全文获取类型
收费全文 | 14301篇 |
免费 | 843篇 |
国内免费 | 1461篇 |
专业分类
林业 | 1960篇 |
农学 | 963篇 |
基础科学 | 593篇 |
3708篇 | |
综合类 | 4785篇 |
农作物 | 713篇 |
水产渔业 | 943篇 |
畜牧兽医 | 1748篇 |
园艺 | 286篇 |
植物保护 | 906篇 |
出版年
2024年 | 99篇 |
2023年 | 279篇 |
2022年 | 455篇 |
2021年 | 492篇 |
2020年 | 571篇 |
2019年 | 601篇 |
2018年 | 467篇 |
2017年 | 700篇 |
2016年 | 860篇 |
2015年 | 742篇 |
2014年 | 777篇 |
2013年 | 1005篇 |
2012年 | 1065篇 |
2011年 | 1033篇 |
2010年 | 808篇 |
2009年 | 786篇 |
2008年 | 699篇 |
2007年 | 768篇 |
2006年 | 718篇 |
2005年 | 521篇 |
2004年 | 432篇 |
2003年 | 350篇 |
2002年 | 278篇 |
2001年 | 261篇 |
2000年 | 231篇 |
1999年 | 215篇 |
1998年 | 179篇 |
1997年 | 136篇 |
1996年 | 165篇 |
1995年 | 189篇 |
1994年 | 104篇 |
1993年 | 115篇 |
1992年 | 118篇 |
1991年 | 92篇 |
1990年 | 89篇 |
1989年 | 78篇 |
1988年 | 49篇 |
1987年 | 25篇 |
1986年 | 16篇 |
1985年 | 13篇 |
1984年 | 2篇 |
1982年 | 3篇 |
1981年 | 2篇 |
1980年 | 5篇 |
1979年 | 2篇 |
1977年 | 1篇 |
1963年 | 1篇 |
1962年 | 1篇 |
1956年 | 2篇 |
1955年 | 3篇 |
排序方式: 共有10000条查询结果,搜索用时 0 毫秒
11.
探讨不同养殖模式下金背鲤 (Cyprinus carpio var. Jinbei) 肠道菌群和鱼肉风味品质差异,对金背鲤的繁殖优化具有重要意义。采用高通量测序技术对稻田放养和池塘养殖模式下金背鲤的肠道微生物进行测序,利用液相色谱和顶空固相微萃取-气相色谱-离子迁移谱联用 (HS-SPME-GC-IMS) 技术测定其滋味物质、挥发性风味化合物,结合感觉阈值计算滋味活性值和相对气味活度值。结果显示:两种养殖模式的金背鲤肠道细菌群落结构差异显著,稻田放养 (FGF) 组以弧菌 (Vibrio)、拟杆菌 (Bacteroides)、交替单胞菌 (Alteromonadales)、希瓦氏菌 (Shewanella)、嗜冷假单胞菌 (Pseudomonas psychrophile) 和Brevinema属为主,池塘养殖 (FGP) 组以莫拉克斯氏菌 (Moraxella) 和克雷伯菌属 (Klebsiella) 为主;FGF组中鲜味肌苷酸含量及其滋味活性值 (1.676 g·kg−1, 6.705) 远高于FGP组 (0.246 g·kg−1, 0.985),FGF组鲜味氨基酸和甜味氨基酸含量 (0.143和2.052 g·kg−1) 高于FGP组 (0.109和2.001 g·kg−1),而其苦味氨基酸 (3.193 g·kg−1) 却低于FGP组 (3.836 g·kg−1);金背鲤的挥发性化合物组分复杂,其关键气味化合物 (ROAV≥1) 和对整体风味有修饰作用的化合物 (0.1≤ROAV<1) 的种类存在差异。菌属与风味物质的相关性分析显示弧菌属、拟杆菌属、克雷伯菌属和摩根菌属 (Morganella) 与风味物质呈显著相关 (0.01≤P<0.05 & 0.001≤P<0.01 & P<0.001)。研究表明,养殖模式影响了金背鲤的肠道微生物,并间接影响了其风味品质。 相似文献
12.
M. von Lützow L. Zelles I. Scheunert J. C. G. Ottow 《Biology and Fertility of Soils》1992,13(3):130-134
Summary Seasonal effects of liming, irrigation, and acid precipitation on microbial biomass N and some physicochemical properties of different topsoil horizons in a spruce forest (Picea abies L.) were measured throughout one growing season. The highest biomass N was recorded in autumn and spring in the upper soil horizons, while the lowest values were obtained in summer and in deeper horizons. The clearest differences between the different soil treatments were apparent in autumn and in the upper horizons. Liming increased the microbial biomass N from 1.7% of the total N content to 6.8% (Olf1 layer) and from 1% to 2% of the total N content in the Of2 layer. The main inorganic-N fraction in the deeper horizons was NO
inf3
sup-
. An increase in cation exchange capacity was observed down to the Oh layer, while soil pH was only slightly higher in the Olf1 and Of2 layers after liming. The effects of irrigation were less marked. The microbial biomass N increased from 1.7% of total N to 4.8% in the Olf1 layer and from 1% to 2% of total N in the Of2 layer. In the Olf1 layer an increase in C mineralization was observed. Acid precipitation decreased the microbial biomass N in the upper horizons from 4.8% of total N to 1.8% in the Olf1 layer and from 2% to 0.5% in the Of2 layer. No significant changes in soil pH were observed, but the decrease in cation exchange capacity may result in a decrease in the proton buffering capacity in the near future. 相似文献
13.
14.
15.
We studied the effects of aggregates of different sizes on the soil microbial biomass. The distribution of aggregate size classes (<2, 2–4, 4–10, >10 mm) in the upper mineral soil horizon (Ah layer) was very different in three sites (upper, intermediate, lower) in a beechwood (Fagus sylvatica) on a basalt hill (Germany). Aggregates of different sizes (<2, 2–4, 4–10 mm) contained different amounts of C and N but the C:N ratios were similar. C and N contents were generally higher in smaller aggregates. The maximum initial respiratory response by microorganisms in intact aggregates and in aggregates passed through a 1-mm sieve declined with the aggregate size, but the difference was more pronounced in intact aggregates. Disruption of aggregates generally increased this response, particularly in 4- to 10-mm aggregates in the lower site. Basal respiration differed strongly among sites, but was similar in each of the aggregate size classes. Aggregate size did not significantly affect the specific respiration (g O2 g–1 microbial C h–1) nor the microbial: organic C ratio, but these parameters differed among sites. Microbial growth was increased strongly by passing the soil through a 1-mm sieve in each of the aggregate materials. The growth of microorganisms in disrupted aggregates was similar, and the effect of aggregate disruption depended on the growth of microorganisms in intact aggregates. 相似文献
16.
Temperate and boreal forests act as major sinks for atmospheric CO2. To assess the magnitude and distribution of the sinks more precisely, an accurate estimation of forest biomass is required. However, the determinants of large-scale biomass pattern (especially root biomass) are still poorly understood for these forests in China. In this study, we used 515 field measurements of biomass across the northeast part of China, to examine factors affecting large-scale biomass pattern and root–shoot biomass allocation. Our results showed that, Picea & Abies forest and coniferous & broadleaf mixed forest had the highest mean biomass (178–202 Mg/ha), while Pinus sylvestris forest the lowest (78 Mg/ha). The root:shoot (R/S) biomass ratio ranged between 0.09 and 0.67 in northeast China, with an average of 0.27. Forest origin (primary/secondary/planted forest) explained 31–37% of variation in biomass (total, shoot and root), while climate explained only 8–15%, reflecting the strong effect of disturbance on forest biomass. Compared with shoot biomass, root biomass was less limited by precipitation as a result of biomass allocation change. R/S ratio was negatively related to water availability, shoot biomass, stand age, height and volume, suggesting significant effects of climate and ontogeny on biomass allocation. Root–shoot biomass relationships also differed significantly between natural and planted forests, and between broadleaf and coniferous forests. Shoot biomass, climate and forest origin were the most important predictors for root biomass, and together explained 83% of the variation. This model provided a better way for estimating root biomass than the R/S ratio method, which predicted root biomass with a R2 of 0.71. 相似文献
17.
Short term soil priming effects and the mineralisation of biochar following its incorporation to soils of different pH 总被引:2,自引:0,他引:2
The aim of this work was to determine the magnitude of the priming effect, i.e. short-term changes in the rate (negative or positive) of mineralisation of native soil organic carbon (C), following addition of biochars. The biochars were made from Miscanthus giganteus, a C4 plant, naturally enriched with 13C. The biochars were produced at 350 °C (biochar350) and 700 °C (biochar700) and applied with and without ryegrass as a substrate to a clay-loam soil at pH 3.7 and 7.6. A secondary aim was to determine the effect of ryegrass addition on the mineralisation of the two biochars.After 87 days, biochar350 addition caused priming effects equivalent to 250 and 319 μg CO2-C g−1 soil, in the low and high pH soil, respectively. The largest priming effects occurred at the start of the incubations. The size of the priming effect was decreased at higher biochar pyrolysis temperatures, which may be a way of controlling priming effects following biochar incorporation to soil, if desired. The priming effect was probably induced by the water soluble components of the biochar. At 87 days of incubation, 0.14% and 0.18% of biochar700 and 0.61% and 0.84% of biochar350 were mineralized in the low and high pH soil, respectively. Ryegrass addition gave an increased biochar350 mineralisation of 33% and 40%, and increased biochar700 at 137% and 70%, in the low and high pH soils, respectively. Certainly, on the basis of our results, if biochar is used to sequester carbon a priming effect may occur, increasing CO2-C evolved from soil and decreasing soil organic C. However, this will be more than compensated for by the increased soil C caused by biochar incorporation. A similar conclusion holds for accelerated mineralisation of biochar due to incorporation of fresh labile substrates. We consider that our results are the first to unequivocally demonstrate the initiation, progress and termination of a true positive priming effect by biochar on native soil organic C. 相似文献
18.
采用现存生殖分配(Standing Reproduction Allocation)的方法研究甘南地区歪头菜(Vicia unijuga)生物量生殖分配。结果表明,不同生长年限植株在整个生长季中,各构件生物量占总生物量的比例随着季节变化表现为营养分配比重不断减少,生殖分配比重不断增加,但营养生物量分配比例占绝对优势,而在蕾期和花期用于有性生殖的生物量(蕾、花生物量)分配比例仅在10%左右;多年生歪头菜种群幼龄时期植株生殖生物量分配仍然随着生长年限的增加而增加,但生殖产量的生物量分配却表现出2年龄5年龄4年龄;2年龄植株蕾-花生物量转换比例和花-荚生物量转换比例分别为1∶1.17和1∶1.36,5年龄植株的分别为1∶0.94和1∶1.31,说明2年龄植株比5年龄植株有较高的生殖利用率,而5年龄植株落花、落荚现象明显。以上结果揭示出,植株对有性繁殖的小比例投资以及生殖转换中产生的生殖损失可能是导致该地区歪头菜种群有性繁殖体种子产量低的重要原因,而影响这一原因的因素可能是生长季过程中的环境干扰和养分竞争等问题。 相似文献
19.
磷、钾对番茄可溶性碳水化合物分配的影响 总被引:3,自引:0,他引:3
胡繁荣 《吉林农业大学学报》2004,26(2):151-154
以番茄苗为试验材料,研究了不同浓度磷、钾对番茄植株可溶性碳水化舍物分配的影响。结果表明:磷、钾亏缺处理45d后,与正常磷、钾处理相比,磷亏缺的植株冠根比下降,而钾亏缺的植株冠根比则上升。钾亏缺的植株叶片中,蔗糖、还原糖和总可溶性糖含量均表现为上升,根中则表现为下降。磷亏缺的植株叶片中,蔗糖、还原糖和总可溶性糖含量基本不变,而在根中则表现为不同程度的增加。在叶和根的总可溶性糖中,钾亏缺和磷亏缺的植株,根部总可溶性糖所占的比例分别为10.71%和45.65%,两者的对照分别为28.63%和33.11%。上述结果表明,钾和磷在光合产物的转运中所起的作用不同,植株中营养元素亏缺不同,干物质在不同部位的分配也不同。 相似文献
20.
单生育期水分胁迫对温室葡萄根际土壤酶活性及微生物群落的影响 总被引:1,自引:0,他引:1
为明确单生育期水分胁迫对土壤酶活性和微生物群落结构的影响,选取5a生'红地球'鲜食葡萄为试验材料,采用单因素完全随机试验设计,以全生育期充分供水为对照(CK),依次在葡萄5个生育期分别设置轻度(M)和重度(S)两个水分胁迫水平进行大田试验,利用Illumina高通量测序技术分析土壤微生物的群落构成和多样性.结果表明:葡... 相似文献