全文获取类型
收费全文 | 19585篇 |
免费 | 3773篇 |
国内免费 | 5051篇 |
专业分类
测绘学 | 1472篇 |
大气科学 | 3631篇 |
地球物理 | 4958篇 |
地质学 | 10032篇 |
海洋学 | 2875篇 |
天文学 | 823篇 |
综合类 | 2165篇 |
自然地理 | 2453篇 |
出版年
2024年 | 114篇 |
2023年 | 362篇 |
2022年 | 1027篇 |
2021年 | 1173篇 |
2020年 | 1019篇 |
2019年 | 1133篇 |
2018年 | 1311篇 |
2017年 | 1117篇 |
2016年 | 1199篇 |
2015年 | 1010篇 |
2014年 | 1249篇 |
2013年 | 1229篇 |
2012年 | 1292篇 |
2011年 | 1283篇 |
2010年 | 1256篇 |
2009年 | 1146篇 |
2008年 | 1019篇 |
2007年 | 947篇 |
2006年 | 777篇 |
2005年 | 734篇 |
2004年 | 555篇 |
2003年 | 506篇 |
2002年 | 450篇 |
2001年 | 515篇 |
2000年 | 586篇 |
1999年 | 816篇 |
1998年 | 653篇 |
1997年 | 626篇 |
1996年 | 575篇 |
1995年 | 463篇 |
1994年 | 451篇 |
1993年 | 397篇 |
1992年 | 335篇 |
1991年 | 229篇 |
1990年 | 190篇 |
1989年 | 148篇 |
1988年 | 115篇 |
1987年 | 90篇 |
1986年 | 62篇 |
1985年 | 50篇 |
1984年 | 38篇 |
1983年 | 39篇 |
1982年 | 31篇 |
1981年 | 17篇 |
1980年 | 10篇 |
1979年 | 15篇 |
1978年 | 9篇 |
1977年 | 6篇 |
1958年 | 11篇 |
1954年 | 5篇 |
排序方式: 共有10000条查询结果,搜索用时 328 毫秒
911.
912.
Dissolved inorganic carbon (DIC) and its carbon isotopic composition in sediment pore waters from the Shenhu area,northern South China Sea 总被引:2,自引:0,他引:2
Tao Yang Shao-Yong Jiang Jing-Hong Yang Ge Lu Neng-You Wu Jian Liu Dao-Hua Chen 《Journal of Oceanography》2008,64(2):303-310
The Shenhu area is one of the most favorable places for the occurrence of gas hydrates in the northern continental slope of
the South China Sea. Pore water samples were collected in two piston cores (SH-A and SH-B) from this area, and the concentrations
of sulfate and dissolved inorganic carbon (DIC) and its carbon isotopic composition were measured. The data revealed large
DIC variations and very negative δ
13C-DIC values. Two reaction zones, 0–3 mbsf and below 3 mbsf, are identified in the sediment system. At site SH-A, the upper
zone (0–3 mbsf) shows relatively constant sulfate and DIC concentrations and δ
13C-DIC values, possibly due to bioturbation and fluid advection. The lower zone (below 3 mbsf) displays good linear gradients
for sulfate and DIC concentrations, and δ
13C-DIC values. At site SH-B, both zones show linear gradients, but the decreasing gradients for δ
13C-DIC and SO4
2− in the lower zone below 3 mbsf are greater than those from the upper zone, 0–3 mbsf. The calculated sulfate-methane interface
(SMI) depths of the two cores are 10.0 m and 11.1 m, respectively. The depth profiles of both DIC and δ
13C-DIC showed similar characteristics as those in other gas hydrate locations in the world oceans, such as the Blake Ridge.
Overall, our results indicate an anaerobic methane oxidation (AMO) process in the sediments with large methane flux from depth
in the studied area, which might be linked to the formation of gas hydrates in this area. 相似文献
913.
Geochemistry of pore waters from the Xisha Trough, northern South China Sea and their implications for gas hydrates 总被引:2,自引:0,他引:2
Shao-Yong Jiang Tao Yang Lu Ge Jing-Hong Yang Hong-Fei Ling Neng-You Wu Jian Liu Dao-Hua Chen 《Journal of Oceanography》2008,64(3):459-470
This paper reports all available geochemical data on sediments and pore waters from the Xisha Trough on the northern continental
margin of the South China Sea. The methane concentrations in marine sediments display a downhole increasing trend and their
carbon isotopic compositions (δ
13C = −25 to −51‰) indicate a thermogenic origin. Pore water Cl− concentrations show a range from 537 to 730 mM, and the high Cl− samples also have higher concentrations of Br−, Na+, K+, and Mg2+, implying mixing between normal seawater and brine in the basin. The SO4
2− concentrations of pore waters vary from 19.9 to 36.8 mM, and show a downhole decreasing trend. Calculated SMI (sulfate-methane
interfaces) depths and sulfate gradients are between 21 and 47 mbsf, and between −0.7 and −1.7 mM/m, respectively, which are
similar to values in gas hydrate locations worldwide and suggest a high methane flux in the basin. Overall, the geochemical
data, together with geological and geophysical evidence, such as the high sedimentation rates, high organic carbon contents,
thick sediment piles, salt and mud diapirs, active faulting, abundant thermogenic gases, and occurrence of huge bottom simulating
reflector (BSR), are suggestive of a favorable condition for occurrence of gas hydrates in this region. 相似文献
914.
915.
916.
917.
Method for evaluating the degrees of land use sustainability of mountainous county and its application in Yunnan Province,China 总被引:4,自引:1,他引:3
The evaluation of sustainable land use is the key issue in the field of studying the sustainable land utilization. In general analysis, the sustainable land use is evaluated respectively from its ecological sustainability, economic sustainability and social sustainability in China and other countries in recent years. Although this evaluation is an important work, it seems insufficient and hard to comprehensively reflect the whole degree of land use sustainability. Thus, to make up this deficiency, this paper brings forward the evaluation indexes, which make it possible to quantitatively reflect the whole degree of land use sustainability, namely, the concept of "degrees of overall land use sustainability" (Dos), and research and measurement development of the method of and calculation in Dos. Taking the evaluation of the degree of land use sustainability in county regions of Yunnan Province as the actual example for analysis, results are basically as follows:
1) The degree of land use sustainability (Dos) is the ration index to organically and systematically integrate the degree of ecological friendliness (DeF), the degree of economic viability (Dev) and the degree of social acceptability (Dsa), able to comprehensively reflect the whole sustainability degree of regional land use
2) Based on the value of Dos, the grading system and standard for the sustainability of land use may be established and totally divided into five grades, namely, the high-degree sustainability, middle-degree sustainability, low-degree sustainability, conditional sustainability and non-sustainability. Meanwhile, the standard for distinguishing sustainability grades has also been confirmed so as to determine the nature of sustainability degrees in different grades. This makes the possibility for the combination of nature determination with ration in research result and provides with the scientific guideline and decision-making gist for better implementation of sustainable land use strategy.
3) The pract 相似文献
1) The degree of land use sustainability (Dos) is the ration index to organically and systematically integrate the degree of ecological friendliness (DeF), the degree of economic viability (Dev) and the degree of social acceptability (Dsa), able to comprehensively reflect the whole sustainability degree of regional land use
2) Based on the value of Dos, the grading system and standard for the sustainability of land use may be established and totally divided into five grades, namely, the high-degree sustainability, middle-degree sustainability, low-degree sustainability, conditional sustainability and non-sustainability. Meanwhile, the standard for distinguishing sustainability grades has also been confirmed so as to determine the nature of sustainability degrees in different grades. This makes the possibility for the combination of nature determination with ration in research result and provides with the scientific guideline and decision-making gist for better implementation of sustainable land use strategy.
3) The pract 相似文献
918.
919.
济南北部地热田地热资源类型属于层状裂隙岩溶型,热源是北部齐河-广饶断裂的沟通导热,盖层是第四系、新近系、石炭-二叠系、侏罗系.可利用的、具有开发价值的热储层为奥陶系灰岩热储,该热储层顶板埋深在700~2500m左右,热储层厚度由南向北逐渐增大,单井涌水量2000m3/d左右,孔口水温一般在38~57℃,地热田东部地热水矿化度1.4~3.5g/L左右,西部5.1~7.2g/L左右,地热水中富含氟、锶、偏硅酸等微量元素,具腐蚀性,结垢性弱,具较好的开发利用价值.经计算奥陶系热储层单井可采资源量为7.3×105m3/a,合理井间距为5000m. 相似文献
920.
枣庄市山亭区位于枣庄市东北部,泰沂山区西南部,属低山丘陵区,全区大小山头1000多座,地形条件复杂,土地总面积1018.64km^2,山地丘陵占全区总面积的80%以上。山亭区的土地利用现状更新调查工作始于2004年,经过1年多的艰苦调查,查清了全区各类土地利用的现状,绘制了山亭区土地利用现状图,建成了山亭区土地利用数据库。2007年7月,山东省国土资源厅对山亭区的土地利用调查更新工作进行了验收。经验收,山亭区土地利用更新调查技术路线正确、方法先进,各项成果符合土地更新调查技术要求。 相似文献