全文获取类型
收费全文 | 2337篇 |
免费 | 374篇 |
国内免费 | 520篇 |
专业分类
测绘学 | 100篇 |
大气科学 | 409篇 |
地球物理 | 686篇 |
地质学 | 1091篇 |
海洋学 | 323篇 |
天文学 | 149篇 |
综合类 | 212篇 |
自然地理 | 261篇 |
出版年
2024年 | 14篇 |
2023年 | 51篇 |
2022年 | 105篇 |
2021年 | 136篇 |
2020年 | 107篇 |
2019年 | 104篇 |
2018年 | 120篇 |
2017年 | 107篇 |
2016年 | 151篇 |
2015年 | 108篇 |
2014年 | 179篇 |
2013年 | 125篇 |
2012年 | 150篇 |
2011年 | 148篇 |
2010年 | 128篇 |
2009年 | 122篇 |
2008年 | 102篇 |
2007年 | 91篇 |
2006年 | 78篇 |
2005年 | 90篇 |
2004年 | 68篇 |
2003年 | 76篇 |
2002年 | 65篇 |
2001年 | 83篇 |
2000年 | 71篇 |
1999年 | 94篇 |
1998年 | 70篇 |
1997年 | 71篇 |
1996年 | 67篇 |
1995年 | 55篇 |
1994年 | 42篇 |
1993年 | 46篇 |
1992年 | 43篇 |
1991年 | 26篇 |
1990年 | 14篇 |
1989年 | 47篇 |
1988年 | 22篇 |
1987年 | 11篇 |
1986年 | 9篇 |
1985年 | 11篇 |
1984年 | 2篇 |
1983年 | 4篇 |
1982年 | 4篇 |
1981年 | 2篇 |
1980年 | 4篇 |
1979年 | 1篇 |
1975年 | 1篇 |
1958年 | 5篇 |
1942年 | 1篇 |
排序方式: 共有3231条查询结果,搜索用时 15 毫秒
991.
992.
悦康药业在开发和生产过程中可能会对区域地下水环境造成影响。基于研究区水文地质条件,建立水文地质概念模型,分别对拟开采的第Ⅲ承压含水层,运用水流运动方程对项目开采15年后的地下水位进行模拟预测;运用溶质运移数学模型对药厂建成后污水处理站对潜水和第Ⅰ承压水进行污染物模拟预测。水位模拟结果表明,15年后含水层(组)中形成降落漏斗大于1 m的范围为0. 45 km~2,形成地面沉降的可能性较小。污染物模拟预测选取COD_(Mn)、氨氮作为预测因子,分别预测污染发生100天、720天及1 800天后污染物迁移情况。污染物模拟结果表明污水站溶质扩散范围较小,5年后COD_(Mn)最大迁移距离为40 m,中心体积质量降为5. 0 mg/L;氨氮最大迁移距离为35 m,中心体积质量降为0. 3 mg/L,对区域地下水水质影响不大。 相似文献
993.
Jinbao Su Shuwen Dong Yueqiao Zhang Licheng Ma Xuanhua Chen Yong Li 《International Geology Review》2018,60(3):365-381
The mid-Neoproterozoic tectonic setting of the Jiangnan Orogen (JO) is uncertain due to the ongoing debate regarding the history of interactions between the Yangtze and Cathaysia Blocks. Extensive magmatic rocks with ages >830 Ma are observed in the eastern JO and are reported to indicate their formation conditions; however, such magmatic rocks are rare in the western JO. This paper presents data from samples collected from two ultramafic intrusions in northern Guangxi province that yield SHRIMP U–Pb ages of 848 ± 7 and 836 ± 5 Ma. These two intrusions have similar geochemical compositions; are enriched in LILE (Rb, Ba, Th, and Pb) relative to HFSE (Hf, Zr, Nb, Ta, and Y), reflecting an arc-like signature; and are derived from the same source. The intrusions have positive εNd(t) and εHf(t) values, implying a depleted mantle source. Comparing the Neoproterozoic mafic–ultramafic rocks of the JO, differences exist between the rocks that formed at 860–830, 830–800, and 800–740 Ma in terms of their mantle sources and formation conditions. Considering the geochemical composition and ages of formation of the strata and the deep structure of the western JO, we speculate that the western JO was a back-arc foreland basin, which experienced shallow subduction-related and arc-like magmatism during the period between 860 and 830 million years. In contrast to the western JO, the eastern JO may have been a back-arc basin with oceanic crustal basement during that time. The JO formed between 830 and 800 million years in association with subduction-related collisional magmatism due to the amalgamation of the Yangtze and Cathaysia Blocks. Subsequently, magmatism occurred in the JO that resulted from the post-orogenic extension. 相似文献
994.
Jinge Wang Aijun Su Qingbing Liu Wei Xiang Hsin-Fu Yeh Chengren Xiong Zongxing Zou Cheng Zhong Junqi Liu Shen Cao 《Landslides》2018,15(7):1425-1435
The Huangtupo landslide is one of the largest and most destructive landslides still deforming in the Three Gorges area of China. In recent years, most studies on this landslide have been based on the data obtained from an investigation conducted in 2001. To further elucidate the geological structure and evolution of the landslide, we began building a field test site in the area of the sliding mass with the fastest deformation velocity in 2009. A group of tunnels with a total length of 1.1 km has been excavated, and nine boreholes with depths between 76.8 and 127.1 m have been drilled into the sliding body. Additionally, relative monitoring devices, such as borehole inclinometers and crack meters, have been installed. Based on the findings of the previous investigation and the latest tunneling, drilling, and monitoring data, a spatial distribution model of the sliding surfaces of the Huangtupo No. 1 riverside sliding mass has been established using the discrete smooth interpolation (DSI) method. Significant differences are revealed between the previous proposed sliding surface and the latest monitoring data. We propose that the Huangtupo No. 1 sliding mass has two sliding surfaces. Thus, the sliding mass can be further divided into two secondary sliding bodies, which are named the No. 1-1 (east) and No. 1-2 (west) sliding masses. The No. 1-1 sliding mass slid first, and the material along the western boundary slid later, producing the No. 1-2 sliding body, which has a smaller volume and shallower depth. The areas, volumes, and thicknesses of each sliding body have been calculated using a digital 3D model. 相似文献
995.
Inter-satellite communication and inter-satellite ranging are the foundation of autonomous navigation for satellite navigation systems. Due to cost limitations, it has been proposed in recent years to equip each satellite with one spot beam antenna, which points to different satellites according to a polling mechanism, resulting in an intermittently connected satellite network. This poses the problem of how to design the inter-satellite link (ISL) contact plan, which determines the evolution of network topology and has important effects on system performance. We propose a new framework for the ISL contact plan design in satellite navigation systems. Considering contact plan design as a multi-parameter and multi-objective optimization problem, the cascade optimization design (COD) is proposed as a method simple to implement and optimize the parameters of the contact plan. COD considers network load and geometry of satellites and has a good adaptability. In the proposed framework, both communication and measurement requirements are taken into account while the contact sequence and the slot length are optimized in two steps. Simulation results show that COD guarantees zero packet drops and achieves the least average delay with a selected network load. When the packet arrival rate is 0.45 packets/s, the packet drop ratio of COD is zero, while that of the traditional simulated annealing design (SAD) is 2.58%. The delay of COD is 22.97 s, which is only two-fifth of the SAD value of 58.77 s. At the same time, using COD the average autonomous navigation weighted dilution of precision decreases from 1.4408 to 0.9671. COD also has strong robustness and performance regardless of the onboard buffer size. 相似文献
996.
新疆贝母具较高的药学利用价值,但现存量稀少,被列为新疆Ⅲ级保护植物。为了探明其天然居群的遗传多样性,本研究选取3个叶绿体基因片段对18个居群的235个个体进行测序。结果表明:新疆贝母总的遗传多样性较高;居群间发生了明显的遗传分化;遗传距离与地理距离呈显著的相关性;昭苏县及新源县的居群具有较高的遗传多样性。居群间的地理障碍及自身的有限传播距离可能导致了居群间的遗传分化。较高的遗传灭绝风险提示应该及时对新疆贝母的天然居群进行保护,尤其在遗传多样性较高的昭苏、新源地区。 相似文献
997.
选择塔里木河下游主要植物胡杨(Populus euphratica)林,以大气温度、太阳净辐射、大气相对湿度、冠层顶风速、地下水位和胡杨树茎横截面积为影响胡杨林耗水量的自变量,基于最小二乘法建立了多重线性回归模型、非线性回归模型和完全二次回归模型,并应用模型对塔里木河下游河岸胡杨林的耗水过程进行了日尺度上的模拟研究。结果表明:3个回归模型均表现出较好的模拟效果,其中完全二次回归模型的模拟精度最高,模型中大气温度、地下水位和胡杨树茎横截面积是影响胡杨耗水量的诸多环境因子中最敏感的因子;胡杨林的耗水量观测值与模拟值表现出较好的相关性,3个回归模型的模拟值与观测值的相关系数依次分别为0.6793、0.7299、0.7574,其相对误差分别为28.7%、26.1%、22.9%,其显著性水平均通过95%显著性检验;3个回归模型中完全二次回归模型具有使用简便、影响因子易测定、有一定精度等优点,能够更好刻画植被腾发量的复杂非线性特性,为干旱区自然植被耗水量估算、模拟和生态需水量计算提供了新的思路和方法。 相似文献
998.
999.
Caiyun Zhang Hongbo Su Tiantian Li Weibo Liu Diana Mitsova Sudhagar Nagarajan Ramesh Teegavarapu Zhixiao Xie Fred Bloetscher Yan Yong 《Ground water》2021,59(2):190-198
Predicting and mapping high water table elevation in coastal landscapes is critical for both science application projects like inundation risk analysis and engineering projects like pond design and maintenance. Previous studies of water table mapping focused on the application of geostatistical methods, which cannot predict values beyond an observation spatial domain or generate an ideal pattern for regions with sparse measurements. In this study, we evaluated the multiple linear regression (MLR) and support vector machine (SVM) techniques for high water table prediction and mapping using fine spatial resolution lidar-derived Digital Elevation Model (DEM) data, and designed an application protocol of these two techniques for high water table mapping in a coastal landscape where groundwater, tide, and surface water are related. Testing results showed that SVM largely improved the high water table prediction with a mean absolute error (MAE) of 1.22 feet and root mean square error (RMSE) of 2.22 feet compared to the application of the ordinary Kriging method which could not generate a reasonable water table. MLR was also promising with a MAE of around 2 feet and RMSE of around 3 feet. The study suggests that both MLR and SVM are valuable alternatives to estimate high water table elevation in Florida. Fine resolution lidar DEMs are beneficial for high water table prediction and mapping. 相似文献
1000.
2021年5月22日青海果洛州玛多县发生MS7.4地震,震中位于( 34.59°N, 98.34°E) ,其震源机制解显示该地震为高倾角走滑型(张喆,许立生, 2021).玛多地震的发震构造为昆仑山口—江错断裂,是东昆仑断裂的一条分支断裂(王未来等, 2021).玉树地震台位于甘孜—玉树断裂附近.玛多地震震中和玉树地震台均位于巴颜喀拉次级地块内,玉树地震台位于巴颜喀拉地块的南边界.此次地震震中处于玉树地震台的NE方向,距巴颜喀拉地块北边界85 km (图1). 相似文献