全文获取类型
收费全文 | 1410篇 |
免费 | 289篇 |
国内免费 | 312篇 |
专业分类
测绘学 | 97篇 |
大气科学 | 200篇 |
地球物理 | 353篇 |
地质学 | 497篇 |
海洋学 | 557篇 |
天文学 | 11篇 |
综合类 | 77篇 |
自然地理 | 219篇 |
出版年
2024年 | 6篇 |
2023年 | 24篇 |
2022年 | 45篇 |
2021年 | 56篇 |
2020年 | 65篇 |
2019年 | 66篇 |
2018年 | 50篇 |
2017年 | 47篇 |
2016年 | 59篇 |
2015年 | 68篇 |
2014年 | 74篇 |
2013年 | 127篇 |
2012年 | 82篇 |
2011年 | 82篇 |
2010年 | 66篇 |
2009年 | 75篇 |
2008年 | 82篇 |
2007年 | 99篇 |
2006年 | 108篇 |
2005年 | 78篇 |
2004年 | 85篇 |
2003年 | 78篇 |
2002年 | 49篇 |
2001年 | 46篇 |
2000年 | 57篇 |
1999年 | 42篇 |
1998年 | 43篇 |
1997年 | 35篇 |
1996年 | 41篇 |
1995年 | 21篇 |
1994年 | 36篇 |
1993年 | 22篇 |
1992年 | 19篇 |
1991年 | 16篇 |
1990年 | 11篇 |
1989年 | 16篇 |
1988年 | 13篇 |
1987年 | 8篇 |
1986年 | 4篇 |
1985年 | 1篇 |
1984年 | 3篇 |
1982年 | 1篇 |
1981年 | 1篇 |
1979年 | 1篇 |
1978年 | 2篇 |
1977年 | 1篇 |
排序方式: 共有2011条查询结果,搜索用时 31 毫秒
991.
992.
为解决塔山煤矿高强度开采条件下瓦斯低含量、高涌出的问题,同时为了弥补大型物理实验和现场试验成本高、操作难的缺点,根据该矿8101工作面所属区域煤层的地质和瓦斯赋存条件,确定了数值试验方案,对地面垂直钻孔预抽特厚煤层瓦斯的效果进行优化分析。基于煤岩(体)的孔隙特征,构建了含瓦斯煤岩(体)破裂过程气-固耦合和渗透率-损伤耦合数学本构模型。采用RFPA2D瓦斯分析版软件建立地面钻孔抽放瓦斯的数值计算模型,设置有关简化条件、边界条件和物性参数,通过数值试验得出:地面垂直钻孔的终孔位置布置在煤层底部比较合理;在综合考虑地面垂直钻孔投入成本和瓦斯抽采效果的基础上,确定地面垂直钻孔间距为50~60 m比较合理。同时,由8101工作面地面垂直钻孔抽采煤层瓦斯的实际应用效果分析可知,当地面垂直钻孔的终孔位置布置在煤层底部,且钻孔间距布置为50 m时,能够实现良好的瓦斯抽放效果,这也从一定程度上进一步验证了数值试验的合理性和可行性。 相似文献
993.
994.
995.
This paper reports results from field experiments and hydrological modelling on the dynamics of runoff generation in highly convergent parts of the landscape in a logged and burnt eucalypt forest in south‐eastern Victoria, Australia. Large‐scale rainfall simulation experiments were conducted to explore runoff generating mechanisms from harvested areas, and to assess the effectiveness of standard water quality protective measures, here a disturbed filter strip, in preventing accession of sediment to near‐stream areas. We then examined the likely effects of varying antecedent moisture conditions on surface and subsurface runoff generating mechanisms. Very small volumes of surface runoff were generated only at very high rainfall intensity rates that exceeded a 100 year recurrence interval event during the simulated experiments. There was little or no identifiable impact of either compaction from logging operations or fire‐induced hydrophobicity on surface infiltration or generation of surface runoff. Measured soil hydraulic properties and soil depths explained the paucity of surface runoff, and the dominance of subsurface storm flow as the prime runoff generating mechanism. Deep lateral subsurface flow was observed from the cut‐face of a fire access track and into a streamhead downslope of the experimental plots. Water balance modelling using Topog_Dynamic indicated the conditions under which saturated overland flow in this environment could be generated are rare, but that care should be taken in siting of roads and tracks in lower parts of convergent landscapes. Copyright © 2004 John Wiley & Sons, Ltd. 相似文献
996.
利川南坪泥炭形成的环境分析 总被引:1,自引:0,他引:1
根据钻孔、孢粉分析、粘土矿物X射线分析、14C测年等资料,本文讨论了鄂西南山原利川一带玉木亚间冰期以来气候波动的历史,分析了在亚热带高压带喀斯特作用和山地条件下,泥炭形成的环境特点。 相似文献
997.
The neutrally stratified flow over the Askervein Hill was simulatedusing a terrain-following coordinatesystem and a two-equation(k - ) turbulence model. Calculations were performed on awide range of numerical grids to assess, among other things, theimportance of spatial discretization and the limitations of theturbulence model. Our results showed that a relatively coarse gridwas enough to resolve the flow in the upstream region of the hill;at the hilltop, 10 m above the ground, the speed-up was 10% lessthan the experimental value. The flow's most prominent feature wasa recirculating region in the lee of the hill, which determinedthe main characteristics of the whole downstream flow. This regionhad an intermittent nature and could be fully captured only in the caseof a time-dependent formulation and a third-order discretization ofthe advective terms. The reduction of the characteristic roughnessnear the top of the hill was also taken into account, showing theimportance of this parameter, particularly in the flow close to theground at the summit and in the downstream side of the hill.Calculations involving an enlarged area around the Askervein Hillshowed that the presence of the nearby topography affected the flowneither at the top nor downstream of the Askervein Hill. 相似文献
998.
Observational data, high-resolution numerical modelling results and a simple analytical theory are combined in this paper to demonstrate the dependence of the volume transports through tidal inlets on topographical or morphological parameters of a Wadden Sea system. The area of interest covers the East Frisian Wadden Sea and consists of seven weakly connected tidal basins. The observations include time series of tidal gauge data and surface currents measured at a pile station in the backbarrier basin of the island Langeoog, as well as several ADCP transects in the Accumer Ee tidal inlet. The numerical simulations are based on the 3-D primitive equation General Estuarine Transport Model (GETM) with a horizontal resolution of 200 m and terrain following vertical coordinates. The model is forced at its open boundaries with sea-level data from an operational model for the German Bight (German Hydrographic Office). The simple theoretical concepts presented illustrate the effect of topography (hypsometry) in the tidal basins on the temporal variability of the exchange of water. This topographic control is effectuated through the bottom slope in the areas prone to drying and flooding. For our study area it takes about twice as long from slack water to maximum flood current than from slack water to maximum ebb current. The underlying physics of this signal modulation from a more or less harmonic forcing at the open-sea boundary and the quantification of the contributing physical processes are the major results of this paper. Estimates based simply on volume conservation are consistent with observations and results from numerical modelling, but they do not completely capture the actual non-linear tidal response. Our analysis shows that at least during part of the tidal cycle characteristic topographic parameters of the inlet/bay system have a major impact on the rate of exchange of waters between the Wadden Sea and the open ocean. This impact is especially strong during the transition between flood and ebb conditions. The possible morphodynamic responses are also addressed focusing on some common (universal) topographic features in seven tidal basins.Responsible Editor: Hans Burchard 相似文献
999.
从INDEPTH-MT结果探讨雅鲁藏布江缝合带的电性结构 总被引:1,自引:0,他引:1
INDEPTH MT研究结果表明,在雅鲁藏布江未发现反映深断裂的电性显示,而在江孜和仁布之间见有规模宏大、底界深达55km、向北倾斜的低阻高导体。这表明该区可能为雅鲁藏布江缝合带在地表出露的实际位置。高导体范围内存在3组反映断裂构造的电性梯度带和畸变带。3条断裂带向北倾斜,沿纵深向主断裂带F3汇聚。其北侧,发育多条南倾断裂,它们共同构成雅鲁藏布江缝合带发散状断裂构造特征。大规模高导体的存在与地下热状态是密切相关的。 相似文献
1000.
下垫面因子影响气候形成和变化的数值试验 总被引:4,自引:0,他引:4
本文用球带范围的耦合模式,研究了地球从均一陆地地表有海陆分布,全球陆地从平坦到真实地形,陆地从一类土壤到几类土壤并存过程中大气环流的演变和气候变化状况。发现没有海陆分布时气候要素场呈纬向带状分布,大气中流场和风场表现为三圈环流和行星风系特征,当有海陆分布后,北半球无论是高层还是低层环流形势均具有和海陆分布相一致的纬向两波结构,海陆分布是形成现代大气环流格局的根本因子,高原地形使高原上的空的气压系统 相似文献