全文获取类型
收费全文 | 7149篇 |
免费 | 1160篇 |
国内免费 | 1233篇 |
专业分类
测绘学 | 491篇 |
大气科学 | 1189篇 |
地球物理 | 1832篇 |
地质学 | 3216篇 |
海洋学 | 1216篇 |
天文学 | 475篇 |
综合类 | 441篇 |
自然地理 | 682篇 |
出版年
2024年 | 22篇 |
2023年 | 73篇 |
2022年 | 227篇 |
2021年 | 294篇 |
2020年 | 229篇 |
2019年 | 313篇 |
2018年 | 398篇 |
2017年 | 367篇 |
2016年 | 414篇 |
2015年 | 327篇 |
2014年 | 438篇 |
2013年 | 513篇 |
2012年 | 417篇 |
2011年 | 473篇 |
2010年 | 462篇 |
2009年 | 442篇 |
2008年 | 406篇 |
2007年 | 368篇 |
2006年 | 323篇 |
2005年 | 316篇 |
2004年 | 290篇 |
2003年 | 255篇 |
2002年 | 272篇 |
2001年 | 257篇 |
2000年 | 217篇 |
1999年 | 222篇 |
1998年 | 188篇 |
1997年 | 165篇 |
1996年 | 136篇 |
1995年 | 95篇 |
1994年 | 102篇 |
1993年 | 97篇 |
1992年 | 76篇 |
1991年 | 62篇 |
1990年 | 53篇 |
1989年 | 35篇 |
1988年 | 35篇 |
1987年 | 29篇 |
1986年 | 25篇 |
1985年 | 25篇 |
1984年 | 19篇 |
1983年 | 11篇 |
1982年 | 16篇 |
1981年 | 7篇 |
1980年 | 9篇 |
1979年 | 3篇 |
1978年 | 3篇 |
1974年 | 2篇 |
1972年 | 3篇 |
1954年 | 3篇 |
排序方式: 共有9542条查询结果,搜索用时 15 毫秒
91.
Edelmann G.F. Akal T. Hodgkiss W.S. Seongil Kim Kuperman W.A. Hee Chun Song 《Oceanic Engineering, IEEE Journal of》2002,27(3):602-609
In July 1999, an at-sea experiment to measure the focus of a 3.5-kHz centered time-reversal mirror (TRM) was conducted in three different environments: an absorptive bottom, a reflective bottom, and a sloping bottom. The experiment included a preliminary exploration of using a TRM to generate binary-phase shift keying communication sequences in each of these environments. Broadside communication transmissions were also made, and single-source communications were simulated using the measured-channel response. A comparison of the results is made and time reversal is shown to be an effective approach for mitigating inter-symbol interference caused by channel multipath. 相似文献
92.
为给单环刺 (U.unicinctus)的苗种生产提供有效的基础资料 ,本文研究了水温对单环刺胚胎发育的影响。结果表明 :单环刺各胚胎发育期的发育速度 (h)随水温 (T)升高而加快 ,有明显的正相关性。求得胚胎发育的生物学零度为平均 2℃。不同水温条件下 ,各期幼虫期的存活率以2 0℃为最高 ,培育水温高于或低于 2 0℃时生存率逐渐降低。幼虫培育适宜温度为 15~ 2 0℃。 相似文献
93.
分别于1986年12月和1985年3月1日—1987年3月1日在海州湾进行了波浪和含沙量观测,运用所获资料以及本区长期水文、地形资料,采用流体力学、沉积学和泥沙运动力学相结合的研究方法,建立了海州湾淤泥质海滩剖面堆积过程的二维计算模式。结果表明,在堆积型淤泥质海滩,由于浮泥的经常性存在,使波浪急剧衰减,其对岸滩的作用甚为微弱,潮流成为塑造淤泥质海滩的主要动力,岸滩在淤涨过程中,在平均高潮位厂沿和平均低潮位附近出现两个凸点,上一个凸点外推速率大于下一个凸点,潮下带变化缓慢。 相似文献
94.
95.
96.
97.
The lateral deflection of a cylindrical diaphragm wall and the associated ground movement induced by deep excavation are analyzed by performing site instrumentations and numerical analyses in the coastal area of Korea. Wall lateral deflection, rebar stress, and pore water pressure were measured and analyzed in eight directions. Variations of soil properties with the decrease of confining pressure are compared by performing various in situ tests before ad after excavation. To calculate the wall lateral deflection accurately, the effects of small strain nonlinearity, confining pressure, and the hysteresis loading/unloading loop developed during excavation are considered in the proposed numerical analysis. By comparing numerical results with measured ones, the importances of considering small strain nonlinearity and confining pressure reduction in the nonlinear (FEM) are emphasized. Also, the effects of wall stiffness on the performance of cylindrical diaphragm walls are studied for future similar excavation in the coastal area. 相似文献
98.
99.
Two piston cores, collected from the western Ulleung Basin of the East/Japan Sea, were used to investigate the Late Quaternary tephrostratigraphy, lithology, and mineralogy of the sediments, as well as the elemental composition of both sediments and interstitial water, and their paleo-environmental implications. The cores show two lapilli tephra layers and one rhyolitic ash layer at the boundaries between sedimentary lithofacies units I, II, and III. These layers can be correlated with the well-known Ulleung-Oki (ca. 9.3 ka; boundary of units I/II), Ulleung-Yamato (ca. 25–33 ka), and Aira-Tanzawa (ca. 25.1 ka; boundary of units II/III) layers, respectively. These data suggest that the cores cover the period from the middle stage of marine isotope stage (MIS) 3 to the Holocene. In each core, a so-called dark laminated mud (DLM) layer in unit II commonly has high contents of Si and Al, suggesting that the DLM layer generally contains significant amounts of fine-grained silicates and/or aluminosilicates. In addition, these DLM layers are enriched in Fe relative to Mn, iron being predominantly bound in framboidal pyrite. The size distribution of pyrite in the DLM layers suggests that these have formed under anoxic (euxinic) conditions at times of reduced water circulation in the basin during sea-level lowstand (euxinic environment). The C/N ratios [5–12] suggest that sedimentary organic matter in the cores is predominantly of marine origin. Total organic carbon (TOC) contents increased shortly before Termination I. This could have been caused by an increased flux of marine organic matter in association with sea-level rise. The C and S values of units II and III (Late Pleistocene sediments; C: <2.0%; S: 0.5–2.1%) suggest a more euxinic environment than that of unit I (Holocene sediments; C: 1.0–3.5%; S: <1.0%). Concentrations of SO42– in the interstitial water decrease with increasing burial depth, whereas CH4 concentrations show the reverse trend. Therefore, it seems that sulfate reduction, probably related to microbial activity, predominates in the upper core sections (<5 m), shifting to methanogenesis in the lower core sections. 相似文献
100.
Shane M. Ohline Malcolm R. Reid Shamus L.G. Husheer Kim I. Currie Keith A. Hunter 《Marine Chemistry》2007
Accurate measurement of seawater pH has long been sought by marine chemists (for example: [Dickson, A.G. 1993a. The measurement of sea water pH. Marine Chemistry, 44, 131–142, Dickson, A.G. 1993b. pH buffers for sea water media based on the total hydrogen ion concentration scale. Deep-Sea Research, 40, 107–118; Zhang, 1996; Tapp, M., Hunter, K.A., Currie, K. and Macaskill, B. 2000. Apparatus of continuous-flow underway spectrophotometric measurement of surface water pH. Marine Chemistry 72(2–4), 193–202; Friis, K., Koetzinger, A., Wallace, D.W.R. 2004. Spectrophotometric pH measurement in the ocean: Requirements, design and testing of an autonomous charge-coupled device detector system. Limnology and Oceanography: Methods 2, 126–136]. Recently, such attempts have taken on greater significance as anthropogenic carbon dioxide emissions may create rapidly changing oceanic pH. Spectrophotometric techniques have been accepted generally as the best for determination of seawater pH. Here we report a new technique using thymol blue as the indicator dye and fitting the entire spectrum from 400 to 900 nm rather than measuring the absorbance values at only two or three points in the spectrum. This full-spectrum modelling enables a reduction in signal to noise over other techniques. In the laboratory, we find with seawater samples a pH precision increase of five-fold “within” a sample and seven-fold “between” samples when comparing the full spectrum to the three-point method of analysis [Zhang, H., Byrne, R.H. 1996. Spectrophotometric pH measurements of surface seawater at in-situ conditions: absorbance and protonation behaviour of thymol blue. Marine Chemistry 52, 17–25]. 相似文献