Multi-colour surface photometry of a sample of HI-detected late type galaxies     

J. Vennik  G. M. Richter  W. Thnert  C. Biering 《Astronomische Nachrichten》1996,317(5):289-314

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Identification and investigation of sulphur plumes along the Namibian coast using the MERIS sensor     

Thomas Ohde  Herbert SiegelJan Reißmann  Monika Gerth 《Continental Shelf Research》2007

In the upwelling area along the Namibian coast of SW-Africa sulphur discolorations were investigated to study the impact of hydrogen sulphide on the ecosystem using satellite imagery. The formation of colloidal sulphur in the upper water layer results from the oxidation of hydrogen sulphide. The occurrence of sulphur plumes as well as their temporal and spatial development was investigated in relation to the driving meteorological and oceanographic conditions. Because of the sporadic occurrence of sulphur events and the limited number of ship-borne investigations in that area remote sensing of ocean colour is the only method to follow these phenomena continuously and synoptically. In the past the sulphur plumes were studied by true colour images derived from ocean colour satellite data like sea-viewing wide field of view sensor or moderate resolution imaging spectroradiometer and identified by their typical milky turquoise discoloration.  相似文献   

欧泊结晶状态和色斑研究的新发现          下载免费PDF全文

尹作为  赵雁 《地球科学》2000,25(3):302-305

欧泊的结晶状态和色斑问题一直以来是人们探讨的重要问题.对于区分天然欧泊与人工合成欧泊的重要鉴别特征“丝绢状”和“蜂巢状”色斑的成因问题, 研究甚少.通过宝石学常规测试、扫描电镜、X -射线粉晶衍射等测试手段, 进行测试和分析, 结果表明: 欧泊是由非晶态→雏晶→亚显微隐晶态→隐晶态的这种连续渐变的状态构成, 各状态之间并无截然的界限, 并且可以是这些不同状态的集合体; 提出了欧泊与玉髓之间的宝石学界定标准, 还揭示了两种色斑形成的不同机制: “丝绢”是由天然欧泊内部的显微构造裂隙对光产生散射而形成的, 而“蜂巢”是由合成欧泊自身结构中SiO₂球体排布与球体本身透光性决定的.对这两种色斑成因的揭示, 为欧泊鉴定提供了理论依据.   相似文献   

光色对中国明对虾(Fenneropenaeus chinensis)稚虾耗氧率昼夜变化节律的影响   总被引：1，自引：0，他引：1  

刘伟  王芳  钟大森  黄国强 《海洋湖沼通报》2011,(3):27-31

采用流水装置测定了中国明对虾(Fenneropenaeus chinensis)稚虾在4种先色处理下耗氧率的昼夜变化.实验设四种光色处理,分别为自然光(590nm)、黄光(580nm)、绿光(525 nm)和蓝光(435nm),光照周期为14L:10D,水温为25.0±0.5℃,实验虾的规格为(5.507±0.147)...  相似文献   

CSRH模拟接收机设计   总被引：1，自引：1，他引：0  

姬国枢  窦玉江  王威  刘飞  陈志军  张坚  颜毅华 《天文研究与技术》2006,3(2):135-142

本文叙述了日像仪实验的方案，双天线干涉仪中模拟接收机的结构，灵敏度，动态范围，噪声，增益的各级分配等问题，基于实验方案设计了日像仪模拟接收机。  相似文献   

Landslide scar/soil erodibility mapping using Landsat TM/ETM+ bands 7 and 3 Normalised Difference Index: A case study of central region of Kenya     

《Applied geography (Sevenoaks, England)》2015

Landsat series multispectral remote sensing imagery has gained increasing attention in providing solutions to environmental problems such as land degradation which exacerbate soil erosion and landslide disasters in the case of rainfall events. Multispectral data has facilitated the mapping of soils, land-cover and structural geology, all of which are factors affecting landslide occurrence. The main aim of this research was to develop a methodology to visualize and map past landslides as well as identify land degradation effects through soil erosion and land-use using remote sensing techniques in the central region of Kenya. The study area has rugged terrain and rainfall has been the main source of landslide trigger. The methodology comprised visualizing landslide scars using a False Colour Composite (FCC) and mapping soil erodibility using FCC components applying expert based classification. The components of the FCC were: the first independent component (IC1), Principal Component (PC) with most geological information, and a Normalised Difference Index (NDI) involving Landsat TM/ETM+ band 7 and 3.The FCC components formed the inputs for knowledge-based classification with the following 13 classes: runoff, extreme erosions, other erosions, landslide areas, highly erodible, stable, exposed volcanic rocks, agriculture, green forest, new forest regrowth areas, clear, turbid and salty water. Validation of the mapped landslide areas with field GPS locations of landslide affected areas showed that 66% of the points coincided well with landslide areas mapped in the year 2000. The classification maps showed landslide areas on the steep ridge faces, other erosions in agricultural areas, highly erodible zones being already weathered rocks, while runoff were mainly fluvial deposits. Thus, landuse and rainfall processes play a major role in inducing landslides in the study area.  相似文献   

Map Libraries     

Mingguang Wu  A-Xing Zhu  Li He 《The Cartographic journal》2013,50(3):273-278

Colour distortion, which is caused by the unavoidable mismatch between a map’s gamut and a device’s gamut, negatively affects the semiotic quality of maps. Cartographic communication often suffers from undesirable colour inconsistency. This method models cartographic colour reproduction as a constrained transform problem, namely, adapting a map’s gamut to fit a device’s gamut while preserving the semiotic quality. First, the characteristics of the map’s gamut are investigated by considering cartographic principles, and the fundamental concerns of preserving semiotic quality are proposed. Then, the self-organizing map method is introduced to iteratively optimize the cartographic colour reproduction. We implement this method and evaluate it based on a series of thematic maps. The results indicate that the proposed algorithm offers better results than two alternatives in terms of facilitating cartographic colour reproduction.  相似文献   

Cross‐shelf colour zonation in northern Great Barrier Reef lagoon surficial sediments     

L. J. Hamilton 《Australian Journal of Earth Sciences》2013,60(2):193-200

A cross‐shelf colour zonation is observed in Great Barrier Reef lagoon surficial sediments from 12 to 18°S, with colours tending to lighten from inner to outer shelf. The phenomenon is particularly well defined south of Cairns where four zones occur. The colour zonation appears to reflect the abrupt facies changes that occur in the lagoon. Visual estimates of relative optical lightness for the zones are strongly related to carbonate content, and lightness class boundaries broadly follow carbonate contours, indicating that the mechanisms leading to the colour zones are related to those governing carbonate distribution.  相似文献   

Arctic Ocean manganese contents and sediment colour cycles   总被引：5，自引：0，他引：5  

Ludvig Löwemark  Martin Jakobsson  Magnus Mörth  & Jan Backman 《Polar research》2008,27(2):105-113

Cyclical variations in colour and manganese content in sediments from the central Arctic Ocean have been interpreted to represent climatically controlled changes in the input of Mn from the Siberian hinterland, and/or variations in the intermediate and deep water ventilation of the Arctic basins, although a diagenetic origin has not been excluded. A reinvestigation of core 96/12-1pc using an Itrax X-ray fluoresence (XRF) core scanner confirms that these colour cycles are indeed controlled by variations in Mn content, although changes in the source region of the sediment may override the Mn colour signal in certain intervals. The prominent Mn cycles show no correspondence to any of the other measured elements. This decoupling of Mn and the bulk chemistry of the sediment is taken to indicate that the cycles observed are caused by variations in water column ventilation and riverine input, rather than variations in sediment source or diagenesis. We therefore conclude that the Mn maxima do represent warm phases with increased ventilation and/or riverine input, and that they therefore could be used for chronostratigraphic correlation between cores from the central Arctic Ocean, where traditional isotope stratigraphy is difficult or impossible to establish because of the lack of calcareous microfossils.  相似文献   

Difference in diet and age structure of blue and white Arctic foxes (Vulpes lagopus) in the Disko Bay area, West Greenland     

Sussie Pagh  & Páll Hersteinsson 《Polar research》2008,27(1):44-51

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