全文获取类型
收费全文 | 3805篇 |
免费 | 1025篇 |
国内免费 | 1337篇 |
专业分类
测绘学 | 598篇 |
大气科学 | 700篇 |
地球物理 | 867篇 |
地质学 | 2430篇 |
海洋学 | 640篇 |
天文学 | 61篇 |
综合类 | 375篇 |
自然地理 | 496篇 |
出版年
2024年 | 24篇 |
2023年 | 85篇 |
2022年 | 228篇 |
2021年 | 253篇 |
2020年 | 218篇 |
2019年 | 301篇 |
2018年 | 236篇 |
2017年 | 244篇 |
2016年 | 231篇 |
2015年 | 284篇 |
2014年 | 269篇 |
2013年 | 310篇 |
2012年 | 340篇 |
2011年 | 327篇 |
2010年 | 306篇 |
2009年 | 293篇 |
2008年 | 253篇 |
2007年 | 277篇 |
2006年 | 280篇 |
2005年 | 206篇 |
2004年 | 162篇 |
2003年 | 124篇 |
2002年 | 137篇 |
2001年 | 136篇 |
2000年 | 92篇 |
1999年 | 101篇 |
1998年 | 55篇 |
1997年 | 61篇 |
1996年 | 65篇 |
1995年 | 55篇 |
1994年 | 32篇 |
1993年 | 25篇 |
1992年 | 30篇 |
1991年 | 14篇 |
1990年 | 25篇 |
1989年 | 13篇 |
1988年 | 11篇 |
1987年 | 13篇 |
1986年 | 5篇 |
1985年 | 11篇 |
1984年 | 6篇 |
1983年 | 4篇 |
1982年 | 2篇 |
1981年 | 2篇 |
1980年 | 6篇 |
1979年 | 5篇 |
1958年 | 1篇 |
1957年 | 2篇 |
1954年 | 3篇 |
1927年 | 1篇 |
排序方式: 共有6167条查询结果,搜索用时 484 毫秒
201.
研究β-1,3/1,6-D-glucan及不同投喂方式对中国明对虾(Fenneropenaeus chinensis)幼体的存活、生长、发育、非特异性免疫及抗副溶血弧菌能力的影响.将β-glucan以0.25%的剂量添加到微黏合饲料中,以不同的投喂方式投喂对虾幼体,即D0(一直投喂基础饲料);D1(一直投喂含0.25%β-葡聚糖饲料);3D1-3D0(3 d投喂含0.25%β-葡聚糖的饲料-3 d投喂基础饲料);1D1-3D0(1 d投喂含0.25%β-葡聚糖的饲料-3 d投喂基础饲料),共4个处理,每个处理随机设置3个重复,对虾幼体养殖于可控温的半开放系统中,每个养殖桶中盛有50 L盐度为30~32消毒海水,养殖密度为100尾/L.实验结果表明,在孵化后14 d,投喂D1饲料组在总存活率,变态指数,体长,特定生长率方面均高于其它各组,虽然有时差异不显著.在免疫指标方面,在9和14 dph分别进行了酚氧化酶(PO)、碱性磷酸酶(ALP)、超氧化物歧化酶(SOD)、酸性磷酸酶(ACP)活力的测定,结果表明,投喂D1饲料组的4个免疫指标均高于其它3组,虽然有时差异不显著.在14 dph的攻毒实验结果表明,对照组的累积死亡率显著高于D1组(P<0.05),而1D1-3D0和3D1-3D0的累积死亡率则与其它各组均不显著.实验结果表明,间隔投喂方式并不适合于对虾幼体,在中国明对虾幼体饲料中使用β-葡聚糖时,建议添加量为0.25%,并采用一直投喂的方式. 相似文献
202.
山东近海溶解态无机营养盐的分布特征研究 总被引:1,自引:0,他引:1
根据2006年8月、12月和2007年4月、10月山东近海海区4个航次海水中溶解无机营养盐等的调查资料,分析了该海域5种溶解无机营养盐(包括PO4-P,NO3-N,NO2-N,NH4-N,SiO3-Si)的平面分布和时空变化特征.结果表明,5种营养盐在胶州湾内出现高值,平面分布整体上呈现沿岸浓度高、外海浓度低的趋势;根据绝对限制和相对限制法则,春季和夏季P为限制因子,秋冬季营养盐结构发生变化,由缺P向缺Si转变;SiO3-Si浓度随季节变化逐渐增加,其他营养盐浓度在春季和夏季较低,秋季达到最大值.秋冬季溶解无机营养盐周日变化受潮汐影响明显. 相似文献
203.
204.
Genetic diversity of two wild Penaeus monodon populations sampled from the coastal waters of Qinglan ( Hainan Province of China, HN) and Malaysia (KD), and the F1 generation of a Thailand broodstock population (CP) were examined by vertical polyacrylamide gel electrophoresis. Of 21 loci encoded by ten enzymes, 11 were polymorphic. The mean proportions of polymorphic loci of HN, KD and CP were 36. 36%, 45.45% and 50.00% , with the average heterozygosities of 0.135, 0.181 and 0.191, and the effective numbers of alleles per loci were 1. 300, 1. 330 and 1. 329, respectively. The divergent indexes of HN, KD and CP were0.023, 0.124, and 0.117, respectively. The genetic distance between the two wild populations was 0.005, and the gene differentiation coefficient was also very low (0.014). The results indicated that the F1 generation population had a higher genetic diversity than the two wild populations, and that the HN population had the lowest one. There was no significant differentiation between HN and KD populations and all populations existed with a slight heterozygote excess. 相似文献
205.
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
206.
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
207.
208.
On tectonic movement in the South China Sea during the Cenozoic 总被引:1,自引:1,他引:0
The tectonic movement taking place at the end of Cretaceous and the beginning of Cenozoic had opened the Cenozoic phase of polycyclic tectonic movements, then the whole crust of the South China Sea had been mainly subjected to the regional stress field of tectonic tension, which was characterized by rifting depression. Seven times of regional tectonic movement and sedimentation had been assembled into a geological development history of polycyclic oscillation. Especially, the tectonic movements were strongly intensified at the end of Cretacious and the beginning of Paleagene, between Late Eocene and MidOligocene, during Mid and Late Miocene. These three times of tectonic movement had built the most important regional tectonic interfaces in the South China Sea. Crust movements of the South China Sea were the result and epitome of interaction of the Eurasia, Pacific and IndoAustralia plates, that is, they were introduced by polycyclic changes of directions, rates and strengths of lithospheric movements and asthenospheric flows across the Pacific and IndoAustralia plates. 相似文献
209.
根据2006年10月和2007年1月的监测资料,对三亚湾在东北季风初始期和盛行期初级生产力的分布特征及其受水体环境的影响因素进行了分析。三亚湾秋、冬季表层潜在初级生产力平均值分别为6.81mgC·m-3·h-1和7.47mgC·m-3·h-1;水柱初级生产力平均值分别为504.96mgC·m-2·d-1和495.33mgC·m-2·d-1。东北季风期间,三亚湾水体垂直混合作用加强,层化现象减弱,水动力过程和营养盐等环境因子是该海湾初级生产力分布特征和季节变化的重要调控因素;其中冬季较高的DIN分布对表层初级生产力有潜在促进作用,而水体扰动增强、真光层深度下降则导致水柱初级生产力低于秋季。三亚河口近岸水域秋、冬季均为营养盐、叶绿素a及初级生产力的高值区,其中表层潜在初级生产力在秋季和冬季分别达到了45.80mgC·m-3·h-1和39.27mgC·m-3·h-1,表明调查期间三亚河营养盐输入对近岸水体浮游植物初级生产过程的显著影响。 相似文献
210.
在某些蓝藻、绿藻和高等植物中,八氢番茄红素脱氢酶是β-胡萝卜素合成过程中的一个关键酶之一,应用巢式PCR方法从雨生红球藻中克隆了八氢番茄红素脱氢酶基因约1kb的5’上游序列。通过生物信息学方法进行序列分析,发现pds基因上游序列中包含了一些可能的顺式元件,如ABRE调控元件、C-repeat/DRE调控元件等。同时,构建了由pds-启动子控制报告基因的重组载体,并转化到雨生红球藻细胞中,进行了报告基因瞬间表达的检测。结果表明,克隆的pds启动子区域具有启动子活性,可以驱使报告基因进行瞬间表达。 相似文献