全文获取类型
收费全文 | 394篇 |
免费 | 45篇 |
国内免费 | 65篇 |
专业分类
测绘学 | 33篇 |
大气科学 | 58篇 |
地球物理 | 89篇 |
地质学 | 197篇 |
海洋学 | 29篇 |
天文学 | 21篇 |
综合类 | 34篇 |
自然地理 | 43篇 |
出版年
2024年 | 1篇 |
2023年 | 3篇 |
2022年 | 12篇 |
2021年 | 23篇 |
2020年 | 19篇 |
2019年 | 12篇 |
2018年 | 29篇 |
2017年 | 28篇 |
2016年 | 27篇 |
2015年 | 20篇 |
2014年 | 31篇 |
2013年 | 29篇 |
2012年 | 22篇 |
2011年 | 17篇 |
2010年 | 27篇 |
2009年 | 27篇 |
2008年 | 17篇 |
2007年 | 14篇 |
2006年 | 14篇 |
2005年 | 9篇 |
2004年 | 8篇 |
2003年 | 12篇 |
2002年 | 4篇 |
2001年 | 5篇 |
2000年 | 9篇 |
1999年 | 11篇 |
1998年 | 16篇 |
1997年 | 10篇 |
1996年 | 9篇 |
1995年 | 6篇 |
1994年 | 4篇 |
1993年 | 7篇 |
1992年 | 4篇 |
1991年 | 4篇 |
1990年 | 1篇 |
1989年 | 2篇 |
1988年 | 3篇 |
1987年 | 1篇 |
1986年 | 1篇 |
1985年 | 1篇 |
1984年 | 1篇 |
1983年 | 1篇 |
1982年 | 2篇 |
1958年 | 1篇 |
排序方式: 共有504条查询结果,搜索用时 15 毫秒
101.
矿山开采活动中地下水与生态环境保护是需要综合利用多学科思想与理论解决的难题,仅从采矿工程学角度难以解决根本问题。文中从生态水文地质学的角度,针对陕北采煤安全必须疏排水和陕北能源基地建设亟须水资源支撑的现状,提出了通过充分地利用煤田地下水满足强劲用水需求来保护水资源的对策,并从矿区水文地质结构、地下水循环条件出发,根据矿区植被生态风险区划、采煤影响地下水区划,提出了建立保护矿山水资源的采煤秩序、不同阶段地下水保护与开发利用区划以及矿山掘进过程中保护性开采地下水的水源地布局规划原则与建设方案。 相似文献
102.
Anh Phan Luu Vladimirov A. G. Kruk N. N. Polyakov G. V. Ponomarchuk V. A. Hoa Tran Trong Phuong Ngo Thi Kuibida M. L. Annikova I. Yu. Pavlova G. G. Kiseleva V. Yu. 《Doklady Earth Sciences》2010,432(2):839-845
Doklady Earth Sciences - Stanniferrous granite-leucogranite massifs in Vietnam to which the bedrock and placer commercial deposits of cassiterite are associated (Timtuc etc.) are of late Cretaceous... 相似文献
103.
In order to understand the effects of a landfill operation on groundwater flow behavior, a 2D horizontal groundwater simulation
model was carried out. The model saved the memory of computer and time consumption, comparing it with the 3D groundwater flow
model. However, the greatest difficulty is the assignment of the collecting pipe boundary at the study site. Therefore, a
2D vertical model was applied to calculate the change of the groundwater table above the collecting pipe. This paper focuses
on examining the validation of the assignment of the collecting pipe boundary by applying the results of the 2D vertical model.
The 2D horizontal model was coupled with the recharge model to solve the partial differential equation of groundwater flow.
The finite difference method and iterative successive over relaxation were applied. The drainage volume of leachate collection
was summed up in the whole landfill site and compared with the average volume of treated wastewater. The study demonstrated
that the results of the 2D vertical model validated and can be applied to the 2D horizontal groundwater flow simulation. 相似文献
104.
105.
D. Lutz R. Genzel D. Kunze D. Rigopoulou H.W.W. Spoon E. Sturm D. Tran A.F.M. Moorwood 《Astrophysics and Space Science》1999,266(1-2):85-90
Spectroscopy from the Infrared Space Observatory ISO has for the first timeprovided the sensitivity to exploit the diagnostic power ofmid-infrared fine structure lines and PAH features for the study ofultraluminous infrared galaxies (LIR >1012
L
). We report on observations obtainedwith SWS, ISOPHOT-S, and the CVF option of ISOCAM. From both fine structure lines and PAH features, we find that the majority of ULIRGs is predominantlypowered by star formation. Our total sample of about 75 ULIRGs allows tosearch for trends within the class of ULIRGs: The fraction of AGNs increaseswith luminosity above 3 × 1012L but there is no obvioustrend for ULIRGs to be more AGN-like with more advanced merger phase. 相似文献
106.
107.
五台山早前寒武纪变质岩中的白云母属二八面体的2M型多型变体,其中五台群中的白云母为富含绿鳞石分子的普通白云母,滹沱群为多硅白云母。通过对这些白云母化学成分和b_0值测定,确定五台群变质条件属中低压相系,滹沱群属中高压相系。五台群绿片岩相的变质压力为0.3—0.5 GPa,滹沱群为0.5—0.6 GPa。基于白云母成分和b_0值的研究,对划分变质级别、变质类型;确定变质作用期次;进行地层对比和构造分析等方面是可行的。 相似文献
108.
利用数十口井的电性、岩性及分析化验资料,将柴达木盆地西部地区古近纪与新近纪沉积相划分为七种相和亚相:洪积锥、水下冲积扇、河道和泛滥平原、滨湖、浅湖、较深湖和三角洲。沉积相的空间展布概括起来分为三大带:(1)阿尔金山前西段陡坡带洪积锥-水下冲积扇-扇三角洲-河道和泛滥平原-湖相 (2)阿尔金山前中段陡坡带洪积锥-水下冲积扇-湖相;(3)昆仑山前洪积锥-河道和泛滥平原-三角洲相。沉积相不仅影响着碎屑岩的成分和结构,而且也影响其物性与含油性。由洪积锥到水下冲积扇,到河道和泛滥平原,到三角洲,到湖相,石英和胶结物含量逐渐升高,岩屑和杂基含量逐渐降低,分选及磨圆变好,颗粒的粒级变细。浅层以河道和泛滥平原及三角洲相的物性最好,深层以三角洲相的物性最好,次为冲积扇,湖相最差。碎屑岩的油气富集以河道、泛滥平原和三角洲相最好,滨浅湖相油气富集最差。 相似文献
109.
Geochemistry and origin of the giant Quaternary shallow gas accumulations in the eastern Qaidam Basin, NW China 总被引:1,自引:0,他引:1
Xiongqi Pang Wenzhi Zhao Aiguo Su Shuichang Zhang Maowen Li Yiqi Dang Fengying Xu Ruilian Zhou Daowei Zhang Ziyuan Xu Zhiqiang Guan Jianfa Chen Sumei Li 《Organic Geochemistry》2005,36(12):1636
This study provided an overview of the geological setting and geochemical characteristics of the Pleistocene shallow gas accumulations in the eastern Qaidam Basin, NW China. The five largest gas accumulations discovered in this region have a combined enclosure area of about 87 km2 and 7.9 trillion cubic feet (tcf) of proven gas reserves. The dominance of methane (mostly more than 99.9%) and the δ13C and δD values of methane (−68.51 to −65.00‰ and −227.55 to −221.94‰, respectively) suggest that these gases are biogenic, derived from the degradation of sedimentary organic matter by methanogens under relatively low temperatures (<75 °C). A sufficient supply and adequate preservation of organic matter in the Pleistocene sediments was made possible by the lake basin’s high altitude (2600–3000 m), high water salinity (>15% TDS) and strong stratification. The deposition and extensive lateral occurrence of lacustrine – shoreline sands/silts in beach sand sheets and sand bars provided excellent reservoirs for the biogenic gas generated from adjacent rocks. Effective but dynamic gas seals are provided by a combination of factors, such as the intermittent vertical variation in the sediment lithologies, hydraulic trapping due to the mudstone water saturation, the hydrocarbon gradient created as the result of gas generation from potential caprocks, and the presence of a regional caprock consisting of 400–800 m of muds and evaporites. It appears that the most favorable traps for large gas accumulations occur on structural slopes near the major gas kitchen, and the prolific gas pools are often those large gentle anticlines with little faulting complication. 相似文献
110.
Yi Yong Park Suong Oh Lee Tam Tran Seong Jun Kim Myong Jun Kim 《International Journal of Mineral Processing》2006,80(2-4):126-132
A simple process to produce fine and low soda α-alumina (α-Al2O3) from a commercial grade aluminium trihydroxide (gibbsite, Al(OH)3) produced by KC Corporation Ltd was developed. There are two options for this process with the first one producing low soda α-alumina (< 0.05% Na2O) having a mean particle size of 50 μm. The second option yields a fine product with a mean size of less than 10 μm. In the first option, a plant aluminium trihydroxide containing 0.20% Na2O was first fluidized with nitrogen at 400–600 °C to yield an amorphous activated alumina. This intermediate product was then treated with acetic or oxalic acid, washed with water and heated to 1200 °C to form calcined α-alumina, having a Na2O content of less than 0.05%. A 20 min leaching using 0.2 M acetic or oxalic acid could yield an alumina product containing 0.04% Na2O. In the second option, a new technique for the preparation of fine and low soda α-alumina was evaluated using an attrition mill working also as a leaching vessel at 80 °C. Fine (< 10 μm in mean particle size) and low soda (< 0.04% Na2O) alumina was produced by a 20 min leaching step with 0.2 M acetic acid and concurrent attrition milling. 相似文献