一株海藻多糖降解菌的分离鉴定及产酶条件优化     

朱大玲  唐啸龙  张宝玉  杨振芳  王乐普  秦乐宁  张蕾 《海洋科学》2017,41(8):99-107

从大型褐藻藻体分离获得一株具有高效降解琼胶和褐藻胶能力的革兰氏阴性菌菌株ST-6。16S rDNA序列分析结果表明,该菌株与海绵假单胞菌的相似度达到99%,NJ法构建系统进化树也与海绵假单胞菌归为一类,鉴定为海绵假单胞菌Pseudomonas pachastrellae ST-6。在2216E培养基、30℃培养条件下,海绵假单胞菌ST-6的生长曲线表明,接种10~48 h为菌株的指数生长期,48~72 h为生长稳定期。产酶结果表明,菌株ST-6在指数生长期时菌液的胞外琼胶酶相对酶活力较高,在接种48 h时,菌液的琼胶酶相对酶活力最高为249.15 U/m L。此外,发现菌株ST-6的琼胶酶和褐藻胶酶的分泌类型分别为非诱导型和诱导型。采用单因素分析法对其生长和产酶条件进行分析,结果表明,海绵假单胞菌ST-6最适生长条件为:温度25~35℃,33值5~9;最适产琼胶酶条件为:温度30℃,33值为7,琼胶浓度0.3%。最适产褐藻胶酶条件为:温度35℃,33值为9。在温度30℃、339和褐藻酸钠浓度0.15%的培养条件下,海绵假单胞菌ST-6获得最高胞外褐藻胶酶相对酶活力为135.54 U/m L。  相似文献   

欧亚大陆冬季温度对北极海冰减少的敏感性及非线性响应研究   总被引：2，自引：1，他引：1  

隋翠娟  张占海  于乐江  李熠  宋米荣 《海洋学报(英文版)》2017,36(8):52-58

The recent decline in the Arctic sea ice has coincided with more cold winters in Eurasia.It has been hypothesized that the Arctic sea ice loss is causing more mid-latitude cold extremes and cold winters,yet there is lack of consensus in modeling studies on the impact of Arctic sea ice loss.Here we conducted modeling experiments with Community Atmosphere Model Version 5(CAM5) to investigate the sensitivity and linearity of Eurasian winter temperature response to the Atlantic sector and Pacific sector of the Arctic sea ice loss.Our experiments indicate that the Arctic sea ice reduction can significantly affect the atmospheric circulation by strengthening the Siberian High,exciting the stationary Rossby wave train,and weakening the polar jet stream,which in turn induce the cooling in Eurasia.The temperature decreases by more than 1°C in response to the ice loss in the Atlantic sector and the cooling is less and more shifts southward in response to the ice loss in the Pacific sector.More interestingly,sea ice loss in the Atlantic and Pacific sectors together barely induces cold temperatures in Eurasia,suggesting the nonlinearity of the atmospheric response to the Arctic sea ice loss.  相似文献   

21世纪北半球中高纬度净初级生产力(NPP)变化及其与气候因子之间的关系   总被引：1，自引：1，他引：0  

施红霞  王澄海 《冰川冻土》2015,37(2):327-335

基于CMIP5模式模拟的净初级生产力(NPP), 对21世纪初期(2016-2035年), 中期(2046-2065年)和末期(2080-2099年)三种排放情景下(RCP2.6、RCP4.5、RCP8.5)北半球中高纬度陆地NPP的时空变化进行了预估, 并结合气候因子分析了NPP的变化和气温、降水、辐射之间的关系. 结果表明: 相对于1986-2005年, 21世纪北半球中高纬度陆地NPP呈增加趋势, RCP8.5情景下NPP的增加比RCP2.6和RCP4.5情景下更为明显; 在季节变化上, 北半球中高纬度NPP也以增加为主, 且NPP在夏季, 尤其是6月增加最显著. NPP对气候变化的响应存在明显的区域差异性, 在中低排放情景下(RCP2.6、RCP4.5), 相对于1986-2005年, 21世纪北半球中高纬度地区温度显著影响的范围在逐渐缩小, 而辐射和降水显著影响的范围在扩大. 在高排放情景下(RCP8.5), 21世纪北半球中高纬度地区NPP的变化主要与温度有关.  相似文献   

地球系统模式FIO-ESM对北极海冰的模拟和预估   总被引：5，自引：3，他引：2  

舒启  乔方利  宋振亚 《海洋学报》2013,35(5):37-45

评估了地球系统模式FIO-ESM(First Institute of Oceanography-Earth System Model)基于CMIP5(Coupled Model Intercomparison Project Phase 5)的历史实验对北极海冰的模拟能力,分析了该模式基于CMIP5未来情景实验在不同典型浓度路径(RCPs,Representative Concentration Pathways)下对北极海冰的预估情况。通过与卫星观测的海冰覆盖范围资料相比,该模式能够很好地模拟出多年平均海冰覆盖范围的季节变化特征,模拟的气候态月平均海冰覆盖范围均在卫星观测值±15%范围以内。FIO-ESM能够较好地模拟1979-2005年期间北极海冰的衰减趋势,模拟衰减速度为每年减少2.24×104 km2,但仍小于观测衰减速度(每年减少4.72×104 km2)。特别值得注意的是:不同于其他模式所预估的海冰一直衰减,FIO-ESM对21世纪北极海冰预估在不同情景下呈现不同的变化趋势,在RCP2.6和RCP4.5情景下,北极海冰总体呈增加趋势,在RCP6情景下,北极海冰基本维持不变,而在RCP8.5情景下,北极海冰呈现继续衰减趋势。  相似文献   

基于HTML 5的HeatMap Web专题地图研究     

张俊涛  王蜜蜂  李晓明  常晓滢 《东北测绘》2012,(5):214-215,218

简要介绍了HTML 5技术和HeatMap的基本概念,从HTML 5技术出发,设计实现了一套基于HTML 5技术的HeatMap Web专题地图制作的API,这套API可与OpenStreet Map,Google Map,Baidu Map等主流Web地图平台方便地集成使用。最后进一步探讨了将HTML 5引入WebGIS地图系统的优势所在。  相似文献   

FG5／240绝对重力仪成套设备的检定测量分析     

纪立东  张宏伟  王应建  肖凡  李建国 《北京测绘》2012,(3):14-18

详细介绍了FG5/240绝对重力仪的技术特点、测量原理和白家疃的试验观测,并就相配套的用于测量梯度的2台CG5相对重力仪(442、444)的检定项目和结果进行说明和分析,结果表明:2台CG5相对重力仪完全满足规范要求,FG5/240绝对重力仪的试验测量结果的标准偏差优于±2.0×10-8 ms-2,能够用于陆态网络工程任务中部分基准站的绝对重力测量。  相似文献   

基于客户端插件体系结构的RIA WebGIS框架原理和实现     

张丰  熊小青 《东北测绘》2012,(2):145-147

WebGIS与RIA（Rich Internet Applications）技术的结合,可以提高系统的交互性和用户体验。但目前,缺乏一个RIAWebGIS下的简洁高效的应用框架体系结构,以适应GIS系统与越来越复杂的业务系统的集成。在研究WebGIS的技术特点与分析现有RIAWebGIS框架基础上,提出一种面向前端插件体系结构的RIAWebGIS开发框架,并对该框架的模型层次和关键技术进行了剖析,最后将此框架应用于实际应用系统,验证了该框架的高效性和可扩展性。  相似文献   

两颗GPS现代化卫星L5载波信号的比较     

吴继忠  管栋良 《测绘科学》2012,37(3):33-34,10

本文分析了GPS现代化信号L5载波的结构及相对于非现代化信号的改进,比较了GPS L5载波和WAAS L5载波的区别;比较了2颗现代化卫星SVN49和SVN62播发的L5载波的信号结构及信噪比,结果表明:SVN49播发的L5载波演示信号的抗干扰能力较差,而SVN62播发的L5载波具有更强的抗干扰能力,满足设计规范要求。  相似文献   

基于HTML5、Ajax和We bService的WebGIS研究   总被引：1，自引：0，他引：1  

徐卓揆 《测绘科学》2012,(1):145-147

为改变WebGIS中各种浏览器缺乏支持矢量数据的标准方法、数据互操作能力有限和空间分析功能较弱的现状,基于新一代HTML5标准、Ajax和Web Service技术,本文提出了开放式WebGIS模型,并开发了实验平台。该平台支持数据共享的Web Services和OGC新规范Web Processing Service,改善了现有WebGIS缺陷,提高了WebGIS的互操作及空间分析能力。  相似文献   

Geology, tectonics, and the 2002-2003 eruption of the Semeru volcano, Indonesia: Interpreted from high-spatial resolution satellite imagery     

Akhmad SolikhinJean-Claude Thouret  Avijit GuptaAndy J.L. Harris  Soo Chin Liew 《Geomorphology》2012,138(1):364-379

The paper illustrates the application of high-spatial resolution satellite images in interpreting volcanic structures and eruption impacts in the Tengger-Semeru massif in east Java, Indonesia. We use high-spatial resolution images (IKONOS and SPOT 5) and aerial photos in order to analyze the structures of Semeru volcano and map the deposits. Geological and tectonic mapping is based on two DEMs and on the interpretation of aerial photos and four SPOT and IKONOS optical satellite images acquired between 1996 and 2002. We also compared two thermal Surface Kinetic Temperature ASTER images before and after the 2002-2003 eruption in order to delineate and evaluate the impacts of the pyroclastic density currents. Semeru's principal structural features are probably due to the tectonic setting of the volcano. A structural map of the Tengger-Semeru massif shows four groups of faults orientated N40, N160, N75, and N105 to N140. Conspicuous structures, such as the SE-trending horseshoe-shaped scar on Semeru's summit cone, coincide with the N160-trending faults. The direction of minor scars on the east flank parallels the first and second groups of faults. The Semeru composite cone hosts the currently active Jonggring-Seloko vent. This is located on, and buttressed against, the Mahameru edifice at the head of a large scar that may reflect a failure plane at shallow depth. Dipping 35° towards the SE, this failure plane may correspond to a weak basal layer of weathered volcaniclastic rocks of Tertiary age. We suggest that the deformation pattern of Semeru and its large scar may be induced by flank spreading over the weak basal layer of the volcano. It is therefore necessary to consider the potential for flank and summit collapse in the future. The last major eruption took place in December 2002-January 2003, and involved emplacement of block-and-ash flows. We have used the 2003 ASTER Surface Kinetic Temperature image to map the 2002-2003 pyroclastic density current deposits. We have also compared two 10 m-pixel images acquired before and after the event to describe the extent and impact of an estimated volume of 5.45 × 10⁶ m³ of block-and-ash flow deposits. An ash-rich pyroclastic surge escaped from one of the valley-confined block-and ash flows at 5 to 8 km distance from the crater and swept across the forest and tilled land on the SW side of the Bang River Valley. Downvalley, the temperature of the pyroclastic surge decreased and a mud-rich deposit coated the banks of the Bang River Valley. Thus, hazard mitigation at Semeru should combine: (1) continuous monitoring of the eruptive activity through an early-warning system, and (2) continuous remote sensing of the morphological changes in the drainage system due to the impact of frequent pyroclastic density currents and lahars.  相似文献