青川县庙底下滑坡稳定性分析及整治

基于现场调查、测绘、勘探以及室内试验成果,阐述了庙底下滑坡的变形特征,分析了滑坡产生的成因机制,对滑坡不同工况下的稳定性进行了分析计算,结果表明滑坡稳定性较好,同时介绍了滑坡整治的具体情况     

MGIS地图符号库的面向对象设计与改进

结合中国矿业大学北京校区矿业地理信息系统（Ｍｉｎｉｎｇ ＧｅｏｇｒａｐｈｉｃａｌＩｎｆｏｒｍａｔｉｏｎ Ｓｙｓｔｅｍ,ＭＧＩＳ）开发研制的实际,论述了基于ＭＧＩ 的地图符号库的特点及其面向对象的设计与实现技术以及用Ｏ）ＤＢＶ外接数据库管理符号属性数据的方法。结合研究开发实际重点论述设计中在符号设计方法、存储方式及符号库结构方面所做的改进。     

基于地区差异性修正因素的川滇地区地震人员伤亡动态评估方法研究

基于建筑物破坏的地震人员伤亡快速评估方法是一种静态评估方法,具有较大的局限性,因此迫切需要建立地震人员伤亡动态评估方法以提高评估结果的有效性.以川滇地区为例,基于历史震例人员伤亡资料和相关科研成果,利用统计分析、案例对比法以及大数据分析等方法,从影响人员易损性因素的地区差异性角度研究地震人员伤亡动态修正方法.为此提出了...     

航海通告自动获取系统的设计与实现

目前,从互联网获取航海通告数据是提高海图产品现势性、保障舰船航行安全的主要途径之一。基于对国内外网站特点、网页结构及网络爬虫技术、数据库技术的研究,提出了自动获取航海通告网页数据的总体方案;通过研发应用系统,实现了通告爬取、数据整理、数据库管理等主要功能。测试结果表明:较之传统工作方式,利用该系统获取的航海通告数据具有准确性、完整性、实时性和高效性,将为海图一体化生产体系提供更高质量的基础数据源支持。     

内蒙古东部地区波速比变化特征研究

以内蒙古地震监测台网的监测能力和资料完整性为基础,结合内蒙古东部地区（41°～51°N,114.5°～124.6°E）实际地震地质构造特点,选取了内蒙古东部地区（41°～51°N,114.5 ° ～ 124.6°E） 2008-2012年的ML≥2.0地震作为研究对象,利用多台和达法计算得出了该区域的平均波速比及其变化特征.通过分析该地区两次中等地震震例,发现内蒙古东部地区在中等地震前后波速比时间变化存在显著异常,符合“下降—低值—恢复—发震”的规律,且存在着震后异常期的变化;在对该区域内波速比绘制空间等值线后,发现该区域内波速比高值主要是沿着大兴安岭分布,其空间分布基本呈现东低西高、北低南高的态势.综合研究了区域地震地质背景和最近一两年研究区域内波速比变化,得出内蒙古东部地区地下介质的应力变化比较显著,具备发生中强地震的地质构造条件.     

应用REE评价地球化学异常的可行性

随着地质找矿工作的深入和找矿难度的加大,对地球化学异常评价提出了更高要求,研究提取地球化学勘查新指标对提高找矿成功率意义重大.通过对乌努格吐山斑岩型Cu-Mo矿床、罕达盖矽卡岩型Fe-Cu矿化以及垦山多元素组合异常REE指标的研究,发现矿致异常与未见矿异常、斑岩型矿化与矽卡岩型矿化REE各项指标存在明显差异,矿化体赋存部位与REE指标空间位置吻合,这一发现使得应用REE评价地球化学异常成为可能.     

Relative importance of wind and buoyancy forcing for interdecadal regime shifts in the Pacific Ocean

Interdecadal variations in the Northern Hemisphere and the North Pacific have been documented in many studies[1 4]. The connection between the subtropical North Pacific and the tropics is regarded as the most important process triggering and maintaining t…     

Comparison of CO2 Effluxes and Their Driving Factors Between Two Temperate Steppes in Inner Mongolia, China

Soil respiration is a key component of the global terrestrial ecosystem carbon cycle. The static opaque chamber method was used to measure the CO2 effluxes from soil of a semiarid Aneurolepidium chinense steppe and a Stipa krylovii steppe in the Xilin River Basin of Inner Mongolia, China from March 2002 to December 2004. The results indicated that the soil respiration rates of the semiarid Aneurolepidium chinense steppe and the Stipa krylovii steppe were both relatively high from mid-May to mid-September of each year and remained low during the rest of the year. The minimum value of soil respiration occurred in December or January and negative effluxes of CO2 appeared for several days during the non-growing season of individual years at the two sampling sites. A high annual variation was found in the two steppes with the coefficients of variance (CV) being over 94%, even high to 131%. The annual sums of soil CO2 efflux of the Aneurolepidium chinense steppe varied between 356.4 gC m?2 yr?1 and 408.8 gC m?2 yr?1, while those of the Stipa krylovii steppe in the three years were in the range of 110.6 gC m?2 yr?1 to 148.6 gC m?2 yr?1. The mean respiration rates of the Aneurolepidium chinense steppe were significantly higher than those of the Stipa krylovii steppe in different statistical periods with the exception of the non-growing season. About 59.9% and 80.6% of the soil respiration variations in both steppes for the whole sampling period were caused by the changes of temperature and soil water content. In the Aneurolepidium chinense steppe, the soil respiration rate has significant or extremely significant positive correlation (r = 0.58 ? 0.85, p < 0.05 or p < 0.01) with air temperature and ground temperature of the topsoil except in 2002; the unique contributions of temperature change to the soil respiration variation of the three years were 53.3%, 81.0% and 58.6%, respectively. But, for the Stipa krylovii steppe in the same time interval, the soil water content (especially that of the 10–20 cm layer) has a greater effect on the change of soil respiration, and the unique contributions of the change of the 10–20 cm soil water content to the variations of soil respiration in 2002 and 2003 were 60.0% and 54.3%, respectively. In 2004, in spite of the higher contribution of temperature than soil water content, the contribution of ground temperature at a depth of 10 cm was only 46.2%, much weaker than that of any single year in the Aneurolepidium chinense steppe.     

极区电离层F2层峰值电子浓度对太阳活动依赖性的共轭研究

本文利用南极中山站(ZHS),以及北极与其地理共轭的Tromso站(TRO)、地磁共轭的Longyearbyen站(LYB)各自约一个太阳活动周的观测数据,对比分析了极区电离层F₂层峰值电子浓度(N_mF₂)对太阳活动的依赖性.结果表明,三个台站N_mF₂月中值随修正太阳10.7 cm通量指数F_10.7P(简称P)增大在总体上呈线性增长,这说明在这三个台站,太阳辐射仍是其F₂层主要电离源.其中TRO站N_mF₂与P线性关系最好,ZHS站的次之,LYB站的最差.在日变化中,TRO站N_mF₂对太阳活动响应最为敏感的时刻出现在地方时中午附近,LYB站出现在磁中午,ZHS站则出现在地方时中午和磁地方时中午之间.这主要是由地理/地磁纬度差异引起的不同强度的光致电离与极区等离子体对流共同作用的结果.在年变化中,TRO站N_mF₂随太阳活动变化上升最快的季节出现在冬季,夏季上升最慢.在ZHS站与LYB站,N_mF₂对太阳活动变化的响应都在两分季最为敏感.这种季节上的差异则是由于三个台站光致电离与中性大气成分R[O/N₂]的不同所致.     

基于能谱纯化结合迭代重建算法在继发性肺结核患者低剂量CT检查中的应用

目的:探讨基于能谱纯化结合迭代重建算法在继发性肺结核患者低剂量CT检查中的应用。方法:选取2019年4月至6月武汉市肺科医院确诊的70例继发性肺结核患者作为研究对象。初检采用常规剂量组:管电压110 kV,参考管电流52 mAs,滤波反投影（FBP）重建图像;复检采用低剂量组（能谱纯化）:管电压Sn 110 kV,参考管电流73 mAs,正弦图迭代重建（SAFIRE）。比较两组图像主观评分、升主动脉CT值、图像噪声、SNR及辐射剂量差异。结果:两组图像主观评分相比无差异,满足临床诊断要求。两组升主动脉CT值无差异;低剂量组图像SNR低于常规剂量组。低剂量组ED（0.36±0.15）mSv与常规剂量组（2.35±0.73）mSv相比降低约84.7％。结论:能谱纯化结合迭代重建算法在继发性肺结核患者检查中能够显著降低患者所受辐射剂量,同时图像质量也能满足临床诊断要求。