全文获取类型
收费全文 | 1740篇 |
免费 | 389篇 |
国内免费 | 372篇 |
专业分类
测绘学 | 37篇 |
大气科学 | 194篇 |
地球物理 | 411篇 |
地质学 | 492篇 |
海洋学 | 1179篇 |
天文学 | 26篇 |
综合类 | 90篇 |
自然地理 | 72篇 |
出版年
2024年 | 5篇 |
2023年 | 25篇 |
2022年 | 45篇 |
2021年 | 67篇 |
2020年 | 53篇 |
2019年 | 67篇 |
2018年 | 50篇 |
2017年 | 66篇 |
2016年 | 70篇 |
2015年 | 72篇 |
2014年 | 109篇 |
2013年 | 93篇 |
2012年 | 104篇 |
2011年 | 94篇 |
2010年 | 100篇 |
2009年 | 121篇 |
2008年 | 117篇 |
2007年 | 138篇 |
2006年 | 109篇 |
2005年 | 86篇 |
2004年 | 104篇 |
2003年 | 82篇 |
2002年 | 93篇 |
2001年 | 73篇 |
2000年 | 66篇 |
1999年 | 78篇 |
1998年 | 65篇 |
1997年 | 56篇 |
1996年 | 36篇 |
1995年 | 34篇 |
1994年 | 46篇 |
1993年 | 37篇 |
1992年 | 29篇 |
1991年 | 27篇 |
1990年 | 16篇 |
1989年 | 18篇 |
1988年 | 12篇 |
1987年 | 6篇 |
1986年 | 2篇 |
1985年 | 9篇 |
1984年 | 3篇 |
1983年 | 4篇 |
1982年 | 7篇 |
1981年 | 2篇 |
1980年 | 2篇 |
1979年 | 3篇 |
排序方式: 共有2501条查询结果,搜索用时 31 毫秒
101.
随着64排以上多层螺旋CT(MSCT)和双源CT(DSCT)的飞速发展,CT冠状动脉成像(CTCA)以其无创、便捷、低风险和低费用等优越性,在临床上得到了越来越广泛应用。但较复杂的心脏血管成像,往往伴随着较高的辐射剂量,因此这就大大地增加了患恶性肿瘤的几率。近年来,CTCA辐射量的问题得到了不少学者的关注,对如何低剂量CTCA做了大量的研究,而管电流与管电压的调节在CT低剂量冠状动脉成像起着重要作用,本文综述了当前管电流与管电压参数优化应用的总体状况,并认为在保证CTCA图像质量的前提下,对于体重指数正常、心率稳定、冠状动脉钙化总评分在100AU以下的患者,采用降低管电压扫描可明显减少辐射剂量,若再联合应用ECG调制电流曝光技术,将进一步减少辐射剂量。但对于肥胖体重、心律不齐及钙化较多者则不适用低剂量CTCA检查。 相似文献
102.
浙江近海夏季流场特征分析 总被引:1,自引:0,他引:1
为了揭示浙江近岸流场特征及沿程变化规律,于2006年和2009年夏季在浙江岸外3个固定点利用ADCP潜标进行了多个潮周期分层海流流速、流向观测。研究结果表明:(1)浙江沿岸流在中北部海域(A和B站位)为旋转流,流向呈顺时针方向旋转,在南部(C站位)涨潮流方向基本为北向,落潮方向为东偏北向;各站位海流在垂向上流向较一致。(2)3个站位垂线平均流速相近(44.4~51.1 cm/s),但平均流速的垂向分布差异明显;各站的最大流速均大于110 cm/s,且均出现在大潮涨急时刻。(3)观测期间,A(北部)、B(中北部)和C(南部)站位平均余流的大小分别为21.9,12.3和22.3 cm/s;受长江冲淡水影响,A和B站位中上层余流为西南向,从中层向底层流向呈逆时针方向偏转,下层流向呈东南向,可能为台湾暖流牵引所致,C站位余流流向在垂向较为一致,均为东北向,主要受季风影响。(4)夏季浙江沿岸流在沿浙江沿岸北上的过程中,在浙江中部(B和C站位中间)逐渐向东偏转(可能受台湾暖流的牵引),流经海域水深变大。(5)在夏季长江径流量偏小时段,浙江中北部近岸海域也存在向南的沿岸流(同冬季),其范围从长江口以南一直至浙江中北部。浙江近岸海流受季风、长江冲淡水和台湾暖流共同制约,但各区域的主要受控因素不同。 相似文献
103.
104.
赤道环电流是引起磁暴扰动的主要电流体系,环电流衰减速率极大地影响着磁层能量收支估计和磁暴预报.本文提出评价环电流衰减率的两条新指标;(1)E指标(磁暴事件总能量收支平衡指标),即磁暴全过程的积分能量收支平衡;(2)L指标(长期总能量收支平衡指标),即几年、十几年或更长时段内积分能量收支平衡.我们用1998~2003年44个磁暴事件以及第23太阳周(1998~2008年)11年的连续资料,分别检验了几类衰减率模型对上述两条指标符合的情况.结果表明,PA1978和XD2010两类模型对E指标符合得最好,即无论磁暴强弱,它们均显示出事件总能量收支平衡的基本特征;同时,这两类模型与L指标符合得也最好,即它们的长期积分能量基本平衡,而且磁暴期间的能量消耗表现出明显增强的重要特征. 相似文献
105.
Boundary shear stress and flow variability due to its interaction with main flow and secondary currents were investigated under conditions that extend previous research on trapezoidal channels. Secondary currents that scale with the flow depth were found over the entire width in all experiments. These findings contradict the widespread perception that secondary currents die out at a distance of 2.5 times the flow depth from the bank, a perception which is largely based on experiments with smooth boundaries. The reported results indicate that a stable pattern of secondary currents over the entire channel width can only be sustained over a fixed horizontal bed if the bed's roughness is sufficient to provide the required transverse oscillations in the turbulent shear stresses. Contrary to laboratory flumes, alluvial river bed always provide sufficient roughness. The required external forcing of this hydrodynamic instability mechanism is provided by the turbulence-generated near-bank secondary currents. The pattern of near-bank secondary currents depends on the inclination and the roughness of the bank. In all configurations, secondary currents result in a reduction of the bed shear stress in the vicinity of the bank and a heterogeneous bank shear stress that reaches a maximum close to the toe of the bank. Moreover, these currents cause transverse variability of 10–15% for the streamwise velocities and 0.2u*2–0.3u*?2 for the bed shear stress. These variations are insufficient to provide the flow variability required in river restoration projects, but nevertheless must be accounted for in the design of stable channels. 相似文献
106.
The spatio-temporal variability of submesoscale eddies off southern San Diego is investigated with two-year observations of subinertial surface currents [O(1) m depth] derived from shore-based high-frequency radars. The kinematic and dynamic quantities — velocity potential, stream function, divergence, vorticity, and deformation rates — are directly estimated from radial velocity maps using optimal interpolation. For eddy detection, the winding-angle approach based on flow geometry is applied to the calculated stream function. A cluster of nearly enclosed streamlines with persistent vorticity in time is identified as an eddy. About 700 eddies were detected for each rotation (clockwise and counter-clockwise). The two rotations show similar statistics with diameters in the range of 5–25 km and Rossby number of 0.2–2. They persist for 1–7 days with weak seasonality and migrate with a translation speed of 4–15 cm s−1 advected by background currents. The horizontal structure of eddies exhibits nearly symmetric tangential velocity with a maximum at the defined radius of the eddy, non-zero radial velocity due to background flows, and Gaussian vorticity with the highest value at the center. In contrast divergence has no consistent spatial shape. Two episodic events are presented with other in situ data (subsurface current and temperature profiles, and local winds) as an example of frontal-scale secondary circulation associated with drifting submesoscale eddies. 相似文献
107.
108.
直流电阻率法装置种类较多,根据实际地质条件选用不同的装置类型,通过对探测结果进行综合对比分析,可全面地反映地下洞室赋存状态.通过对一地下人工洞室进行多种装置类型直流电阻率法勘查,综合分析了各种装置类型探测结果的视电阻率异常特征,并论述了直流电阻率法探测地下人工洞室的有效性. 相似文献
109.
Fourteen acoustic Doppler current profilers (ADCPs) were deployed on the shelf and slope for 1 year just west of the DeSoto Canyon in the Northeastern Gulf of Mexico by the Naval Research Laboratory (NRL) as part of its Slope to Shelf Energetics and Exchange Dynamics (SEED) project. The winter and spring observations are discussed here in regards to the low-frequency current variability and its relation to wind and eddy forcing. Empirical orthogonal function (EOF) analyses showed that two modes described most of the current variability. Wind-forced variability of the along-shelf flow was the main contributor in Mode 1 while eddies contributed much of the variability in Mode 2. Wind-stress controlled currents on the shelf and slope at time scales of about a week. On longer time scales, variations in the currents on both the outer shelf and slope appear to be related to seasonal variations in the time-cumulated wind stress curl. Winds were dominant in driving the along-shelf transports, particularly along the slope. However, the effective wind stress component was found to be aligned with the west Florida shelf direction rather than the local shelf direction. Eddy intrusions, which were more numerous in winter and spring than in summer and fall, and winds were found to contribute significantly to cross-shelf exchange processes. 相似文献
110.
The cross-shore variation of long-term average longshore current velocity was investigated on the basis of a 15-year data set of longshore current, wave and wind. The longshore current velocities were measured once a day along a 427-m-long pier. The results show that the direction of the long-term average longshore current velocity away (>200 m) from the shore was the opposite to that near the shore. The southward current was dominant offshore, whereas the northward current was dominant near the shore. The cross-shore variation of the long-term average longshore current velocity was formed owing to a difference between the wave and wind conditions when the northward and southward currents developed. When the northward current developed, the offshore wave height was relatively small and the frequency of the southward wind velocity was almost equal to that of the northward one. As a result, the northward current developed only near the shore and decayed outside the narrow surf zone. On the other hand, when the southward current developed, the offshore wave height was relatively large and the southward wind velocity was predominant, which resulted in the southward current developing not only in the wide surf zone but also outside the surf zone. The superposition of the two cross-shore variations produced a cross-shore variation of the long-term average longshore current velocity with a northward velocity near the shore and a southward velocity away from the shore. 相似文献