干旱区不同土地利用方式下土壤呼吸日变化差异及影响因素

利用开路式土壤碳通量测量系统-LI-8100对塔里木河下游6种土地利用方式下土壤呼吸速率的日变化进行了野外定位测量,并就水热因子及土壤理化性质对土壤日呼吸速率差异的影响进行了分析。结果表明,梨园、弃耕地、棉田、人工林、草地和天然林土壤呼吸速率日变化均呈单峰曲线,土壤日呼吸速率差异显著。大气温度和土地利用方式是造成土壤日呼吸差异的主要因素,其中土地利用方式通过改变地表温度、土壤水分、电导率、pH、盐分含量及机械组成等影响土壤日呼吸速率。     

中国互联网用户增长的省际差异及其收敛性分析

进入21世纪以来,中国的互联网事业得到了飞速发展;但同时互联网发展的区域差异仍表现得十分明显。采用σ-收敛、β-收敛和俱乐部收敛3种分析方法,对1997~2008年期间中国(港澳台地区除外)互联网用户增长的收敛性进行了探析,并对影响互联网普及率的关键因素进行了条件β-收敛的检验。结果发现,中国互联网用户增长的省际差异变动存在着较为明显的σ-收敛和β-收敛。控制人均GDP、城镇化水平、基础设施水平、受教育程度、对外开放度、地理位置等变量后,地区间存在条件β-收敛。东、中、西三大区域存在着较为显著的俱乐部收敛趋势,收敛速度则表现为东部慢于中部,中部慢于西部。     

滑动最小二乘法求解地震波波动方程

本文首次将固体力学领域中的滑动最小二乘拟合法用于求解地震波波动方程.与有限差分法相比,该方法所采用的拟合思想使得解在全空间域更加连续,同时仍然保持高精度的特性;与有限元法相比,该方法绕过变分原理,经过算法的有限差分化之后,其所需的计算量及数据存储量均可大大降低.薄膜震动的数值算例表明了该方法的上述特点.最后,通过对几个模型的合成地震模拟试验,进一步证明了滑动最小二乘法用于波动方程数值模拟的可行性.     

太平洋双色鳗鲡(Anguilla bicolor pacifica)与其它3种鳗鲡的形态差异分析

通过传统形态学数据和框架结构数据相结合,应用方差、聚类、判别和主成分等4种多元分析方法,分析了太平洋双色鳗鲡与日本鳗鲡、美洲鳗鲡和花鳗鲡的形态差异。结果表明:(1)太平洋双色鳗鲡背鳍前端与臀鳍前端之间的垂线距离占全长的1.4%,属短鳍型鳗鲡。(2)太平洋双色鳗鲡与其它3种鳗鲡形态差异显著。在可数性状中,太平洋双色鳗鲡的总脊椎骨数显著小于日本鳗鲡,显著大于美洲鳗鲡和花鳗鲡,背鳍前脊椎骨数显著大于其它3种鳗鲡;在可量性状中,太平洋双色鳗鲡的吻长显著小于美洲鳗鲡和花鳗鲡,显著大于日本鳗鲡;在框架结构性状中,太平洋双色鳗鲡有6项性状与其它3种鳗鲡差异显著。(3)太平洋双色鳗鲡的背鳍起点与其它3种鳗鲡相比最靠后,背鳍起点在鳗鲡分类研究中可作为重要的框架结构定位点。本研究可为太平洋双色鳗鲡的合理引进和种质保护提供资料。     

1870-2011年全球海域SST变化趋势

利用来自英国气象局哈德莱中心(Met Office Hadley Centre)的海表面温度(Sea Surface Temperature, SST)资料, 对全球海域近140余年来SST的长期变化进行分析。研究发现:(1)1870—2011年期间, 全球大部分海域的SST表现出显著的逐年线性递增趋势, 在两极大部分海域、格陵兰南部海域呈显著的递减趋势, 仅在部分小范围海域及一些零星海域的SST无显著变化。近海的递增趋势强于大洋, 大洋西岸的递增趋势强于大洋东岸。(2)近140余年来, 整体上全球的SST以0.0038℃/a的速度显著增加, 其中1870—1910年表现出较为显著的递减趋势, 1910年至今表现出较强的递增趋势。(3)1870—1910年期间, 全球大范围海域的SST无显著变化; 呈显著递减的海域主要分布于东海、阿拉斯加半岛南部海域、北大西洋30°N附近海域、冰岛南部海域、南印度洋西风带海域、新西兰附近海域; 呈显著递增的区域较为分散。1910—2011年期间, 全球大范围海域的SST逐年显著递增, 在两极大部分海域呈显著的递减趋势。(4)1870—1960年期间, 两极的SST走势较为平缓; 1960—2011年期间, 南极尤其是威德尔海的SST表现出显著的递减趋势, 其中逐8月的递减趋势尤为强劲; 北极逐2月、逐5月的SST呈显著性递减, 逐8月呈显著性递增且趋势较为强劲, 达到0.0402℃/a, 逐11月的SST无显著变化。     

Sedimentation and morphological changes at Yuantuojiao Point,estuary of the North Branch,Changjiang River

The North Branch, separated by the Chongming Island, was once the main channel in the estuary of the Changjiang River. Reclamation and a decrease in runoff to the North Branch had led to the narrowing and shallowing of the channel. The Yuantuojiao Point is located at the intersecting point connecting the North Branch of the Changjiang River and the Jiangsu coastline. Erosion cliffs are developed between the typical silty-muddy tidal flat and the salt marsh occupied by Spartina alterniflorea, and this has changed rapidly over the past few years. The sediment grain size analysis results of the surficial and two core samples indicate that the Yuantuojiao Point tidal flat experienced continuous accretional processes. Based upon 137 Cs analysis results of the YT and YY Cores sampled from the tidal flat at the Yuantuojiao Point, the average sedimentation rate of the YT Core was 2.30 cm/a from 1963 to 2007, and 2.38 cm/a from 1954 to 2007 for the YY Core. The sedimentation rates of both core locations have declined since the 1960s corresponding to the seaward reclamation at the Yuantuojiao Point. The average sedimentation rates at the Yuantuojiao Point were similar to that of the silty-muddy tidal flat at the northern Jiangsu coast, but lower than that of the south of the Changjiang River Estuary. According to field morphological investigations from 2006 to 2008 on the salt marsh at the Yuantuojiao Point, cliffs retreated markedly by storm surges and disappeared gradually because of the rapid sedimentation on the silty-muddy tidal flat. The maximum annual retreat reached 10 m. The recent sedimentation and morphological changes of the Yuantuojiao Point tidal flat not only displayed the retreat of the salt marsh and the disappearance of cliffs, but also was accompanied by rapid sedimentation of the silty-muddy tidal flat and the salt marsh, indicating the responses to the tidal currents, storm surges, Spartina alterniflorea trapping sediments and large-scale reclamation. The sediment grain size and their trends, southward coastal flow, and sandspits of the longshore bars suggest that the main sediment source at the Yuantuoijao Point, estuary of the North Branch was possibly from the Changjiang River before 1958, since then, it has been from the south of the submarine radial sand ridges of the southern Huanghai Sea (Yellow Sea).     

甲壳动物精子生物学的研究进展(英文)

甲壳动物精子生物学的研究对于甲壳动物的人工繁育及遗传育种等工作有重要意义。本文归纳了甲壳动物精子生物学的最新研究进展,包括精子的形态结构、发生、活力、体外保存及顶体反应等方面,并对该领域今后的研究方向提出了展望。     

Effects of the Anthropogenic Activities on the Morphological Evolution of the Modaomen Estuary, Pearl River Delta, China

Owing to the intensive human activities, the Modaomen Estuary has been significantly modified since 1950s, which has resulted in considerable changes of hydrodynamics and morphodynamics in the area. In this paper, the effects of the anthropogenic activities on the hydrodynamics and morphological evolution in the estuary at different stages are systematically assessed based on the detailed bathymetric data and field survey. The results show that the human activities have caused the channelization of the enclosed sea area in the Modamen Estuary; fast seaward movement of the mouth bar with high siltation; expansion of the channel volume due to channel deepening. The paper also highlights the main hydrodynamic changes in the estuary, including the rise of the water level; the distinguishing changes of tidal range before and after the 1990s (decrease and increase respectively); as well as the increase of the divided flow ratio. It is found that reclamation is the main factor promoting the transition of nature of the estuary from runoff dominant to runoff and wave dominant, and sand mining activities are mainly to strengthen the tidal dynamic and to low the water level. The results provide useful guidance for better planning of the future developments in the estuary and further research in the area.     

双频载波相位求差法在周跳探测与修复中的应用

载波相位测量中小周跳的探测与修复一直是高精度GPS定位研究中的热点领域。分析了L1和L2载波相位观测值的关系,通过相邻历元的相位观测值求差来探测周跳,并结合伪距差分约束条件来确定及修复周跳。结合实例分析,证明该方法可以有效地探测并修复周跳,并通过Matlab编程实现了算法的程序化。     

Conus pennaceus: a phylogenetic analysis of the Mozambican molluscan complex

The genus Conus has over 500 species and is the most species-rich taxon of marine invertebrates. Based on mitochondrial DNA, this study focuses on the phylogenetics of Conus, particularly the pennaceus complex collected along the Mozambican coast. Phylogenetic trees based on both the 16S and the 12S ribosomal genes grossly revealed the same groupings: one that clustered the individuals from the north (Pemba, Nacala and Island of Mozambique), another that grouped the individuals from the central/southern coast (Pomene/Massinga and Inhambane) and a third that assembled the specimens from the central/southern islands (Bazaruto and Inhaca). The 16SrRNA-based trees further distinguished the northern group into a Nacala group and a Pemba+Island of Mozambique group. In all trees, C. p. bazarutensis and C. lohri collected on the central/southern islands grouped separately from the C. p. bazarutensis and C. lohri collected on the central/southern coast, suggesting a genetic similarity between these species. Likewise, C. praelatus revealed greater proximity to C. pennaceus from Pemba. Although different topologies were produced by each gene (low bootstrap support in some nodes), we support the hypothesis of a southward ancestral colonisation pattern, indicated by the 16SrRNA trees. The common ancestor would have shifted from planktonic to non-planktonic larval development and this weak vagility would have promoted the divergence between north and south specimens. Our results suggest that the separation of these groups might have been a relatively recent event, and part of the current morphological variability could be the outcome of phenotypic plasticity and/or ecological adaptation.