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81.
82.
研究降水和氮沉降对荒漠草原植物叶形态性状的影响,对于预测未来全球变化下荒漠草原植物的生态适应具有重要意义。对增减雨(±50%)和氮添加(10 g·m-2·a-1)及其交互作用对乌拉特荒漠草原区优势植物叶形态性状的影响研究结果表明:(1)沙生针茅(Stipa glareosa)、碱韭(Allium polyrhizum)和骆驼蓬(Peganum harmala)比叶面积(SLA)、叶干物质含量(LDMC)对增减雨和氮添加的响应存在差异。增雨处理下仅碱韭的SLA显著降低,减雨处理下骆驼蓬的SLA显著降低,LDMC显著增加(P<0.05);氮添加处理下仅骆驼蓬的LDMC显著降低(P<0.05)。(2)水氮交互作用仅对骆驼蓬有显著影响(P<0.05),氮添加使减雨处理对其SLA和LDMC无显著影响(P>0.05)。(3)减雨、氮添加和增雨与氮添加的交互作用处理下SLA和LDMC显著负相关(P<0.05)。沙生针茅叶性状较稳定,碱韭SLA对增雨响应较敏感,骆驼蓬叶性状对减雨敏感,而增氮可降低减雨对其叶片的胁迫,荒漠草原区不同的植物通过不同的可塑性和生态策略响应和适应区域环境变化。 相似文献
83.
选取中国沿海海洋站中与验潮室并址的22个GNSS基准站近9 a的观测资料,利用最大似然估计法分析各站时间序列的噪声特性,建立最优噪声模型;然后顾及有色噪声,利用最优噪声模型估计测站速度,并与纯白噪声模型和GLOBK获取的速度及误差进行对比分析。结果表明:1)沿海海洋站的GNSS时间序列均含有有色噪声,各分量的噪声特性不完全一致,E方向和U分量均以白噪声+闪烁噪声为主,N分量以白噪声+闪烁噪声和白噪声+一阶马尔科夫噪声+随机漫步噪声为主。2)全国沿海3个海区N、E分量的白噪声和闪烁噪声基本呈现越往南噪声越大的规律,南海海区U分量的白噪声和闪烁噪声最大。3)顾及有色噪声的速度中误差是仅考虑白噪声和GLOBK估计的速度中误差估计值的5~10倍,这种差异比内陆观测站的要大。4)在对海洋站GNSS时间序列进行速度分析时,为获取正确的速度值,应该先准确判断噪声的类型,再顾及有色噪声的影响估计测站速度。 相似文献
84.
Yong Zhang Tao Yang Junbo Zhang Baoyi Lv Xiangsheng Cheng Yin Fang 《中国海洋大学学报(英文版)》2020,19(3):633-642
The Sanchi oil tanker collision in the East China Sea on January 6th, 2018 has caused worldwide attention due to its uniqueness. A considerable amount of h 相似文献
85.
针对北斗卫星导航系统(BDS)完备性研究较少的现状,该文提出了一种导航星历中轨道观测数据的完备性监测新方法。采用轨道积分方法分析了北斗卫星的轨道残差均方根值;通过概率统计的方法,分别计算所有北斗卫星的轨道残差极限误差值(告警限差),剔除误差超限甚至粗差卫星,实现事后轨道完备性监测。另外通过比较分析剔除监测标记出的误差卫星之前和之后对测站精密单点定位的影响,验证完备性的风险性。最后通过实测数据对该算法进行了验证和分析。实验结果表明:该算法可以实现卫星轨道的监测示警,标记误差卫星,达到轨道完备性监测效果。 相似文献
86.
运用交互胁迫、耦合协调模型,结合主观均方差分析法和客观结构熵值法确定指标权重,通过建立指标体系研究2000-2014年浙江省生态环境和城市化的交互胁迫关系和协调类型.结果表明:浙江省生态环境和城市化之间存在交互胁迫关系,演变状态符合双指数函数;前者对后者有显著的约束作用,后者对前者有显著的胁迫作用.对城市化综合水平影响程度大小依次为经济、社会与人口城市化,对生态环境综合水平影响程度大小依次为生态环境压力、状态与响应.2000-2014年浙江省综合协调耦合类型分为磨合协调阶段(2000-2003年)、基本协调阶段(2003-2005年)、拮抗协调阶段(2005-2010年)和良好协调阶段(2010-2014)4个阶段. 相似文献
87.
Climate change impacts on regional rice production in China 总被引:1,自引:0,他引:1
Zunfu Lv Yan Zhu Xiaojun Liu Hongbao Ye Yongchao Tian Feifei Li 《Climatic change》2018,147(3-4):523-537
Rice (Oryza sativa L.) production is an important contributor to China’s food security. Climate change, and its impact on rice production, presents challenges in meeting China’s future rice production requirements. In this study, we conducted a comprehensive analysis of how rice yield responds to climate change under different scenarios and assessed the associated simulation uncertainties of various regional-scale climate models. Simulation was performed based on a regional calibrated crop model (CERES-Rice) and spatially matched climatic (from 17 global climate models), soil, management, and cultivar parameters. Grain-filling periods for early rice were shortened by 2–7 days in three time slices (2030s, 2050s, and 2070s), whereas grain-filling periods for late rice were shortened by 10–19 days in three time slices. Most of the negative effects of climate change were predicted to affect single-crop rice in central China. Average yields of single-crop rice treated with CO2 fertiliser in central China were predicted to be reduced by 10, 11, and 11% during the 2030s, 2050s, and 2070s, respectively, compared to the 2000s, if planting dates remained unchanged. If planting dates were optimised, single-crop rice yields were predicted to increase by 3, 7, and 11% during the 2030s, 2050s, and 2070s, respectively. In response to climate changes, early and single-crop rice should be planted earlier, and late rice planting should be delayed. The predicted net effect would be to prolong the grain-filling period and optimise rice yield. 相似文献
88.
Zhang Xiaoxuan Hu Yonghong Jia Gensuo Hou Meiting Fan Yanguo Sun Zhongchang Zhu Yuxiang 《Theoretical and Applied Climatology》2017,129(3-4):965-976
The influence of spatial scales on surface fluxes is an interesting but not fully investigated question. This paper presents an analysis on the influence of spatial scales on surface fluxes in the north Tibetan Plateau based on eddy covariance (EC) and large aperture scintillometer (LAS) data at site Nagqu/BJ, combined with the land surface temperature (LST) and normalized difference vegetation index (NDVI) of moderate-resolution imaging spectroradiometer (MODIS). The analysis shows that sensible heat fluxes calculated with LAS data (H_LAS) agree reasonably well with sensible heat fluxes calculated with EC data (H_EC) in the rain and dry seasons. The difference in their footprints due to the wind direction is an important reason for the differences in H_EC and H_LAS. The H_LAS are statistically more consistent with H_EC when their footprints overlap than when their footprints do not. A detailed analysis on H_EC and H_LAS changes with net radiation and wind direction in rain and dry season indicates that the spatial heterogeneity in net radiation created by clouds contributes greatly to the differences in H_EC and H_LAS in short-term variations. A significant relationship between the difference in footprint-weighted averages of LST and difference in H_EC and H_LAS suggests that the spatial heterogeneity in LST at two spatial scales is a reason for the differences in H_EC and H_LAS and that LST has a positive correlation with the differences in H_EC and H_LAS. A significant relationship between the footprint-weighted averages of NDVI and the ratio of sensible heat fluxes at two spatial scales to net radiation (H/Rn) in the rain season supports the analysis that the spatial heterogeneity in canopy at two spatial scales is another reason for differences in H_EC and H_LAS and that canopy has a negative correlation with (H/Rn). An analysis on the influence of the difference in aerodynamic roughness lengths at two spatial scales on sensible heat fluxes shows that the influence is greater in the dry season and smaller in the rain season because the ratio of z0m_LAS to z0m_EC is big in the dry season and is close to 1.0 in the rain season. This study on spatial scales on surface fluxes in the Tibetan Plateau will be helpful in analyzing and understanding its influence on climate. 相似文献
89.
90.
泥沙淤积问题直接影响着三峡水库的使用寿命及综合效益的发挥,研究其入库水沙特性对于解决水库泥沙淤积问题具有重要意义。根据水文站实测数据,分析了三峡水库入库水沙输移特性及来源组成变化,重点研究了金沙江下游梯级水库运行后的三峡水库高洪水期入库水沙特性。结果表明:2003—2021年,三峡水库入库泥沙集中于汛期的高洪水期,2013年以后该现象更为显著,泥沙来源也由金沙江为主转变为嘉陵江为主。寸滩站洪峰流量高于50000 m3/s的高洪水期三峡入库沙量显著大于30000~50000 m3/s区间的高洪水期,三峡水库泥沙调度关键在于上游发生编号洪水期间。三峡水库上游沱江或嘉陵江等支流发生流域性大洪水时,易引起高洪水期入库水沙出现“小水大沙”的特点。金沙江下游梯级水库运行后,三峡水库高洪水期入库泥沙大幅减少,中小洪水调度期间泥沙淤积量也大幅减小。研究结果可为三峡水库的泥沙精细化调度和长期高效使用提供基础数据支撑。 相似文献