互花米草入侵对河口盐沼湿地食物网的影响

盐沼湿地因其在河口及沿岸水域生态系统中的重要地位而被普遍关注,近年来互花米草在长江口乃至整个东南沿海地区的入侵及迅速蔓延更是引起了广泛重视。由于对维系本区域湿地生态系统运转的食物网结构的了解仍很有限,从而难以准确评估互花米草入侵后对原有生态系统的影响。本研究通过基于碳、氮稳定同位素测定结果的IsoSource软件估算和聚类分析,对长江口盐沼湿地内不同初级生产者的相对营养贡献大小进行了初步评估。结果显示在该湿地食物网中,底栖微藻和本土陆源C3植物是主要的营养来源。入侵C4植物互花米草的营养贡献不显著,在本次研究中仅有堇拟沼螺这一腹足类消费者在夏季较为确定地表现出对源自互花米草的富δ13C的有机质的摄取。随着互花米草的迅速扩散,其在长江口湿地的有机质产出中所占比例还将不断增加,这将可能从营养基础的层面自下而上对该食物网的结构和功能造成影响。     

37°N断面营养盐和溶解氧的四季分布特征及变化*

以2006年7月至2007年10月期间,4个季节的4个航次对37°N断面的调查资料为依据,分析并讨论了该断面四季生源要素的分布特征以及变化趋势.结果表明:该断面受黄海冷水团和陆源输入的影响,东西两侧的生源要素及温盐特征明显不同.夏季断面东倒由于受到冷水团的控制,底层出现明显的低温、高盐、高营养盐和高溶解氧的特征,并且跃层明显;西侧浅水区的温盐及生源要素的变化则相对均匀.冬季由于温跃层的消失,上下水体混合均匀,故而温盐及生源要素的垂直分布趋于均匀,断面西侧由于受到陆源输入的影响营养盐的浓度明显较东侧高.春季是增温降盐,营养盐逐渐消耗,东侧温跃层逐渐形成的过程;而秋季则恰恰相反.     

OGC CSW规范实现探讨

OGC CSW规范的实现,主要包括元数据信息模型建立、属性项映射、结果编码格式定义和软件实现,实现过程中需要注意参数格式标准化、参数约束条件、参数变化、元数据信息模型、名称空间以及该规范的局限性。介绍OGC CSW规范与目录服务标准及相关规范的关系,回顾该规范实现情况,结合全国测绘成果目录服务系统研发建立的工作实践,对OGC CSW规范的实现步骤和需要注意的问题进行讨论,并以全国测绘成果目录服务系统为例,介绍OGC CSW规范的应用效果。     

基于GIS的物流配送中心选址模型研究

配送中心是物流网络中的重要节点,对于优化企业物流系统,合理配置库存资源,提高物流的共同化程度发挥着重要作用。本文应用G IS网络分析方法和改进P中心选址算法,建立了配送中心选址优化模型。该模型由几何网络确定配送中心与需求点间距离、并引入租金、坡度、库存量等因素参与模型计算,通过总费用最小化确定仓库的最佳位置。因采用多因素参与决策和算法的改进,提高了配送中心选址精度,降低了用户选择的盲目性。     

海洋微型和小型底栖生物相互作用研究综述

The microscopic organisms from sediments are classified into microbenthos and meiobenthos. The former groups are usually referred to protozoa, microalgae and bacteria, whereas the latter comprise micrometazoa defined by mesh-size. Micro- and meiobenthos have been suggested as being one complex and are characterized by their small size, relative short life spans, high turnover rate, and complicated trophic structure. The quantification of the exchange rate of carbon seems a prerequisite for understanding the processes regulating the trophic structure in this complex, where the basic interactions of micro- and meiobenthos include nutrition, competition, synergy and inhibition, etc. The ecological processes mediating the interactions between these groups are poorly understood and invite our attention to more detailed studies. In this paper, we summarize literature data to outline the interactions of the two major assemblages and discuss the main progress in benthic microbial food web.     

NUFFT-Based Iterative Reconstruction Algorithm for Synthetic Aperture Imaging Radiometers

Synthetic aperture imaging radiometers (SAIRs) are powerful sensors for high-resolution observation of the Earth at low microwave frequencies. However, the future application of this new technology is limited by its large number of element antennas and receiving channels. In order to further reduce the complexity of the whole system, the circular and rotating array configurations have been proposed. Their disadvantages lie primarily in more complicated image reconstruction, because the conventional fast Fourier transform (FFT) method could not be used directly for image reconstruction. This letter introduces an iterative method for the reconstruction of radiometric brightness temperature maps from nonuniform visibility function samples. This method combines the conjugate gradient algorithm with min-max nonuniform FFT approach, which has been shown to provide considerably improved image quality relative to the traditional gridding method. Simulations for SAIRs were performed and showed better image quality in comparison to the traditional frequency interpolation method.     

测绘工程专业人力资源现状与毕业生需求研究

随着国民经济的快速发展,测绘行业得到了迅速发展壮大.江苏省是测绘人力资源大省,同时是测绘教育大省.通过抽样调查方法对江苏省测绘工程专业人力资源现状与毕业生需求情况进行了详细研究.研究得出江苏省测绘行业人才队伍不断壮大,未来需求量不断增加,有利于毕业生就业.     

Water, organic matter, nitrogen and phosphorus contents in sediment of a large-scale mariculture area in the Zhelin Bay of eastern Guangdong Province, China

The Zhelin Bay is one of the most important bays for large-scale mariculture in Guangdong Province, China. Owing to the increasing human population and the expanding mariculture in the last two decades, the ecological environment has greatly changed with frequent harmful algal blooms. A monthly survey of water content, organic matter （TOM）, and various forms of nitrogen and phosphorous in sediment from July 2002 to July 2003 in the bay was conducted. The results showed that the water content was correlated significantly with TOM and various forms of nitrogen and phosphorus and can be used as proxy for quick and rough estimate of these factors in the future surveys. TOM was also correlated significantly with various forms of nitrogen and phosphorus, indicating that it was one of the key factors affecting the concentrations and distributions of nitrogen and phosphorus in the investigated waters. Average total Kjeldhal nitrogen （TkN） content was（ 1 113.1 ± 382.5）μg/g and average total phosphorus （TP） content was（567.2± 223.3）μg/g, and both were much higher than those of similar estuaries in China and elsewhere. Average nitrogen and phosphorus tended to be higher inside than outside the bay, higher at aquaculture than non-aquaculture areas, and higher at fish-cage culture than oyster culture areas, suggesting that large-scale mariculture inside the bay played an important role in the eutrophication of the Zhelin Bay. Various forms of nitrogen and phosphorus concentrations were higher during the warm season （July--September）, which was due to the increased decomposition and concentration of organic matter resulted from the fast growth and high mortality of the cultured species. Compared with July 2002, TkN and TP contents were much higher in July 2003, in consonance with the eutrophication of the Zhelin Bay. Because exchangeable phosphorus （Ex-P）, iron-bounded phos- phorus （Fe-P） and organic phosphorus （OP） combined accounted for 34.3% of the TP and authigenic phosphorus （Au-P     

Pristine or altered: low-Mg calcite shells survived from massive dolomitization? A case study from Miocene carbonates

Low-Mg calcite shells have been widely used to reconstruct the chemistry of ancient seawater. There is always a question: are the shells chemically pristine? This paper presents the isotope and elemental geochemistry of low-Mg calcite bivalve shells in late Miocene platform carbonates, SE Spain. The platform carbonates were extensively dolomitized, and limestone is restricted to older stratal units, and to units mainly in topographically higher and more landward strata. Low-Mg calcite oyster shells were completely dissolved out in the basinward dolomite, but are well preserved in the limestone. These shells appear to retain the original growth microstructures, based on hand samples. Under the microscope, however, dissolution and recrystallization, as well as pristine growth lines are all present. Sr isotopes in these shells range from that of normal Miocene seawater to radiogenic values. δ¹⁸O and δ¹³C values, and Mg, Sr, and Na concentrations in these shells are rather variable. The high end members are consistent with the typical values of modern/late Miocene normal-seawater low-Mg calcite shells, whereas the low end members are close to those of diagenetic calcite cements, which have low δ¹⁸O, δ¹³C, Sr and Na values, and radiogenic Sr. The Nijar shells were altered physically and chemically to different degrees by diagenesis, although these shells are consistent with some “criteria” of unalteration. The isotopic and trace-element data collected in altered and pristine (or less altered) portions coexisting in the same shells are clearly differentiable. Quantitative simulation of covariations of geochemical pairs indicates that solid mixing of unaltered and altered portions by sampling is consistent with the variations in isotopic and elemental data recorded in the Nijar shells. The geological significance of this study is that ancient fabric-retentive calcite shells may have been altered geochemically although they may appear pristine. Calcite shells that underwent intensive diagenesis should be examined rigorously under the microscope, coupled with investigations of multiple geochemical proxies to assess chemical alteration. Only the data of unaltered shells can be used to reconstruct the chemistry of ancient seawater.     

Numerical study on salinity stratification in the Pamlico River Estuary

The variations of current circulation, salt intrusion, and vertical stratification under different river flow and wind conditions in the Pamlico River Estuary (PRE) were investigated in this paper using a three-dimensional numerical model. The model was calibrated and verified against water level variation, temperature, and salinity variations during 2003 and 2001, respectively. Eight sensitivity tests were conducted with different river flow and wind conditions specified in the model. Model results show that salinity intruded further upstream under scenarios with low flow, downriver local wind, and remote-wind-caused water level set-up conditions. In contrast, the responses of salinity stratification to different environmental forcing functions were different in different portions of the estuary. Salinity stratification was enhanced under high flow condition at the lower part of the estuary, under upriver wind near the river mouth, under downriver wind at the upstream to middle portion of the estuary, and under remote-wind-caused water level set-up condition at the majority of the estuary except near the river mouth. Model results also show that across-channel wind tended to reduce salt intrusion and salinity stratification in the PRE through increased vertical mixing.