全文获取类型
收费全文 | 1380篇 |
免费 | 151篇 |
国内免费 | 282篇 |
专业分类
测绘学 | 25篇 |
大气科学 | 107篇 |
地球物理 | 352篇 |
地质学 | 414篇 |
海洋学 | 570篇 |
天文学 | 6篇 |
综合类 | 99篇 |
自然地理 | 240篇 |
出版年
2024年 | 13篇 |
2023年 | 51篇 |
2022年 | 61篇 |
2021年 | 65篇 |
2020年 | 57篇 |
2019年 | 94篇 |
2018年 | 49篇 |
2017年 | 55篇 |
2016年 | 54篇 |
2015年 | 61篇 |
2014年 | 85篇 |
2013年 | 104篇 |
2012年 | 74篇 |
2011年 | 71篇 |
2010年 | 83篇 |
2009年 | 76篇 |
2008年 | 75篇 |
2007年 | 64篇 |
2006年 | 83篇 |
2005年 | 73篇 |
2004年 | 73篇 |
2003年 | 47篇 |
2002年 | 59篇 |
2001年 | 38篇 |
2000年 | 26篇 |
1999年 | 30篇 |
1998年 | 22篇 |
1997年 | 22篇 |
1996年 | 23篇 |
1995年 | 15篇 |
1994年 | 9篇 |
1993年 | 13篇 |
1992年 | 7篇 |
1991年 | 6篇 |
1990年 | 5篇 |
1989年 | 3篇 |
1988年 | 6篇 |
1987年 | 4篇 |
1986年 | 6篇 |
1985年 | 17篇 |
1984年 | 11篇 |
1983年 | 10篇 |
1982年 | 5篇 |
1981年 | 7篇 |
1978年 | 1篇 |
排序方式: 共有1813条查询结果,搜索用时 15 毫秒
131.
M. Koike Y. Kondo W.A. Matthews P.V. Johnston H. Nakajima A. Kawaguchi H. Nakane I. Murata A. Budiyono M. Kanada N. Toriyama 《Journal of Atmospheric Chemistry》1999,32(1):121-145
The column amounts of nitrogen dioxide (NO2) and ozone (O3) were measured using a visible spectrometer based on the twilight zenith-sky technique at two observatories located at similar latitudes in the northern part of Japan separated by a distance of 150 km. The measurements began in April 1991 at the Moshiri Observatory (44.4°N, 142.3°E) and in April 1994 at the Rikubetsu Observatory (43.5°N, 143.8°E). Since weather conditions and the possible influence from tropospheric pollution were not always identical at these two observatories, the overall accuracy of the measurements was studied comparing these data sets. The first year data obtained at a solar zenith angle of 90 degrees indicated that the NO2 slant column values at sunrise and sunset agreed within 0.36 and 0.54 × 1016 cm-2, respectively, corresponding to 5 % (June) and to 12 % (December) of the columns. The O3 values agreed within 0.76 × 1019 cm-2, corresponding to 4 % (March) 6 % (August) of the columns, although a part of the difference was systematic. The O3 column amounts were also compared to those obtained by the Dobson spectrometer at Sapporo (43.5°N, 143.8°E), whose latitude is similar to these observatories. When an air mass factor of 17.5 was used, the two-year Moshiri vertical column values agreed with the Dobson direct sun values to within 15 Dobson Units, or 3 6 % of the column. The difference between the two values was found to be due partly to the change in the air mass factor caused by seasonal and day-to-day changes in the shape of the O3 vertical profiles. These results confirm the reliability of the NO2 and O3 measurements by visible spectrometers at these sites for the Network for the Detection of Stratospheric Change (NDSC). 相似文献
132.
133.
134.
多目标地球化学调查土壤样品中氮和碳的快速测定 总被引:2,自引:1,他引:2
详细研究了元素分析仪的工作条件,建立了直接固体进样同时测定多目标地球化学调查土壤样苎支氮、碳的方法。方法简便、快速,检出限为氮14.5μg/g、碳0.013%。经土壤国家一级标准物质分析验证,测定值与标准值相符,精密度(RSD,n=12)为氮1.49%-3.27%、碳0.64%~3.63%。 相似文献
135.
Stella M. Resende 《Journal of Atmospheric Chemistry》2007,56(1):21-32
The atmospheric reaction between HS and NO2 was theoretically investigated at 298 K and 1 atm of pressure. Our results show that the first reaction step will lead to the formation of HSNO2 or HSONO, spontaneously and exothermically. HSONO easily decomposes into HSO + NO. On the other hand, HSNO2 can hardly dissociate in the reactants, and its isomerization to other adducts is much hindered. Production of HNO + SO and SNO + OH was found to be unfavorable. Thus, the main products would be HSO + NO and HSNO2, and new investigations focusing on the atmospheric fate of HSNO2 are suggested. A general discussion of the fate of HS under atmospheric conditions is presented. Recent investigations indicate that NO2, O2 and N2O should be the most important oxidants of HS, while the O3 influence will not be significant. 相似文献
136.
Potential salinity limitations on nitrogen fixation in sediments from Mono Lake, California 总被引:2,自引:0,他引:2
David B. Herbst 《International Journal of Salt Lake Research》1998,7(3):261-274
Mono Lake is a hypersaline alkaline lake in the high altitude Great Basin desert of eastern California. Algal productivity
of the lake is nitrogen-limited, and a contributing source is derived from benthic nitrogen fixation. Lake level and salinity
have fluctuated with natural climatic variations but have also been affected by the diversion of tributary streams. This research
examines the influence of varied salinity and lake level on the potential for benthic nitrogen fixation in Mono Lake. A sediment-surface
microbial mat community was exposed directly, and in acclimated cultures, to a range of Mono Lake salinities under anaerobic
incubations and the activity of nitrogenase assayed by acetylene reduction. Activity was stimulated in light, but also occurred
in darkness. Over an experimental salinity range from 50 to 150 g L−1 TDS, nitrogenase activity was reduced by 90 per cent, with the activity persisting at the highest salinity being attributable
to dark fixation alone. Between a salinity of 50 g L−1, occurring in Mono Lake over 50 years ago, and 100 g L−1, nitrogenase activity was reduced by nearly half. Changes in the area of the littoral zone at varied lake levels also affect
the total amount of potential benthic nitrogen fixation in the lake. An accounting of yearly inputs of nitrogen to Mono Lake
suggests N2-fixation could contribute as much as 76–81 percent of the total. Inhibition of nitrogen fixation rates by increased salinity
could limit the long-term nutrient supply and benthic primary productivity of this ecosystem. 相似文献
137.
The reaction coefficients of nitrogen dioxide and nitrous acid with monodisperse sodium chloride and ammonium sulphate aerosols have been measured in a flow reactor at atmospheric pressure. These experiments were performed at relative humidities above and below the deliquescence points of both aerosols (r.h. 50 and 85%) at 279 K. The results for NO2 afford a reaction coefficient in the range (2.8–10) × 10-4 and for HONO, (2.8–4.6) × 10-3. For both species, there appears to be an enhancement of the reaction coefficient on sodium chloride aerosol at 50% r.h. The results are compared with reaction coefficients determined by other experimental methods. A good agreement is found for both gases between this method and the coated denuder method previously developed in our research laboratories (Msibi et al., 1993) and with the majority of other published data for NO2. In the case of HONO, our estimate of reaction coefficient is smaller than, or at the lower limits of the ranges reported by other published studies. 相似文献
138.
Wen-yuan Huang Russ W. Keim Yao-chi Lu N. D. Uri Terry Kelley 《Environmental Geology》1998,34(2-3):116-127
The economic and environmental consequences of soil nitrogen tests can have significant impacts on agricultural production.
Some of these are explored here. The pre-side-dress soil N-test is evaluated for a hypothetical farmer growing corn at the
ARS Sustainable Agriculture Demonstration Farm site in southern Maryland. For a farmer not currently using a soil N-test,
adoption of this technology can lead to the enhancement of net farm income and the reduction in nitrogen loss to the environment.
This will transpire only if the farmer is currently underestimating nitrogen carryover by more than 25% or applying nitrogen
fertilizer based solely on an expected plateau-yield goal.
Received: 13 February 1997 · Accepted: 13 May 1997 相似文献
139.
为从一种组成未知的商用复合菌中分离并筛选出优势发酵菌株,本实验采用稀释平板培养法,对菌种进行分离纯化,同时参照《真菌鉴定手册》和《常见细菌鉴定手册》,根据其形态学特征、生理生化特性,并分别结合16S r DNA和18S r DNA序列的比对分析对菌种进行鉴定。另外,本研究通过生长曲线测定,单菌种发酵试验以及多菌种混合发酵发酵试验,以游离氨基酸态氮为指标,以期筛选出发酵低值水产品制备菌肥的最佳菌株组合。结果显示,共分离得到4株菌,分别为a热带假丝酵母、b罗伦隐球菌、c枯草芽孢杆菌、d蜡样芽胞杆菌。且菌种组合acd发酵后游离氨基酸态氮的含量较对照组上升最显著,为8.276g/L。故可确定最佳发酵菌株配方为acd(热带假丝酵母+枯草芽孢杆菌+蜡样芽胞杆菌)。 相似文献
140.
温度和盐度对埋栖性双壳类泥蚶(Tegillarca granosa) 呼吸、排泄的影响 总被引:1,自引:0,他引:1
在人工条件下采用静水封闭呼吸瓶的方法研究了温度、盐度对泥蚶(Tegillarca granosa)呼 吸、排泄的影响, 并综合分析了温度、盐度交互作用对呼吸、排泄的影响程度, 为泥蚶基础生物学研 究积累了资料。结果表明, 在设定的不同温度条件下泥蚶耗氧率变化范围0.63-4.47mg/(g·h), 单因 素方差分析结果显示4 个盐度条件下泥蚶耗氧率的差异均极显著(P<0.01); 排氨率的变化范围 123.11-955.68μg/(g·h), 排氨率受温度的影响也均极显著(P<0.01); 经回归发现, 在温度13-31℃ 范 围内, 耗氧率和排氨率均与温度的变化呈显著的指数相关。除温度为18℃ 时, 其它各温度条件下, 不同盐度梯度间的耗氧率差异不显著(P>0.05), 盐度对排氨率影响的变化趋势不一致。在温度 (13-31℃)和盐度(18-28)时, 温度和盐度对耗氧率、排氨率的影响均存在交互作用, 耗氧率(Y)、排 氨率(Y)与温度(T)和盐度(S)之间的二元线性回归关系为Y=a+bT+cS+dT×S.泥蚶呼吸排泄的O:N 比 在4.50-13.07 之间, 平均值为7.16.泥蚶呼吸排泄的代谢活动受温度、盐度的影响显著。 相似文献