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921.
实际地震作用是多维的、随机的,框架节点在2个方向同时受力,其抗震能力相比于单向地震作用会降低。目前,对节点核心区在2个方向同时受力时抗剪承载力的研究尚未完善。在双向受力下,节点核心区2个方向传来的剪力形成合剪力作用面,在节点核心区内部形成不同于单向受力下的斜向斜压杆。本文基于软化拉-压杆模型,针对水平双向受力相同的空间边节点,在合剪力作用面内建立抗剪承载力计算模型,确定空间边节点核心区斜压杆以及钢筋拉杆的计算方法。利用有限元软件建立不同参数空间边节点模型,并收集部分空间节点试验数据,将剪力计算值与模拟值或试验值进行对比。结果表明,基于软化拉-压杆模型建立的双向受力下钢筋混凝土框架,其边节点抗剪承载力计算值与模拟值或试验值吻合良好。 相似文献
922.
Spatial distribution and temporal trends of rainfall and erosivity in the Eastern Africa region 总被引:1,自引:0,他引:1
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Ayele Almaw Fenta Hiroshi Yasuda Katsuyuki Shimizu Nigussie Haregeweyn Takayuki Kawai Dagnenet Sultan Kindiye Ebabu Ashebir Sewale Belay 《水文研究》2017,31(25):4555-4567
Soil erosion by water is one of the main environmental concerns in the drought‐prone Eastern Africa region. Understanding factors such as rainfall and erosivity is therefore of utmost importance for soil erosion risk assessment and soil and water conservation planning. In this study, we evaluated the spatial distribution and temporal trends of rainfall and erosivity for the Eastern Africa region during the period 1981–2016. The precipitation concentration index, seasonality index, and modified Fournier index have been analysed using 5 × 5‐km resolution multisource rainfall product (Climate Hazards Group InfraRed Precipitation with Stations). The mean annual rainfall of the region was 810 mm ranging from less than 300 mm in the lowland areas to over 1,200 mm in the highlands being influenced by orography of the Eastern Africa region. The precipitation concentration index and seasonality index revealed a spatial pattern of rainfall seasonality dependent on latitude, with a more pronounced seasonality as we go far from the equator. The modified Fournier index showed high spatial variability with about 55% of the region subject to high to very high rainfall erosivity. The mean annual R‐factor in the study region was calculated at 3,246 ± 1,895 MJ mm ha?1 h?1 yr?1, implying a potentially high water erosion risk in the region. Moreover, both increasing and decreasing trends of annual rainfall and erosivity were observed but spatial variability of these trends was high. This study offers useful information for better soil erosion prediction as well as can support policy development to achieve sustainable regional environmental planning and management of soil and water resources. 相似文献
923.
地基抗液化能力评估方法讨论 总被引:1,自引:1,他引:0
为了评估地基抵抗液化的能力及其影响因素,本文介绍了标准贯入试验、静力触探试验以及剪切波速试验三种评估地基抗液化能力方法的研究成果,分析了震级比例系数、覆盖压力与倾斜地面的修正系数、地震震级与峰值加速度的影响,并对地基抗液化能力的概率分析方法进行了讨论,得到的结论可为地基的抗液化能力评估提供参考。 相似文献
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925.
砌体结构是一种传统的结构形式,在抗震设防区,钢筋混凝土—砖组合砌体结构与同层数的框架房屋相比,其经济效益相当明显,对此本文论述了钢筋混凝土—砖组合砌体结构的定义及相关计算公式。 相似文献
926.
927.
考虑了气候系统中一些变量突变时对预测关系的改变作用,用多元门限回归模型的建模方法建立长江下游地区夏季旱涝趋势预测模型。拟合效果较理想,用1994-1995年的独立资料检验,预测结果与实况较为接近。 相似文献
928.
Lingbo Xiao 《地球科学进展》2020,35(5):478-487
Based on records on famine kept in historical documents, 2950 famine events counted with “county time” in North China during 1736-1911 were collected, and annual famine index series in North China was reconstructed using weighted average method according to the severity of famine. Spatio-temporal distribution of famine and its relationship with climate, disaster and harvest was analyzed. The research shows that variation of temperature and precipitation has significant negative correlation with poor harvest and famine. The drought has a more significant correlation with harvest and famine than flood. In 1736-1795 when was at the peak of the Qing dynasty, the sensitivity of poor harvest and famine to drought was significantly lower than in 1796-1911 when was in decline, because effective social response to disaster could reduce the risk of poor harvest and famine. Using the kernel density estimation method, three main high risk areas of famine were indentified: Fen River Valley in south Shanxi Province, south-central He'nan Province, and the junction of Hebei, Shandong and He'nan Province. In general, there is significant corresponding relationship between the spatial distribution of drought, poor harvest and famine, however, abnormally high probability of famine in south-central He'nan Province might be related to local special socio-economic vulnerability. This study would enhance our understanding of the nature of interactions between climate change and socioeconomic system. Further research would focus on the mechanism by which famine originated in the past, and the pathway through which climatic impacts were delivered in human society. 相似文献
929.
Artemi Cerda Susanne Schnabel Antonio Ceballos Dionisia Gomez-Amelia 《地球表面变化过程与地形》1998,23(3):195-209
Soil hydrology was investigated in the Guadelperalón experimental watershed in order to determine the influence of land use and vegetation cover on runoff and infiltration within the Dehesa land system. Five soil–vegetation units were selected: (1) tree cover, (2) sheep trials, (3) shrub cover, (4) hillslope grass and (5) bottom grass. The results of the simulated rainfall experiments performed at an intensity of 56·6 mm h−1 during one hour on plots of 0·25 m2, and the water drop penetration time test indicate the importance of water repellency in the Dehesa land system under drought conditions. Low infiltration rates (c. 9–44 mm h−1) were found everywhere except at shrub sites and in areas with low grazing pressure. Soil water repellency greatly reduced infiltration, especially beneath Quercus ilex canopies, where fast ponding and greater runoff rates were observed. The low vegetation cover as a consequence of a prolonged drought and grazing pressure, in conjunction with the soil water repellency, induces high runoff rates (15–70 per cent). In spite of this, macropore fluxes were found in different locations, beneath trees, on shrub-covered surfaces, as well as at sites with a dominance of herbaceous cover. Discontinuity of the runoff fluxes due to variations in hydrophobicity causes preferential flows and as a consequence deeper infiltration, especially where macropores are developed. © 1998 John Wiley & Sons, Ltd. 相似文献
930.