排序方式: 共有53条查询结果,搜索用时 15 毫秒
1.
随着气候变化和人类活动对水资源影响越来越显著,大量水文序列的统计规律不再满足一致性要求而出现了变异。水资源日益重要的社会地位,要求在对水文变异进行检测的同时,需进一步量化影响其变异的因素,但目前归因分析的研究仍以定性或半定量为主。由于降雨和径流是水循环中关键的水文要素,且分别可以反映气候变化和人类活动对水资源的影响,利用降雨-径流关系提出了定量研究水资源变异的归因分析方法。结合乌力吉木仁河三级区1956~2000的年径流和年降雨序列,在对其分别进行变异诊断的基础上,定量地分析了造成该区水文变异的原因。计算结果表明:气候变化对乌力吉木仁河三级区水资源变异的贡献率为24%,而人类活动影响的贡献率为76%,可见人类活动是造成该区水资源变异的主要因素。 相似文献
2.
三峡库区大型的赵树岭滑坡区滑坡灾害极为发育。三峡工程蓄水后,水位上升导致原先许多非饱水的松散岩土体处于饱水状态,严重破坏了其稳定性。文章针对该滑坡区内广泛分布的松散岩土的基本类型和特点,设计了4种不同的浸泡环境,进行水-松散岩土相互作用的室内控制试验,通过监测阴离子浸出特征来揭示其化学变化规律。试验结果表明:在不同的pH值、不同的搅拌速度、不同的流速、以及同时改变pH值和搅拌速度的试验环境中,水岩化学作用所浸出的阴离子特征各异。研究结果可以为松散岩土-水化学作用机理研究提供资料,也对赵树岭滑坡体的工程治理具有重要指导意义。 相似文献
3.
应用特征光合色素研究东海和南海北部浮游植物的群落结构 总被引:23,自引:0,他引:23
应用高效液相色谱并结合二极管阵列检测器分析技术,研究了东海与南海北部典型断面浮游植物的光合色素组成,进而由CHEMTAX软件估算浮游植物群落结构。结果表明:东海断面浮游植物叶绿素a生物量大于南海北部断面。受海水层化结构影响,东海PN断面浮游植物群落结构形成上层和下层两种类型,上层以蓝藻为主要优势类群;下层以硅藻为主要优势类群。南海北部S断面浮游植物群落形成近岸与离岸两种类型,近岸以硅藻、隐藻、绿藻为主要优势类群;离岸以定鞭金藻、蓝藻、原绿球藻为主要优势类群。初步分析了研究海区浮游植物群落结构与环境因子的关系。 相似文献
4.
东、黄海典型海区分粒级浮游植物叶绿素a的周日波动及影响因子 总被引:3,自引:0,他引:3
本文分析了东、黄海典型海区3个测站在2000~2003年间4个航次的叶绿素a周日变动特征,结果表明由于地理环境、水文特征以及季节差异,各海区叶绿素a表现出各自不同的变动特点.在东海陆架区,日变化上表层各粒级主要以半日周期为主,受黑潮入侵程度不同而略有变化;长江口由于受到潮汐的影响,各粒级的日变化同潮汐的涨落相对应,主要为半日周期;黄海中部海区叶绿素a尤其是NANO级浮游植物在周日变化上以全日周期为主,受黄海冷水团强弱不同而不同.本文进一步应用渐近回归初步分析了多种环境因子对叶绿素a周日变化的影响. 相似文献
5.
Perciformes, the largest order of vertebrates with 20 suborders, is the most diverse fish order that dominates vertebrate
ocean life. The complete mitochondrial control region (CR) of Trichiurus japonicus (Trichiuridae, Scombroidei) and Pampus sp. (Stromateidae, Stromateoidei) were amplified and sequenced. Together with data from GenBank, the tandem repeats in the
mitochondrial CR from 48 species, which covered nine suborders of Perciformes, are reported in this study. The tandem repeats
tend to be long in the suborder Percoidei and Stromateoidei. The identical repeats in 21 species of Cichlidae suggest a common
origin and have existed before species divergence. Larimichthys crocea shows tandem repeats instead of the typical structure of the central conserved sequence blocks, which was first reported
in Perciformes and vertebrates. This might have resulted from interruption of the polymerase activity during the H-strand
synthesis. The four broader patterns presented here for the tandem repeats, including those in both the 5′ and 3′ ends, only
in the either 5′ or 3′ end, and in the central conserved domain of the control region, will be useful for understanding the
evolution of species. 相似文献
6.
松辽盆地三肇凹陷扶余油层(下白垩统泉 4段)储集层的渗透率平均值为1.53 × 10-3 μ m2,属于典
型的低渗透储集层。文中通过岩石铸体薄片、扫描电镜及 X衍射等技术,对三肇凹陷扶余油层储集层的岩石组
分、孔隙类型、成岩作用特征进行了识别鉴定。分析认为:储集层主要岩石类型为长石岩屑细砂岩和岩屑细砂
岩,成熟度较低;次生溶蚀孔隙提供了大量有效储集空间,所占比例甚至可达25%;储集层经历了压实、胶结、
交代、溶解、破裂等成岩作用,主要处于晚成岩阶段 A1期和A2期。压实、胶结作用等破坏性成岩作用使原生
孔隙遭到破坏,形成致密储集层;交代作用对储集层物性影响不大;溶解、破裂作用等建设性成岩作用使储集
层物性得到改善,形成次生孔隙发育带。孔隙度随深度增加呈逐渐增大趋势,与由有机质分解形成的酸性流体
使储集层中不稳定矿物发生溶蚀密切相关。这一研究对三肇凹陷低渗透储集层的开发具有指导作用。 相似文献
7.
为获得四川盆地及其邻区地壳和上地幔精细结构,并据此对该区域整体构造运动初步进行动力学解释,本研究采用接收函数、线性反演与H-kappa扫描相结合的方法,获得以下结论:研究区域地壳厚度东西向差异巨大,其厚度差高达29 km。四川盆地地表具有较厚沉积层,属于刚性块体。龙门山南段与四川盆地交接地区存在某些区域的波速比较高,推测这些地区可能存在地幔物质上涌导致地壳中铁镁质成分增加。松潘-甘孜地块的地壳厚度存在58~65 km的横向变化,中下地壳存在梯形低速层,可能由于青藏高原向东俯冲过程中遭遇四川盆地刚性块体的阻挡而引起该地块的挤压变形,该区域具有较高的波速比,综合分析推测其可能存在区域性的部分熔融。 相似文献
8.
Study on respiratory electron transport system (ETS) of phytoplankton in Taiwan Strait and Xiamen Harbour 总被引:1,自引:0,他引:1
Phytoplankton respiratory electron transport system (P-ETS) activities were studied in two cruises in Taiwan Strait (Aug. 1997 and Feb. -Mar.1998) and two cruises in Xiamen Harbour (Oct., 1997 and Apr.,1998). Results showed that P-ETS activity in the surface water of southern Yaiwan Strait in summer was homogeneous [mean value of 0.106 μ102/(L.h)], inhomogeneous in northern Yaiwan Strait in winter. Variation of P-ETS activity in middle part of the Strait was not obvious between summer and winter. Mean P-ETS activity of Xiamen Harbour in autumn was 0.255 μ102/(L.h) with a little higher value in Jiulong River estuary areas. In spring, P-ETS activity was more homogeneously distributed and the mean value was 1.076 μ102/(L.h). P-ETS activity in spring was obviously higher than in autumn in Xiamen Harbour. Vertical distribution of P-ETS in Taiwan Strait was homogeneous at some stations in winter and in summer. An obvious daily variation of P-ETS activity was recorded at Stn 9837, high at midnight and low in the early morning. Significant correlation between P-ETS activity and Chl-a was observed. Results also showed that the ratio of estimated respiratory rate to photosynthetic rate varied seasonally, high in winter (0.41) and low in summer (0.12). 相似文献
9.
The genome size(C-value) of an organism is referring to the DNA content of its non-replicated haploid chromosome complement,generally deduced from measuring somatic diploid nuclei.We presented genome size(C-value) data obtained by flow cytometry for four commercially important crabs(Portunus trituberculatus,Charybdis japonica,Scylla paramamosain,and Eriocheir sinensis) common in the coast of China.Gallus domesticus(2C=2.5 pg) was used as the internal standard.The results showed that the C-value for P.trituberculatus,C.japonica,S.paramamosain,and E.sinensis were(2.31±0.01) pg,(2.33±0.03) pg,(1.64±0.02) pg,and(2.29±0.03) pg,respectively.The C-value of P.trituberculatus,C.japonica and S.paramamosain were reported for the first time.The data represented by the four species indicated that they had lower DNA contents than average DNA values in crustaceans((4.99±0.48) pg),and three of the four values were very similar if not identical.The results provide useful data for future studies in the fields of biodiversity,species conservation,and phylogeny of these commercial crabs.They will also be helpful in instructing the hybridization breeding program and estimating the cost of the whole genome sequencing project. 相似文献
10.
末次盛冰期以来中国湖泊记录对环流系统及气候类型的响应 总被引:4,自引:1,他引:3
为了探讨中国长时间尺度湖泊时空演变规律和潜在的驱动机制,本文在柯本气候分区和中国季风—非季风区的划分基础上,对中国34个有明确数据的典型湖泊运行CCSM 3.0气候模拟系统和水量能量平衡模型模拟其水位变化,同时利用NCEP/NCAR再分析资料对中国按水汽输送划分的季风区进行验证。结果表明,末次盛冰期以来中国湖泊演化主要受千年尺度大气环流的驱动影响,在各个柯本气候区内没有明显的规律性。末次盛冰期以来,在季风区中国湖泊演化主要有早中全新世湖泊水位相对较高以及末次盛冰期和早全新世湖泊水位均较高2种演变规律;在东亚干旱区主要有中晚全新世期间湖泊水位相对较高以及末次盛冰期和中全新世湖泊水位均较高2种演变规律。本文为中国过去气候变化及湖泊演化机制研究提供新的证据,同时为人类全面认识末次盛冰期以来湖泊水位变化提供了新的视角。 相似文献