首页 | 本学科首页   官方微博 | 高级检索  
文章检索
  按 检索   检索词:      
出版年份:   被引次数:   他引次数: 提示:输入*表示无穷大
  收费全文   19篇
  免费   3篇
  国内免费   4篇
测绘学   1篇
大气科学   5篇
地球物理   6篇
地质学   1篇
海洋学   5篇
综合类   2篇
自然地理   6篇
  2022年   2篇
  2021年   2篇
  2020年   1篇
  2019年   2篇
  2018年   1篇
  2016年   2篇
  2013年   1篇
  2012年   1篇
  2011年   1篇
  2010年   1篇
  2009年   3篇
  2008年   4篇
  2007年   1篇
  2006年   1篇
  2003年   1篇
  1998年   1篇
  1994年   1篇
排序方式: 共有26条查询结果,搜索用时 15 毫秒
1.
土壤水分是沙区主要的生态限制因子,其分布受气候、地形和植被等众多因素的影响。以腾格里沙漠沙坡头地区3种类型的沙丘(固定沙丘、半固定沙丘和流动沙丘)为研究对象,利用方差分析和冗余分析(RDA)等方法对沙丘不同部位和不同深度土壤水分的分布特征及其与地形-植被因子之间的关系进行了综合分析。结果表明:(1) 不同类型沙丘上0~300 cm的土壤水分随着深度的增加而增加,表层土壤水分的波动程度大于中层和深层。(2) 固定沙丘不同部位及不同深度的土壤水分之间没有明显的差异,半固定沙丘和流动沙丘迎风坡与丘底的土壤水分高于背风坡和丘顶。(3) 固定沙丘上的土壤水分受地形-植被因子的影响较半固定沙丘和流动沙丘小,影响固定沙丘土壤水分的主要因子有坡向、高差和灌木多度。(4) 地形-植被因子与研究区绝大多数半固定沙丘和流动沙丘的土壤水分均有负相关关系。研究揭示了腾格里沙漠土壤水分的分布规律及其与地形-植被因子的关系,对制定相应的防风固沙措施以及建立科学合理的植物固沙模式有积极的指导作用。  相似文献   
2.
There is a pressing need to determine the relationships between driving variables and landscape transformations. Human activities shape landscapes and turn them into complex assemblages of highly diverse structures. Other factors, including climate and topography, also play significant roles in landscape transitions, and identifying the interactions among the variables is critical to environmental management. This study analyzed the configurations and spatial-temporal processes of landscape changes from 1998 to 2011 under different anthropogenic disturbances, identified the main variables that determine the landscape patterns and transitions, and quantified the relationships between pairs of driver sets. Landsat images of Baicheng and Tekes from 1998, 2006 and 2011 were used to classify landscapes by supervised classification. Redundancy analysis (RDA) and variation partitioning were performed to identify the main driving forces and to quantify the unique, shared, and total explained variation of the sets of variables. The results indicate that the proportions of otherwise identical landscapes in Baicheng and Tekes were very different. The area of the grassland in Tekes was much larger than that of the cropland; however, the differences between the grassland and cropland in Baicheng were not as pronounced. Much of the grassland in Tekes was located in an area that was near residents, whereas most of the grassland in Baicheng was far from residents. The slope, elevation, annual precipitation, annual temperature, and distance to the nearest resident were strong driving forces influencing the patterns and transitions of the landscapes. The results of the variation partitioning indicated complex interrelationships among all of the pairs of driver sets. All of the variable sets had significant explanatory roles, most of which had both unique and shared variations with the others. The results of this study can assist policy makers and planners in implementing sustainable landscape management and effective protection strategies.  相似文献   
3.
Late-glacial lake sediments containing the Laacher See Tephra (LST, 11 000 yr B.P.) have been analyzed for their pollen and diatom content at three sites at varying distances from the volcano and on different bedrock geologies. The aim was to test the null hypothesis that this major volcanic eruption had no effect on terrestrial pollen or aquatic diatom assemblages. The pollen spectra at all sites show a short-lived increase in grass pollen following the LST. Partial redundancy analysis and associated Monte Carlo permutation tests suggest, however, that the LST had no statistically significant effect at two sites but it had a statistically significant impact on the pollen assemblages at the site nearest (60 km) to the volcano.The diatom assemblages at the three sites changed individualistically after the LST deposition, with increases inAchnanthes minutissima at one site, an expansion ofAulacoseira species at another, and an increase ofAsterionella formosa andFragilaria brevistriata at the third site. Partial redundancy analysis and associated permutation tests suggest a statistically significant change in diatoms in relation to the LST and associated changes in sediment lithology at the one site situated on acidic bedrock. No significant impacts were found at the sites on volcanic or calcareous rocks. Due to the interaction between tephra and sediment lithology, it is not possible to conclude if the statistically significant diatom changes were a direct result of the LST deposition or an indirect result of lithological changes following LST deposition.This is the first paper in a series of papers published in this issue on high-resolution paleolimnology. These papers were presented at the Sixth International Paeolimnology Symposium held 19–21 April, 1993 at the Australian National University, Canberra, Australia. Dr A. F. Lotter and Dr. M. Sturm served as guest editors for these papers.  相似文献   
4.
5.
A self-organizing map (SOM) was used to cluster the water quality data of Xiangxi River in the Three Gorges Reservoir region. The results showed that 81 sampling sites could be divided into several groups representing different land use types. The forest dominated region had low concentrations of most nutrient variables except COD, whereas the agricultural region had high concentrations of NO3N, TN, Alkalinity, and Hardness. The sites downstream of an urban area were high in NH3N, NO2N, PO4P and TP. Redundancy analysis was used to identify the individual effects of topography and land use on river water quality. The results revealed that the watershed factors accounted for 61.7% variations of water quality in the Xiangxi River. Specifically, topographical characteristics explained 26.0% variations of water quality, land use explained 10.2%, and topography and land use together explained 25.5%. More than 50% of the variation in most water quality variables was explained by watershed characteristics. However, water quality variables which are strongly influenced by urban and industrial point source pollution (NH3N, NO2N, PO4P and TP) were not as well correlated with watershed characteristics.  相似文献   
6.
7.
利用2003年西苕溪TM数据和DEM模型计算了55个样点上游3种空间尺度下(亚流域、河岸带和局部)的土地利用类型,通过冗余分析筛选出能够在显著水平上最大程度解释西苕溪流域底栖动物分布的最小变量组合——氨氮、荫蔽度、电导率、亚流域农田百分比以及栖境复杂度.方差分解结果表明氨氮是研究区域影响底栖动物分布的最重要环境变量,亚流域尺度农田百分比也是一个重要影响变量.在50%-100%适合度范围内最终筛选得到短脉纹石蛾Cheumato-psyche sp.1和Cheumatopsyche sp.2作为关键环境变量指示种.在一定范围内短脉纹石蛾的数量随着水体氨氮浓度和亚流域尺度农田百分比的上升而增加.短脉纹石蛾分布广泛、采集容易、具备一定的耐污能力和主动漂流能力、幼虫个体较大且在水中的生活史较长以及具有一定的生态可塑性等优点决定了短脉纹石蛾可以作为西苕溪流域的受干扰水体氨氮和亚流域尺度农田百分比的指示种.  相似文献   
8.
为了探索高寒草甸土壤理化性质对海拔和坡向的响应及其与植被的关系,以东祁连山高寒草甸为研究对象,分析了7个海拔和2个坡向高寒草甸的土壤养分含量和生态化学计量比变化规律及其与植被的关系。结果表明:(1) 土壤含水量、电导率、有机碳、全氮、全钾、碱解氮、速效磷、速效钾含量、碳磷比(C/P)和氮磷比(N/P)随海拔的升高呈先升高后降低的趋势,土壤容重、全磷和碳氮比(C/N)呈先降低后升高的趋势。(2) 同一海拔,大部分海拔梯度阳坡的土壤土壤容重、速效钾、电导率和全磷高于阴坡,阳坡的土壤含水量、速效磷、C/P和N/P低于阴坡,海拔3200 m梯度以下阳坡的土壤有机碳、全氮、碱解氮和C/N低于阴坡。(3) 不同海拔和坡向的高寒草甸土壤C/N、C/P和N/P处于14.55~38.13、12.61~87.94和0.27~5.01之间。(4) 冗余分析(RDA)发现,土壤容重、全氮和速效磷是影响高寒草甸植被的关键土壤因子,聚类分析发现海拔3200~3400 m的阴坡和阳坡聚为一类。综上所述,东祁连山高寒草甸土壤养分和生态化学计量比随海拔和坡向的变化呈规律性变化,基于对N/P比的分析发现,该区域高寒草甸类草原的初级生产力主要受土壤氮限制且低海拔和高海拔区域尤为明显,基于聚类分析发现,海拔3000 m和3400 m是该区域草地植被和土壤特征发生变化的临界线。建议在高寒草甸类草原的管理过程中,应该充分考虑海拔和坡向的分异性特征。  相似文献   
9.
CINRAD/SA雷达日常维护及故障诊断方法   总被引:17,自引:6,他引:17  
胡东明  伍志方 《气象》2003,29(10):26-28
CINRAD雷达系统,具有完善的自动定标系统和可靠的故障自诊断系统,利用其“故障报警信息”和“RDA性能参数”,能够完成该雷达系统的日常维护任务;参照“RDA适配数据”,再配合简单的测量工具,可以实现故障的隔离和定位。  相似文献   
10.
介绍了对新一代多普勒天气雷达进行回波强度、速度、速度谱宽和空间位置等各项参数的标定和测试方法.  相似文献   
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号