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661.
662.
POM模式边界条件的数值试验及其在环台湾岛海域风生流模拟中的应用 总被引:3,自引:0,他引:3
通过一个数值试验,对运用POM模式做风生流模拟时边界条件的选取方案做了初步的讨论。试验表明,POM“外模式”采用辐射边条件、“内模式”采用辐射方案的改进形式是一种可行的方法:如果用水位作为控制条件,也可以使用辐射边条件。文章同时给出了环台湾岛海域冬、夏风季生流的模拟结果。 相似文献
663.
采用响应面法对1株高产琼胶酶的南极海冰菌Pseudoalteromonassp. NJ21的发酵条件进行优化。首先分别以温度、pH、不同碳源、不同氮源、不同金属离子作为唯一变量进行单因素实验, 筛选出对酶活有显著影响的单因素取值范围; 参考单因素实验结果, 采用Plackett-Burman实验设计筛选出影响酶活主要因素, 再利用Box-Behnken设计及响应面分析法进行回归分析以确定最佳发酵条件。结果表明, D-甘露糖、蛋白胨、CaCl2和培养温度与酶活存在着显著的相关性, 通过求解回归方程得到Pseudoalteromonassp. NJ21的最佳培养基组成为D-甘露糖5.52g/L; 蛋白胨7.4g/L; CaCl25.84mmol/L; 最佳发酵温度为15℃; 优化后发酵液中琼胶酶酶活由3.5U/mL提高到25.76U/mL, 比优化前提高了6.36倍。 相似文献
664.
天津近岸台风暴潮漫滩数值模式研究 总被引:2,自引:0,他引:2
基于对POM(Princeton Ocean Model)模式的改进,采用Flather-Heaps干湿网格法和两重网格嵌套的数值计算格式,针对天津近岸海域的地形和易受风暴潮漫滩灾害侵袭的特点,建立了天津近岸海域三维动边界风暴潮漫滩模型,对天津近岸区域台风影响下的风暴潮漫滩进行了数值模拟研究。选取7203,8509,9216,9711号典型台风过程,计算了风暴潮漫滩水位变化,通过与塘沽站点实测数据的比较,计算的增水曲线过程与实测结果吻合较好,基本能够真实反映天津近岸的风暴潮水位变化情况及漫滩范围。研究结果验证了改进POM模式为动边界数值模型并应用于浅海区域是可行性的。 相似文献
665.
666.
森林防火地理信息系统的设计与开发 总被引:5,自引:0,他引:5
将GIS技术应用于森林防火,实现了C/S与B/S相混合的森林防火信息监测模式。以湖北森林防火系统为例,给出了系统软件结构、功能实现及数据库的设计,为实现基于GIS的森林防火系统提供参考。通过系统运行过程中的数据采集、历史数据累积,可以实现森林防火数据的分析、挖掘,为有效防治森林火灾提供重要途径。 相似文献
667.
WANG Deming 《《地质学报》英文版》2007,81(4):525-538
Zosterophyllum longa sp.nov.is reported from the Lower Devonian Pingyipu Formation, Jiangyou District,northern Sichuan of China.This new plant has vertically elongate sporangia differing from all known species of Zosterophyllum,demonstrating morphological variations in Zosterophyllophytina.New materials of Zosterophyllum yunnanicum from the Lower Devonian Xujiachong Formation,Qujing District,eastern Yunnan of China show that fertile axes of this species are anisotomous or pseudomonopodial or K-shaped in branching.Sometimes fertile lateral axes are very short and bear an axUlary axis at the dividing point.Distinct thickening occurs along the whole margin of a sporangium,with sporangial lobes undeveloped.The evolution of Zosterophyllum is tentatively discussed.A biostratigraphic method of Gerrienne and Streel is introduced and applied to dating of the Lower Devonian Xujiachong Formation,which is considered as of the late Pragian-early Emsian. 相似文献
668.
Feasibility of grain-size analysis methods for determination of vertical hydraulic conductivity of streambeds 总被引:4,自引:0,他引:4
Jinxi Song Xunhong Chen Cheng Cheng Deming Wang Susan Lackey Zongxue Xu 《Journal of Hydrology》2009,375(3-4):428-437
Accurate estimation of streambed vertical hydraulic conductivity (Kv) is of great importance in the analysis of water quantity exchange and solute transfer between a stream and its sediments. The paper analyzed the inaccuracy of hydraulic conductivity values of sediments derived from grain-size distribution (Kg), which were determined from eight empirical grain-size methods to represent streambed Kv. In this study, the values of Kv for a streambed were derived using falling-head standpipe permeameter tests conducted at eight study sites in the Elkhorn River, Nebraska, and the tested streambed columns were then collected for grain-size analysis by sieving. These empirical methods were used to calculate the Kg values of the streambed from grain-size distribution data of sediments. Unlike many other studies, this study verifies Kg from grain-size distribution with Kv from permeameter tests on the basis of the same samples of streambed sediments. The Kg values derived from the eight empirical methods were larger than the Kv from permeameter tests; there are five methods that give Kg values of about 3–6 times larger than these Kv. The Kg values from the Kozeny formula followed by the Hazen formula give the largest overestimation error if they are used to represent the Kv of the streambed. The USBR and Shepherd formulas generated Kg values close to Kv, but these Kg values are still larger in general than the Kv values. Moreover, the new values of coefficient C for the empirical formulas were revised so that they can be used to calculate the approximate Kv of a streambed. Among the eight methods, the ratios of the original C values to the average new C range from 1.3 to 5.9. It can be hypothesized that smaller C values must be used in the estimation of Kv for general soil samples if these empirical formulas are used to calculate Kv. 相似文献
669.
Peng Zhang Linlin Kou Yan Zhao Zhongwei Bi Deming Sha Renping Han Zhumin Li 《地学前缘(英文版)》2020,(2):547-563
TheWulong lode deposit contains over 80 tonnes of gold with an average grade of 5.35 g/t.It is one of the largest deposits in Dandong City,Liaoning Province in northeast China.Previous studies on the deposit focused on its geological characteristics,geochemistry,fluid inclusions,and the timing of gold mineralization.However,controversy remains regarding the origin of the ore-forming fluids and metals,and the genesis of the gold deposit.This paper presents zircon UePb and pyrite RbeSr ages and S,Pb,He,and Ar isotopic results along with quartz H and O isotopic data for all litho-units associated with the deposit.Laser ablation inductively coupled mass spectrometry measurements yielded zircon UePb dates for samples of pre-mineralization rocks like granite porphyry dike,the Sanguliu granodiorite,fine-grained diorite,and syn-mineralization diorite,as well as post-mineralization dolerite,and lamprophyre;their emplacement ages are 1261 Ma,1241 Ma,1231 Ma,1201 Ma,1192 Ma,and 1152 Ma,respectively.The pyrite RbeSr isochron age is 1191 Ma,indicating that both magmatism and mineralization occurred during the Early Cretaceous.The d18OH2O values of ore-forming hydrothermal fluids from the quartzepolymetallic sulfide vein stage vary from 4.8&to 6.5&,and the dDV-SMOW values are between67.7&and75.9&,indicating that the ore-forming fluids were primarily magmatic.The noble gas isotope compositions of fluid inclusions hosted in pyrite suggest that the ore-forming fluids were dominantly derived from crustal sources with minor mantle input.Sulfur isotopic values of pyrite vary between 0.2&and 3.5&,suggesting that S was derived from a homogeneous magmatic source or possibly from fluids derived from the crust.The Pb isotopic compositions of sulfides(207Pb/204Pb?15.51 e15.71,206Pb/204Pb?17.35e18.75,208Pb/204Pb?38.27e40.03)indicate that the Pb of the Wulong gold deposit is a mixture of crust and mantle components.Geochronological and geochemical data,together with the regional geological history,indicate that Early Cretaceous magmatism and mineralization of the Wulong gold deposit occurred during the rollback of the subducting Paleo-Pacific Plate,which resulted in lithospheric thinning and the destruction of the North China Craton(NCC),which indicates that the deposit is of magmaticehydrothermal origin. 相似文献
670.
乡村旅游的乡村性测评模型——以江西婺源为例 总被引:5,自引:1,他引:4
乡村性是乡村旅游的本质特性,对乡村性进行测评是乡村旅游可持续发展研究的基础,是指导乡村旅游开发、经营和管理的重要依据。本文采用定性与定量相结合的方法,通过理论分析选取了5个潜在因素和17个观测因子构建了乡村性测评的指标体系,运用结构方程原理,建立了乡村性CFA测评模型,并以江西婺源为例进行了实证研究。通过对婺源乡村旅游典型地区的抽样调查,获取了相关数据,建立了多元回归方程,运用SPSS软件进行回归分析,获得模型的路径系数和随机误差,并对每个回归方程进行了F检验和拟合度检验,结果显示回归方程具有较高的可靠性。对模型中的路径系数进行了t检验,t值在2.319~86.895之间,其显著性概率P小于0.01或0.05,模型中的因果关系显著,与研究的假设条件相符合,模型可以接受。 相似文献