全文获取类型
收费全文 | 2435篇 |
免费 | 319篇 |
国内免费 | 366篇 |
专业分类
测绘学 | 208篇 |
大气科学 | 286篇 |
地球物理 | 696篇 |
地质学 | 1021篇 |
海洋学 | 343篇 |
天文学 | 126篇 |
综合类 | 161篇 |
自然地理 | 279篇 |
出版年
2024年 | 10篇 |
2023年 | 39篇 |
2022年 | 103篇 |
2021年 | 112篇 |
2020年 | 107篇 |
2019年 | 107篇 |
2018年 | 146篇 |
2017年 | 120篇 |
2016年 | 124篇 |
2015年 | 120篇 |
2014年 | 151篇 |
2013年 | 133篇 |
2012年 | 126篇 |
2011年 | 156篇 |
2010年 | 136篇 |
2009年 | 139篇 |
2008年 | 112篇 |
2007年 | 103篇 |
2006年 | 82篇 |
2005年 | 78篇 |
2004年 | 74篇 |
2003年 | 77篇 |
2002年 | 117篇 |
2001年 | 100篇 |
2000年 | 69篇 |
1999年 | 48篇 |
1998年 | 59篇 |
1997年 | 57篇 |
1996年 | 36篇 |
1995年 | 42篇 |
1994年 | 29篇 |
1993年 | 28篇 |
1992年 | 34篇 |
1991年 | 18篇 |
1990年 | 10篇 |
1989年 | 18篇 |
1988年 | 9篇 |
1987年 | 9篇 |
1986年 | 4篇 |
1985年 | 7篇 |
1984年 | 6篇 |
1983年 | 6篇 |
1982年 | 5篇 |
1981年 | 7篇 |
1980年 | 10篇 |
1979年 | 7篇 |
1978年 | 8篇 |
1976年 | 3篇 |
1975年 | 5篇 |
1973年 | 3篇 |
排序方式: 共有3120条查询结果,搜索用时 31 毫秒
961.
962.
改进的双参数层状地基模型 总被引:8,自引:3,他引:5
文克尔地基模型广泛应用于弹性地基梁、板的设计计算,但由于该模型过于简化,不能正确反映地基土的工程性质。为此,提出了一种改进的双参数层状地基模型。该模型是Vlazov模型的延伸和发展,由一系列的弹性层组成,对每一层的应力应变分布做了一定的假设。通过积分变换的方法,可以求出该模型每一层表面位移与力的关系,进而形成层刚度矩阵。按照有限元法的原理,将每一层的刚度矩阵凝聚成总体刚度矩阵求解,与Vlazov模型计算结果的比较,证明该方法是正确的,还得到了荷载作用于层状地基模型内部的解,为双参数层状地基模型用于桩基分析打下了理论基础。 相似文献
963.
964.
965.
966.
967.
968.
Yalu Hu Rui Ma Yanxin Wang Qixin Chang Shuo Wang Mengyan Ge Jianwei Bu Ziyong Sun 《水文研究》2019,33(14):1942-1960
Significant uncertainty remains in understanding the groundwater flow pathways in the northeastern Qinghai–Tibet Plateau. Hydrogeochemical and isotopic data as well as hydrogeological data were combined to explore the groundwater flow path in a representative cold alpine catchment in the headwater region of the Heihe River. The results indicate that the suprapermafrost groundwater chemical components were mainly affected by calcite dissolution and evaporation, whereas the geochemistry of subpermafrost groundwater was controlled by dolomite and gypsum dissolution, calcite precipitation, and albite and halite dissolution. Distinct hydrogeochemical characteristics and controlling processes suggest a poor hydraulic connectivity between the suprapermafrost and subpermafrost groundwater. The hydraulic connectivity between permafrost groundwater and groundwater in the seasonally frozen area was confirmed by their similar hydrogeochemical features. In the seasonally frozen area, a silty clay layer with low permeability separates the aquifer into the deep (depth >20 m) and shallow (depth <20 m) flow paths. The deep groundwater was characterized by the enhanced dedolomitization and enhanced cation exchange processes compared with the shallow groundwater. Groundwater in the seasonally frozen area finally discharges as base flow into the stream. These results provide useful information about the groundwater flow systems in the unique alpine gorge catchments in Qinghai–Tibet Plateau. The above findings suggest that the permafrost distribution and the aquifer structures within the seasonally frozen area have significant impact on groundwater flow paths. Cross‐validation by drilling work and hydrograph data confirms that the hydrogeochemical and isotopic tracers combined with field investigations can be relatively low‐cost tools in interpreting the groundwater flow paths in similar alpine catchments. 相似文献
969.
Wen-Chen Chou Gwo-Ching Gong Chun-Mao Tseng David D. Sheu Chin-Chang Hung Lo-Ping Chang Li-Wen Wang 《Marine Chemistry》2011,123(1-4):44-55
Measurements of dissolved inorganic carbon (DIC), pH, total alkalinity (TA), and partial pressure of CO2 (pCO2) were conducted at a total of 25 stations along four cross shelf transects in the East China Sea (ECS) in January 2008. Results showed that their distributions in the surface water corresponded well to the general circulation pattern in the ECS. Low DIC and pCO2 and high pH were found in the warm and saline Kuroshio Current water flowing northeastward along the shelf break, whereas high DIC and pCO2 and low pH were mainly observed in the cold and less saline China Coastal Current water flowing southward along the coast of Mainland China. Difference between surface water and atmospheric pCO2 (ΔpCO2), ranging from ~ 0 to ? 111 μatm, indicated that the entire ECS shelf acted as a CO2 sink during winter with an average flux of CO2 of ?13.7 ± 5.7 (mmol C m? 2 day? 1), and is consistent with previous studies. However, pCO2 was negatively correlated with temperature for surface waters lower than 20 °C, in contrast to the positive correlation found in the 1990s. Moreover, the wintertime ΔpCO2 in the inner shelf near the Changjiang River estuary has appreciably decreased since the early 1990s, suggesting a decline of CO2 sequestration capacity in this region. However, the actual causes for the observed relationship between these decadal changes and the increased eutrophication over recent decades are worth further study. 相似文献
970.