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                HydroScat-6p(plus)后向散射测量仪

                HydroScat-6p(plus)后向散射测量仪
                <
                • HydroScat-6p(plus)后向散射测量仪
                >
                产品报价: 面议
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                034 (HydroScat-6p)
                北京
                详细说明

                测量范围:
                6个波长的后向散射,角度140°
                2个波长的荧光

                特色:
                超高的光学性能和精确的标定
                内部数据储存
                实时数据输出,波特率可达9600-57600
                内部可充电电池,外部电源10-15V
                电池可供24小时不间断使用,可连续数个星期间断使用
                通过电磁开关或软件指令来激活
                优越的HydroSoft软件
                用户可以根据需要选择波长及闪存-能增大数据容量,可容纳百万个采样
                最大工作深度可达500米
                铜制的显象管可防止腐烂

                该系列产品有以下型号可选:
                HydroScat-2,DeepHydroScat-2,HydroScat-4及HydroScat-6

                HydroScat-2
                两个波长后向散射(?[140°]andbb),(标准波长420,700nm)
                一个荧光(叶绿素)
                深度(330m,其他可选)
                DeepHydroScat-2(深海测量4000m)
                两个波长后向散射(?[140°]andbb),(标准波长420,700nm)
                一个荧光(叶绿素)
                深度4000m
                HydroScat-4
                四个波长后向散射(?[140°]andbb)或▲三个波长后向散射(?[140°]andbb)外加荧光
                标准波长:420,470,532&700nm或420,532,700nm加荧光
                深度(330m,其他可选)
                HydroScat-6
                六个波长后向散射(?[140°]andbb)
                标准波长:420,442,470,510,590及700nm(可定制其他波长)
                两个波长的荧光
                标准:700nmexcitedby420nm(chlorophyll),510nmexcitedby442nm
                深度:(330m,500m可选)
                产地:美国

                HydroScat 后向散射仪 文献目录
                1.Dariusz Stramski, Rick A. Reynolds, Mati Kahru, et al. Estimation of Particulate Organic Carbon in the Ocean from Satellite Remote Sensing. Science,1999, 285 (5425): 239 - 242
                2.Annamarie Hatcher, Paul Hill , Jon Grant. Optical backscatter of marine flocs . Sea Research, 2001,1(46):1-12
                3.David McKee,Alex Cunningham.Evidence for wavelength dependence of the scattering phase function and its implication for modeling radiance transfer in shelf seas. Applied Optics, 2005, 1(44):126-135
                4.Ryszard Hapter, Slawomir Kaczmarek, and Joanna Ston. Bio-optical relationships and ocean color algorithms for the north polar region of the Atlantic. Geophysical research, 2003,108(C5,3143):1-17
                5.G. H. Tilstone, G. F. Moore, K. S?rensen. et al. Regional Validation of MERIS Chlorophyll products in North Sea coastal waters. Development of Generic Earth Observation Technologies,2001
                6.M. A. Moline, T. Bergmann, W. P. Bissett, J. et al. Integrating Optics And Biology: Estimation Of Bioluminescence Leaving Radiance From An Autonomous Vertical Profiler.1-10
                7.Stavn, Robert H., Spiering, Bruce A.,Gould, Richard W...d Biogeo-Optics:Backscattering Cross Sections for Suspended Mineral and Organic Matter in the Coastal and Near-Coastal Ocean. Physical And Dynamic Oceanography Optics,2004,10
                8.EJ DSa, RL Miller. Bio-optical properties in waters influenced by the Mississippi River during low flow conditions. Remote Sensing of Environment, 2003,538-549
                9.Donald C. Pierson, Niklas Str?mbeck. Estimation of radiance reflectance and the concentrations of optically active substances in Lake M?laren, Sweden, based on direct and inverse solutions of a simple model. The Science of The Total Environment,2001,1-3,14(268):171-188
                10. E.N. Flory, P.S. Hill T.G. Milligan et al. The relationship between floc area and backscatter during a spring phytoplankton bloom. Deep Sea Research Part I: Oceanographic Research Papers, 2004, 51(2):213-223

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