Three-image matching. For 3-D linear object tracking     

SHAO Juliang Clive Fraser 《地球空间信息科学学报》2000,3(2):13-18,40

1　ＩｎｔｒｏｄｕｃｔｉｏｎＴｈｒｅｅｄｉｍｅｎｓｉｏｎａｌ(3＿Ｄ)ｌｉｎｅａｒｏｂｊｅｃｔｔｒａｃｋｉｎｇｉｓａｋｅｙｏｐｅｒａｔｉｏｎｆｏｒａｎｕｍｂｅｒｏｆｓｔｅｒｅｏｖｉｓｉｏｎａｐｐｌｉ ｃａｔｉｏｎｓ,ｆｏｒｅｘａｍｐｌｅ ,ａｕｔｏｎｏｍｏｕｓｏｎ＿ｒｏａｄｖｅｈｉｃｌｅｎａｖｉｇａｔｉｏｎ[2 ,5 ,9] ａｎｄｍｏｂｉｌｅｍａｐｐｉｎｇ[3,1 1 ,1 8] .Ｓｕｃｈｓｙｓｔｅｍｓｔｙｐｉｃａｌｌｙｅｘｐｌｏｉｔｔｗｏｓｔｅｒｅｏｉｍａｇｅｓｏｎｌｙｆｏｒｌｉｎｅａｒｏｂｊｅｃｔｔｒａｃｋｉｎｇ .Ｂｉ…  相似文献   

Seismic and Petrophysical Relationships from UK Continental Shelf Rocks at Elevated Pressures     

Solomon Assefa  Clive McCann  Jeremy Sothcott 《Marine Georesources & Geotechnology》2000,18(2):119-140

There are few published seismic (P- and S-waves) properties for seafloor bedrocks. At low pressures (1 to 10 MPa), velocities and attenuations are determined mainly by open microcracks. At higher pressures, the microcracks close, and the velocities and attenuations depend primarily on the matrix porosity. We have investigated both the relationships between the acoustic, petrophysical, and geological properties of the rocks at 40 MPa pressure and the effect of microcracks on the acoustic properties at 10 MPa pressure. In this paper we discuss the former; the latter will be discussed separately. P- and S-wave velocity and attenuation measurements were carried out on a suite of seabed sedimentary and igneous rocks at effective pressures from 10 to 40 MPa at ultrasonic frequencies. The porosities and permeabilities of the rocks ranged from 0% to 32% and 0 to 110 mDarcy, respectively. Characterization of the rocks revealed that most of the sandstones have a substantial clay content (kaolinite, illite, and chlorite) and fractures. Most of the igneous rocks are chloritized. The seismic properties of the rocks are markedly lower than those of similar continental rocks because of the microporosity formed by the alteration of feldspars, micas, and mafic minerals to clays (e.g., chloritization of pyroxenes) and the corresponding reduction of the elastic moduli. The results of this study suggest that the values of velocities and quality factors used for ocean acoustic propagation models are lower than normally assumed.  相似文献   

Strategies for Sustainable Development: Experiences from the Pacific     

Jon Barnett 《New Zealand geographer》2000,56(1):56-57

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Towards fair local outcomes in adaptation to sea-level rise     

Sonia Graham  Jon Barnett  Ruth Fincher  Colette Mortreux  Anna Hurlimann 《Climatic change》2015,130(3):411-424

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Three decades of water quality measurements from the Upper Severn experimental catchments at Plynlimon,Wales: an openly accessible data resource for research,modelling, environmental management and education   总被引：1，自引：0，他引：1  

Colin Neal  Brian Reynolds  Dave Norris  James W. Kirchner  Margaret Neal  Phil Rowland  Heather Wickham  Sarah Harman  Linda Armstrong  Darren Sleep  Alan Lawlor  Clive Woods  Bronwen Williams  Matt Fry  Gwen Newton  Dan Wright 《水文研究》2011,25(24):3818-3830

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Anisotropy and depth‐related heterogeneity of hydraulic conductivity in a bog peat. II: modelling the effects on groundwater flow     

Clive W. Beckwith  Andrew J. Baird  A. Louise Heathwaite 《水文研究》2003,17(1):103-113

Anisotropy and heterogeneity of hydraulic conductivity (K) are seldom considered in models of mire hydrology. We investigated the effect of anisotropy and heterogeneity on groundwater flow in bog peat using a steady‐state groundwater model. In five model simulations, four sets of K data were used. The first set comprised measured K values from an anisotropic and heterogeneous bog peat. These data were aggregated to produce the following simplified data sets: an isotropic and heterogeneous distribution of K; an isotropic and homogeneous distribution; and an anisotropic and homogeneous distribution. We demonstrate that, where anisotropy and heterogeneity exist, groundwater flow in bog peat is complex. Fine‐scale variations in K have the potential to influence patterns and rates of groundwater flow. However, for our data at least, it is heterogeneity and not anisotropy that has the greater influence on producing complex patterns of groundwater flow. We also demonstrate that patterns and rates of groundwater flow are simplified and reduced when measured K values are aggregated to create a more uniform distribution of K. For example, when measured K values are aggregated to produce isotropy and homogeneity, the rate of modelled seepage is reduced by 28%. We also show that when measured K values are used, the presence of a drainage ditch can increase seepage through a modelled cross‐section. Our work has implications for the accurate interpretation of hydraulic head data obtained from peat soils, and also the understanding of the effect of drainage ditches on patterns and rates of groundwater flow. Copyright © 2002 John Wiley & Sons, Ltd.  相似文献   

Northern waters: the resource — security relationship: International colloquium on northern waters: Resources and security issues,Ellon, Scotland, 17–19 September 1980     

Clive Archer 《Marine Policy》1981,5(2):156-157

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Erratum to: Radio AGN in the local universe: unification,triggering and evolution     

Clive?TadhunterEmail author 《Astronomy and Astrophysics Review》2016,24(1):12

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A new section of Lower Palaeozoic rocks in Kayin State (Southeast Myanmar)     

Mongkol Udchachon  Punya Charusiri  Hathaithip Thassanapak  Clive Burrett 《Proceedings of the Geologists' Association. Geologists' Association》2018,129(2):215-226

Lower Palaeozoic rocks have been mapped in Kayin State in an area previously shown on published maps as either metamorphic or possibly Lower or Upper Palaeozoic rocks. Three new formations, with a total thickness of over 900?m, apparently overlain by an, at least, 100?m thick Upper Palaeozoic formation are mapped along the Salween River and along the road from Yinbaing, in Myanmar, to Tha Song Yang, in Thailand. The Lower Palaeozoic succession consists of the predominantly siliciclastic Kyaukpulu and Kushwe–e–we formations and an overlying, predominantly carbonate Meseik Ashe Formation which contains Middle Ordovician (Darriwilian) conodonts. The older two formations are probable correlates of the Ngwetaung and Lokeypin formations of the southern Shan State of Myanmar and the Lower Ordovician siliciclastics of western Thailand. The overlying, peritidal to shallow subtidal carbonates of the Meseik–Ashe Formation are correlates of the Wunbye and Sitha formations of Shan State, Myanmar. The thick–bedded, quartz arenites of the Nyaungwiang Formation are faulted against the Ordovician carbonates and are probable lithological correlates of the Carboniferous Taungnyo Formation. The folds in the Lower Palaeozoic rocks are overturned to the northeast and deformation was in one major phase between the Tournaisian and the Early Permian. The Lower Palaeozoic strata may probably be followed as a ridge for at least 100?km towards the NNW, close to the western border of the Sibuma Block which is separated by a postulated cryptic suture from the Irrawaddy Block to the west.  相似文献   

Soil Paleocatenas,Prehistoric Land Use,and Coastal Landscape Dynamics at Druridge Bay,Northeast England     

Robert W. Payton  Clive Bonsall 《Geoarchaeology》2016,31(5):388-411

Coastal erosion of sand dune systems along Druridge Bay, northeast England, has progressively exposed parts of the subdune mid‐Holocene landscape, including paleocatenas, indicating former soil hydrosequences with localized wetland habitats, and archaeological evidence of human activities and land use from the Late Mesolithic to the Romano‐British period. Archaeological investigations and pedostratigraphic studies of paleosols provide a unique spatial–chronological framework to interpret soil and land use change over several millennia in the context of a changing coastal environment. Evidence includes dating of archaeological remains, the stratigraphy, morphology and micromorphology of buried soils and sediments, and the palynology and radiocarbon dating of subdune peats. Early Bronze Age burial sites were preferentially located on well‐drained hillocks also used for grazing. Adjacent wetland depressions provided areas of marshy grassland and swamp over deep fen peat soils that started to develop c. 5435 cal. yr B.P. in response to a rising groundwater table stimulated partly by slow sea‐level rise. The backslopes of the paleocatena were occupied by imperfectly to poorly drained soils that supported open oak‐hazel woodland with evidence for progressive clearance and use for agriculture. Windblown sand started to accumulate on the study site sometime between 3930 and 3670 cal. yr B.P., well before the Little Ice Age date for dune formation suggested by previous researchers.  相似文献