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Jiaozhou Bay data collected from May 1991 to February 1994, in 12 seasonal investigations, and provided the authors by the Ecological Station of Jiaozhou Bay, were analyzed to determine the spatiotemporal variations in temperature, light, nutrients (NO3^--N, NO2^--N, NH4^ -N, SIO3^2--Si, PO4^3--P), phytoplankton, and primary production in Jiaozhou Bay. The results indicated that only silicate correlated well in time and space with, and had important effects on, the characteristics, dynamic cycles and trends of, primary production in Jiaozhou Bay. The authors developed a corresponding dynamic model of primary production and silicate and water temperature. Eq. ( 1 ) of the model shows that the primary production variation is controlled by the nutrient Si and affected by water temperature; that the main factor controlling the primary production is Si; that water temperature affects the composition of the structure of phytoplankton assemblage; that the different populations of the phytoplankton assemblage occupy different ecological niches for C, the apparent ratio of conversion of silicate in seawater into phytoplankton biomas and D, the coefficient of water temperature‘s effect on phytoplankton biomass. The authors researched the silicon source of Jiaozhou Bay, the biogeochemical sediment process of the silicon, the phytoplankton predominant species and the phytoplankton structure. The authors considered silicate a limiting factor of primary production in Jiaozhou Bay, whose decreasing concentration of silicate from terrestrial source is supposedly due to dilution by current and uptake by phytoplankton; quantified the silicate assimilated by phytoplankton, the intrinsic ratio of conversion of silicon into phytoplankton biomass, the proportion of silicate uptaken by phytoplankton and diluted by current; and found that the primary production of the phytoplankton is determined by the quantity of the silicate assimilated by them. The phenomenon of apparently high plant-nutrient concentTations but low phytoplankton biomass in some waters is reasonably explained in this paper. 相似文献
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1 INTRODUCTION Terrestrial matter is continuously loaded into ocean by rivers and up taken by myriad organisms who would ultimately sink to the sea bottom, whichconstitutes a complete process of transferring terrestrial matter from land to sea. Among this dynamic process, diatoms are very important in theNo.1 YANG et al.: Silicon limitation on primary production and its destiny 73material cycle. Phytoplankton is a prime mover in the conversion from inorganic matter to organic in marine… 相似文献
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文章通过对地球的许多自然现象的研究, 首次提出“地球生态系统”理论, 阐述了地球生态系统的定义、结构、目标、内容和意义, 说明了地球生态系统的特征, 揭示了地球生态系统的变化过程和运行机制。通过“地球生态系统” 理论的应用, 充分阐述了地球生态系统的三大补充机制和北太平洋的生态动力。借助于地球生态系统的3 个生态子系统: 陆地生态系统、海洋生态系统和大气生态系统, 展示了硅的运行轨迹。在地球生态系统的三大补充机制理论指导下, 预测了地球未来的气候模式。 相似文献
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Silicon limitation on primary production and its destiny in Jiaozhou Bay, China V: Silicon deficit process 总被引:1,自引:0,他引:1
Silicon is a necessary nutrient for diatoms, silicon uptake in diatom reproduction decreased seawater silicon content. This paper clarified the characteristics of silicon transferring in the sea, which plays an important role in phytoplankton growth, zooplankton graze and marine ecosystem. Analysis revealed that silicate is supplied by terrestrial sources, through plankton uptake, death, and eventually deposits to the sea bottom, and cannot diffuse upward. This is a general silicon deficit process. Many global marine waters showed the same silicon transfer route: land→silicon biogeochemical process→sea bottom. River flow brings abundant silicate into marine waters, silicate concentration in the waters decreased in the distance away from the river estuaries. In discussion of silicon characteristics and its transfer route, it was considered that the main factor controlling the mechanism of diatom and non-diatom red tides occurrence is silicon, and the changes in silicon source. Human activities, such as sea-route cutting by building embankment and dam, and silicon supplement by the sea, such as sandstorm, rainstorm and storm tide, have largely impaired the earth ecosystem and hugely threatened the human existence. It is suggested in this paper that man should resume the original face of the Si input into the sea to keep natural ecosystem in sustainable pattern. 相似文献
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针对传统道路提取方法应用于新数据泛化能力不足的问题,研究了通过特征迁移和编解码网络实现跨数据域的道路提取方法。首先,构建了基于编解码网络的道路提取基本模型,用于实现单一数据来源的道路提取任务。然后,基于道路提取网络结构和循环一致性原则,提出了用于跨数据域图像特征迁移的循环生成对抗网络,使目标域图像映射入源域特征空间。使用预训练的道路提取模型处理特征迁移后的目标域图像,即可实现跨数据域道路提取任务。试验结果表明,本文所提方法能够拓展道路提取网络的泛化能力,准确有效地提取跨数据域图像中的道路目标。相较于未特征迁移的结果,本文所提方法大幅改善了道路提取指标,使得F1提升了50%以上。本文方法不需要目标域的标注信息,也不需要对道路提取网络进行微调训练,而只需训练由目标域向源域的特征迁移模型,所耗时间和人力成本较低,因而具有良好的应用价值。 相似文献
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CDntnbutionNo.3236fromtheInstituteofthenology,ChinaseAcadeInyofSdenas.KeyprojeCt396MandProjeCt4M76274supp0rtedbyNSFC,andabosupportedbypnsident'sboofCh1nereAedernyofSdenas.IwnODUruONThemonsoonisacirculationfeaturethatisplanetaryinscaleandhasanidentiliablesignalregardingitSsubsequentintensitysomeninemonthspriortotheaCtivestageofthesummrmonsoon(WbsterandYang,l992,Vemekar,l994).Furthertnre,thernagnitudeofthemons00n'svariabilityissubstantialandidentifiableoveralargearmindudingthePadficd… 相似文献
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营养盐限制浮游植物的生长是近年来国际研究的热点。探讨了目前营养盐限制的判断方法,认为仅靠氮和磷比值来得到磷限制或氮限制的结论是不完善的。根据营养盐限制的判断方法和法则,对长江口水域进行综合分析,认为在长江口及其附近海域,磷不是浮游植物生长的限制因子,而且氮、磷的浓度值都高于限制浮游植物生长的阈值,满足浮游植物的生长。通过1985年8月至1986年8月的长江口调查数据分析,发现从长江河口到远海水域的有些断面上,磷酸盐浓度并不一定离岸越远越低,且也没有周期性的季节变化。因此,尚须对河口区磷酸盐来源作进一步研究。 相似文献
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