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71.
三峡库区地震精定位中确定速度模型的方法 总被引:2,自引:1,他引:1
研究三峡库区地震精定位中确定速度模型的方法,分析不同速度模型对地震定位精度的影响,并选取多种方法来定量评价不同速度模型的地震定位精度。当地震分布或台站能够较好的覆盖研究区域,采用Kissling方法拟合观测数据得到的速度模型地震定位精度最高。当地震分布不能较好的覆盖研究区域,由人工地震测深结果得到的速度模型地震定位精度次之。当没有足够的观测数据,也没有人工地震测深结果,综合研究区域内的相关研究成果确定的速度模型也是可用的,但是地震定位的精度不高,特别是震源深度的精度很差。 相似文献
72.
73.
北京山区沟域经济发展的空间结构 总被引:1,自引:0,他引:1
Valley economy is a new mode in mountainous area development that is defined by various characters of valley development, and is a distinguishing economical geographic pattern for mountainous area development. The special spatial coupling relations in the distribution of different mountainous elements in valleys are new subjects for the mountain development studies, and such studies are meaningful both for researches and practices. Based on the long term researches on mountainous area development and following a brief exploration into the connotations and the spatial organizing process of valley economy, the authors analyzed the present situations of the development of valley economy in Beijing’s mountainous areas, studied the characteristics and the impacts of the spatial structural changes of the valley economy in Beijing’s mountainous areas, and finally proposed a rational arrangement of the spatial structure of the valley economy in Beijing’s mountainous areas. It is considered in this study that valley economy plays an important role in the development and functional transformation in Beijing’s mountainous areas in the new epoch. Firstly, valley economy is not outlined by the administrative boundaries, and it connects most of the villages in the mountainous areas roughly along the major transportation lines. Therefore, valley economy can exert positive influence on the development in the mountainous areas, at least in the aspects such as the rearrangement of industrial structure in the mountainous areas and the coordinated development of rural and urban areas. In addition, it is found that the valley economy in Beijing’s mountainous areas is evolved in a spatial organizing stage of secondary concentration, which is characterized by resource-saving, ecological protection and industrial optimization. Therefore, the development of valley economy will be helpful to the coordination between ecological protection and economic development in the mountainous areas, and will promote the integrated development of the mountainous areas. The developing mode of the valley economy in Beijing’s mountainous areas will provide the basis for the decision-making in the transformation of the functional roles of Beijing’s mountainous areas, and on the other hand, will present experiences for the studies in the mountainous areas outside of Beijing. 相似文献
74.
Empirical models of calculating phreatic evaporation from bare soil in Tarim river basin,Xinjiang 总被引:1,自引:0,他引:1
Based on the experimental data at the Akesu Water Balance Experimental Station (AWBES) from 1990 to 1996, the control conditions
of establishing calculation models of phreatic evaporation have been analyzed, the empirical formulae for calculating the
phreatic evaporation have been presented. The results show that as for a given phreatic depth, the phreatic evaporation increases
nonlinearly with pan evaporation, when pan evaporation reaches the infinity, the phreatic evaporation is close to limiting
phreatic evaporation. The new models overcome the disadvantages of phreatic evaporation overestimation when atmospheric evaporation
demand is great and the linear relationship between phreatic evaporation and pan evaporation. With a high accuracy, the new
models are appropriate to be applied in similar regions without observed data. 相似文献
75.
IASPEI新震级标度与传统震级标度的对比 总被引:1,自引:0,他引:1
通过对世界上主要地震台网中心几十年来震级测定结果的对比分析,针对数字地震记录频带宽、动态范围大的特点,国际地震学与地球内部物理学协会(IASPEI)震级工作组于2003年提出了新的震级标度和测定方法,新的震级标度包括地方性震级ML、面波震级Msc(20)和Ms(BB)、体波震级mb和mB、区域Lg震级mb(Lg)和矩震级MW,本文介绍了这些新震级及其测定方法,并将这些震级与我国传统震级mb、mB、MS7、Ms在计算公式、振幅量取、周期范围和震中距范围几个方面进行了详细的比较。 相似文献
76.
Shaking table tests and dynamic analyses of masonry wall buildings with frame-shear walls at lower stories 总被引:1,自引:0,他引:1
David Xiong 《地震工程与工程振动(英文版)》2008,7(3):271-283
This paper describes shaking table tests of three eight-story building models: all are masonry structures in the upper stories, with or without frame-shear walls of one- or two- stories at the bottom. The test results of damage characteristics and seismic responses are provided and compared. Then, nonlinear response analyses are conducted to examine the reliability of the dynamic analysis. Finally, many nonlinear response analyses are performed and it is concluded that for relatively hard sites under a certain lateral stiffness ratio (i.e., the ratio of the stiffness of the lowest upper masonry story to that of the frame- shear wall story), the masonry structure with one-story frame-shear wall at the bottom performs better than a structure built entirely of masonry, and a masonry structure with frame-shear wall of two stories performs better than with one-story frame- shear wall. In relatively soft soil conditions, all three structures have similar performane. In addition, some suggestions that could be helpful for design of masonry structures with ground story of frame-shear wall structure in seismic intensity region VII, such as the appropriate lateral stiffness ratio, shear force increase factor of the frame-shear wall story, and permissible maximum height of the building, are proposed. 相似文献
77.
78.
基于生态恢复的塔里木河干流生态需水量预测 总被引:1,自引:0,他引:1
以2005年为现状年,用定额法、潜水蒸发法和地下水储量变化法估算出塔里木河干流的生态需水量,其结果分别为33.89×108 m3、23.97×108 m3和33.07×108 m3,通过分析得到现状年合理的生态需水量为30.31×108 m3.并根据阿克苏、沙雅、库车、轮台、库尔勒、尉犁和铁干里克7个气象站1995-2004年的月平均蒸发量,采用阿维里扬诺夫公式和群克水均衡场公式对塔里木河干流天然植被的月潜水蒸发量进行计算,在此基础上计算月生态需水量.通过分析发现,植被生长期(4-10月)的生态需水量占全年生态需水量的86%,尤其是植被生长旺盛时期的5-8月的生态需水量占全年的59%.根据制定的生态恢复方案,用定额法和潜水蒸发法预测3个目标年的生态需水量,将两者计算结果加以算术平均,得到2010、2015及2020年合理的生态需水量分别为31.88×108 m3、34.08×108 m3及36.84×108 m3,为塔里木河流域的水资源优化配置提供科学依据. 相似文献
79.
80.
古尔班通古特沙漠植被与环境关系分析 总被引:2,自引:0,他引:2
The Gurbantunggut Desert is the largest stable and semi-stable sand desert in China, yet few data exist on vegetation pattern and species-environment relationships for these diverse desert landscapes. The sand dunes of the survey area are mainly of the longi- tudinal form from north to south, but checkerboard-shaped and honeycomb-shaped forms are also present, with the height of 10-50 m. We measured vegetation and soil data on north-south transects and compared them with vegetation and soil data on east-west transects. Analysis revealed that the varying trend and strength of the species diversity, dominance and cover of the plant communities in the longitudinal and transverse directions across the landscape are significantly different. The results of CCA ordination show that the microhabitats of soil organic matter (OM), soil salts (TS), sorting index ( σ ), topsoil water-content (SM) and pH relate to the differences in vegetation observed as differences in species assemblage from salt-intolerant ephemerals, micro-subshrubs and subshrubs to salt-tolerant shrubs and micro-arbors. The terrain (alt.) and soil texture (the contents of Mz and Ф 1) affect the spatial differentiation of many species. However, this spatial differentiation is not so marked on transects running longitudinally with the landscape, in the same direction as the dunes. The species of the desert vegetation have formed three assemblages under the action of habitat gradients, relating to three sections running transversely across the landscape, at right angles to the direction of the dune crests. In the mid-east section of the study area the topography is higher, with sand-lands or dune-slopes with coarse particles. Here the dominant vegetation comprises shrubs and subshrubs of Seriphidium santofium and Ephedra distachya, with large numbers of ephemeral and ephemeroid plants of Senecio subdentatus, and Carex physodes in spring and summer. On the soil of the dune-slopes in the mid-west of the study area, with coarse partic 相似文献