综合护理对心力衰竭患者心功能及血液流变学的影响

目的：观察综合护理对心力衰竭患者心功能及血液流变学指标的影响。方法：将76例心力衰竭患者随机分为观察组及对照组,每组各38例。2组均给予利尿、强心、扩血管等药物治疗,对照组采用西医常规护理,观察组在对照组基础上应用中医综合护理干预,包括穴位贴敷、情志护理、饮食辨证护理。比较2组干预前后心功能指标［B型利钠肽（BNP）、左室收缩末期容积（LVESV）、左室射血分数（LVEF）］及血液流变学指标［全血低切黏度（LBV）、全血高切黏度（HBV）、血浆黏度（PV）］的变化。结果：干预后观察组BNP、LBV、HBV及PV低于对照组,LVESV及LVEF高于对照组,差异均具有统计学意义（P<0.01）。结论：综合护理能够有效增强患者心功能,改善其血液循环供应状况,值得推广。     

屏南旅游业开发探讨

文化是旅游业发展的灵魂.屏南有着丰富的旅游资源和深厚的文化积淀,然而由于旅游业起步晚,受交通网络、资金投入等方面的制约,旅游业发展滞后.文章从旅游文化角度分析了屏南旅游开发的有利条件及旅游业发展现状,提出了塑造旅游形象、挖掘旅游文化内涵、发展特色旅游的几点建议,以便使屏南尽快发展成为闽东地区旅游的新热点.     

旅游资源分布图分类符号系统的创新设计

旅游资源分类符号是旅游资源分布图的重要元素.当前各县市旅游资源调查中,常见的旅游资源分类符号系统存在缺憾.本文通过对照地图符号设计的原则,在分析其优点和不足的基础上,按照地图符号的设计要求并结合当前常用计算机软件平台的应用提出创新设计方案.     

中日美韩"地震减灾国际研讨会"简介

应韩国气象厅气象研究所的邀请,中国地震局地球物理研究所的郑需要研究员和郑秀芬博士于2005年12月18日至23日期间,赴韩国济州岛参加了由韩国气象厅气象研究所主办的第五届中、日、美、韩“地震减灾国际研讨会”(THE 5 TH INTERNATIONALW ORK-SHOP ON THE FUNDAMENTAL RESEARCH     

巴西桑托斯盆地构造演化与油气勘探前景

位于巴西东岸的南大西洋被动大陆边缘盆地——桑托斯盆地是我国海外油气勘探的重要区块.通过地震资料分析,结合叠合盆地演化原理以及南大西洋演化历程,将桑托斯盆地的构造演化阶段划分为前裂谷期、裂谷期、过渡期、漂移期4个阶段,对应克拉通、裂谷、坳陷、被动大陆边缘4类原型盆地.原型盆地的时空匹配关系为桑托斯盆地形成超大型的含油气系...     

相对差分GPS精度分析

近年来,全球定位系统(GPS)以其精度高、速度快、经济方便等优点,在布设各种形式的控制网、变形监测及精密工程测量等诸多方面都得到迅速广泛的应用。但由于美国的SA和AS政策,使其精度下降,因此各国都在研究如何提高其精度,本文就此问题给出一些观点。     

论"工程测量"课程的教学改革

从教学内容、教学方法、教学手段、实践教学和教师应不断拓宽知识面等方面对当前“工程测量”教学改革作了初步的探讨。     

基于Citespace的无人机遥感研究知识图谱分析

为清晰了解国内外无人机遥感应用研究现状及发展态势,以Web of Science核心期刊为数据源,运用文献计量方法与Citespace可视化分析工具对无人机遥感研究的相关文献进行统计分析。结果表明：无人机遥感相关研究文献呈快速增长趋势,与遥感科学、工程学和影像科学摄影技术三门学科联系最为密切;美国、中国、西班牙等国家发文量较多,具备较强研究力量;中国科学院发文量最多,而西班牙最高科研理事会h指数最高,均有较大影响力;澳大利亚学者Lucieer A和西班牙学者Zarco-Tejada PJ的h指数较高,为该领域的代表性学者;无人机遥感技术包含多个研究方向,其中研究热点包括无人机遥感在农业科学和生态学等领域的应用研究、遥感影像分类方法的研究、摄影技术和计算机视觉技术的研究等三方面。     

印尼贯穿流源区马鲁古海与哈马黑拉海水团来源的季节和年际变化

So far, large uncertainties of the Indonesian throughflow(ITF) reside in the eastern Indonesian seas, such as the Maluku Sea and the Halmahera Sea. In this study, the water sources of the Maluku Sea and the Halmahera Sea are diagnosed at seasonal and interannual timescales and at different vertical layers, using the state-of-the-art simulations of the Ocean General Circulation Model(OGCM) for Earth Simulator(OFES). Asian monsoon leaves clear seasonal footprints on the eastern Indonesian seas. Consequently, the subsurface waters(around 24.5σ_θ and at ～150 m) in both the Maluku Sea and the Halmahera Sea stem from the South Pacific(SP) during winter monsoon, but during summer monsoon the Maluku Sea is from the North Pacific(NP), and the Halmahera Sea is a mixture of waters originating from the NP and the SP. The monsoon impact decreases with depth, so that in the Maluku Sea, the intermediate water(around 26.8σ_θ and at ～480 m) is always from the northern Banda Sea and the Halmahera Sea water is mainly from the SP in winter and the Banda Sea in summer. The deep waters(around27.2σ_θ and at ～1 040 m) in both seas are from the SP, with weak seasonal variability. At the interannual timescale,the subsurface water in the Maluku Sea originates from the NP/SP during El Ni?o/La Ni?a, while the subsurface water in the Halmahera Sea always originates from the SP. Similar to the seasonal variability, the intermediate water in Maluku Sea mainly comes from the Banda Sea and the Halmahera Sea always originates from the SP. The deep waters in both seas are from the SP. Our findings are helpful for drawing a comprehensive picture of the water properties in the Indonesian seas and will contribute to a better understanding of the ocean-atmosphere interaction over the maritime continent.     

2015年台风“彩虹”过境后下山冷急流引起的南海北部海域异常海面降温

This study deals with a unusual cooling event after Typhoon Mujigea passed over the northern South China Sea(SCS) in October 2015. We analyze the satellite sea surface temperature(SST) time series from October 3 to 18,2015 and find that the cooling process in the coastal ocean had two different stages. The first stage occurred immediately after typhoon passage on October 3, and reached a maximum SST drop of –2℃ on October 7 as the usual cold wake after typhoon. The second stage or the unusual extended cooling event occurred after 7d of the typhoon passage, and lasted for 5d from October 10 to 15. The maximum SST cooling was –4℃ and occurred after 12d of typhoon passage. The mechanism analysis results indicate that after landing and moving northwestward to the Yunnan-Guizhou Plateau(YGP), Typhoon Mujigea(2015) met the westerly wind front on October 5. The lowpressure and positive-vorticity disturbances to the front triggered meridional air flow and low-pressure trough,thus induced a katabatic cold jet downward from the Qinghai-Tibet Plateau(QTP) passing through the YGP to the northwestern SCS. The second cooling reached the maximum SST drop 4d later after the maximum air temperature drop of –9℃ on October 11. The simultaneous air temperature and SST observations at three coastal stations reveal that it is this katabatic cold jet intrusion to lead the unusual SST cooling event.