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951.
The 3-D spatial distributions of vegetation are of great significance for water and soil conservation but are rarely concerned in literatures. The live vegetation volume (LVV) was used to relate to water/soil loss under 144 natural erosive rainfall events from 2007 to 2010 in a typical water-eroded area of southern China. Quadratic polynomial regression models were established for five pure tree (Pinus massoniana Lamb) plots between LVV and water (rtmoff)/soil conservation effects (RE/SE). RE/SE corresponds to the ratios of runoff depth/soil loss of the pure tree plots to that of the control plot under each rainfall event. Increasing LVV exhibits descending (DS), descending-ascending (DA), ascending-descending (AD), and ascending (AS) trends in the LVV-RE and LVV-SE curves. The effects of soil conservation on the plots were generally more noticeable than the effects of water conservation, and most of the RE and SE values reflected the positive effects of water and soil conservation. The effects were mainly positive under heavy rains (e.g., rainfall erosivity, R = 140 MJ mm ha-l h, maximum 30 min intensity, I30 = 16 mm h-l), whereas the effects were mainly negative under light rains (e.g., R = 45 MJ mm ha-1 h, I30 = 8 mm h-l). The trees' water/soil conservation effects notably transformed when rainfall erosivity and intensity were lower than the positive or negative effects to a certain threshold. About 50% rainfall events led to obvious transform effects when LVVs were near 0.5 or 0.6. These results are able to aid in the decision making on the forest reconstruction in water-eroded areas.  相似文献   
952.
西藏打加错南北向地堑系处于冈瓦纳大陆北缘,地堑系总体延伸方向(175~190°),延伸长度>50 km,延伸宽度5~15 km.根据该地堑构造带内发育的鱼鳞山组(N2Qy)玄武岩测年结果以及地堑构造带内发育的活动温泉,判断该地堑构造活动时期早于13.43 Ma,现今仍在强烈活动.在打加错地堑系东西两侧的地垒中共发现5处金属矿(化)点,各矿(化)点与中酸性岩体活动及近SN断裂构造有密切关系,特别是近南北向展布的中酸性小岩体更易形成斑岩型铜矿.  相似文献   
953.
The Qinghai-Tibet Plateau plays a very important role in studying severe weather in China and around the globe because of its unique characteristics. Moreover, the surface emissivities of the Qinghai-Tibet Plateau are also important for retrieving surface and atmospheric parameters. In the current study, a retrieval algorithm was developed to retrieve the surface emissivities of the Qinghai-Tibet Plateau. The developed algorithm was derived from the radiative transfer model and was first validated using simulated data from a one-dimensional microwave simulator. The simulated results show good precision. Then, the surface emissivities of the Qinghai-Tibet Plateau were retrieved using brightness temperatures from the advanced microwave-scanning radiometer and atmospheric profile data from the moderate resolution imaging spectroradiometer. Finally, the features of the time and space distribution of the retrieved results were analyzed. In terms of spatial characteristics, a spatial distribution con- sistency was found between the retrieved results and surface coverage types of the Qinghai-Tibet Plateau. In terms of time characteristics, the changes in emissivity, which were within 0.01 for every day, were not evident within a one-month time scale. In addition, surface emissivities are sensitive to rainfall. The reasonability of the retrieved results indicates that the algorithm is feasible. A time-series surface emissivity database on the Qinghai-Tibet Plateau can be built using the developed algorithm, and then other surface or atmospheric parameters would have high retrieval precision to support related geological re- search on the Qinghai-Tibet Plateau.  相似文献   
954.
抑螺防病林建设中生物材料的筛选及抑螺机理研究进展   总被引:1,自引:0,他引:1  
血吸虫病是一种严重危害人们身体健康的重大传染病,林业血防生态工程建设是防治血吸虫病的有效手段,生物材料的筛选是林业血防建设的重要环节。阐述了抑螺防病林建设中生物(植物、微生物)材料筛选及研究进展,并从钉螺生理响应和解剖结构等方面系统分析了生物材料抑螺机理。  相似文献   
955.
综合不同的泥石流评价因子对泥石流危险性进行了研究,利用地理信息系统( GIS)来计算潜在的泥石流危险区域。选取虹口乡高原村与庙坝村共处坡面为研究区域,在ArcGIS中生成研究区域的坡面立体图。选取适当的评级指标,确定了流域内主要的泥石流影响因子。采用层次分析法得出各主要因子的权重值,将各因子划分为五个不同等级,并分别对各个因子进行数值化和归一化处理。利用ArcGIS形成各评价因子专题层,再分别给不同评价栅格赋权重值,最终运用叠置分析与插值分析得出研究坡面的不同色带所表示的危险等级区划图,从而实现单坡面泥石流危险性的评价。  相似文献   
956.
针对我国特种行业的管理现状,提出一种结合GIS和物联网的特种行业管理信息系统的概念,阐述该系统的体系架构、主要功能模块及系统所涉及的三网融合、室内三维建模、智能GIS分析等关键技术,并重点介绍GIS技术和物联网技术在特种行业自动化、网络化、数字化管理方面的重要应用。  相似文献   
957.
彭丕洪  郭先春  马霞 《北京测绘》2013,(1):44-46,54
多边形拓扑重建是城市地图更新建库工作中关键性的一步,针对MapStar中拓扑重建的存在的问题,笔者采用MapGIS建拓朴,MapStar赋属性两者相结合的一种方法,能快速完成的多边形拓扑关系的重建,提高建库速度,实验证明,采用此方法,在城市地图更新建库工作过程中可提高30%-40%的工作效率。  相似文献   
958.
本文采用基于决策树的人工智能方式,通过对点云数据分割、提取分割片轮廓,手动设置地物的约束条件来提取LiDAR点云中的地物。两组实验表明,本文的方法能够成功提取点云数据中的建筑物、车辆等地物;要提高精度,需增加点云密度,因此本文方法适用于较平坦的城镇地区。  相似文献   
959.
An unprecedented heavy rainfall event occurred in Henan Province, China, during the period of 1200 UTC 19 -1200 UTC 20 July 2021 with a record of 522 mm accumulated rainfall. Zhengzhou, the capital city of Henan, received 201.9 mm of rainfall in just one hour on the day. In the present study, the sensitivity of this event to atmospheric variables is investigated using the ECMWF ensemble forecasts. The sensitivity analysis first indicates that a local YellowHuai River low vortex (YHV) in the southern part of Henan played a crucial role in this extreme event. Meanwhile, the western Pacific subtropical high (WPSH) was stronger than the long-term average and to the west of its climatological position. Moreover, the existence of a tropical cyclone (TC) In-Fa pushed into the peripheral of the WPSH and brought an enhanced easterly flow between the TC and WPSH channeling abundant moisture to inland China and feeding into the YHV. Members of the ECMWF ensemble are selected and grouped into the GOOD and the POOR groups based on their predicted maximum rainfall accumulations during the event. Some good members of ECMWF ensemble Prediction System (ECMWF-EPS) are able to capture good spatial distribution of the heavy rainfall, but still underpredict its extremity. The better prediction ability of these members comes from the better prediction of the evolution characteristics (i.e., intensity and location) of the YHV and TC In-Fa. When the YHV was moving westward to the south of Henan, a relatively strong southerly wind in the southwestern part of Henan converged with the easterly flow from the channel wind between In-Fa and WPSH. The convergence and accompanying ascending motion induced heavy precipitation.  相似文献   
960.
利用1961—2017年中国地面观测站日降水资料、全球大气多要素和海表温度月资料,分析华南区域持续性强降水过程的气候特征,诊断并比较与华南前汛期、后汛期区域持续性强降水年际变化相关的大气环流和海表温度异常特征。结果表明,3—12月华南都可能出现持续性强降水过程,其中汛期4—9月的占了94.4%。伴随着区域持续性强降水的年际变化,华南本地垂直上升运动显著异常是前汛期和后汛期的共同点,但前汛期、后汛期在华南及周边环流异常、水汽输送来源以及海温异常分布等方面都存在一定差异。在前汛期华南区域持续性强降水偏重年,赤道西太平洋区域海温偏低,由于大气罗斯贝波响应使西太平洋副热带高压偏强,热带西太平洋向华南区域水汽输送加强,从而有利于区域持续性强降水偏重。后汛期华南区域持续性强降水偏重年的海温异常分布是赤道中东太平洋区域正异常、东印度洋至西太平洋暖池区负异常,海温异常通过西北太平洋副热带高压、南海热带季风强度、水汽输送和垂直环流等多方面,导致后汛期区域持续性强降水偏重。   相似文献   
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