ISSR 标记在牙鲆(Paralichthys olivaceus)与石鲽(Kareius bicoloratus)种间杂交一代的分离方式分析

利用ISSR标记对牙鲆♀与石鲽♂单对杂交亲本及其子一代(全同胞家系)的分离方式进行了研究。结果表明,8个ISSR引物共扩增出181个标记,其中116个为多态性,占总数的64.09%;标记在F1代呈三种分离方式:符合孟德尔分离比例、偏离孟德尔分离比例和异常分离。符合孟德尔分离比例的情况包括:不分离(代表了亲本基因型的5种组合:AA×AA、AA×Aa、Aa×AA、AA×aa、aa×AA);1︰1分离(代表了亲本基因型的2种组合:Aa×aa、aa×Aa);3︰1分离(代表了亲本基因型的1种组合:Aa×Aa)。偏分离的标记包括:亲本中呈多态而在子代中偏离1︰1分离的标记和亲本均有而在子代中偏离3︰1分离的标记。异常分离的标记包括:F1代出现双亲均不具备的标记和双亲或单亲有而子代却无的标记。3种分离位点出现的频率和数量分别为:82.87%、150,11.05%、20,6.08%、11;双亲共有标记中85.33%的不发生分离,单亲特有标记中28.57%—35.85%发生正常分离,该研究结果可为进一步利用该群体构建牙鲆和石鲽遗传连锁图谱奠定良好的工作基础并提供一定的理论依据。     

无锡光伏产业链中的全球-本地联系

以无锡市为例,通过实地调研当地光伏产业链中多晶硅生产、电池元件生产、组件制造、相关设备生产、光伏设备运维服务,以及光伏用户等不同环节,从全球生产网络的视角,考察全球-本地联系在当地光伏产业链形成演化和技术发展动态中的具体表现。结论指出：① 无锡光伏产业在短短10 a之内从“两头在外”的发展模式到形成全产业链竞争优势,体现了新兴技术的全球生产网络技术加速更新和产业快速转移的新特点;② 本地相关产业集群通过技术引进、消化和改进为新技术突破规模化瓶颈,获取市场竞争力打下基础,并由此对全球光伏技术发展的路径产生了关键影响;③ 产业进一步发展需要针对能源转型的长期目标,着重探索能源消费侧的技术转型路径。     

空间运输联系的生成与增长规律研究

空间运输联系是指在自然、社会、经济诸要素综合作用下，区域间通过交通运输设施进行旅客和货物的交流。区域差异与互补是空间运输联系产生的直接原因，交通设施是空间运输联系实现的基础。本文以世界不同类型国家和我国近半个世纪的运输活动及其社会经济背景值作为研究对象，采用定量与定性相结合的实证分析方法，经过归纳、演绎和推理，深入研究了运输联系生成的内在机制和增长演变的趋势，得出了旅客生成密度和客运强度随经济增长而增长、货物生成密度和货运强度随经济增长而降低的结论。在评价指标方面，提出了生成密度、运输强度等概念和指标，并对世界主要国家的运输发展进行了对比分析。     

利用外资与发展国际产业联系——山东半岛韩国投资企业典型调查分析

基于对山东半岛韩国投资企业进行典型企业访问调查的数据和认识,力图从企业角度认识我国外资和发展国际产业联系之间的关系,了解和分析韩国投资者的具体投资动机及其对当地投资环境的评价,深入认识我国山东半岛地区和韩国之间资金流动以及经济技术联系的主要机制和动态格局。通过对韩国投资企业产业联系基本特征的解剖分析,论证韩国投资对我国发展国际产业联系,推动我国地方经济参与国际劳动地域分工的作用。从而为进一步加强中     

开源网管系统在地震监测网络中的应用

使用Nagios、Cacti、NagVis等开源系统在天津市地震局行业网络中搭建开发了一套运行监控系统,可实现对区域内各类网络设备、仪器与服务的集中监控,同时建立于系统的故障报警与值班系统的联动机制,提高了网络环境中各专业台网整体运行监控与故障响应能力.     

东北亚运输合作: 中国与朝鲜半岛陆路交通联系与运输组织战略

本文从促进东北亚地区经济合作健康发展角度出发,以分析预测中国与朝鲜半岛间潜在的运输需求为基础,阐述了构建中国与朝鲜半岛陆路交通联系对完善东北亚和黄海经济区交通运输体系的战略意义;构想了组织陆路交通联系的地域模式,并简要评价了不同模式的可行性和经济效益潜力。提出了以“轴－辐”模式组织中国与朝鲜半岛的陆路交通联系是最合理的观点。     

The influence of pre-existing structure on the growth of syn-sedimentary normal faults in a deltaic setting,Niger Delta

Three dimensional seismic-reflection data from the western Niger Delta were used to investigate the segmentation and linkage of a syn-sedimentary normal fault array and to estimate the influence of a pre-existing normal fault on the geometry and growth of younger faults. The nucleation, growth and linkage of a regional (seaward-dipping) deltaic fault system were analyzed on reflectivity time-/horizon slices and vertical seismic sections. In the deep subsurface, a master fault that consists of two segments (northwestern, NW, and southeastern, SE) grew through time into a single fault by lateral tip propagation reaching a final length of about 15 km. After attaining this length, displacement along the fault system developed non-uniformly through time. The analysis of the hanging-wall sediments of the deep-seated master fault shows two different processes of vertical linkage above the NW and SE segment. The SE segment links vertically to several younger faults contemporaneously with displacement accumulation on the master fault; in contrast, fault linkage above the NW segment occurred only after an interval of master-fault inactivity connecting the deep-seated structure upwards to a single syn-sedimentary normal fault. The observed differences in fault development suggest that although multi-segment deltaic faults form single fault systems after segment linkage, individual pre-linkage characteristics can be preserved, supporting a possibly diverse upward growth and connection to younger faults in the overburden. The geological interpretations presented highlight the influence of large deep-rooted structures on the development, location and geometry of shallow deltaic faults, documenting the influence of an older structural grain on delta tectonics.     

A linkage criterion for segmented normal faults

A detailed field study of 39 centimetre- to metre-scale relay ramps from two outcrops was performed to investigate the development of a linkage criterion for segmented normal faults. We analysed the displacement distribution and the geometry of fault arrays containing three types of relay ramp: open, linked, and fully breached, in order to identify which parameters are relevant to fault linkage, and to establish a linkage criterion. Each relay ramp geometry has a specific graphical field on a relay displacement–separation diagram. The field including all the linked geometries (initiation of linkage) separates open and fully breached relay ramps and is interpreted as a value of relay displacement to separation ratio for which faults link during their overlap. A ‘linkage threshold’, in each studied fault system, is defined as the best-fit linear trend of linked relays. We discuss the scaling and the variability of the linkage criterion using published datasets from a wide variety of settings and scales. The observed linkage threshold is linear, with a slope value varying less than one order of magnitude. This suggests that linking relay ramps have self-similar geometries from centimetre- to kilometre-scale and that normal fault linkage is governed by similar fault interaction across a broad range of scales. The linkage criterion, which can be an effective tool to estimate relay ramp geometry at depth or at the earth surface, could therefore be used to improve investigations in determining fluid entrapment or in the evaluation of potential surface of seismic ruptures.     

属性数据与空间数据连接对土壤有机碳储量估算的影响

土壤有机碳(Soil Organic Carbon, SOC) 库在陆地生态系统中具有重要作用。在基于GIS利用土壤类型法估算SOC储量时,由于土壤图比例尺的限制,属性数据与空间数据的连接会导致对SOC储量的估算结果产生很大不确定性。利用中国滇黔桂地区（云南省、贵州省和广西壮族自治区）798个土壤剖面及1∶[KG-*2]50万土壤图在不同的制图单元水平上,分别采用算术平均值法、中值法和面积加权平均值法（以土种志中的面积为权重）估算了该地区1 m深度SOC储量,并与基于土壤学专业知识连接方法（Pedological Knowledge Based Method, PKB）的估算结果进行了比较。结果表明：面积加权平均值法比中值法和算术平均值法的估算结果更为准确,而且在土类、亚类和土属水平上应用面积加权平均值法对SOC储量的估算结果差异不大。在采用较大比例尺、较为详细的土壤图时,PKB法较理想;反之,则面积加权平均值法较好。     

Topological invariants of field lines rooted to planes

Abstract

Two open curves with fixed endpoints on a boundary surface can be topologically linked. However, the Gauss linkage integral applies only to closed curves and cannot measure their linkage. Here we employ the concept of relative helicity in order to define a linkage for open curves. For a magnetic field consisting of closed field lines, the magnetic helicity integral can be expressed as the sum of Gauss linkage integrals over pairs of lines. Relative helicity extends the helicity integral to volumes where field lines may cross the boundary surface. By analogy, linkages can be defined for open lines by requiring that their sum equal the relative helicity.

With this definition, the linkage of two lines which extend between two parallel planes simply equals the number of turns the lines take about each other. We obtain this result by first defining a gauge-invariant, one-dimensional helicity density, i.e. the relative helicity of an infinitesimally thin plane slab. This quantity has a physical interpretation in terms of the rate at which field lines lines wind about each other in the direction normal to the plane. A different method is employed for lines with both endpoints on one plane; this method expresses linkages in terms of a certain Gauss linkage integral plus a correction term. In general, the linkage number of two curves can be put in the form L=r + n, |r|≦1J2, where r depends only on the positions of the endpoints, and n is an integer which reflects the order of braiding of the curves.

Given fixed endpoints, the linkage numbers of a magnetic field are ideal magneto-hydrodynamic invariants. These numbers may be useful in the analysis of magnetic structures not bounded by magnetic surfaces, for example solar coronal fields rooted in the photosphere. Unfortunately, the set of linkage numbers for a field does not uniquely determine the field line topology. We briefly discuss the problem of providing a complete and economical classification of field topologies, using concepts from the theory of braid equivalence classes.