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991.
1 IntroductionDeseamcation. defined as land degradation in tri4 send-arid and dry SUb-htald areas reSulhng fromvarious factors, including cljjnatic variahons and human activihes, is a world-wide phenomenon whichcauses the end's ecosystems to deteriorate. Nowadays it edicts about tWo-thirds of the coUntries of theworld, and one-third of the earth's surface, on which one-ffe of the world population liVe.Desertilicahon is accompanied by a reduction in the natUI'al potenhal Of the land ecosyst… 相似文献
992.
随着交通网络向偏远地区辐射,桥梁结构会不可避免的出现靠近断层的情况,受到近断层地震动的影响显著。为了研究近场地震作用下简支梁桥的搭接长度需求,基于ANSYS平台建立了简支梁桥的弹塑性分析模型。通过动力响应分析、弹塑性分析和抗剪能力分析,探讨了近场地震动的脉冲效应对简支梁桥搭接长度的影响。研究表明:近场地震动的脉冲效应放大了结构的地震响应,脉冲型地震和非脉冲地震作用时的最大墩梁相对位移分别为115.1 cm和41.5 cm;两类地震作用时的最大剪力分别为1 892.5 kN和1737.8 kN,最大剪力剪切强度比为0.82;当PGA≥0.4 g时,脉冲型地震作用下桥墩底部塑性铰区的最大转角超过极限转角,桥墩发生破坏,而非脉冲型地震PGA=1.0 g时的塑性铰转角小于极限转角;当PGA=1.0 g时,塑性铰破坏前墩梁相对位移为37 cm,占规范搭接长度的41.8%,近场地震作用下简支梁桥的搭接长度需求满足规范要求。 相似文献
993.
The Effect of Tide on the Global Climate Change 总被引:1,自引:0,他引:1
The differential rotation between the solid and fluid spheres caused by tidal force could explain the 1500 to 1800 - year cycle of the worlds temperature. Strong tide increases the vertical and horizontal mixing of water in the oceans,dra-wing the cold Pacific water from the depths to the surface and the warm water from the west to the east, where it cools or warms the atmosphere above, absorbs or releases CO2 to decrease or increase greenhouse effect and to make La Nina or El Nino occur in the global.
The moons declination and obliquity of the ecliptic affect the tidal intensity. The exchange of tidal energy and tide -generating force caused by the sun, moon and major planets makes the earths layers rotate in different speeds. The differenti-al rotation between solid and fluid of the earth is the basic reason for El Nino and global climate change. 相似文献
994.
某学科核心期刊是指发表该学科论文数量较多,文摘率、引文率、读者利用率相对较高,在本学科学术水平较高、影响力较大的那些期刊。 相似文献
995.
DENSIFICATION PROCESS WITHIN THE NEAR-SURFACE LAYER OF THE ANTARCTIC ICE SHEET 总被引:1,自引:0,他引:1 下载免费PDF全文
The densification process within the near-surface layer of Antarctic Ice Sheet is dominated by the environment and exhibits geographic zonality, In this article, the processes are found to be of three types: warm, cold and alternate, on the basis of the studies on a lot of shallow snow/firm cores from Wilkes Land, Antarctica, and the available data. Warm type densification takes place mainly on the periphery of the Antarctic Ice Sheet, where the mean annual temperature is about --10----15℃. High temperature in summer and consequent melting and infiltration are the main factors influencing the densification process. Cold type densification occurs in the huge central region of the Antarctica, where the mean annual temperature is below --25℃, with the maximum below 0℃ in summer. In this region, ice sintering is a main cause for the densification. The alternate type densification occurs in the transition zone between the above two regions, where the mean annual temperature is --15----25℃ and the highest 相似文献
996.
GUO Qingxia 《东北亚地学研究》2002,(1)
With the using of new full 3-D interpretative technology, the carefully interpretation of the micro ?amplitude structures and faults by the reprocessed 3-D seismic data in IES (Interactive Exploration System) interpretative system of Sun workstation is obtained. Because of the application of the well - advanced predictive technique for reservoir lithological changes, the predictive accuracy rate of drilling for 31 wells drilled in 1996 achieved 100% and the economic and social benefits are desirable. 相似文献
997.
You Zhendong Han Yujing Zhong Zengqin Sang Longkang Chen Nengsong Zhang Zeming 《中国地质大学学报(英文版)》1995,(1)
Petrogenesis of Eclogites in the Light of PunctuatedMetamorphic Evolution in Dabie Terrane,China¥YouZhendong;HanYujing;ZhongZ... 相似文献
998.
Based on observations from buoys, it is found that the wave age is well correlated with the nondimensional wave height, and this correlation is best described by a 3/5-power law. This similarity law is valid in the cases of wind waves as well as swells under natural sea states. On the basis of the 3/5-power law combined with the well-known 3/2-power law, it is shown that the wave-induced wind stress increases rapidly with wave age, indicating that the traditional observations or analytic techniques have only given the turbulent Reynolds stress induced by short wind waves, but excluded the long-wave-induced wind stress. The latter constitutes a small fraction to the total wind stress when the wave age is smaller than 1.0. The increase of sea-surface roughness with wave age can be attributed to wave breaking. 相似文献
999.
袁超 《矿物岩石地球化学通报》2020,(6):1324-1324
流体是控制地球内部能量传递和物质迁移的重要媒介之一。俯冲带流体循环对弧火山的形成、全球物质循环和地震的发生能起着至关重要的作用。因此,准确限定流体在俯冲带的分布范围和迁移机制对理解全球动力学具有重要意义。早期的研究普遍认为:俯冲洋壳脱水产生的流体只在较深的深度(通常在弧火山以下~105 km处)才开始进入上覆地幔,降低地幔物质部分熔融的温度,进而控制弧火山的位置。 相似文献
1000.
Sequence Stratigraphy of Upper Proterozoic Glacigenous Rocks in Southeastern Margin of Yangtze Platform 总被引:1,自引:0,他引:1
INTRODUCTIONTheUpperProterozoicglacigrnousrocksarewidelydistributedinthesoutheasternmarginoftheYangtzeplatformandaflpreservedinHunan,Hubei,GulhouandGuanghProvince.PreviousbarkontheSestudhasbeendonebyLuetal.(1985)andLiuetal.(1991).TheysUggeStedthatthesegladgenousrockscanbeusedasbarkersforhighresolutionstratigl'aphiccoagulationfromcontinenttocontinent,andadoptedtheconceptofPrecambrianglobaliceagepearland,1900.ReCentresea~showthattheSestudhaveah~useaschronostratigraphicmarkers.InrejeC… 相似文献