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通过对东印度洋钻孔CJ01-185的生物硅来探讨东印度洋古生产力的变化和古气候演化的响应。CJ01-185钻孔的生物硅含量在末次冰期最低,为0.86%;而到了全新世晚期生物硅含量达到1.89%。全新世晚期生物硅的堆积速率明显大于末次冰期。随着全新世海平面的快速上升,巽他海峡贯通,来自爪哇海的陆源物质输入到东印度洋,导致全新世的生物硅含量和生物硅的堆积速率增加。研究表明:巽他海峡贯通前,研究区的古生产力主要受东南季风变化和上升流的活动影响;而巽他海峡贯通后,古生产力很明显受到陆源物质输入的控制,东南季风变化和上升流的影响较弱。  相似文献   
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—Based on a linear model of the pressure difference between two sides of a porous wall and thefluid velocity inside it.an analytic solution is established for wave diffraction from a cylinder with an outerporous column and an inner solid column.Numerical experiments are carried out to examine the effects ofthe wave force on a porous low-column cylinder and the wave elevations outside and inside the cylinderdue to the porous character of the outer column and the ratio between the radii of the inner and outer col-umns.The numerical results show that the increase in the coefficient of porosity of the outer column of adouble column cylinder will reduce the wave elevation around the cylinder and the wave load on it.The ra-dius of the inner column does not affect too much the wave elevation around the cylinder and the totalforce on the cylinder.  相似文献   
3.
We present a reservoir simulation framework for coupled thermal-compositional-mechanics processes. We use finite-volume methods to discretize the mass and energy conservation equations and finite-element methods for the mechanics problem. We use the first-order backward Euler for time. We solve the resulting set of nonlinear algebraic equations using fully implicit (FI) and sequential-implicit (SI) solution schemes. The FI approach is attractive for general-purpose simulation due to its unconditional stability. However, the FI method requires the development of a complex thermo-compositional-mechanics framework for the nonlinear problems of interest, and that includes the construction of the full Jacobian matrix for the coupled multi-physics discrete system of equations. On the other hand, SI-based solution schemes allow for relatively fast development because different simulation modules can be coupled more easily. The challenge with SI schemes is that the nonlinear convergence rate depends strongly on the coupling strength across the physical mechanisms and on the details of the sequential updating strategy across the different physics modules. The flexible automatic differentiation-based framework described here allows for detailed assessment of the robustness and computational efficiency of different coupling schemes for a wide range of multi-physics subsurface problems.  相似文献   
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海底铁锰结壳和结核是重要的海底矿产资源,蕴含着丰富的金属元素并且具有巨大的经济价值。本文主要以南海多金属结壳(核)为研究对象,采用X射线粉晶衍射(XRD)、激光拉曼光谱、红外光谱分析(FTIR)以及X射线光电子能谱对铁锰矿物的矿物学和谱学特征进行了系统的分析和研究。粉晶衍射和拉曼光谱分析结果表明,南海多金属结壳的矿物组成为水羟锰矿、石英和长石,结核的矿物组成为钡镁锰矿、水羟锰矿、石英和长石,铁相矿物均为无定形铁氧化物/氢氧化物,并且锰相矿物和铁相矿物的结晶程度均较差。红外光谱分析结果显示多金属结核和结壳中的铁锰矿物具有大量表面羟基,这些含质子表面羟基官能团,可为海水中各成矿元素的络合提供丰富的活性位点。XPS分析表明多金属结核和结壳中铁锰矿物表面以Fe、Mn和O元素为主,其中Fe呈正三价态,Mn以正四、正三价为主,可能还含有少部分正二价态。对比南海多金属结壳(核)与太平海山结壳,南海多金属结壳(核)具有更为显著的表面羟基氧(-OH)含量,而太平洋海山结壳则以晶格氧(O2-)为主,表明太平洋海山结壳铁锰矿物结晶程度较南海多金属结壳(核)高。综合研究表明,在海底铁锰结壳和结核中(氢)氧化锰/铁矿物与海水之间界面效应对金属离子的富集机理主要有:(1)金属离子与矿物表面羟基进行络合反应,形成以配位键相连的羟基络合物,或与表面的质子交换生成稳定的内层络合物;(2)矿物的带电表面与金属离子通过静电作用形成双电层,生成外层络合物;(3)金属离子与矿物结构中的Mn、Fe离子同晶置换而成为结构阳离子。  相似文献   
5.
基于支撑向量机的遥感影像分类方法比较研究   总被引:1,自引:0,他引:1  
对支撑向量机的分类方法作简单介绍,并通过对MSS遥感影像数据的分类实验与多种常用的遥感影像分类方法进行对比,发现在分类精确度上,支撑向量机优于其他分类方法,但是速度稍慢,这也是支撑向量机需要改进的.  相似文献   
6.
Horizontal and vertical distributions of δ~(18)O and δ~(13)C were investigated in shells of four planktonic foraminiferal species, Globigerinoides ruber, Globigerinoides sacculifer, Pulleniatina obliquiloculata and Neogloboquedrina dutertrei, from a total of 62 core-top sediment samples from the Indonesian throughflow region. Results were compared to modern hydrologic conditions in order to explore potential of proxies in reconstructing fluvial discharge and upper ocean water column characteristics in this region. Our results show that, in the Makassar Strait, both of depleted δ~(18)O and δ~(13)C of these four species were linked to freshwater input. In the Bali Sea,however, depleted δ~(18)O and δ~(13)C for these species may be due to different reasons. Depleted δ~(18)O was a result of freshwater input and as well influenced by along-shore currents while depleted δ~(13)C was more likely due to the Java-Sumatra upwelling. Comparison of shell δ~(18)O records and hydrographic data of World Ocean Atlas 2005 suggests that G. ruber and G. sacculifer calcify within the mixed-layer, respectively at 0–50 m and 20–75 m water depth, and P. obliquiloculata and N. dutertrei within the upper thermocline, both at 75–125 m water depth. N.dutertrei calcifies at slightly deeper water depth than P. obliquiloculata does. In general, δ~(13)C values of both G.ruber and G. sacculifer are larger than those of P. obliquiloculata and N. dutertrei at all sites, possibly related to depth habitats of these species and vertical distribution of nutrients in the Indonesian throughflow region.  相似文献   
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海浪和潮汐风暴潮耦合过程的数值研究   总被引:1,自引:0,他引:1  
海浪和风暴潮是重要的海洋灾害。对它们的精确预测和预报对沿岸海洋灾害的风险评估及海洋工程的设计具有极其重要的社会和经济价值。过去人们本多对波浪和风暴潮单独进行预报。实际上,风既产生浪又产生风暴潮,因此它们的产生必然存在相互作用。本研究的目的就是要建立一个渤海高分辨率的双向耦合的海浪和潮汐风暴潮数值模式,研究各耦合机制的影响,以期为黄河三角洲沿岸风暴潮海浪漫堤、漫滩风险评估提供更为准确的海浪风暴潮预测预报结果。 作者在研究中基于国际上先进的第三代海浪数值模式和潮汐风暴潮模式,建立了渤海2''×2''的海浪和潮汐风暴潮耦合数值模式。耦合模式充分考虑了三个主要耦合物理机制:依赖海浪状态的表面风应力,波-流相互作用底应力和辐射应力。波浪模式主要基于国际上第三代WAM模式,并对其进行了浅水效应的改进,以包括浅水深度破碎引起的能量耗散;潮汐风暴潮模式计算中开边界考虑了10个主要分潮K1,O1,P1,Q1,M2,S2,N2,K2,Sa,Ssa。依赖海浪状态的表面风应力取自Donelan等(1993)的结果,波-流相互作用底应力取自Signell等(1990)对 Grant and Madsen(1979)简化的结果,辐射应力以海浪谱表示。耦合计算中,两个模式通过三个耦合机制双向传递所需参量。 运用胜利油田中心一号观测的2个同步浪、潮、流资料对所建的耦合模式进行了检验,并通过耦合和非耦合模式结果的对比对各耦合机制的影响效应进行分析研究。研究结果表明,不同物理机制对波高的影响主要由能量方程中以辐射应力表示的波流相互作用所决定;在波-潮耦合作用中,依赖波令的表面风应力和辐射应力对水位是正效应,而波流相互作用底应力对水位是负效应。三个物理机制的综合净效应是正,可增加水位达25cm。比较显示,耦合模式的结果无论对波高还是水位都比非耦合模式的结果好,特别在峰值处。 本研究显示耦合模式的结果将改进海浪和风暴潮的模拟精度。所建立的耦合模式将对渤海海浪和风暴潮预报精度的提高,以及为黄河三角洲近岸海浪和风暴潮灾害的风险评估,提供更可靠的参数,具有重要的价值。  相似文献   
8.
一次罕见水稻稻瘟病发病条件分析和预防措施   总被引:3,自引:0,他引:3  
通过对一次罕见的水稻稻瘟病调查,介绍水稻稻瘟病发病症状、发病条件及预防措施。  相似文献   
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