L5载波的信号质量分析

增加第三民用频率L5载波是GPS现代化措施中的一项,目前美国已经有4颗卫星具有L5观测值。从L5的信号结构上进行分析,应用L5载波的实际观测数据,与L1载波和L2载波相比较,L5载波不但在信噪比上得到提高,而且其多路径效应的影响也比较小,具有较好的数据观测质量。     

多频电离层残差法用于周跳的探测与修复

周跳的探测与修复是高精度GNSS定位的核心问题,随着GNSS现代化的逐步实施,L5载波观测值的增加给周跳的探测提供了一种新的方法。文中结合三频组合观测值的一些特性,提出一种多频电离层残差法用于周跳的探测与修复。实验表明,文中方法不仅能探测出双频条件下不能探测出的一些特殊周跳组合,还可以单历元间直接解算得到单个频率上的周跳值。     

大叶藻形态及生长发育特征

对威海双岛湾大叶藻的形态及生长发育特征进行了实地观察和精细解剖研究。结果表明, 大叶藻的形态特征主要表现为: 营养枝具4～8 片叶, 互生, 具管状叶鞘, 叶片线型; 根状茎匍匐于底泥; 每节生两簇不定根; 雌雄同株异花, 佛焰苞花序, 两雄一雌单性无花被花交互排列于花序轴两侧, 花粉胶质丝状; 瘦果。其主要生长发育特征表现为: 叶和节间的基部具有分生组织, 叶和节间生长主要体现为基部的生长; 腋芽的发育具有明显的窗口期; 先出叶先于侧枝萌发; 实生苗或克隆分株的端枝经过近一年的生长分化为成生殖枝, 开化结果后即死亡; 同一花序内的雌花先于雄花开放, 水中受精, 果实败育率较高。大叶藻营养、生殖器官形态结构的特化和它们生长发育的时序优化充分体现了该种对海洋水生环境的高度适应性。     

黄渤海典型鳗草海草床重金属生态风险评估

为全面了解我国黄渤海鳗草(Zostera marina L.)床重金属污染水平, 本研究以大连林阳北海、葫芦岛兴城、唐山乐亭-曹妃甸和青岛湾四处鳗草床为研究对象。于夏季采集鳗草、海水和沉积物样品并分析其重金属(Cu、Zn、Pb和Cd)含量。以此分析海草的重金属富集特征, 并对比评估不同鳗草床重金属潜在生态风险。结果表明, 夏季四处鳗草床海水重金属含量由高到低依次为: Zn > Cu > Pb > Cd, 均低于国家一级水质标准; 对沉积物来说, 重金属含量由高到低依次为: Zn > Pb > Cu > Cd, 均低于国家一级沉积物质量标准。鳗草对重金属的富集因重金属种类和海草积累部位而异, 其地上组织对Cu、Zn、Cd的富集能力高于地下组织。研究区域海水中Cu、Zn、Pb和Cd潜在风险等级均处于低风险水平。而对沉积物而言, 葫芦岛兴城鳗草床Cd的潜在风险等级处于较高风险水平(E_i值为156.9)。唐山乐亭-曹妃甸和青岛湾鳗草床的地质累积指数(I_geo)由大到小依次为: Cd > Pb > Zn > Cu。综合所有元素的潜在生态风险指数(I_R), 葫芦岛兴城鳗草床的潜在生态风险值最高。     

牙鲆病原秦皇岛弧菌的血清型及荧光抗体检验

用分离于病(死)牙鲆(Paralichthys olivaceus L.)的一种新病原弧菌——秦皇岛弧菌(Vibrio qinhuangdaora sp.nov.)的代表菌株(HQ010712-1株),分别制备全菌(OK)及热处理(121℃作用1h)的菌体(O)免疫原,强化免疫接种家兔制备相应抗血清,对供试12株秦皇岛弧菌进行了血清型检定,结果表明均存在同种的K抗原和同种的O抗原(血清同源),其中O抗原具有强免疫原性、K抗原的免疫原性弱但具有强O凝集抑制作用;以相应OK抗血清为第一抗体,以标准的羊抗兔IgG荧光抗体为第二抗体,对12株秦皇岛弧菌的纯培养物及用代表菌株(HQ010712-1)人工感染病死牙鲆的肝组织进行了间接荧光抗体染色,结果显示了特异的荧光反应。     

梯度淹水胁迫下全日潮海区秋茄幼苗的生长和生理反应

以秋茄(Kandelia candel L.Druce)幼苗为材料,在全日潮海区广西英罗湾开展为期5个月的野外梯度淹水胁迫实验。3座平台作为重复,每座设置8个梯度,相邻高程组间的高度相差10cm。实验5个月后测定幼苗的生长状况和一些生理指标。结果表明:秋茄幼苗的生长高度、节数、叶数和大根数这4个外部形态特征指标的最大值均出现在360cm高程组。生长高度、节数、叶数的曲线较为一致,幼苗大根数的略有不同,但总体上可看出太低的高程均不利于这4个指标的增长。叶面积对淹水胁迫的反应与叶数一致,但高程组之间的差异更大。叶绿素含量则表现长时间淹水胁迫促进含量增高。在任一高程组,秋茄幼苗各新生器官生物量分配均表现为:茎>根>叶。各新生器官及全株生物量的最大值出现在360cm高程组,它们的干重曲线表现比较一致。幼苗根系中的活性氧清除酶类活性均高于叶片。根系中SOD酶和POD酶的分布规律较为一致,都以360cm高程组的活性最高。叶片中SOD酶和POD酶的变化则相反,叶片SOD酶随高程增大而降低,POD酶则随高程增大而增大。根系中活性氧清除酶类活性的水平与幼苗全株生物量的关系均呈显著相关,叶片中的则无此相关性。360cm及以上高程组幼苗全部存活,较低高程组有部分死亡。综合本文实验结果,可初步判断北部湾沿海秋茄造林的滩涂高程不宜低于当地平均海平面。     

A new orbit for comet C/1858 L1 (Donati)

A new orbit for comet C/1858 L1 (Donati), based on 1036 observations in α and 971 in σ made between 7 June 1858 and 5 March 1859, is calculated using iteratively reweighted least squares. Residuals were weighted by the Welsch weighting function. The orbit represents a high eccentricity ellipse, e = 0.996265, with large semi‐major axis, a = 154.8612 AU, and long period, P = 1927.22 yr. The residuals are relatively random, a 10.7% chance of being random, but with a slight indication of possible nongravitational forces influencing the motion. The comet will not return until the year 3759, when it will pass 0.8442 AU from the Earth. (© 2014 WILEY‐VCH Verlag GmbH & Co. KGaA, Weinheim)     

川蔓藻在湖泊水位重建和环境变化研究中的应用

沉水被子植物川蔓藻广泛分布于海湾、泻湖、河口湿地以及内陆湖泊、沼泽、湿地中,是水生动物重要的食物和栖息地,具有改善水质和保护堤岸的作用。由于川蔓藻只能在小于0.5~4m深的浅水环境中生存,因此原地保存在湖泊沉积物中的化石种子可作指示古湖水深的定量指标。该项指标在闭流型湖泊水位重建和气候变化研究中有着不可忽视的重要作用。科学管理川蔓藻,对水体环境的改善、海洋污染的治理和湿地生物多样性下降的缓解具有重要价值。     

Chronology of Early to Mid-Pleistocene sediments in the northern North Sea: New evidence from amino acid and strontium isotope analyses

Sediments deposited during glacial-interglacial cycles through the Early to Mid-Pleistocene in the North Sea are chronologically poorly constrained. To contribute to the chronology of these units, amino acid racemization (AAR) and strontium (Sr) isotope analyses have been performed on samples from four shallow borings and one oil well along a transect in the northern North Sea. D/L Asp (aspartic acid) values obtained through reverse-phase liquid chromatography in the benthic foraminiferal species Elphidium excavatum is focused on because of consistent results and a good stratigraphic distribution of this benthic species. For the Early Pleistocene, an age model for the well 16/1–8, from the central part of the northern North Sea based on Sr ages allows for dating of the prograding wedges filling the pre-Quaternary central basin. A regional calibration curve for the racemization of Asp in Elphidium excavatum is developed using published ages of radiocarbon-dated samples and samples associated with the previously identified Bruhnes/Matuyama (B/M) paleomagnetic boundary and a Sr age from this study. Based on all the available geochronological evidence, samples were assigned to marine oxygen isotope stages (MIS) with uncertainties on the order of 10–70 ka.Sr ages suggest a hiatus of <2 million years (Ma) possibly due to non-deposition or low sedimentation between the Utsira Formation (Pliocene) and the Early Pleistocene. An increase in sedimentation rates around 1.5 ± 0.07 Ma (∼MIS 51) may partly be due to sediment supply from rivers from the south-east and partly due to the extension of ice sheet around 1.36 ± 0.07 Ma from the Norwegian coast to the central North Sea. A possible basin-wide glaciation occurred around 1.1 Ma (∼ MIS 32) (upper regional unconformity/top of unit Q4 in this study), resulting in erosion and regional unconformity. Two interglacials in the Norwegian Channel have been dated: the Radøy Interglacial to 1.07 ± 0.01 Ma (possibly MIS 31, the ‘super interglacial’), and the Norwegian Trench Interglacial to 0.50 ± 0.02 Ma (possibly MIS 13). A massive till unit identified at the same stratigraphic level in all shallow borings may partly represent an extensive MIS 12 glaciation. This study shows that the combined use of amino acid racemization data and Sr isotope chronology can refine the chronological ambiguities of Quaternary North Sea sediments related partly to the impact of glacial processes.