全文获取类型
收费全文 | 3998篇 |
免费 | 693篇 |
国内免费 | 843篇 |
专业分类
测绘学 | 106篇 |
大气科学 | 682篇 |
地球物理 | 1171篇 |
地质学 | 2022篇 |
海洋学 | 403篇 |
天文学 | 769篇 |
综合类 | 144篇 |
自然地理 | 237篇 |
出版年
2024年 | 15篇 |
2023年 | 37篇 |
2022年 | 88篇 |
2021年 | 89篇 |
2020年 | 100篇 |
2019年 | 129篇 |
2018年 | 88篇 |
2017年 | 117篇 |
2016年 | 115篇 |
2015年 | 157篇 |
2014年 | 176篇 |
2013年 | 144篇 |
2012年 | 180篇 |
2011年 | 238篇 |
2010年 | 164篇 |
2009年 | 333篇 |
2008年 | 279篇 |
2007年 | 295篇 |
2006年 | 340篇 |
2005年 | 246篇 |
2004年 | 272篇 |
2003年 | 214篇 |
2002年 | 186篇 |
2001年 | 153篇 |
2000年 | 208篇 |
1999年 | 241篇 |
1998年 | 204篇 |
1997年 | 120篇 |
1996年 | 108篇 |
1995年 | 97篇 |
1994年 | 72篇 |
1993年 | 87篇 |
1992年 | 42篇 |
1991年 | 38篇 |
1990年 | 35篇 |
1989年 | 22篇 |
1988年 | 26篇 |
1987年 | 18篇 |
1986年 | 9篇 |
1985年 | 10篇 |
1984年 | 10篇 |
1983年 | 5篇 |
1982年 | 5篇 |
1980年 | 4篇 |
1979年 | 3篇 |
1978年 | 6篇 |
1977年 | 2篇 |
1976年 | 1篇 |
1975年 | 1篇 |
1954年 | 4篇 |
排序方式: 共有5534条查询结果,搜索用时 960 毫秒
301.
水泄铜钴矿区地质条件较为复杂,控矿因素较多,通过分析认为主要受断层及岩性控制,地层初始富集,构造及区域变质作用提供通道及热源。水的循环、溶解作用形成热卤水成矿。 相似文献
302.
Sokrat Amataj Todor Anovski Ralf Benischke Romeo Eftimi Laurence L. Gourcy Liliana Kola Ioannis Leontiadis Eftim Micevski Alqiviadis Stamos Jovan Zoto 《Environmental Geology》2007,51(5):749-753
Prespa Lake and Ohrid Lake constitute a hydraulic system shared between Albania, FYR of Macedonia and Greece. Karst rocks
separate both lakes. The elevation of Prespa Lake is about 150 m higher than that of Ohrid Lake. Considering these facts,
Cvijić formulated in 1906 the hypothesis that Prespa Lake recharges the St. Naum and Tushemisht springs at Ohrid lakeside.
Environmental isotopes demonstrated that Prespa Lake recharges about 37–42 and 52–54% of water emerging in St. Naum, and Tushemisht
springs, respectively. An artificial tracer experiment carried out in 2002 physically demonstrated the underground connection
between both lakes. This experiment confirmed the supposed underground connection and brought important information about
the groundwater velocity, transit time, and karst water conduits development. 相似文献
303.
Hanifi Canakci 《Environmental Geology》2007,53(4):915-922
This paper focuses on an investigation of the possible causes for the collapse of limestone caves in Gaziantep, Turkey. The
city contains a lot of man-made caves, at a shallow depth, of various width and length. These caves were mainly excavated
to provide work or storage space. As the city has been growing fast with increased population, many structures were constructed
over these caves. Recently, two caves collapsed and five houses were damaged. These caves are all made of limestone and it
was observed after the collapse that the limestone was saturated with water due to sewer pipe leakage and surface water. Tests
were carried out on the limestone and it was determined that the compressive strength of limestone decreases by about 50%
and the tensile strength decreased by about 80% when saturated with water. It was concluded that the reduced strength of the
limestone combined with additional loads due to the factors mentioned above seem to be the main reason for these collapses. 相似文献
304.
305.
采用有机溶剂与蒸馏水混和浸提杉木枯枝落叶腐解9个月后化感物质,应用杉木种子发芽试验进行生物检测.结果表明:杉木枯枝落叶腐解9个月后,杉木枯枝落叶中的弱极性化感物质对绝对发芽率、绝对发芽势、胚根长、胚轴长及干物质量等指标表现为抑制作用,对鲜物质量则表现为轻微的促进作用;极性化感物质对杉木种子发芽各指标均等表现为抑制作用.腐解土中的弱极性化感物质对杉木种子发芽各指标均表现为抑制作用,极性化感物质对绝对发芽率、绝对发芽势、胚轴长及干物质量等表现为抑制作用,但对胚根长、鲜物质量表现为促进作用. 相似文献
306.
威连滩冲沟砂黄土的风蚀与降雨侵蚀模拟实验 总被引:3,自引:0,他引:3
通过风洞与模拟降雨实验,研究了风力与降雨对青海省贵南县威连滩冲沟砂黄土的复合侵蚀作用。实验得出:①风蚀后的降雨使砂黄土表面在风干过程中形成了一层较为坚硬的结壳,增大了土壤的抗蚀性,降低了第二次风洞实验后期的风蚀率;②土壤水分与人为扰动是影响土壤风蚀的两个重要因素。当土壤水分较小时,风蚀率受人为扰动影响巨大;当土壤水分较大时,人为扰动对土壤风蚀的影响较小;③在持续降雨的实验条件下,砂黄土的产流、产沙量随着雨强的变化而改变。这种变化与表土的侵蚀率、可蚀性物质的多少、土壤水分以及土壤的入渗率等都有很大的关系。 相似文献
307.
In the work reported here the comprehensive physics‐based Integrated Hydrology Model (InHM) was employed to conduct both three‐ and two‐dimensional (3D and 2D) hydrologic‐response simulations for the small upland catchment known as C3 (located within the H. J. Andrews Experimental Forest in Oregon). Results from the 3D simulations for the steep unchannelled C3 (i) identify subsurface stormflow as the dominant hydrologic‐response mechanism and (ii) show the effect of the down‐gradient forest road on both the surface and subsurface flow systems. Comparison of the 3D results with the 2D results clearly illustrates the importance of convergent subsurface flow (e.g. greater pore‐water pressures in the hollow of the catchment for the 3D scenario). A simple infinite‐slope model, driven by subsurface pore‐water pressures generated from the 3D and 2D hydrologic‐response simulations, was employed to estimate slope stability along the long‐profile of the C3 hollow axis. As expected, the likelihood of slope failure is underestimated for the lower pore pressures from the 2D hydrologic‐response simulation compared, in a relative sense, to the higher pore pressures from the 3D hydrologic response simulation. The effort reported herein provides a firm quantitative foundation for generalizing the effects that forest roads can have on near‐surface hydrologic response and slope stability at the catchment scale. Copyright © 2006 John Wiley & Sons, Ltd. 相似文献
308.
Saltmarsh vegetation significantly influences tidal currents and sediment deposition by decelerating the water velocity in the canopy. In order to complement previous field results, detailed profiles of velocity and turbulence were measured in a laboratory flume. Natural Spartina anglica plants were installed in a 3 m length test section in a straight, recirculating flume. Different vegetation densities, water depths and surface velocities were investigated. The logarithmic velocity profile, which existed in front of the vegetation, was altered gradually to a skimming-flow profile, typical for submerged saltmarsh vegetation. The flow reduction in the denser part of the canopy also induced an upward flow (the current was partially deflected by the canopy). The skimming flow was accompanied by a zone of high turbulence co-located with the strongest velocity gradient. This gradient moved upward and the turbulence increased with distance from the edge of the vegetation. Below the skimming flow, the velocity and the turbulence were low. The structure of the flow in the canopy was relatively stable 2 m into the vegetation. The roughness length (z0) of the vegetation depends only on the vegetation characteristics, and is not sensitive to the current velocity or the water depth. Both the reduced turbulence in the dense canopy and the high turbulence at the top of the canopy should increase sediment deposition. On the other hand, the high turbulence zone just beyond the vegetation edge and the oblique upward flow may produce reduced sedimentation; a phenomenon that was observed near the vegetation edge in the field. 相似文献
309.
Pb and Th in settling particles in the western Northwest Pacific Ocean: Particle flux and scavenging
A mooring of three conical time-series sediment traps was deployed at two sites in the western Northwest Pacific Ocean for 9 months. Total mass fluxes and activities of 210Pb and 230Th were determined for the settling particles to elucidate their scavenging and transport processes. Sediment samples also were analyzed for 210Pb activities. Total mass fluxes, 210Pb fluxes and 230Th fluxes showed large seasonal variations and their weighted mean fluxes tended to increase with depth, with an especially large increase near-bottom. The ratios of the observed 210Pb fluxes to the 210Pb deficiency fluxes in the upper traps at the two sites were only 0.02 and 0.12, and were attributable to advective export of 210Pb from the surface waters. Those ratios in the near-bottom traps ranged between 1.22 and 2.63. This suggests that these high ratios are due to effective particle scavenging, large lateral 210Pb import and input of resuspended particles that have not become incorporated into the sediments. The mean total 230Th fluxes at the near-bottom traps were 4.2–6.7 times higher than that expected from production in the overlying water column. The 210Pb activities in the surficial sediments were much lower than those in the near-bottom traps. The 210Pb accumulation rates estimated from the excess 210Pb inventory in the sediment column were 40–70% higher than the mean 210Pb fluxes at the near-bottom traps. The ratios of the 210Pb accumulation rates to the 210Pb deficiency fluxes at the near-bottom traps ranged between 2.0 and 3.7. The high fluxes of particulate 210Pb and 230Th at the near-bottom traps reflected a combination of enhanced scavenging of dissolved nuclides and the lateral redistribution of particulate matter by downslope and alongshore transports. However, it was not possible to discriminate among the various processes contributing to high nuclide fluxes. 相似文献
310.