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341.
Preliminary investigation of seismic damage to two steel space structures during the 2013 Lushan earthquake 总被引:2,自引:2,他引:0
Severe damage to steel space structures is rarely reported when compared to other structural systems damaged during past major earthquakes around the world.Two gymnasiums of steel space structures in downtown Lushan County that were damaged during the 2013 M7.0 Lushan earthquake in China were investigated and the observations are summarized in this paper.Typical damage to these two steel space structures ranges from moderate to severe.Moderate damage includes global buckling and dislocation of bolted connections of truss members,and inelastic elongation of anchor bolts and sliding of pedestal plates of supports.Severe damage includes member fracture caused by local buckling,and fracture failure of anchor bolts and welds.The distribution of structural damage to these two structures is described in detail and future research opportunities are suggested. 相似文献
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本文在分析中国生物质能产业发展现状的基础上,认为当前中国生物质能产业发展受到资源家底不清、政策环境不完善和生态保护压力等因素制约,存在着产业发展总体水平低,产业体系不健全,生产成本高,产业技术水平低,行业发展无序等问题。结合这些问题,立足我国资源环境承载能力,适应市场需求变化和科技进步趋势,本文提出今后重点加强生物质能产业发展政策扶持,生物质能原料资源调查评估,生物质能转化利用技术开发和能源产业示范基地建设,以期促进生物质能产业健康快速发展。 相似文献
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Plant drought tolerance trait is the key parameter in improving the modeling of terrestrial transpiration in arid and semi-arid regions 总被引:1,自引:0,他引:1
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Xintao Liu Xingjie Lu Shulei Zhang Zhongwang Wei Nan Wei Shupeng Zhang Hua Yuan Wei Shangguan Shaofeng Liu Jianfeng Huang Lu Li Xiulan Ye Jinxuan Zhou Wenke Hu Yongjiu Dai 《大气和海洋科学快报》2022,15(1):35-41
陆面过程蒸腾作用的模拟制约着天气,气候降水预测的精确度.近几十年来,为了更好地描述植被蒸腾的水力约束,陆面过程模式发展了基于植物性状的植物水力胁迫方案.然而,我们对于植物性状在蒸腾模拟中的地位仍然缺乏了解,植物性状对蒸腾的重要性仍需进一步量化.本研究利用Morris方法评估植物性状参数在通用陆面模式植物水力胁迫方案(CoLM-P50HS)中的重要性,针对17种植物性状,筛选出最为重要的:耐旱性状(P50),气孔性状,和光合作用性状.在12个FLUXNET站点中,参数的重要性由归一化敏感度来衡量.P50的重要性随着降水的减少而增加,而气孔性状和光合作用性状的重要性则随着降水的减少而减少.在干旱或半干旱地区,P50比气孔性状和光合作用性状更重要,这意味着当植物经常经历干旱时,水力安全策略比植物生长策略更关键.而耐旱性状的巨大变异性进一步暗示了多种植物水力安全策略的共存.忽视P50的变异性可能会对陆面过程模式蒸腾作用的模拟造成严重误差.因此,为了更好地表示植物水力功能的变异性,需要增加对耐旱性状的观测并耦合到陆面模式中. 相似文献
346.
马脑壳金矿床位于中国重要的"川、甘、陕"成矿远景区的川西北地区,是川西北地区与构造蚀变带有关的微细浸染型金矿的典型代表。近年来深部勘查、外围找矿和矿山开采发现了许多与原有认识不一致的地质现象,特别是越往深部,构造控矿和热液流体活动的迹象明显增强。根据对矿床地质特征的进一步研究,分析了矿床控矿因素,总结了成矿规律,探讨了矿床成因,指出了进一步找矿的方向。认为马脑壳金矿床以构造控矿为主,构造破碎岩带是主要矿体赋存部位,构造变形程度控制着矿体的空间分布、产出形态和矿化富集程度。多组构造复合部位是重要的赋矿部位,虽然矿(化)体总体呈北西向展布,但北北东向构造、北西向以及南北向构造复合部位是寻找富大矿体的主要方向。矿床表现出的层控性特点,主要与不同物理化学性质岩层的岩石组合有关,能干性(渗透障)与非能干性(不渗透障)岩层的交互叠置和有序排列,导致所有金矿体都产于能干性和非能干性的转换部位,即砂岩、板岩的接触部位。马脑壳矿床的成矿与传统的卡林型金矿有较大的差异,构造—岩浆活动对成矿起了重要的控制作用,有深部流体参与成矿的迹象,属多因复式成矿特征的大型中低温热液金矿床。 相似文献
347.
Causes of landslide recurrence in a loess platform with respect to hydrological processes 总被引:2,自引:1,他引:1
Irrigation-induced landslide is a recurring problem in the Heifangtai loess platform of northwest China. The landslide sites are characterized by a concave topography. Numerical modeling indicates that the groundwater table at the past-landslide site rises more quickly than the other natural platform borders under irrigation conditions. This is consistent with the field observations that seepage of the groundwater appeared in the hollow is higher than that of lateral slopes. In order to investigate the response of soil behavior due to rise in groundwater table, stress-path tests were performed on undisturbed specimens. It has been observed that the increase in pore water pressure in loess can trigger soil liquefaction and eventually results in landslide. Hence, the concave past-landslide site is much more prone to landsliding, which contributed to the landslide recurrence. 相似文献
348.
Research on thermal shock resistance of mullite-bauxite-silicon carbide castable refractory 总被引:1,自引:0,他引:1
Nobuaki Chiyoda 《中国地球化学学报》2012,31(2):204-208
Effects of different silicon carbide contents on thermal shock resistance properties of mullite-bauxite castable refractory were analyzed respectively by taking the mullite,bauxite as main raw materials and taking calcium aluminate cement as a binding system.After 24 h curing in mould and another 24 h curing at 110℃ after demoulding,the samples were heated at 1000,1300 and 1500℃for 3 h in air,respectively.The bulk density,thermal expansion coefficient and thermal shock resistance were examined.The results showed that there was a great effect of content of SiC on bulk density,thermal expansion coefficient and thermal shock resistance of mullite-bauxite castable.Under the experimental conditions,the castable performed the best thermal shock resistance when w(SiC)=5%-10%. 相似文献
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350.
The 2010 Yushu earthquake triggered landslide hazard mapping using GIS and weight of evidence modeling 总被引:11,自引:3,他引:8
Chong Xu Xiwei Xu Yuan Hsi Lee Xibin Tan Guihua Yu Fuchu Dai 《Environmental Earth Sciences》2012,66(6):1603-1616
The Yushu County, Qinghai Province, China, April 14, 2010, earthquake triggered thousands of landslides in a zone between
96°20′32.9″E and 97°10′8.9″E, and 32°52′6.7″N and 33°19′47.9″N. This study examines the use of geographic information system
(GIS) technology and Bayesian statistics in creating a suitable landslide hazard-zone map of good predictive power. A total
of 2,036 landslides were interpreted from high-resolution aerial photographs and multi-source satellite images pre- and post-earthquake,
and verified by selected field checking before a final landslide-inventory map of the study area could be established using
GIS software. The 2,036 landslides were randomly partitioned into two subsets: a training dataset, which contains 80 % (1,628
landslides), for training the model; and a testing dataset 20 % (408 landslides). Twelve earthquake triggered landslide associated
controlling parameters, such as elevation, slope gradient, slope aspect, slope curvature, topographic position, distance from
main surface ruptures, peak ground acceleration, distance from roads, normalized difference vegetation index, distance from
drainages, lithology, and distance from all faults were obtained from variety of data sources. Landslide hazard indices were
calculated using the weight of evidence model. The landslide hazard map was compared with training data and testing data to
obtain the success rate and predictive rate of the model, respectively. The validation results showed satisfactory agreement
between the hazard map and the existing landslide distribution data. The success rate is 80.607 %, and the predictive rate
is 78.855 %. The resulting landslide hazard map showed five classes of landslide hazard, i.e., very high, high, moderate,
low and very low. The landslide hazard evaluation map should be useful for environmental recovery planning and reconstruction
work. 相似文献