我国地面太阳辐射量的时空变化研究   总被引：30，自引：1，他引：30  

查良松 《地理科学》1996,16(3):232-237

在分析我国到达地面太阳辐射量（１９５７￣１９９２年）时空变化分布规律基础上，阐述了火山爆发产生的气溶胶和城市发展带来的人工气溶胶对太阳辐射量变化的影响，以及大气中气溶胶增加和地面太阳总辐射量的减少在环境研究中的问题。  相似文献   

南极磷虾的生长与复眼直径关系的研究          下载免费PDF全文

孙松  王荣 《极地研究》1996,8(1):4-11

本文对南极磷虾复眼的直径与磷虾体长之间的关系、在负生长状态下磷虾复眼直径的变化等进行了研究。实验结果表明：在正常情况下（磷虾身体不出现负生长），磷虾复眼的直径与体长之间存在指数函数关系。雌性磷虾的眼径（ＥＤ）与体长（ＢＬ）之间的关系为：ＥＤ＝０．５８９８ｅ０．０２８２ＢＬ（ｒ＝０．９６１３，ｎ＝２４１９）；雄虾的眼径与体长之间的关系为：ＥＤ＝０．５４４ｅ０．０３０９ＢＬ（ｒ＝０．９６２２，ｎ＝１９２０）。在相同体长的情况下，雄性磷虾的复眼直径比雌虾的大。从活体培养的结果来看，当南极磷虾出现负生长时，复眼直径保持不变，即眼径不受负生长的影响。在正常情况下（不存在负生长），雌虾的体长与眼径之间的比率（ＢＬ／ＥＤ）平均为２１．３２±０．０４（ｎ＝１３４７），雄虾的体长与眼径之间的比率平均为２０．６８±０．０７（ｎ＝７４８），未成体虾的体长与复眼直径之间的比率平均为２１．５４±０．０６（ｎ＝１０７２）。利用体长与眼径之间的比率可以准确地将在实验室内活体培养后已存在负生长的磷虾与其它处于正常状态的磷虾分开。体长与眼径之间的比率也可以作为磷虾种群是否存在负生长的监测指标  相似文献   

CHINA: A COUNTRY OF THE THIRD WORLD OR THE THIRD GREAT POWER?     

Hu Zhaoliang 《地理学报(英文版)》1996,(3)

l.TheRapidEcono1ulcDevelopmentofCho1aSinceeconoAncreformandopen-doorpolicy,Cltinahasgrownrapidly.GDPinl993is3.4tilllesasmuChasti1atinl978.Annualgrowtlrateis9.2percent.li1ti1isresped,itisworthwniletostudyWhereChinaislocatedinti1eecononticltistoryoftheworld,andwhatthetrendofcurrentdeveoPmentwillChangeinto.Indevelopedcountriesofh1eWest,whentherateofecononhcdevelopmotwasthelligheSt,itwasnotltigherti1anthatofCltina'seconol11icdevelopmentafterreforl11andopen-doorpolicy.U.K.,forexample,Whichh…  相似文献   

Changes in the mullet fishery of Lake Manzala,Egypt     

Magdy T. Khalil 《International Journal of Salt Lake Research》1996,5(3):241-251

Growth rates of the main mullet species (Liza ramada andMugil cephalus) in Lake Manzala are low compared to those in other Egyptian lakes. But average growth rates during the period 1989–1993 were relatively faster than in the 1960's. Spawning and migration seasons have been determined for every species, and their distribution in the lake, in terms of certain ecological parameters (salinity, turbidity and dissolved oxygen) have been investigated. Changes in the mullet fishery in the lake during the past 70 years have been studied. Due to an increase in nutrient loading and a decrease in salinity, mullet declined from 65 per cent of the total catch during the 1920's to only 2.2 per cent during the early 1980's. As a result of fisheries management and development programmes from 1989 to 1993, mullet production increased to 9.2 per cent of the total catch.  相似文献   

知识经济时代的地理综合研究   总被引：10，自引：1，他引：10  

杨勤业  李双成 《地理科学进展》1998,17(3):20-25

２１世纪科学技术和知识将取代资本与劳动成为经济增长和社会发展的主导因子。知识经济时代所需求的经济增长方式，资本、信息、资源的配置格局，以及生命支撑系统的服务功能将与工业时代有很大的不同。这些变化对地理学综合研究大发展既是挑战又是机遇。本文从地理学综合研究的迫切性入手，分析了在知识经济时代综合研究的不同层次及可能涉及的领域。在此基础上，提出了地理学综合研究应在四个方面进一步深化和革新以适应知识经济时代的需求：①拓展地理综合研究的空间；②构建要素综合的非均衡观；③充分考虑科技和知识对自然和社会经济系统的强势作用；④逐步整合社会经济系统和自然环境系统。  相似文献   

Pacific-type orogeny revisited: Miyashiro-type orogeny proposed   总被引：30，自引：0，他引：30  

Shigenori  Maruyama 《Island Arc》1997,6(1):91-120

Abstract The concept of Pacific-type orogeny is revised, based on an assessment of geologic data collected from the Japanese Islands during the past 25 years. The formation of a passive continental margin after the birth of the Pacific Ocean at 600 Ma was followed by the initiation of oceanic plate subduction at 450 Ma. Since then, four episodes of Pacific-type orogeny have occurred to create an orogenic belt 400 km wide that gradually grew both oceanward and downward. The orogenic belt consists mainly of an accretionary complex tectonically interlayered with thin (<2 km thick), subhorizontal, high-P/T regional metamorphic belts. Both the accretionary complex and the high-P/T rocks were intruded by granitoids ～100 million years after the formation of the accretionary complex. The intrusion of calc-alkaline (CA) plutons was synchronous with the exhumation of high-P/T schist belts. Ages from microfossils and K-Ar analysis suggest that the orogenic climax happened at a time of mid-oceanic ridge subduction. The orogenic climax was characterized by the formation of major subhorizontal orogenic structures, the exhumation of high-P/T schist belts by wedge extrusion and subsequent domed uplift, and the intrusion-extrusion of CA magma dominantly produced by slab melting. The orogenic climax ended soon after ridge subduction, and thereafter a new Pacific-type orogeny began. A single Pacific-type orogenic cycle may correspond to the interaction of the Asian continental margin with one major Pacific oceanic plate. Ophiolites in Japan occur as accreted material and are not of island-arc but of plume origin. They presumably formed after the birth of the southern Pacific superplume at 600 Ma, and did not modify the cordilleran-type orogeny in a major way. Microplates, fore-arc slivers, intra-oceanic arc collisions and the opening of back-arc basins clearly contributed to cordilleran orogenesis. However, they were of secondary importance and served only to modify pre-existing major orogenic components. The most important cause of cordilleran-type orogeny is the subduction of a mid-oceanic ridge, by which the volume of continental crust increases through the transfer of granitic melt from the subducting oceanic crust to an orogenic welt. Accretionary complexes are composed mainly of recycled granitic sediments with minor amounts of oceanic material, which indicate that the accretion of oceanic material, including huge oceanic plateaus, was not significant for orogenic growth. Instead, the formation and intrusion of granitoids are the keys to continental growth, which is the most important process in Pacific-type orogeny. Collision-type orogeny does not increase the volume of continental crust. The name ‘Miyashiro-type orogeny’ is proposed for this revised concept of Pacific-type or cordilleran-type orogeny, in order to commemorate Professor A. Miyashiro's many contributions to a better understanding of orogenesis.  相似文献   

地面沉降规律预测新模式   总被引：5，自引：0，他引：5  

Yan Tongzhen 《地球科学》1989,(2)

文章讨论了地面沉降当前一般研究及其防治措施;提出了若干尚待深入研究的有关问题。概括了地面沉降区的几种重要沉积模式和沉降机理。以世界上记录到的最大的美国加州中部谷地和规模较小的中国浙江宁波市地面沉降为例,重点对其动态规律作了概要讨论;以其监测数据为背景,采用Verhulst氏生物模型原理和灰色控制系统理论分别对两者进行了控制预测及预测控制。结果表明,在一定控制条件下,可以预测出二者沉降寿命分别为140年和90年;若严格予以控制,宁波市可望免于沉没海水面之下。  相似文献   

Tree-ring evidence for 1842–1843 eruptive activity at the Goat Rocks dome,Mount St. Helens,Washington     

David K Yamaguchi  Donald B Lawrence 《Bulletin of Volcanology》1993,55(4):264-272

Until the 18 May 1980 eruption of Mount St. Helens, a debris fan and adjacent forest downslope from the dacitic Goat Rocks dome, on the north flank of the volcano, contained evidence that the dome was active in 1842 or 1843. The fan was destroyed by the debris avalanche of 18 May. Before 1980, the oldest tree cored on the debris fan showed that the fan predated 1855 by a few years. The young age of this tree suggests that the dome was active several decades after extrusion of the nearby andesitic floating island lava flow, dated to 1800. An anomalous series of narrow rings that starts with the 1843 ring is present in cores from two older trees adjacent to the fan. These ring-width patterns imply that these trees were damaged in late 1842 or early 1843 by flowage material from the dome; the trees were probably singed by an ash-cloud surge that originated on the dome as a hot-rock avalanche. Several lines of evidence suggest that the anomalous ring patterns record tree injury by surge, rather than by lahars or nonvolcanic causes (climate or insects). First, comparable ring patterns formed in all sampled trees that survived the 18 May surge, but formed in only a few sampled trees abraded or partially buried by 18 May lahars. Second, a 13-cm fine-ash layer, consistent with either tephra fall or surge emplacement, was present on the 1840s forest floor; yet the lack of similar tree-ring responses to 1980 tephra fall shows that such minor tephra fall could not have caused the ring patterns. Third, identical 1843 narrow-ring patterns are absent in control trees further from the volcano. The ring patterns of the trees adjacent to the Goat Rocks fan provide the first field evidence that the dome was active in late 1842 or early 1843. Thus, the new tree-ring dates confirm stratigraphic evidence for the youth of the activity of the Goat Rocks dome. They also link historical accounts of mid nineteenth century volcanism at Mount St. Helen with continuing dome extrusion. The dates additionally corroborate and revise the dacite-andesite-dacite petrologic cycle interpretation of Mount St. Helens' Goat Rocks eruptive period (1800–1857). They constrain the cycle to no more than 43 years. Lastly, the dates support the notion that the vent that erupted the 1800 dacitic T tephra was different from the one that produced the Goat Rocks dome. We infer that the magma that formed the floating-island lava flow plugged the T tephra vent. This forced residual magma from the compositionally zoned magma chamber into an alternate conduit. The second conduit produced the unnamed 1842 lithic tephra and the Goat Rocks dome.  相似文献   

Crustal Growth Rate of the North China Platform：a Method of Estimating Mass Equilibrium between Crust and Mantle     

Zheng Haifei  Zhang Benren  Han Yinwen  Ouyang Jianping 《中国地球化学学报》1994,13(3):284-288

The following equation is proposed in this paper to estimate the crustal growth rate of the North China Platform on the basis of mass equilibrium between the crust and the mantle:

相似文献    950. 新疆准噶尔地区花岗岩中微粒闪长质包体特征及后碰撞花岗质岩浆起源和演化   总被引：20，自引：0，他引：20   李宗怀韩宝福  李辛子杜蔚 杨斌 《岩石矿物学杂志》2004,23(3):214-226 新疆准噶尔地区也布山、庙儿沟两个晚古生代后碰撞准铝一过铝质花岗岩体中，广泛发育大量的暗色微粒闪长质包体。岩石学、矿物学、主量元素和微量元素地球化学研究表明，包体与其寄主岩存在明显的亲缘关系。东准噶尔也布山黑云母花岗岩体中的暗色微粒包体与寄主岩有相似的地球化学成分，表明它是与寄主花岗岩相同成因的同源包体，是来自上地幔的基性岩浆经过高度演化、结晶分异的产物；西准噶尔庙儿沟二长花岗岩体中含钾长石斑晶的微粒包体则主要是由幔源的下地壳基性岩部分熔融形成的残余体，被酸性岩浆携带并发生成分上的同化和混染，最后在上地壳侵位的产物。同准噶尔碱性花岗岩一样，载荷包体的准铝一过铝质花岗岩是晚古生代后碰撞阶段构造一岩浆活动的岩石类型之一，其形成和演化标志了准噶尔地区后碰撞幔源岩浆底侵作用导致大陆地壳垂向生长的过程。  相似文献    [首页] « 上一页 [90] [91] [92] [93] [94] 95 [96] [97] [98] [99] [100] 下一页 » 末  页»