排序方式: 共有27条查询结果,搜索用时 15 毫秒
1.
2.
Hu Sheng Qiu Haijun Wang Ninglian Wang Xingang Ma Shuyue Yang Dongdong Wei Na Liu Zijing Shen Yongdong Cao Mingming Song Zhaopeng 《Landslides》2022,19(6):1265-1295
Landslides - According to local villagers, the main Beiguo landslide on the Heyang Loess Tableland in China occurred several decades ago (the specific time is unknown). After the initial occurrence... 相似文献
3.
大洼地区毗邻大型生油洼陷—清水洼陷,多级断裂及多期不整合面构成复合油气输导体系,成藏条件优越。但本区火山岩储层岩性岩相复杂、喷发环境多变。为进一步明确储层发育特征及油气成藏主控因素,本次研究利用15 口井107.73 m的岩心、270块薄片及测井资料综合分析,认为大洼地区Mz-Ⅰ段形成于水下喷发环境,发育溢流相玻质碎屑岩亚相玄武质火山角砾岩及溢流相熔岩亚相玄武岩;Mz-Ⅱ段形成于水上喷发环境,发育爆发相凝灰亚相流纹质凝灰岩及溢流相熔岩亚相安山岩。其中玄武质火山角砾岩储集性能最好,平均孔隙度19.3%,平均渗透率6.71×10~(-3) μm~2,玄武岩物性最差,平均孔隙度9.2%,平均渗透率0.23×10~(-3) μm~2。根据录测井及地震资料分析,认识到大洼地区中生界火山岩具有良好源储配置关系且发育多期次断裂及不整合面组成的复合油气输导体系。结合试油试采资料进一步确定油气藏的分布,明确成藏主控因素,建立油气成藏模式。研究表明,储层品质受控于岩性岩相、火山喷发环境及构造活动,油气成藏主要受控于源储配置关系及输导体系,油藏类型为构造-岩性复合型油藏,西侧近油源且近台安—大洼断层的有利岩性岩相带为有利勘探目标区。 相似文献
4.
地图数字注记识别的神经网络方法 总被引:1,自引:0,他引:1
讨论了基于径向基函数网络(RBFN)的地图数字注记识别问题。在分析了网络结构和训练算法的基础上,用地回扫描数据进行了识别实验。结果表明,本文提出的方法用于地图数字注记识别是非常有效的。 相似文献
5.
6.
固体酸是70年代末发展起来的一类新型的催化材料,对有机反应具有较强的催化活性,且副反应少,产物易分离,污染少[1]。粘土固体酸是以蒙脱石类粘土为基质材料,通过采用不同的物理或化学方法在不同的条件下调控层间域而制备的,其催化活性和选择性与其表面酸的类型、浓度及强度等有关[2],为此我们采用离子交换法,以不同类型的阳离子为取代剂,在不同条件下取代交换进入蒙脱石层间,研究制备方法及条件对表面酸性的影响,并考察了催化性能。1 实验部分1-1 原料与试剂钠基膨润土(浙江临安产,主要成分为蒙脱石,用沉降法提… 相似文献
7.
8.
社区尺度下南京鼓楼区养老设施综合评价研究 总被引:1,自引:0,他引:1
针对南京市鼓楼区提出的打造"15 min养老圈"规划,该文选取养老助餐设施为研究对象,基于百度交通距离,结合社区精细尺度,从养老助餐设施数量、服务规模、空间可达性等多维度构建养老助餐设施综合评价模型,测度鼓楼区各社区养老助餐设施建设成果.结果表明:①鼓楼区现有养老助餐设施已覆盖95.5%的老龄人口,基本实现"15 min养老圈"规划,并揭示了未来养老助餐设施重点布局区域;②高斯两步移动搜索法有效地测度了鼓楼区养老助餐设施的空间可达性,鼓楼区约有91个社区的可达性属于中等及以上水平,占比75.8%;③鼓楼区养老助餐设施综合评价达到中等及以上水平的社区占比93.3%,同时也存在养老供需不匹配的问题. 相似文献
9.
Haitao Zhang Jinfeng Bi Gaofeng He Zijing Guo 《Marine Georesources & Geotechnology》2013,31(4):467-476
ABSTRACTThe purpose of this paper is to analyze the stability of submarine slope during the natural gas hydrate dissociation. A model is deduced to calculate the excess pore fluid pressure. In addition, a new method is proposed to define and calculate the factor of safety (FoS) of the submarine slope. Case study is also performed, results of which show that dissociation of hydrates would decrease the stability of submarine slope. If the cohesion of the hydrate-bearing sediments is small, the submarine slope would become unstable because of the shear failure. If the cohesion of the hydrate-bearing sediments is large enough, the tensile failure would happen in the hydrate-bearing sediments and the excess pore pressure may explode the submarine slope. Under the drained condition, the submarine slope may remain stable because the buildup of excess pore fluid pressure could not take place. Moreover, FoS would be underestimated by the assumption that natural gas hydrates dissociate in the horizontally confined space, but would be overestimated by only taking into account of the base of the natural gas hydrate-bearing sediments. The compressibility factor of natural gas should also be considered because treating natural gas as ideal gas would underestimate the stability of submarine slope. 相似文献
10.