全文获取类型
收费全文 | 1841篇 |
免费 | 181篇 |
国内免费 | 180篇 |
专业分类
测绘学 | 770篇 |
大气科学 | 168篇 |
地球物理 | 421篇 |
地质学 | 267篇 |
海洋学 | 213篇 |
天文学 | 187篇 |
综合类 | 101篇 |
自然地理 | 75篇 |
出版年
2024年 | 6篇 |
2023年 | 6篇 |
2022年 | 18篇 |
2021年 | 59篇 |
2020年 | 72篇 |
2019年 | 74篇 |
2018年 | 42篇 |
2017年 | 95篇 |
2016年 | 85篇 |
2015年 | 108篇 |
2014年 | 119篇 |
2013年 | 135篇 |
2012年 | 116篇 |
2011年 | 96篇 |
2010年 | 92篇 |
2009年 | 95篇 |
2008年 | 96篇 |
2007年 | 111篇 |
2006年 | 126篇 |
2005年 | 88篇 |
2004年 | 76篇 |
2003年 | 66篇 |
2002年 | 73篇 |
2001年 | 50篇 |
2000年 | 41篇 |
1999年 | 29篇 |
1998年 | 38篇 |
1997年 | 40篇 |
1996年 | 33篇 |
1995年 | 20篇 |
1994年 | 23篇 |
1993年 | 16篇 |
1992年 | 20篇 |
1991年 | 10篇 |
1990年 | 10篇 |
1989年 | 8篇 |
1988年 | 2篇 |
1987年 | 4篇 |
1986年 | 2篇 |
1984年 | 1篇 |
1981年 | 1篇 |
排序方式: 共有2202条查询结果,搜索用时 15 毫秒
141.
142.
143.
使用1994—2007年在1.56m反射望远镜CCD照相机拍摄的资料,测定了上海天文台余山工作站夜天亮度的变化。由于上海城市的发展,佘山工作站的夜天亮度在V波段从每平方角秒约19mag变到15.8mag,也就是说,夜天亮度自1994年以来变亮了约20倍。国际上优良台站的夜天亮度在V波段等于或暗于21.5mag。上述夜天亮度是优良台站的200多倍。现在在佘山工作站使用1.56m反射望远镜对暗于V=14mag的星做精确测光已经很困难了。 相似文献
144.
研究了国家天文台兴隆观测基地1m反射望远镜新安装的VersArray1340×1300BCCD照相机的性能。它有几乎没有图案的良好本底(bias),极低的读出噪声和暗流。用平场序列露光来检测其线性时,能得到线性良好的转移曲线(transfercurve)。但是,不论在平场露光(面光源)还是在恒星(点光源)的观测中,当像元值约高于55000adu时(增益3.7e^-/adu),都会产生溢出。此时CCD并未满井。因此,使用它做点扩散函数分析研究时,要避免使用太亮的星像。不过,由于电荷守恒原理,对产生溢出的孤立亮星像,仍然可以做孔径测光。此外,该相机的快门函数也已测定。 相似文献
145.
利用线阵CCD分辨率高、像素均匀等特点对光栅莫尔条纹进行细分是目前广泛采用的一种新技术。由于CCD具有自扫描能力,能将光强随空间分布的莫尔条纹信号转换成随时间变化的电信号,从而可以对光栅刻线的像的移动进行精确定位和直接数字化,改变传统莫尔条纹位相细分方法,实现对光栅栅距进行高倍数的细分。 相似文献
146.
��������ұ궨�Զ�����ϵͳ 总被引:1,自引:0,他引:1
?????Я???????????????????????????????????????????????????????????????????????????????????????????????????????????????????????????????????????? 相似文献
147.
148.
Artificial neural networks are used to predict the micro‐properties of particle flow code in three dimensions (PFC3D) models needed to reproduce macro‐properties of cylindrical rock samples in uniaxial compression tests. Data for the training and verification of the networks were obtained by running a large number of PFC3D models and observing the resulting macro‐properties. Four artificial networks based on two different architectures were used. The networks used different numbers of input parameters to predict the micro‐properties. Multi‐layer perceptron networks using Young's modulus, Poisson's ratio, uniaxial compressive strength, model particle resolution and the maximum‐to‐minimum particle ratio showed excellent performance in both training and verification. Adding one more variable—namely, minimum particle radius—showed degrading performance. Copyright © 2009 John Wiley & Sons, Ltd. 相似文献
149.
The first application of the SHETRAN basin‐scale, landslide erosion and sediment yield model is carried out for a major landsliding event in the upper 505 km2 of the Llobregat basin, in the eastern Spanish Pyrenees, in November 1982. The model simulates the spatial distribution of shallow landslides and their sediment yield. Acknowledging uncertainty in the model parameter evaluation, the aim of the application was not to reproduce the observed occurrence of landslides as accurately as possible with one simulation, but to bracket the observed pattern with several simulations representing uncertainty in the key input conditions. Bounds on the landslide simulations were thus determined as a function of uncertainty in the vegetation root cohesion (used in the model factor of safety calculations). The resulting upper bound considerably overestimates the observed pattern (17 000 landslides compared with an observation of around 700), but it reproduces several of the principal clusters in the observed pattern. The lower bound contains around 500 landslides. The sediment yield estimates (2670–14 630 t km?2) are comparable to measurements elsewhere in the Pyrenees for extreme events. The results demonstrate an ability to simulate the basin‐scale landslide response to a rainfall event and the resulting sediment yield. They also highlight the need for further research in setting the uncertainty bounds and in avoiding large overestimates of landslide occurrence arising in part from a current inability to model small‐scale controls for a basin of the given size. Copyright © 2006 John Wiley & Sons, Ltd. 相似文献
150.
SARAL/AltiKa has a Dual Frequency Microwave Radiometer (DFMR), and Jason-2 has an Advanced Microwave Radiometer (AMR). Both microwave radiometer sensors include a 23.8 GHz primary water sensing channel. The measurement consistencies between DFMR and AMR are important for establishing a consistent altimetry data set between SARAL/AltiKa and Jason-2 in order to accurately assess sea level rise in a long-term time series. This study investigates the measurement consistency in the 23.8 GHz channel between DFMR and AMR at the Simultaneous Nadir Overpasses (SNO's) between the two satellites and also at coldest ocean brightness temperature locations. Preliminary results show that while both instruments show no significant trends over the one year since the launch of SARAL, a consistent relative bias of 2.88 K (DFMR higher than AMR) with a standard deviation of 0.98 K is observed. The relative bias at the lowest brightness temperature from the SNO method (-3.82 K) is consistent with that calculated from coldest ocean method (-3.74 K). The relative bias exhibits strong latitude (and scene temperature) dependency, changing from -3.82 K at high latitudes to -0.92 K near the equator. There also exists an asymmetry between the northern and southern hemisphere. The relative bias increases toward the lower end of brightness temperature. 相似文献