转化,以及动能与降水的联系。研究表明:在此次过程中各尺度之间都有位能向动能的大量转化,为系统发展提供能量。在对流单体发展到M CS成形前,中低层天气尺度动能减少,天气尺度动能向β中小尺度动能转换,促进对流单体的发展;高层天气尺度动能增强,对应高空急流增强,促进对流系统发展;β中小尺度系统在中层对α中尺度系统有动能输送,促进MCS形成。在MCS形成和发展阶段,各尺度位能向α中尺度和β中小尺度动能转化达到最大。在MCS减弱阶段,天气尺度系统和α中尺度系统在中高层对β中小尺度系统有一定的抑制作用,使β中小尺度系统发展减弱。此次过程中β中小尺度系统是降水的直接成因,动能变化的正值中心对应大的降水中心。  相似文献   

川西坳陷中段陆相地层水纵向变化特征及水—岩相互作用初探   总被引：6，自引：2，他引：4  

沈忠民  刘四兵  吕正祥  罗小平  宫亚军 《沉积学报》2011,29(3):495-502

地层水是孔隙流体的重要组成部分,在空间变化上受控于流体动力场,时间演化上主要受控于流体—岩石相互作用过程。通过川西坳陷300余个地层水化学数据的系统分析,对研究区地层水化学特征及其所反映的成岩作用过程进行了初步探讨:川西坳陷上侏罗统到须家河组可分为地层水交替阻滞带和地层水交替停滞带2个水化学作用带,大气水作用的范围在530 m以上地层;黏土矿物大规模脱水的淡化作用是地层水交替阻滞带离子浓度随深度变大而变小的主要因素,而该带中HCO3-随埋藏深度的增加而不断增加的原因则可能主要与有机质成熟过程中CO2的加入有关;盐岩溶解可能是交替阻滞带地层水Na+富集的主要因素,Ca2+的富集则可能主要由蒙皂石的伊利石化和少量碳酸盐岩的溶解造成;钙长石的钠长石化是研究区地层水交替停滞带的一项重要的水—岩作用过程,同时存在的成岩作用类型还包括绿泥石化、碳酸盐矿物的溶解以及钠长石的溶解。  相似文献   

记载了早中生代壳幔演化的赤峰-凌源地质走廊   总被引：6，自引：1，他引：5  

邵济安  杨进辉 《岩石学报》2011,27(12):3525-3534

本文从内蒙赤峰至辽西凌源南北近200km的地质走廊中,选择早中生代(237～206 Ma)形成不同深度、不同产状的8种火成岩作为研究对象,探讨早中生代华北克拉通北缘的地质演化.这8种岩石包括:火山岩、岩墙群和闪长岩、碱性花岗岩、碱性杂岩、镁铁质麻粒岩、堆晶岩及其捕获的地幔岩包体.研究表明,在底侵作用的背景下,华北早中生代发生了强烈的壳幔相互作用和岩石圈地幔富集过程,伴随早中生代大陆地壳的增生和深部结构的调整,地表相应出现快速的差异抬升和剥蚀.  相似文献   

Introduction to thematic section on hydrodynamic ;tudies of mineralization     

Guoxiang Chi 《地学前缘(英文版)》2011,(3):421-422

1.Introduction Most metallic mineral deposits formed from hydrothermal fluids,and the mineralization processes include both chemical (e.g.,fluid-rock and fluid-fluid interactions)and physical(e.g., fluid flow)aspects.More attention has been paid to the chemical processes than the physical ones,even though the latter is equally important in controlling the formation of mineral deposits and their localization.Nevertheless,a number of studies have been carried out regarding the hydrodynamics of fluid flow associated with ore mineralization(e.g.,Cathles,1981,1997; Garven and Raffensperger,1997;Cathles and Adams,2005; Cox,2005;Ingebritsen et al.,2006),and it is timely to eval-  相似文献   

《矿物岩石地球化学通报》2011年(第30卷)总目次     

《矿物岩石地球化学通报》2011,(4):477-480

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