全文获取类型
收费全文 | 1023篇 |
免费 | 159篇 |
国内免费 | 404篇 |
专业分类
测绘学 | 6篇 |
大气科学 | 135篇 |
地球物理 | 160篇 |
地质学 | 1016篇 |
海洋学 | 176篇 |
天文学 | 5篇 |
综合类 | 33篇 |
自然地理 | 55篇 |
出版年
2024年 | 4篇 |
2023年 | 27篇 |
2022年 | 31篇 |
2021年 | 40篇 |
2020年 | 40篇 |
2019年 | 33篇 |
2018年 | 45篇 |
2017年 | 31篇 |
2016年 | 40篇 |
2015年 | 40篇 |
2014年 | 58篇 |
2013年 | 64篇 |
2012年 | 56篇 |
2011年 | 68篇 |
2010年 | 63篇 |
2009年 | 64篇 |
2008年 | 90篇 |
2007年 | 92篇 |
2006年 | 90篇 |
2005年 | 55篇 |
2004年 | 59篇 |
2003年 | 69篇 |
2002年 | 61篇 |
2001年 | 57篇 |
2000年 | 43篇 |
1999年 | 41篇 |
1998年 | 61篇 |
1997年 | 32篇 |
1996年 | 25篇 |
1995年 | 26篇 |
1994年 | 13篇 |
1993年 | 10篇 |
1992年 | 4篇 |
1991年 | 7篇 |
1990年 | 9篇 |
1989年 | 5篇 |
1988年 | 5篇 |
1987年 | 6篇 |
1986年 | 6篇 |
1985年 | 9篇 |
1984年 | 4篇 |
1983年 | 1篇 |
1982年 | 2篇 |
排序方式: 共有1586条查询结果,搜索用时 15 毫秒
31.
32.
光催化氧化法处理难降解废水的研究进展 总被引:8,自引:3,他引:8
综述了光催化氧化处理难降解废水的研究现状及发展趋势。介绍了影响光催化氧化反应速率的因素及光催化氧化法在处理难降解废水中的应用。 相似文献
33.
通过对近几年来十红滩地区铀矿勘查资料及找矿成果的综合研究,系统阐述了吐哈盆地西南缘十红滩矿床的地质构造、含矿岩系沉积环境、砂体分布、层问氧化带发育特征等铀成矿条件,对矿区南、北矿带控矿层间氧化带分带性、矿体形态、规模、空间展布、铀存在形式、成矿年龄及铀成矿规律进行了详细研究。进一步总结了区域砂岩型铀成矿条件和找矿前景,指出吐哈盆地西南缘随着找矿工作进展可望成为大型地浸砂岩型铀资源基地,并对指导天山造山带及类似地区地浸砂岩型铀矿找矿具有重要意义。 相似文献
34.
运用烃类勘察地球化学方法,对鄂尔多斯盆地南部彬县大佛寺井田钻遇中休罗统煤层的耽钻孔,进行了垂向剖面多指标的综合地球化学研究。结果表明:剖面中所有岩样中的烃类物质均为热解烃生成初期演化阶段的煤成烃产物,具明显的同一性;由煤层至地表黄土,所有岩样中的烃类呈明显的、规律性垂直向上运移。这证实地下煤层烃类在近地表具有很好的地球化学信息显示,利用勘察地球化学方法找煤/煤层气是可行的。 相似文献
35.
介绍了自然电场形成的原理及在寻找层间氧化带砂岩型铀矿中的应用.根据氧化带与还原带的自然电位变化特征,利用自然电场法可以确定盆地层间氧化带前锋线,由此推测层间氧化带砂岩型铀矿大体空间位置. 相似文献
36.
37.
A. Heusel-Waltrop K. Diehl S. K. Mitra H. R. Pruppacher 《Journal of Atmospheric Chemistry》2003,44(2):211-223
Laboratory experiments have been carried out to investigate the uptake of sulfur dioxide by water drops containing heavy metal ions where the metal ions serve as catalysts to oxidise the taken up S(IV) into S(VI). During the gas uptake the drops were freely suspended at their terminal velocity in the airstream of the Mainz vertical wind tunnel. Two series of experiments were carried out, one with large millimeter size water drops containing manganese or iron ions, and the other with small water drops containing manganese ions and having radii in hundreds of micron size range. The experimental results were compared against model computations using the Kronig–Brink model and the fully mixed model, modified for the case that heavy metal ions present in the liquid phase act as catalysts for the oxidising process. The results of the model calculations show that there are only small differences between the predicted gas uptake according to the two models. In addition it was found that the experimental obtained results from the uptake of SO2 by water drops containing heavy metal ions for both, large and small water drops did agree with the model results. 相似文献
38.
从淮南谢—矿五层煤(C_(13)、B_(11b)、B_(10)、B_(4b)和A_3)中精选出镜煤、壳质暗煤、惰性暗煤及构造煤,采用重量法,分别测定它们的甲烷吸附量,从而研究不同成分组成的煤其甲烷吸附性能。 相似文献
39.
于心科 《中国地球化学学报》1997,16(2):189-192
The atmospheric concentration of methane is steadily increasin.Lacking of precise estimates of source and sink strengths for the atmospheric methane severely limits the current understanding of the global methane cycle.Agood budget of atmospheric methane can enhance our understanding of the global carbon cycle and global climate change,The known estimates of the main source and sink strengths are gresented in this paper,In terms of carbon isotopic studies,it is evidenced that the earth‘s primodial methane,which was trapped in the earth during its formation,may be another source of methane,with extensive,earth‘s degassing which is calleld the “breathing“ process of the earth and played an important role in the formation of the promitive atmosphere,large amounts of methane were carried from the deep interior to the surface and then found its way into the atmosphere. 相似文献
40.
Heavy metal retention in secondary precipitates from a mine rock dump and underlying soil, Dalarna, Sweden 总被引:7,自引:2,他引:7
This study investigates the retention of heavy metals in secondary precipitates from a sulfidic mine rock dump and underlying
podzolic soils by means of mineralogical and chemical extraction methods. The rock dump, which is at least 50 years old, consists
of a 5–10-cm-thick leached zone and an underlying 110–115-cm-thick accumulation zone. Optical microscopy and electron microprobe
analyses confirm that pyrrhotite weathering has proceeded much further in the leached horizon relative to the accumulation
horizon. The weathering of sulfides in the leached zone has resulted in the migration of most heavy metals to the accumulation
zone or underlying soils, where they are retained in more stable phases such as secondary ferric minerals, including goethite
and jarosite. Some metals are temporarily retained in hydrated ferrous sulfates (e.g., melanterite, rozenite).
Received: 28 October 1996 · Accepted: 24 February 1997 相似文献