A Comparative Study on the Microbiological Characteristics of Soils Under Different Land—Use Conditions from Karst Areas of Southwest China

Microbiological and physical-chemical characteristics of subtropical forest,grassland and cropfield soils from the karst areas of Southwest China were investigated.The study revealed that the conversion of natural forest to other forms of land would lead to a reduction in soil organic C(26.2%-35.3%),total N(37.2%-55.8%),totalP(32.9%-43.6%),microbial biomass C(35.4%-49.1%),N(37.2%-55.8),and P(25.8%-41.9%).Comparative analysis of microbial activity in terms of basal soil respiration showed maximum activity in forest soil and minimum in cropfield soil.Analysis of microbial metabolic respiratory activity indicated a relatively greater respiratory loss of CO2-C per unit microbial biomass in cropfield and grassland than in forest soil.Considering the importance of microbial components in soil,it is concluded that land use in different ways will lead to the reduction of biological stabilty of soil.     

A Physical Method of Analyzing theMechanism of Continental StrongShocks from Crustal Movement

In order to analyze the mechanism of continental strong shocks from the angle of crustal movement using the data of repeated geodetic survey, this paper has proposed a physical method; it analyzes the mechanism of density change due to the occurrence of strong shocks by use of the physical quantity that reflects the time change of crustal density. ( 1 ) The general theory of the time change of density in the earth‘ s interior and the theory of the time change of single layer density have been introduced, and an algorithm of stepwise iteration has been proposed; (2) The effect of the change of single layer density caused by fault dislocation has been analyzed in brief; (3) The characteristics of the time change of crustal density in the south of the seismogenic region before the 1996 Lijiang earthquake with ML = 7.0 have been studied; (4) The precursor model or causal mechanism of strong shocks possibly existing in the time change of crustal density has been investigated preliminarily.     

松辽盆地庆安地区白垩纪沉积体系和目的层地球化学特征及与铀矿化的关系

本在分析松辽盆地所处大地构造背景和构造演化特征的前提下，着重研究了松辽盆地庆安地区白垩系的沉积特点、沉积体系特点和泉头组目的层地球化学特征，初步论述该地区砂岩型铀矿成矿特点及与白垩纪地层的关系，并提出了该地区可能产出的铀矿床类型。     

对盐津县地质灾害防治的思考

盐津县境内的地质灾害类型主要为滑坡、崩塌、泥石流、危岩、地面裂缝、潜在不稳定斜坡等多种地质灾害并存,其形成原因主要与大气降水强度、河水淹没和侵蚀作用、地形地貌、岩土类型、地质结构、地震及人类不合理工程活动等相关。针对该县目前地质灾害形势,提出了“以防为主、防治结合、全面规划、综合治理”的防治对策。     

基于Android的自驾游天气手机应用的设计与实现

为了让用户快速获取目的地的天气实况与预报及景点周边的吃住游购等信息,合理规划旅游线路,使用Java开发语言包JDK 1.7和MyEclipse平台开发工具设计并实现了一款基于Android平台的手机APP。整个系统由手机客户端、后台管理系统、Web服务器、API接口系统组成。本文重点介绍了手机客户端主要功能模块和API接口系统的设计与实现。客户端聚合了气象信息、地理信息和景点信息等,并首次将IDV制作的图形化产品应用于APP,为旅游用户及时获取目的地天气预报、线路天气和旅游景点等综合服务信息提供便利,提升了移动端旅游气象服务能力。开发的API接口系统,所整合的气象部门服务产品资源,不但服务于手机App,还可应用于第三方网站进行气象服务产品数据查询,最大限度地实现了资源共享。     

中心静脉导管相关性血流感染的临床及病原学的回顾性调查分析

目的 了解重症监护室（ICU）中心静脉导管相关性血流感染（CRBSI）的感染率、危险因素、病原菌种类、耐药性及临床结局,对有效抗感染治疗及预防CRBSI的发生提供指导。方法 回顾性分析2010年4月~2014年4月共483例留置过中心静脉导管（CVC）的患者。计算感染率、感染相关性因素及筛选危险因素分析并应用SPSS20.0统计软件进行多因素Logistic回归分析。结果 共有17例患者发生CRBSI,感染率为3.5%;不同置管者、置管地点、置管部位构成的比较,差异有统计学意义（P<0.05）。经多因素Logistic回归分析,发现影响CRBSI的独立危险因素是抗生素大量使用和导管日,OR值分别为7.898和1.044。革兰阳性菌（gram-positive bacteria,G⁺）占35.3%,革兰阴性菌（gram-negative bacteria,G^-）占47.1%,真菌占17.6%;G⁺菌感染患者,经治疗后病情100% 好转;G^-菌感染患者,87.5% 好转,12.5% 恶化;真菌感染患者,66.7% 好转,33.3% 恶化。结论 CRBSI的发生率随抗生素大量使用以及导管日延长而增加。患者经治疗后,大部分好转,但真菌感染者病死率相对较高,应引起临床关注。     

北祁连山东段活动断裂带的分段性研究

根据北祁连山东段活动断裂带１：５万地质填图资料,系统分析了断裂带的几何学特征,位移分布,滑动速率,古地震及历史地震活动在时空上的非均匀性特征,研究了断裂带的破裂分段性。     

Combined study between the chromospheric flare models and hard X-ray observation

By comparison between SMM HXRBS observation and ground observation of H and Caii K lines for the 2B flare on February 3, 1983, we found that there was a temporal correlation between H intensity and hard X-ray flux at the early stage of the impulsive phase while different peaks in the hard X-ray flux curve represented bursts at different locations. When we combined SMM HXRBS observation with chromospheric flare models, we further found that the temporal coincidence between H intensity and hard X-ray flux could be explained quantitatively by the fact that the H flare was indeed due to the heating by non-thermal electron beams responsible for the emission of hard X-rays. Together with the discussion on coronal density based on chromospheric flare models, it was also shown that the source of electrons seemed to be situated around the top of the flare loop and the column density at the top of the chromosphere in semi-empirical flare models could not be taken as the total material above the top of the chromosphere.     

珠江口台风增水对热带气旋参数改变的反响

通过计算，研究热带风暴中心气压下降示度、最大风速半径、热带气旋登陆地点、热带气旋登陆时的入射角、热带气旋移动速度等参数改变条件下，珠江口５个测站风暴潮的变化。结果表明，各站的反响很不一致，在风暴潮预报中对地形的特点、热带气旋移动速度及热带气旋登陆地点等应给予足够的重视。     

冲绳海槽浮岩岩浆活动模式浅析

本文根据部冲绳海槽的地下结构、地温场特征、以及浮岩中斑晶矿物的结晶温度和榴辉岩的熔融相关系等，综合分析了冲绳海槽酸性浮岩岩浆的活动模式。提出：在冲绳海槽中部和东部地下１５ｋｍ以下的地幔物质部分熔融、产生橄榄拉斑玄武质岩浆，而在海槽中部地壳一结构层中（７－１５ｋｍ）熔融产生少量安山质岩浆。因此，在冲绳海槽地下存在有双层岩浆房结构，并且二者之间中部有岩浆通道。来自地幔的拉斑玄武质岩资源下部地壳中一方面