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电子探针分析结果表明,沱沱河地区赛多浦岗日二长花岗岩中黑云母具有富MgO、SiO_2、(Na_2O+K_2O),相对贫Al_2O_3、FeO~t的特征;镁质率(M=0.60~0.65)高,∑Al值(1.30~1.39)偏低,中等Fe/(Mg+Fe)(0.42~0.44)比值,为镁质黑云母;估算其结晶温度为580℃~645℃,且岩浆体系具有较高的氧逸度。黑云母的成分特征显示其寄主岩体为造山背景下形成的钙碱性花岗岩,其源区具有壳-幔混源的特征。 相似文献
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东海赤潮高发区表层沉积物中部分脂类标记物的分布与来源 总被引:2,自引:1,他引:1
通过对2005年和2006年东海赤潮高发区表层沉积物部分脂类标记物(正构烷烃、脂肪酸等)的分析,初步探讨了表层沉积物有机物的来源。沉积物中正构烷烃的碳优势指数Icp值及姥鲛烷/植烷的质量比(Pr/Ph)普遍较低,而n-C16,n-C18的质量分数较高。分析表明,石油烃是东海赤潮高发区表层沉积物脂肪烃的主要成分。来源于细菌、海洋微藻和陆生高等植物的脂肪酸如直链饱和脂肪酸、支链饱和脂肪酸、不(多不)饱和脂肪酸等在2005~2006年间的组成和分布比较稳定:直链脂肪酸含量普遍较高,其次为支链脂肪酸和单不饱和脂肪酸,多不饱和脂肪酸含量相对较少。利用生物标记物分析表明,海洋自生生物源(细菌、海洋微藻等)是沉积物中脂肪酸的主要来源,陆源脂肪酸对东海赤潮高发区表层沉积物的贡献较小。 相似文献
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The double-body heave wave energy converter(WEC) is one of the most conducive devices to absorb the wave energy from relative motion while the law of which is not well understood. This paper makes an in-depth study on this wave energy converter, by means of the combination of theoretical analysis and physical model experiment. The hydrodynamic characteristics and energy capture of the double-buoy under constant and linear Power Take-Off(PTO) damping are investigated. Influences of absolute mass and mass ratio are discussed in the theoretical model.Relative displacement amplitude and average power output are tested in the experiment to analyze the effect of the wave period and outer buoy's mass, while the capture width ratio(CWR) is also calculated. Results show that the wave period and mass of the buoys have a significant effect on the converter. Different forms of PTO damping have no influence on the optimal wave period and mass ratio of this device. It is recommended to select the double-buoy converter with a mass ratio of 0.80 and to place it in an area with the frequent wave period close to the natural period of the outer buoy to achieve the optimal energy capture. 相似文献
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内河DOM降解的三维荧光、紫外光谱研究——以白马河为例 总被引:3,自引:0,他引:3
利用三维荧光光谱、紫外光谱手段,研究白马河水样中DOM在微生物作用下的分解情况,经过微生物分解204 h后DOC的浓度下降为23%.根据双指数方程拟合,水样中易分解组分占总量的63.2%,易分解组分与难分解组分的分解常数分别为0.102 h-1,0.002 57 h-1.随着培养时间的延长,水样三维荧光光谱中单位浓度有机物的荧光强度有不同程度的提高.根据水样的紫外吸收光谱分析,培养过程中SUVA254 nm有逐步升高的趋势,而溶液250 nm与365 nm吸收的比值没有明显变化. 相似文献
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A Finite Volume Method with Unstructured Triangular Grids for Numerical Modeling of Tidal Current 总被引:1,自引:1,他引:1
The finite volume method (FVM) has many advantages in 2-D shallow water numerical simulation. In this study, the finite volume method is used with unstructured triangular grids to simulate the tidal currents. The Roe scheme is applied in the calculation of the intercell numerical flux, and the MUSCL method is introduced to improve its accuracy. The time integral is a two-step scheme of forecast and revision. For the verification of the present method, the Stoker's problem is calculated and the result is compared with the mathematically analytic solutions. The comparison indicates that the method is feasible. A sea area of a port is used as an example to test the method established here. The result shows that the present computational method is satisfactory, and it could be applied to the engineering fields. 相似文献
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大同盆地高砷地下水系统沉积物环境磁学特征 总被引:1,自引:0,他引:1
为了研究高砷含水层沉积物中砷与磁性矿物的关系, 对大同盆地高砷地区含水层钻孔样品进行了环境磁学和地球化学分析, 结果表明亚铁磁性矿物是决定含水层沉积物磁性特征的主要磁性矿物.通过对比砷和磁性参数在垂向上的变化趋势发现, 高砷含量往往对应着低的饱和等温剩磁(SIRM) 值, 揭示出砷和顺磁性矿物之间也存在联系.沉积物砷含量与磁性参数的相关系数均小于0.5 (α=0.05), 表明砷和亚铁磁性矿物及不完整反铁磁性矿物之间不存在明显的联系.在所有磁性参数中磁化率(χ)和砷含量之间相关性最显著, 相关系数均在0.4 (α=0.05) 左右, 低的相关系数与亚铁磁性矿物和不完整反铁磁性矿物对顺铁磁性矿物的稀释有关.该地区高砷地下水的形成可能与水铁矿及纤铁矿等砷的赋存矿物在还原条件下的还原溶解有关. 相似文献
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This study proposed a wave power system with two coaxial floating cylinders of different diameters and drafts.Wavebob’s conceptual design has been adopted in the wave power system. In this study, a basic analysis of the wave energy extraction by the relative motion between two floats is presented. The maximum power absorption was studied theoretically under regular wave conditions, and the effects of both linear and constant damping forces on the power take-off(PTO) were investigated. A set of d... 相似文献
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福建长汀河田盆地的马尾松林碳储量时空动态变化 总被引:1,自引:0,他引:1
以福建省长汀县侵蚀退化严重的河田盆地为例,重点研究该区水土流失生态修复的主要树种——马尾松林的碳储量动态变化.通过2011年的野外样地调查获得了马尾松林的实测数据,并将其与同期SPOT5影像对应样地改进的归一化植被指数(MNDVI)数据进行回归分析,建立了河田盆地2011年马尾松林碳储量的反演模型.进一步通过不变特征法对所获得的2011年模型进行校正,使其能够推广应用于2004年和2009年的马尾松林碳储量反演,以揭示河田盆地马尾松林碳储量在2004—2011年间的时空变化.研究结果表明,这期间河田盆地马尾松林的总碳储量和碳密度均呈逐步上升的趋势:总碳储量由2004年的9.28×105 t增加到2011年的12.49×105 t,碳密度由27.31×10-4 t/m2增加到35.84×10-4 t/m2,总的说明该区马尾松林的碳汇能力在这期间有了明显的增加,而且在2009—2011年间表现得更为明显. 相似文献
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