中国台风强度等级与可能灾害损失标准研究

台风灾害给中国沿海地区造成了严重损失,进行台风风险评估将为台风灾害有效规避提供科学依据,探讨台风强度等级和灾害损失之间的关系是台风风险定量评估的基础。利用1954-2008年间登陆中国东南沿海的174场成灾台风路径数据和对应的灾情记录数据,对台风强度等级和承灾体(农作物、人口、房屋和社会经济)的8项指标的损失数量关系进行分析,并对台风强度等级与各项损失率指标之间的关系进行拟合,得出各项灾损指标的损失率曲线。基于台风强度等级划分标准和损失率曲线,建立了适合于我国的四个强度等级的台风灾害损失标准划分方案:微度、轻度、中度和重度,对应的损失率用承灾体的社会经济指标来表征。研究表明:当台风强度等级达到第4等级时,灾害造成的损失率均有较大幅度的增加。本文构建的台风灾害损失标准可为进一步定量评估承灾体脆弱性及损失风险提供依据和参考。     

Lake Area Changes and the main causes in the hinterland of Badain Jaran Desert during 1973–2010, China

Lake area information in the Badain Jaran Desert in 1973, 1990, 2000, and 2010 was obtained by visual interpretation and water index analysis of remote sensing images, based on the spatial and temporal characteristics of lake area changes during 37 years. Results indicated that the number of lakes declined from 94 to 82 and the total surface area was reduced by 3.69 km² during 1973–2010. The desert lake area reduced by different degrees in different periods, but this occurred most rapidly during 1973–1990. According to the statistics of lake area changes, lake area decreases mainly occurred in the lakes with areas less than 0.2 km², while the areas of lakes greater than 0.9 km² only fluctuated. The changes of lake areas were probably due to changes in the quantity of underground water supplies rather than the effects of local climate change or human factors.     

Tectonic-Thermal Evolution History and Its Controls on Petroleum Geology of Weibei Uplift

<正>1 Introduction The Weibei Uplift is located in the southwest of the North China Plate,where is the stable block(the Ordos Block)in the north and the active belt(the QinlingOrogenic Belt)in the south(Ren et al,2014,2015).And the belt is separated from the Weihe basin.The Weibei uplift has a uniform crystalline basement with the North     

山东福吉山铜矿构造控矿因素分析

福吉山铜矿成矿地质特点不同于山东已有的铜矿类型,属于构造热液成因类型。近SN向的平移断裂同时具有张扭性和压扭性双重力学性质,其中张扭性破碎带造就成矿空间,造成了矿体近等间距雁列式排列。受断裂构造的影响,矿区内节理、裂隙发育,为成矿热液的运移和积聚提供了良好的空间。区内沿裂隙充填形成的石英脉、褐铁矿脉、铜矿脉发育。     

青海省祁连县大拉洞柏杨沟矿区煤岩层对比研究

通过研究太原组的沉积特征及聚煤变化规律,采用了标志层、煤岩层组合特征、层间距、测井曲线形态等方法,对矿区内煤层、岩层进行了综合对比。确定了该区主要煤层的赋存层位、形态、分布及变化特征,对周边地区找煤工作具有一定的指导作用。     

Influence of the Choice of Core-Envelope Transition Point on the Binary Merger of Two Main-sequence Components

We have studied the influence of different choices of core-envelope transition point on the final merger of contact binaries with two main-sequence components. A binary of 1.00 + 0.90M⊙ with an initial orbital period of 0.35d is examined. The mass fraction of the primary mixed with the matter of the secondary, qmix, determined by the chosen core-envelope transition point, ranges from 0.04 to 1.00 in our analysis. If as qmix< 0.8, none of the     

泰安市矿产开发监督管理工作的思考

根据泰安市区域矿产开发特点,及时掌握矿山企业开采情况,通过加强采矿登记现场预审查、开展矿山开采督察和采矿权人矿产资源开发利用年查等措施,强化了矿产资源开发过程中的监督管理,维护了正常开采秩序及采矿权人的合法权益。     

栖霞地区金矿床特征及找矿方向

栖霞地区金矿点繁多,但仅有两处规模近中型的金矿床。根据对马家窑、台前金矿床特征及成矿地质条件的分析,并与招莱地区金矿床进行类比,认为栖霞地区金矿成矿条件与招莱地区基本相似,但由于重熔花岗岩体侵位较深,含矿热液未能运移至浅部,因而热液矿床赋存深度较大,地表及浅部金矿呈现“矿点多,规模小”的分布特点。栖霞地区深部找金潜力很大,重点勘查区应为隐伏的深熔、重熔花岗岩发育区,以及ＮＥ、ＮＮＥ向断裂及其下盘次级断裂所在部位。     

樟子松固沙林带间植被恢复及其对林草界面作用的响应

调查了海拉尔市巴音岱林场不同分布格局、不同带间距的人工樟子松林带内植被恢复过程及物种多样性的差异,分析了林草界面生态学效应,研究了林草界面对带间植被自然恢复的作用。结果表明,宽的带间距带内物种多样性和生物量变化曲线出现了两个高峰,而窄的带间距带内只有一个高峰,说明该地区林带之间距离不应小于12 m;当林带之间距离为16~28 m时草本物种多样性出现最大值。植被恢复效果表现为带间距12 m差于带间距24 m,虽然都差于天然植被,但边际效应大大地加速了群落演替的进程。研究区樟子松林草界面边缘效应影响域为20 m, 其小尺度范围内生境异质性也很明显。行带式造林带间距离不应大于40 m,超出边缘效应影响域不利于带间植被恢复。