基于6S模型的MODIS影像逐像元大气校正及其应用

以获取地物真实反射率为目的,介绍了逐像元大气校正的方法。应用6S模型逐像元综合考虑太阳天顶角、传感器天顶角、相对方位角、大气气溶胶厚度、观测波段以及地表海拔这6个参数,生成查找表,统计分析各参数关于反射率的敏感度;并与以往单一参数校正的方法比较了校正的效果。结果表明,逐像元大气校正算法更加接近地物的真实反射率。利用MODIS地表反射率产品对大气校正的结果进行验证,单一参数、逐像元大气校正的相对误差分别控制在26.9%和12.7%以内;在以植被指数(NDVI)为例的后续遥感定量化反演过程中,逐像元比单一参数大气校正方法计算的NDVI平均高出14.4%。     

Assessing the influence of the Merzbacher Lake outburst floods on discharge using the hydrological model SWIM in the Aksu headwaters,Kyrgyzstan/NW China

Glacial lake outburst floods (GLOF) often have a significant impact on downstream users. Including their effects in hydrological models, identifying past occurrences and assessing their potential impacts are challenges for hydrologists working in mountainous catchments. The regularly outbursting Merzbacher Lake is located in the headwaters of the Aksu River, the most important source of water discharge to the Tarim River, northwest China. Modelling its water resources and the evaluation of potential climate change impacts on river discharge are indispensable for projecting future water availability for the intensively cultivated river oases downstream of the Merzbacher Lake and along the Tarim River. The semi‐distributed hydrological model SWIM was calibrated to the outlet station Xiehela on the Kumarik River, by discharge the largest tributary to the Aksu River. The glacial lake outburst floods add to the difficulties of modelling this high‐mountain, heavily glaciated catchment with poor data coverage and quality. The aims of the study are to investigate the glacier lake outburst floods using a modelling tool. Results include a two‐step model calibration of the Kumarik catchment, an approach for the identification of the outburst floods using the measured gauge data and the modelling results and estimations of the outburst flood volumes. Results show that a catchment model can inform GLOF investigations by providing ‘normal’ (i.e. without the outburst floods) catchment discharge. The comparison of the simulated and observed discharge proves the occurrence of GLOFs and highlights the influences of the GLOFs on the downstream water balance.
69; 2013 The Authors. Hydrological Processes Published by John Wiley & Sons Ltd.     

Active tectonics around the junction of Southwest Japan and Ryukyu arcs: Control by subducting plate geometry and pre‐Quaternary geologic structure

The origin of active faults in the Inner zone of the western part of Southwest Japan was explained by a decrease of the minimum principal stress and reactivation of ancient geologic structures. Although the E–W maximum principal stress in Southwest Japan due to the collision of the Southwest and Northeast Japan arcs along the Itoigawa–Shizuoka Tectonic Line is assumed to decrease westward, the density of active strike‐slip faults increases in the western margin of the Southwest Japan Arc (western Chugoku and northern Kyushu) where the subducting Philippine Sea Plate dips steeply. The E–W maximum compressional stress is predominant throughout Southwest Japan, while the N–S minimum principal stress that is presumably caused by coupling between Southwest Japan arc and Philippine Sea Plate decreases due to the weak plate coupling as the plate inclination increases under the western margin of Southwest Japan. The increase of the fault density in the western margin of the arc is attributed to a decrease of the minimum principal stress and consequent increase of shear stress. Low slip rates of the active faults in this region support the view that the westward increase of fault density is not a response to increasing maximum stress. These faults of onshore and offshore lie in three distinct domains defined on the basis of fault strike. They are defined domains I, II, and III which are composed of active faults striking ENE–WSW, NW–SE, and NE–SW, respectively. Faulting in domains I, II, and III is related to Miocene rift basins, Eocene normal faults, and Mesozoic strike‐slip faults, respectively. Although these active faults are strike‐slip faults due to E–W maximum stress, it is unclear whether their fault planes are the same as those of pre‐Quaternary dip‐slip faults.     

Variations in stress and driving pore fluid pressure ratio using vein orientations along megasplay faults : Example from the Nobeoka Thrust,Southwest Japan

The Nobeoka Thrust of Southwest Japan is an on‐land example of an ancient megasplay fault that provides an excellent record of deformation and fluid flow at seismogenic depths. The present study reports: (i) temporal stress changes for the seismogenic period of the Nobeoka Thrust; and (ii) spatial heterogeneities in driving pressure ratios P* obtained from mineral veins around the Nobeoka Thrust fault zone. Many quartz veins that filled mode I cracks can be observed in the hanging wall and footwall of the thrust. Inversion for stress orientation suggests that normal faulting dominated in both the hanging wall and footwall, with similar stress axis orientations in both. The orientation of σ₃ for the estimated stress regime is parallel to the slip direction of the Nobeoka Thrust. The detected normal‐faulting‐type stress regimes likely resulted from post‐seismic stress buildup after megathrust earthquakes. The hanging wall of the Nobeoka Thrust has smaller P* values than the footwall. Two possible explanations are proposed for the observed spatial variations in the driving pore fluid pressure ratio, P*: spatial variations in pore fluid pressure P_f are directly responsible for P* variations, or P* variations are controlled by differences in mechanical properties between the hanging wall and footwall.     

Large‐scale erosion and overbank deposition caused by the July 2013 flood of the Abu River,Yamaguchi City,Japan

This paper reports on the erosion, transport, and deposition processes associated with an overbank deposit formed by the flooding of the Abu River on July 28, 2013, in Yamaguchi City, Japan. At the study site, river flows overtopped the levee revetment upstream of a meander bend cutting it off and flowing back into the main channel downstream. In this sequential process, it deposited large amounts of sediments, ranging from mud to cobbles, on the floodplain. The surface of paddy fields adjacent to a railway line, located at the center of the affected floodplain, was severely eroded by the flood flows. Overbank deposits composed of both upstream finer sediments and eroded coarser terrestrial sediments are laid down in the affected area. Large amounts of pebbles and cobbles originating from the eroded terrestrial area formed a gravelly pile on top of the sand and gravel sediments derived from the river. This finding indicates that sands and gravels were deposited prior to the formation of the gravelly pile, probably before and during peak flood flows. An inverse grading structure is evident in the lower to middle part of these comparatively thick deposits, most likely due to differences in transport pattern between entrained terrestrial gravels and upstream finer sediments.     

邯郸6井水氡观测环境与震例分析

从邯郸6井水氡1986年以来的月均值曲线分析,2001年以来水氡处于高值异常变化,2003年5月月均值一阶差分出现超出2倍均方误差的单点异常。在以往日常资料分析中,如果邯郸6井水氡出现一些显著变化,往往习惯性地怀疑其观测环境特殊性影响资料的信度,即将其归因于邯郸6井停泵、观测水样为井网混合水所致。随着分析的深人,认为如此分析过于简单。鉴于以上原因,本文拟对该井多年资料进行深人分析,对资料的映震能力做进一步探讨。     

融合蛋白IL6-OmpW的质粒构建及表达纯化

以重组质粒pMD18-T/IL6和pMD18-T/OmpW为模板,分别扩增红笛鲷IL-6基因和哈维氏弧菌外膜蛋白OmpW基因,运用PCR重叠延伸剪切技术,将IL-6和OmpW基因融合,将融合基因定向克隆到原核表达载体pET-32a(+),转化大肠杆菌BL21(DE3)感受态,经异丙基-β-D-硫代半乳糖苷(IPTG)诱导融合蛋白高效表达,融合蛋白分子质量约为66.6 ku。优化后表达条件为温度37℃,IPTG浓度0.2 mmol·L-1,诱导时间5 h。用HisTrap HP亲和柱纯化重组蛋白,最佳咪唑洗脱浓度为400 mmol·L-1,纯化蛋白的质量浓度为480μg·mL-1。Western-blot分析显示,该融合蛋白可与鼠抗His-tag单克隆抗体发生特异反应,表明目的蛋白得以正确表达。     

鲈鱼FBP基因的克隆和表达分析

果糖-1,6-二 磷酸酶(fructose-1,6-bisphosphatase,FBP, EC 3. 1.3.11)可催化果糖-1,6-二磷酸水解成果糖-6-磷酸和无机磷酸盐,是糖异生途径中的关键酶之一。本研究运用SMART RACE技术从鲈鱼Lateolabrax japonicus肝脏中分离克隆了FBP基因的全长cDNA序列,该基因全长1 357 bp,其中5’非翻译区和3’非翻译区分别为42 bp和301 bp,开放阅读框为1 014 bp,共编码337个氨基酸。蛋白质分子量约为36.7 kD,理论pI为6.90。氨基酸序列分析表明,鲈鱼FBP与其它动物的肝脏型FBP相似性很高,与裸盖鱼、彩虹胡瓜鱼、斑马鱼、异育银鲫和大西洋鲑的肝脏型FBP的同源性分别为94.3%,90. 8%,89.3%,88.1%和84.1%。系统发育分析显示,鲈鱼FBP与其它鱼类的肝脏型FBP成簇后再与哺乳动物的肝脏型FBP聚成一支,然后才与哺乳动物的肌肉型FBP汇成簇。同时用RT-PCR分析了FBP基因在鲈鱼肝脏、肌肉、心脏、眼、肠、肾脏、脂肪、脾脏、鳃和大脑等10个组织的表达,结果表明FBP仅在肝脏、肾脏和肠这3个组织中有较高的表达,与糖异生发生组织基本一致,因此推测该FBP属于肝脏型。     

基于体验视角的历史街区旅游复兴——以福州市三坊七巷为例

目前国内历史街区在旅游开发上存在模式雷同、体验质量相似等问题,从旅游体验视角探讨了历史街区旅游复兴的新思路,分析了历史街区旅游体验要素,提出包含审美怀旧、文化教育、休闲娱乐、遁世逃避、社交生活和情感升华在内的6E体验模型及各体验要素营造方法。以福州市三坊七巷旅游发展策划为例,具体阐释了6E模型在历史街区旅游复兴中的应用,结合体验的层次性、综合性和场地分析,将整个街区由动到静、由表层到深度体验过渡,依次划分为南后老街摩尔、温馨休闲之巷、安泰水岸风情和小众定制名坊四个功能区。应用6E模型解决历史街区旅游功能分区和产品策划,有益于从文化、社会、经济层面上再造老街区的鲜活面貌,是一种可持续发展的思路。