强磁场中的逆Compton散射与γ射线爆能谱     

詹善群  史天一 《中国天文和天体物理学报》1993,(1)

本文认为强磁场中的逆Compton散射可能是γ射线爆的主要辐射机制.其能谱是由源区质子产生的低频光子经强磁场中非热电子的Compton散射形成的.我们利用非相对论情形(B/B_(cr)≤1,hv_i/m_ec~2≤1)下强磁场中的Compton散射微分截面,导出了上述Compton散射的辐射谱公式,由此很好地拟合了典型γ射线爆GB811016的观测能谱.  相似文献   

DISSOLVED OXYGEN DISTRIBUTION AND O_2 FLUXES ACROSS THE SEA-AIR INTERFACE IN EAST CHINA SEA WATERS     

宋金明  詹滨秋  李鹏程 《中国海洋湖沼学报》1996,(4)

This study on the sectional and vertical distribution of dissolved oxygen (DO) and the O_2 fluxes acrossthe sea-air interface in East China Sea (ESC) waters shows that the waters were in steady state and thatthe difference of DO was great in upper and bottom waters in Apr. 1994; but that seawater mixingwas strong and the difference of DO was small in upper and bettom waters in Oct. 1994. The above con-dusions were specially obvious in continental shelf waters under 100m. The DO maximum in subsurfacelayer waters appeared only at several stations and in general the DO in the waters decreased with depth.The horizontal distributions of O_2 fluxes across the sea-air interface appeared in stripes in Leg 9404 whenmost regions covend were supersaturated with O_2. seawater to air flux wn large, and that on section No.1was 1.594 L/m~2·d. The horizontal distribution of O_2 fluxes across the sea-air interface appeared lumpy inLeg 9410, when most regions covered were unsaturated with O_2. O_2 was dissolved from air  相似文献   

一个拱桥状爆发日珥的运动情况     

钟树华  占腊生 《天文研究与技术》2005,2(1):12-18

分析了1991年3月7日太阳东北边缘一个拱桥状爆发日珥上升、下降和半径膨胀的运动情况。该日珥的上升阶段和下降的开始阶段高度随时间的变化比较迅速,而且基本是线性的变化,但在下降的结束阶段则比较缓慢,也基本是线性的变化。它的下降运动不仅受到重力作用自由下落,而且还受到不均匀的大气阻力,磁场等力的共同作用而下落。而速度,喷射出以后总的在逐渐减弱,上升阶段减弱较快。下降阶段初期有一次跳跃式的变化,先迅速减弱,然后又很快增加,在下降后期速度减弱较慢。日珥到达最大高度的时间比日珥半径膨胀到达最大尺度的时间早4min左右。上升下降速度最大时半径膨胀速度最小,而上升下降速度最小时半径膨胀的速度最大。  相似文献   

The polypeptide in Chlamys farreri can protect human dermal fibroblasts from ultraviolet B damage     

张玉江  战松梅  曹鹏利  刘宁  陈雪红  王跃军  王春波 《中国海洋湖沼学报》2005,23(3):357-362

~~The Polypeptide in Chlamys farreri can protect human dermal fibroblasts from ultraviolet B damage@张玉江$Qingdao University, Medical College,Qingdao Shandong 266021,China @战松梅$Qingdao University, Medical College,Qingdao Shandong 266021,China @曹鹏利$Qingdao University, Medical College,Qingdao Shandong 266021,China @刘宁$Qingdao University, Medical College,Qingdao Shandong 266021,China @陈雪红$Qingdao University, Medical College,Qingdao Shandong 266021,China @…  相似文献   

汶川M_S8.0级地震成因三“层次”分析——基于深部电性结构   总被引：2，自引：1，他引：1       下载免费PDF全文

赵国泽  陈小斌  肖骑彬  王立凤  汤吉  詹艳  王继军  张继红  H. Utada  M. Uyeshima 《地球物理学报》2009,52(2):553-563

2008年5月12日汶川M_S8级地震的发生不是局部地区孤立的构造事件,研究汶川地震的孕震机制,应该把局部分析和区域分析相结合,关注地壳上地幔直至地幔过渡带的深部结构.基于近年来在东北、华北和汶川地震附近地区进行的深部结构电磁探测结果,结合地震学等其他资料,从太平洋板块的俯冲、印度板块的碰撞和松潘甘孜地块的推挤三个“层次”探讨分析汶川特大地震的成因.太平洋板块向亚洲大陆的俯冲作用,导致中国大陆东部地幔过渡带深度较普遍地存在着停滞的板片,它对汶川地震的影响不可忽视.印度板块与青藏高原的碰撞,使组成高原的各地块发生向北和向东的运动,各地块向东的运动作用于南北地震带中南段,影响到该区域的地震活动.松潘甘孜地块向四川地块的推挤,使松潘甘孜地块运动方向和龙门山断裂带形成“丁”字形结构,龙门山断裂带显示为较陡直的电性边界,加剧了汶川地震前的应力积累,可能是汶川地震发生的最直接的诱因.  相似文献   

TEQC检验在福建省GPS连续观测基准站勘选中的应用   总被引：1，自引：0，他引：1  

林淑冰  占惠  王海清 《华北地震科学》2009,27(3):35-40

介绍了福建省30个GPS连续观测基准站的勘选过程中,应用TEQC数据预处理软件,对勘选到的基准站进行24h的测试,并做出质量分析。从而勘选出满足规范、可靠、安全、科学的GPS连续观测基准站站址,为下一步GPS连续观测基准站建站提供依据。  相似文献   

Deep electrical structure of the Sulu orogen and neighboring areas   总被引：2，自引：0，他引：2  

XIAO QiBin  ZHAO GuoZe  WANG JiJun  ZHAN Yan  CHEN XiaoBin  TANG Ji  CAI JunTao  WAN ZhanSheng  WANG LiFeng  MA Wei & ZHANG JiHong Institute of Geology  China Earthquake Administration  Beijing  China  Earthquake Administration of Sh  ong Province  Jinan 《中国科学D辑(英文版)》2009,52(3):420-430

Because of the discovery of ultrahigh pressure metamorphic (UHPM) belt beneath the Sulu (Jiangsu Province-Shandong Province) orogen, this area has become a focused subject of current geoscience, as it has a close relationship with the evolution of the orogen and the neighboring North China craton. Probing the deep structure beneath this area would be of great significance for the geological interpretation of this issue. In this study, we make an analysis of magnetotelluric (MT) data along a profile across the Sulu orogen to provide evidence of deep structure below this region. The profile begins in west from the North China block, extending in S129°E, across the Tan-Lu fault, Sulu UHPM zone, and Sulu high pressure metamorphic (HPM) zone, and terminates in the Yangtze block in east. We use the nonlinear conjugate gradient method and TE-TM combined mode to perform inversion and interpretation of the MT data, and obtain an electrical structure image above depth of 150 km along the profile. It shows that the structure can be divided into seven sections in lateral direction, between which the electric boundaries coincide well with the major faults, such as the Tan-Lu, Haizhou-Siyang, and Jiashan-Xiangshui faults. In vertical direction the electrical structure can be subdivided into six layers of different resistivities. It is noted that there exist high-conductivity areas in crust below the North China block and Yangtze block, while such a feature is not present beneath the Sulu orogen, which is very different from the Dabie orogen. It is also observed that a fairly continuous zone of relatively low-resistivity exists at depths of 50–90 km of the electrical structure image, which is presumably a weak zone in the uppermost mantle. Just below this low-resistivity zone are the relatively high- resistivity layer of the North China block, relatively low-resistivity layer of the Sulu orogen, and relatively high-resistivity layer of the Yangtze block, all in the shallow upper mantle, respectively. From the whole 2D electrical structure image, there is no abnormally low-resistivity layer in the shallow upper mantle beneath the Sulu orogen and neighboring areas, indicating that no hot asthenoshperic material associated with lithospheric thinning exists at present. Supported by National Natural Science Foundation of China (Grant No. 40534023) and Director Foundation of Institute of Geology, China Earthquake Administration (Grant No. DF-IGCEA-0608-2-16)  相似文献   

新疆三工河流域农业需水量预测与分析   总被引：2，自引：1，他引：1  

占车生  丰华丽  马灵玲  姜小光  王飞 《干旱区地理》2009,32(3)

依据新疆三工河流域的农业生产发展情况以及农业用水现状,综合考虑该流域土地资源状况和农业发展方向,结合国家西部大开发战略和相关的宏观经济调整政策,预测2005年、2010年和2020年流域三个水平年的农业需水量,分析了未来20年的农业需水态势.同时,结合该地区工业、生活、生态环境需水量的未来变化趋势,平衡分析了在满足未来农业需水条件下的社会-经济-生态复合系统水资源配置的合理性,并提出从农业灌溉中节水,尽量追求内涵式发展的农业模式,这才是谋求三工河流域社会-经济-生态复合系统可持续发展的有效之路.同时,这也为国家对该地区的国土开发、经济建设布局以及长远水资源利用问题进行宏观决策提供了参考依据.  相似文献   

我国防控外来物种入侵的立法思考   总被引：3，自引：0，他引：3  

詹长英 《湿地科学与管理》2009,5(4):49-52

我国防控外来物种入侵相关法律缺乏应有的系统性和协调性,各职能部门基本上是"各立各的法、各管各的事",有时甚至相互矛盾。相关法律、法规比较分散,立法角度也不相同,不能全面地解决和控制外来入侵种对我国可能造成的生态、经济和健康的破坏,需要着手研究《防止外来物种入侵法》的立法。本文尝试性地对外来物种入侵的相关法律、法规进行考察和分析,并对构建防止外来物种的入侵提出立法思考,为制定《防止外来物种入侵法》提出立法原则和理论参考。  相似文献   

台湾海峡海表气溶胶干沉降通量研究   总被引：1，自引：0，他引：1  

詹建琼  陈立奇  张远辉  杨绪林  李伟  林奇  杜俊民  林红梅 《台湾海峡》2010,29(2):257-264

在已改进的Williams模型中,应用GW03海表动力学粗糙度参数化方案,考虑波浪对干沉降速率的影响,结合卫星资料和再分析资料,计算了台湾海峡海表气溶胶干沉降速率,并利用2006～2007年走航观测结果计算了台湾海峡总悬浮颗粒物的入海通量.其结果表明：台湾海峡海表气溶胶干沉降速率及总悬浮颗粒物干沉降通量具有明显的时空变化特征.台湾海峡海表气溶胶干沉降速率范围为5.83～6.17 cm/s,平均值为6.00 cm/s.其中冬季气溶胶干沉降速率最大,平均值为6.08 cm/s;夏季气溶胶干沉降速率最小,平均值为5.85 cm/s.台湾海峡气溶胶总悬浮颗粒物的干沉降通量也呈现出冬季的高[均值为7.31μg/（m2.s）],夏季的低[均值为2.23μg/（m2.s）]的特征.从空间分布上看,台湾海峡海表气溶胶干沉降速率出现1个高值中心,位于台湾海峡北部海域.总悬浮颗粒物干沉降通量出现2个高值中心和1个低值中心,分别位于台湾海峡北部海域、汕头至厦门海域和南海中北部海域.  相似文献