基于TCP/IP协议的前兆数据管理软件     

李忠伟  温岩  陈波  邵喜彬 《地震地磁观测与研究》2004,25(4):42-47

为了实现地震前兆数据向中国地震局的报送、数据及时录入SQL数据库,本文介绍了一种前兆数据管理方案,并且在TCP／IP协议上使用VB编写了软件,介绍了程序编写的主要方法。  相似文献   

Several strategies on 3D modeling of manmade objects     

SHAOZhenfeng LIDeren CHENGQimin 《地球空间信息科学学报》2004,7(1):67-71

Several different strategies of 3D modeling are adopted for different kinds of manmade objects. Firstly, for those manmade objects with regular structure, if 2D information is available and elevation information can be obtained conveniently, then 3D modeling of them can be executed directly. Secondly, for those manmade objects with complicated structure comparatively and related stereo images pair can be acquired, in the light of topology-based 3D model we finish 3D modeling of them by integrating automatic and semi-automatic object extraction. Thirdly, for the most complicated objects whose geometrical information cannot be got from stereo images pair completely, we turn to topological 3D model based on CAD.  相似文献   

长江口-杭州湾毗连海区的现代沉积速率   总被引：30，自引：9，他引：21  

夏小明  杨辉  李炎  李伯根  潘少明 《沉积学报》2004,22(1):130-135

运用沉积地层同位素210 Pb、137Cs测年技术,估算长江口 杭州湾毗连海区的现代沉积速率。研究结果表明,以泗礁水道为界,东侧的马鞍列岛区受外海高盐水的顶托,长江来沙少,淤积缓慢;西侧至长江口、杭州湾海岸交汇点 (南汇咀 )之间水域,是长江泥沙扩散南下的主要通道。其中,受长江冲淡水次级锋和杭州湾锋面输沙影响的湾口浅滩区,沉积速率约 3cm/a;洋山港区,水深大于 20m的峡道区,受强动力作用而处于侵蚀状态,峡道两端出口的浅水区,沉积速率为0.3～ 1.6cm/a;马迹山港区,位于典型的峡道沿岸淤泥质陡坡,其沉积过程不稳定,正常沉积速率为 0.7～ 3.4cm/a,但常有快速淤积和地层滑塌流失现象发生.  相似文献   

震后短期和长期形变模拟——以1960年智利Mw9.5地震为例   总被引：2，自引：1，他引：1       下载免费PDF全文

邵志刚  傅容珊  薛霆虓  查显杰 《地震学报》2008,(4)

以1960年5月智利瓦尔迪维亚(Valdivia)Mw9.5地震为例分析震后不同时期的形变,实现了以Burgers体为粘弹介质模型来模拟震后粘弹松弛效应有限元数值模拟.计算结果表明,该粘弹介质模型可以模拟地震引起的瞬时同震弹性响应及震后粘弹松弛的短期和长期响应.由1960智利Mw9.5地震震后模拟的应变率显示以Burgers体为粘弹介质模型可以解决Maxwell体在模拟震后短期和长期形变不协调问题.  相似文献   

The characteristics of soil water cycle and water balance on steep grassland under natural and simulated rainfall conditions in the Loess Plateau of China   总被引：3，自引：0，他引：3  

Hongsong Chen  Mingan Shao  Yuyuan Li 《Journal of Hydrology》2008,360(1-4):242-251

Large-scale vegetation restoration has been helpful to prevent serious soil erosion, but also has aggravated water scarcity and resulted in soil desiccation below a depth of 200 cm in the Loess Plateau of China. To understand the dynamic mechanism of soil desiccation formation is very important for sustainable development of agriculture in the Loess Plateau. Based on natural and simulated rainfall, the characteristics of soil water cycle and water balance in the 0–400 cm soil layer on a steep grassland hillslope in Changwu County of Shaanxi Loess Plateau were investigated from June to November in 2002, a drought year with annual rainfall of 460 mm. It was similarly considered to represent a rainy year with annual rainfall of 850 mm under simulated rainfall conditions. The results showed that the temporal variability of water contents would decrease in the upper 0–200 cm soil layer with the increase in rainfall. The depth of soil affected by rainfall infiltration was 0–200 cm in the drought year and 0–300 cm in the rainy year. During the period of water consumption under natural conditions, the deepest layer of soil influenced by evapotranspiration (ET) rapidly reached a depth of 200 cm on July 21, 2002, and soil water storage decreased by 48 mm from the whole 0–200 cm soil layer. However, during the same investigation period under simulated rainfall conditions, soil water storage in the 0–400 cm soil layer increased by only 71 mm, although the corresponding rainfall was about 640 mm. The extra-simulated rainfall of 458 mm from May 29 to August 10 did not result in the disappearance of soil desiccation in the 200–400 cm deep soil layer. Most infiltrated rainwater retained in the top 0–200 cm soil layer, and it was subsequently depleted by ET in the rainy season. Because very little water moved below the 200 cm depth, there was desiccation in the deep soil layer in drought and normal rainfall years.  相似文献   

Spatial distribution of surface rock fragment on hill-slopes in a small catchment in wind-water erosion crisscross region of the Loess Plateau   总被引：3，自引：0，他引：3  

YuanJun Zhu  MingAn Shao 《中国科学D辑(英文版)》2008,51(6):862-870

The cover and size distributions of surface rock fragment in hillslopes were investigated by using digital photographing and treating technique in a small catchment in wind-water erosion crisscross region of the Loess Plateau. The results indicated that the maximal cover of rock fragment was pre-sented at mid-position in steep hillslope. Rock fragment presented a general decreasing-trend along the hillslope in gentle hillslope. Rock fragment cover was positively related to gradient, rock fragment size decreased generally along the hillslope, and the size reduced with the gradient. The mean size of rock fragment was at a range of 6―20 mm in the steep hillslope, rock fragment size > 50 mm was rarely presented. The covers of rock fragment at different positions were markedly related to the quantities of rock fragment < 40 mm. The area of rock fragment of 2―50 mm accounted for 60% or more of the total area, dominating the distribution of rock fragment in the hillslopes.  相似文献   

利用WSBV的引物扩增中国对虾的杆状病毒DNA     

汪岷  苏冬梅  包振民  邵济钧  戴继勋 《中国海洋大学学报(自然科学版)》1998,(4)

利用台湾报道的ＷＳＢＶ的ＰＣＲ引物,成功地扩增出了１４００ｂｐ左右的中国对虾的杆状病毒的ＤＮＡ片段,与预计的产物长度吻合。该引物对经初步离心处理的病虾组织也能扩增出特异性ＤＮＡ条带,而对正常虾组织ＤＮＡ、昆虫杆状病毒（ＡｃＭＮＰＶ）ＤＮＡ进行扩增,均获得阴性结果。说明该引物的特异性较高,对中国对虾的杆状病毒的检测具有一定的实际应用价值。实验结果同时说明ＷＳＢＶ与中国对虾的杆状病毒有同源序列存在,具有一定的保守性;用该引物进行的ＰＣＲ扩增为中国对虾的杆状病毒与其他相关病毒的比较研究提供了一种技术手段。  相似文献   

On the Choice of Soil Hydraulic Models in Land-Surface Schemes   总被引：9，自引：0，他引：9  

Yaping Shao  Parviz Irannejad 《Boundary-Layer Meteorology》1999,90(1):83-115

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Numerical Modelling of Saltation in the Atmospheric Surface Layer     

Yaping Shao  An Li 《Boundary-Layer Meteorology》1999,91(2):199-225

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Multivariate Correlation in the Framework of Support and Spatial Scales of Variability     

J. A. Vargas-Guzmáan  A. W. Warrick  D. E. Myers 《Mathematical Geology》1999,31(1):85-103

This paper extends the concept of dispersion variance to the multivariate case where the change of support affects dispersion covariances and the matrix of correlation between attributes. This leads to a concept of correlation between attributes as a function of sample supports and size of the physical domain. Decomposition of dispersion covariances into the spatial scales of variability provides a tool for computing the contribution to variability from different spatial components. Coregionalized dispersion covariances and elementary dispersion variances are defined for each multivariate spatial scale of variability. This allows the computation of dispersion covariances and correlation between attributes without integrating the cross-variograms. A correlation matrix, for a second-order stationary field with point support and infinite domain, converges toward constant correlation coefficients. The regionalized correlation coefficients for each spatial scale of variability, and the cases where the intrinsic correlation hypothesis holds are found independent of support and size of domain. This approach opens possibilities for multivariate geostatistics with data taken at different support. Two numerical examples from soil textural data demonstrate the change of correlation matrix with the size of the domain. In general, correlation between attributes is extended from the classic Pearson correlation coefficient based on independent samples to a most general approach for dependent samples taken with different support in a limited domain.  相似文献