全文获取类型
收费全文 | 514篇 |
免费 | 103篇 |
国内免费 | 53篇 |
专业分类
测绘学 | 32篇 |
大气科学 | 49篇 |
地球物理 | 210篇 |
地质学 | 143篇 |
海洋学 | 63篇 |
天文学 | 15篇 |
综合类 | 20篇 |
自然地理 | 138篇 |
出版年
2022年 | 17篇 |
2021年 | 19篇 |
2020年 | 22篇 |
2019年 | 17篇 |
2018年 | 21篇 |
2017年 | 21篇 |
2016年 | 22篇 |
2015年 | 24篇 |
2014年 | 31篇 |
2013年 | 39篇 |
2012年 | 26篇 |
2011年 | 36篇 |
2010年 | 19篇 |
2009年 | 29篇 |
2008年 | 34篇 |
2007年 | 19篇 |
2006年 | 31篇 |
2005年 | 29篇 |
2004年 | 20篇 |
2003年 | 17篇 |
2002年 | 15篇 |
2001年 | 21篇 |
2000年 | 20篇 |
1999年 | 19篇 |
1998年 | 9篇 |
1997年 | 7篇 |
1996年 | 20篇 |
1995年 | 8篇 |
1994年 | 12篇 |
1993年 | 7篇 |
1992年 | 9篇 |
1991年 | 6篇 |
1990年 | 5篇 |
1989年 | 5篇 |
1988年 | 2篇 |
1987年 | 4篇 |
1986年 | 5篇 |
1984年 | 1篇 |
1980年 | 1篇 |
1978年 | 1篇 |
排序方式: 共有670条查询结果,搜索用时 562 毫秒
1.
This paper briefly reviews the formulations used over the last 40 years for the solution of problems involving tensile cracking, with both the discrete and the smeared crack approaches. The paper focuses on the smeared approach, identifying as its main drawbacks the observed mesh‐size and mesh‐bias spurious dependence when the method is applied ‘straightly’. A simple isotropic local damage constitutive model is considered, and the (exponential) softening modulus is regularized according to the material fracture energy and the element size. The continuum and discrete mechanical problems corresponding to both the weak discontinuity (smeared cracks) and the strong discontinuity (discrete cracks) approaches are analysed and the question of propagation of the strain localization band (crack) is identified as the main difficulty to be overcome in the numerical procedure. A tracking technique is used to ensure stability of the solution, attaining the necessary convergence properties of the corresponding discrete finite element formulation. Numerical examples show that the formulation derived is stable and remarkably robust. As a consequence, the results obtained do not suffer from spurious mesh‐size or mesh‐bias dependence, comparing very favourably with those obtained with other fracture and continuum mechanics approaches. Copyright © 2006 John Wiley & Sons, Ltd. 相似文献
2.
3.
密度和压缩系数的散射层析成像法 总被引:1,自引:1,他引:0
本文在速度成像的基础上研究了同时对密度和压缩系数成像的散射波层析成像法.对不同散射角度的计算可以得到一系列反演图像,拟合这些图像,从而可以有效地达到对密度和压缩系数(或速度)成像的目的.与单纯的速度成像相比,增加了反演的难度.首先是对资料的方位性要求增加;其次是对资料的利用率下降.即便如此,从对较少量的炮点和检波点资料的数值计算来看,仍取得了满意的成像结果.我们对组成字母“A”的散射体结构进行了成像计算,结果能够同时再现密度和压缩系数,成像清晰,表明了方法的可行性,并能应用于复杂结构的成像问题. 相似文献
4.
5.
6.
Optimizing interpolation of shoot density data from a Posidonia oceanica seagrass bed 总被引:1,自引:0,他引:1
Michele Scardi Lorenzo A. Chessa Eugenio Fresi Antonio Pais & Simone Serra 《Marine Ecology》2006,27(4):339-349
A case study on the optimization of Posidonia oceanica density interpolation, using a data set from a large meadow at Porto Conte Bay (NW Sardinia, Italy), is presented. Ordinary point kriging, cokriging and a weighted average based on inverse square distance were used to interpolate density data measured in 36 sampling stations. The results obtained from different methods were then compared by means of a leave‐one‐out cross‐validation procedure. The scale at which interpolation was carried out was defined on the basis of the Hausdorff dimension of the variogram. Optimizing spatial scale and data points search strategy allowed obtaining more accurate density estimates independently of the interpolation method. 相似文献
7.
秦皇岛砂滩海洋线虫的数量研究 总被引:4,自引:2,他引:4
张志南 《中国海洋大学学报(自然科学版)》1991,(1)
在两年的周期内,对秦皇岛4个砂滩的海洋线虫进行了6次芯样采集。灯塔、新煤码头、汤河口和北戴河赤土山4个砂滩均系分选好的细砂或中细砂,其中值粒径为140-285μm。对连续16个芯样计数的变异性所做的测试证明,1,2和3个芯样计算所得95%C.L.分别是0.539X—1.855X,0.647X—1.547X和0.700X—1.428X。秦皇岛砂滩海洋线虫的年平均密度:中潮带上区为1381±441 inds.10cm~(-2)。中潮带下区为1264±538 inds.10cm~(-2)。灯塔和新煤码头砂滩,8月出现高密度值,与温度的季节变化相符合,而汤河口则出现最低值,可能与污染物的大量排出有关。多数砂滩的大部分芯样显示了明显的重直分布,即种群数量的大部分集中在芯样顶部的两个分层:0~4和5~8cm。没有发现垂直分布的季节变化趋势。与世界其他海区砂滩的资料进行了比较。 相似文献
8.
9.
R.P. Gupta D.P. Kanungo M.K. Arora S. Sarkar 《International Journal of Applied Earth Observation and Geoinformation》2008
Evaluation of maps generated from different conceptual models or data processing approaches at spatial level has importance in many geoenvironmental applications. This paper addresses the spatial comparison of different landslide susceptibility zonation (LSZ) raster maps of the same area derived from various procedures. 相似文献
10.
Strength and stability of frictional sliding of gabbro gouge at elevated temperatures 总被引:7,自引:1,他引:7
To investigate the strength of frictional sliding and stability of mafic lower crust, we conducted experiments on oven-dried gabbro gouge of 1 mm thick sandwiched between country rock pieces (with gouge inclined 35° to the sample axis) at slip rates of 1.22 × 10− 3 mm/s and 1.22 × 10− 4 mm/s and elevated temperatures up to 615 °C. Special attention has been paid to whether transition from velocity weakening to velocity strengthening occurs due to the elevation of temperature.Two series of experiments were conducted with normal stresses of 200 MPa and 300 MPa, respectively. For both normal stresses, the friction strengths are comparable at least up to 510 °C, with no significant weakening effect of increasing temperature. Comparison of our results with Byerlee's rule on a strike slip fault with a specific temperature profile in the Zhangbei region of North China shows that the strength given by experiments are around that given by Byerlee's rule and a little greater in the high temperature range.At 200 MPa normal stress, the steady-state rate dependence a − b shows only positive values, probably still in the “run-in” process where velocity strengthening is a common feature. With a normal stress of 300 MPa, the values of steady-state rate dependence decreases systematically with increasing temperature, and stick-slip occurred at 615 °C. Considering the limited displacement, limited normal stress applied and the effect of normal stress for the temperatures above 420 °C, it is inferred here that velocity weakening may be the typical behaviour at higher normal stress for temperature above 420 °C and at least up to 615 °C, which covers most of the temperature range in the lower crust of geologically stable continental interior. For a dry mafic lower crust in cool continental interiors where frictional sliding prevails over plastic flow, unstable slip nucleation may occur to generate earthquakes. 相似文献