全文获取类型
收费全文 | 650篇 |
免费 | 125篇 |
国内免费 | 127篇 |
专业分类
测绘学 | 32篇 |
大气科学 | 26篇 |
地球物理 | 104篇 |
地质学 | 524篇 |
海洋学 | 46篇 |
综合类 | 39篇 |
自然地理 | 131篇 |
出版年
2024年 | 5篇 |
2023年 | 4篇 |
2022年 | 16篇 |
2021年 | 26篇 |
2020年 | 25篇 |
2019年 | 31篇 |
2018年 | 16篇 |
2017年 | 19篇 |
2016年 | 17篇 |
2015年 | 37篇 |
2014年 | 43篇 |
2013年 | 51篇 |
2012年 | 33篇 |
2011年 | 44篇 |
2010年 | 47篇 |
2009年 | 41篇 |
2008年 | 55篇 |
2007年 | 39篇 |
2006年 | 37篇 |
2005年 | 45篇 |
2004年 | 38篇 |
2003年 | 23篇 |
2002年 | 32篇 |
2001年 | 26篇 |
2000年 | 22篇 |
1999年 | 21篇 |
1998年 | 18篇 |
1997年 | 16篇 |
1996年 | 8篇 |
1995年 | 8篇 |
1994年 | 19篇 |
1993年 | 10篇 |
1992年 | 7篇 |
1991年 | 4篇 |
1990年 | 5篇 |
1989年 | 4篇 |
1988年 | 1篇 |
1987年 | 2篇 |
1986年 | 2篇 |
1985年 | 3篇 |
1983年 | 1篇 |
1979年 | 1篇 |
排序方式: 共有902条查询结果,搜索用时 0 毫秒
61.
62.
珠江三角洲经过系统的1∶250000区域土壤地球化学调查发现,在三角洲冲积平原存在氟的高含量分布区。氟高含量区分布于第四纪海相和海陆交互相,从海相→海陆交互相→陆相含量逐渐降低,相同沉积相含量变化很小。从地表至深部,含量变化与沉积相关系密切,海陆交互相含量变化很小,而陆相含量变化较大。氟高含量区空间分布特征明显,控制因素显著,属于在沉积地质作用过程形成的。可能与珠江三角洲形成过程,西江、北江和东江带来大量含氟物质,加上海水富含氟,导致海相和海陆交互相沉积物氟含量较高而出现大面积的高含量区。 相似文献
63.
64.
65.
元素地球化学研究表明,长江与黄河对冰后期的苏北滨海平原发育与苏北南黄海潮成砂体的形成影响巨大。冰后期早期长江物质影响大于黄河。黄河供给泥沙量较少,且对本区影响主要在北部、中部地区。公元1128年黄河改道由苏北入海之后,黄河影响范围明显大于长江。长江仅由个别狭窄的汊道提供有限的物质而影响范围较小。古长江主流并未由琼港地区入海,而携带大量物质建设潮成砂体。最近2000年来本区沉积物主要由黄河提供。分析表明元素地球化学方法在沉积物物源判别时,可有效的避免水动力因素影响,取得较好的效果。 相似文献
66.
67.
68.
ABSTRACTThe point dilution test is a single-well technique for estimating horizontal flow velocity in the aquifer surrounding a well. The test is conducted by introducing a tracer into a well section and monitoring its decreasing concentration over time. When using a salt tracer, the method is easy and inexpensive. Traditionally, the horizontal Darcy velocity is calculated as a function of the rate of dilution and is based on the simple assumption that the decreasing tracer concentration is proportional both to the apparent velocity into the test section and to the Darcy velocity in the aquifer. In this article, an alternative approach to analyse the results of point dilution tests is proposed and verified using data acquired at a test site in the middle Venetian plain, northeast Italy. In this approach, the one-dimensional equilibrium advection–dispersion equation is inverted using the CXTFIT model to estimate the apparent velocity inside the test section. Analysis of the field data obtained by the two approaches shows good agreement between the methods and suggests that it is possible to use the equilibrium advection–dispersion equation to estimate apparent velocity over a wide range of velocities.
Editor D. Koutsoyiannis; Associate editor K. Heal 相似文献
69.
The lower coastal plain of the Southeast USA is undergoing rapid urbanisation as a result of population growth. Land use change has been shown to affect watershed hydrology by altering stream flow and, ultimately, impairing water quality and ecologic health. However, because few long‐term studies have focused on groundwater–surface water interactions in lowland watersheds, it is difficult to establish what the effect of development might be in the coastal plain region. The objective of this study was to use an innovative improvement to end‐member mixing analysis (EMMA) to identify time sequences of hydrologic processes affecting storm flow. Hydrologic and major ion chemical data from groundwater, soil water, precipitation and stream sites were collected over a 2‐year period at a watershed located in USDA Forest Service's Santee Experimental Forest near Charleston, South Carolina, USA. Stream flow was ephemeral and highly dependent on evapotranspiration rates and rainfall amount and intensity. Hydrograph separation for a series of storm events using EMMA allowed us to identify precipitation, riparian groundwater and streambed groundwater as main sources to stream flow, although source contribution varied as a function of antecedent soil moisture condition. Precipitation, as runoff, dominated stream flow during all storm events while riparian and streambed groundwater contributions varied and were mainly dependent on antecedent soil moisture condition. Sensitivity analyses examined the influence of 10% and 50% increases in analyte concentration on EMMA calculations and found that contribution estimates were very sensitive to changes in chemistry. This study has implications on the type of methodology used in traditional forms of EMMA research, particularly in the recognition and use of median end‐member water chemistry in hydrograph separation techniques. Potential effects of urban development on important hydrologic processes (groundwater recharge, interflow, runoff, etc.) that influence stream flow in these lowland watersheds were qualitatively examined. Copyright © 2011 John Wiley & Sons, Ltd. 相似文献
70.
山西寿阳—阳泉地区石炭—二叠系沉积环境及其沉积特征 总被引:1,自引:0,他引:1
本区石炭—二叠系是在海湾背景下发育的一套由滨海平原—三角洲平原—冲积平原沉积组成的海退层系。主要沉积环境是三角洲平原,其上部为冲积平原包括网状河和辫状河;下部为海湾(或分支间湾)、潮下碳酸盐岩、潮间介壳滩、碎屑岩潮坪及滨海沼泽湿地等。三角洲为河控浅水三角洲。上述沉积环境,随海水退却在时空上具明显的规律性变化。 相似文献