卤虫的发育与蜕皮   总被引：2，自引：0，他引：2  

廖承义  欧毓麟  程樱 《中国海洋大学学报(自然科学版)》1990,(2)

我国北方孤雌生殖卤虫在盐度为60,水温为19—28℃的条件下,自卵内孵出无节幼虫长成至性成熟产仔(无节幼虫或卵),需经蜕皮12—15次,其中多数为14次,历时15—18天,随后每次产仔即行蜕皮一次,本文描述了卤虫各个不同令期发育的外部形态变化,并根据其蜕皮次数和形态特征,将卤虫的发育分为十五令(15th instar)。此外还观察到在孤雌生殖的卵中有发育成为雄性的个体。  相似文献   

黑鲷早期鳞被的形成     

丁彦文  李加儿  区又君 《热带海洋学报》1991,(3)

黑鲷Sparus macrocephalus(Basilewsky)幼苗鳞被最早出现的部位是在躯干部胸鳍基后至肛门直上方的侧线处。黑鲷只具一个鳞被起始中心。最早出现鳞片的个体为体长9.5—14.1mm,平均11.51±0.85mm,全长11.2—16.5mm,平均13.65±1.01mm,孵后日龄23—35d。鳞被发育完全时的最小个体为体长12.1—18.5mm,平均14.57±1.55mm,全长14.8—23.5mm,平均17.99±2.17mm,孵后日龄27—42d。  相似文献   

The effects of sediment from an industrial outfall area on a marine planktonic ecosystem     

Wu Jinping 《海洋学报(英文版)》1990,9(1):151-158

-Sediment from Xiamen industrial area was added to marine ecosystem enclosures to test the effects on the planktonic communities in Xiamen Bay, China, in April, 1985. Sediments were added at two concentrations, 11.2 and 112 ppm dry wt. respectively. The species of phytoplankton did not change as compared with the control, but the number of diatoms markedly decreased in the sediment treated enclosures. A suppression of photosynthesis was presumed to be due to light attenuation by the added sediment. Microflagellates, zooplankton and bacteria were resistant to sediment increase in water column.  相似文献   

The ionospheric eclipse factor method (IEFM) and its application to determining the ionospheric delay for GPS   总被引：4，自引：1，他引：3  

Y. Yuan  C. C. Tscherning  P. Knudsen  G. Xu  J. Ou 《Journal of Geodesy》2008,82(1):1-8

A new method for modeling the ionospheric delay using global positioning system (GPS) data is proposed, called the ionospheric eclipse factor method (IEFM). It is based on establishing a concept referred to as the ionospheric eclipse factor (IEF) λ of the ionospheric pierce point (IPP) and the IEF’s influence factor (IFF) . The IEF can be used to make a relatively precise distinction between ionospheric daytime and nighttime, whereas the IFF is advantageous for describing the IEF’s variations with day, month, season and year, associated with seasonal variations of total electron content (TEC) of the ionosphere. By combining λ and with the local time t of IPP, the IEFM has the ability to precisely distinguish between ionospheric daytime and nighttime, as well as efficiently combine them during different seasons or months over a year at the IPP. The IEFM-based ionospheric delay estimates are validated by combining an absolute positioning mode with several ionospheric delay correction models or algorithms, using GPS data at an international Global Navigation Satellite System (GNSS) service (IGS) station (WTZR). Our results indicate that the IEFM may further improve ionospheric delay modeling using GPS data.  相似文献   

Ammonium regeneration in intertidal sediments of the Yangtze estuary during air-exposure     

L.J. Hou  M. Liu  J.J. Lu  S.Y. Xu  D.N. Ou  Y. Yang  D.G. Zheng 《Environmental Geology》2006,49(7):937-945

The influences of exposure to the atmosphere on ammonium cycle in the intertidal surface sediments were in situ studied with a geochemical approach at a typical station in the Yangtze Estuary during three tidal cycles in September 2003. During an about 8-h emersion period of each diurnal tide, six high-resolution vertical profiles of adsorbed and dissolved ammonium were measured. It was observed that both adsorbed and dissolved ammonium generally had an increasing trend in sediment cores during the exposure. The rate of ammonium regeneration in sediments was estimated using the accumulation amount of ammonium including adsorbed and soluble fractions during the daytime emersion. The calculation result showed that there was relatively high ammonification rate (˜500 nmol N cm⁻³ day⁻¹), which reflected that organic nitrogen in sediments was quickly decomposed with a residence time of ˜52.7 days. Due to the dramatic temperature difference observed in sediment profiles, free convection was considered an important mechanism of regulating the efflux of produced ammonium into overlying waters. The total estimated amount of regenerated ammonium was ˜1.35×10⁵ t N year⁻¹ in the intertidal flat of the Yangtze Estuary, which occupied 7.6% of the total inorganic nitrogen annually transported to the estuarine ecosystem.  相似文献   

永城煤矿区矿井经济环境价值综合评价     

刘金平张幼蒂  王明明 《中国煤田地质》2005,17(2):40-42

在初步估算永城煤矿区的环境成本的基础上，对该矿区某矿井经济环境综合价值进行了评价和分析。当考虑矿区煤炭环境成本时，煤炭资源开采的净现值变小，该矿井煤炭资源开采的经济环境综合价值变小。进一步计算了不同环境成本和贴现率时的净现值，为动态决策服务。  相似文献   

中国西南部强震带大震复发机制     

安欧 《地震研究》1997,20(4):378-385

我国西南部鲜水河断裂带、红河断裂带、安宁河断理解带和龙门山断裂带四个测区内，用Ｘ射线法 得的宏观残余应力场和用震源机制解Ｐ轴显示的发震时现今应力场的水平最大主压应力方向基本吻合。这种叠加应力场的水平最大主压力分布方向与发震断裂带总体走 交角约为４０－５５°左右，使断裂带易于发生剪切错动。宏观残余水平最大剪应 值区的分布，也与区内大震震中的分布基本吻合，岩石裂面在３００℃和３００ＭＰａ围压下经１０天  相似文献   

Spatial-temporal Frame,Evolution and Mineralization of the Northern Qilian Metallogenic Province   总被引：1，自引：0，他引：1  

Sun Haitian  Wu Jieren  Li Jinping Institute of Mineral Deposits  Chinese Academy of Geological Sciences  Beijing Xi''an Institute of Geology  Mineral Resources  Chinese Academy of Geological Sciences  Xi''an  Shaanxi Institute of Mineral Deposits  Chinese Academy of Geological Sciences  Beijing 《《地质学报》英文版》1997,71(2):204-216

Four metallogenic epochs occurred in different tectonic environments during theevolution of the Northern Qilian metallogenic province through the geological time. The Mid-dle Proterozoic metallogenic epoch witnessed the tectonic environment of crustal breakupcaused by mantle diapirism, in which ultramafic-mafic rocks were intruded along beep faultbelts and the superlarge Jinchuan magmatic Cu-Ni sulphide deposit was formed. In theMiddle-Late Proterozoic metallogenic epoch the crust was further broken to form anintracontinental rift, in which the Chenjiamiao style massive Cu-Fe sulphide deposits hosted bybasic volcanic tuff were formed in the lower volcano-sedimentary sequence, while the largesedex type Jingtieshan style Fe-Cu deposits were formed within the upper abyssal carbon-richargillaceous sedimentary sequence. The Early Palaeozoic saw the aulacogen environment, with-in which the Baiyinchang style superlarge massive base and precious metal sulphide depositshosted by quartz keratophyric tuff were formed in the Middle-Late Cambrian rifted island arcand the massive Cu-Zn sulphide deposits and magmatic chromite deposits associated with theophiolite suite were formed in the Early-Middle Ordovician, and the Honggou style massiveCu-Fe sulphide deposits hosted by spilite were formed in the Late Ordovician back-arc basinenvironment. In the Late Palaeozoic-Meso-Cenozoic, the metallogenic province went into anintracontinental orogenic stage characterized by compressive tectonic environment, in whichthere occurred carbonate-quartz vein type and tectono-alteration gold deposits associated withductile-shear structures.  相似文献   

陕西粮食供需平衡的思考          下载免费PDF全文

颜胜安  何晓嫒 《山西气象》2004,(4):21-24

证券营业部计算机房和计算机网络的雷电防护是一个庞大而又复杂缜密的工程，电力保护、信号保护、等电位连接和各种接地中任何一个环节疏漏都可能带来灾难性后果。据统计，近年来因受雷电电磁脉冲而损失的计算机网络设备大幅上升，造成难以估算的经济损失。如1996年6月6日，重庆市农业银行大厦的计算机网络设备，因遭雷击损失107万元，其下属的信托公司证券部通信网络中断数小时，引起股民恐慌。  相似文献   

闽东干旱概况及夏季人工增雨作业天气形势分析     

陈德汶  王金萍  林友爱  刘锐志  陈安芳 《气象科技》2005,(Z1)

对闽东干旱的成因和干旱的环流形势进行了探讨,着重分析了夏旱期间人工增雨作业的天气形势以及不同形势、不同云型下的降水情况。结果表明:闽东干旱的形成与大型环流形势、地理因素、土壤植被等有关,平均而言,沿海干旱明显多于内陆山区;夏季发生干旱的机率最大而且强度级别高,西太平洋副热带高压是致旱的主要天气系统;在夏季,台风型(T)、弱流场型(R)是进行人工增雨作业的优势天气型,Cb、Cu、Sc云是开展人工增雨作业比较适合的作业云。这些结果为夏旱期间开展人工增雨作业提供了理论依据。  相似文献