全文获取类型
收费全文 | 1296篇 |
免费 | 84篇 |
国内免费 | 109篇 |
专业分类
林业 | 74篇 |
农学 | 86篇 |
基础科学 | 29篇 |
529篇 | |
综合类 | 478篇 |
农作物 | 46篇 |
水产渔业 | 68篇 |
畜牧兽医 | 121篇 |
园艺 | 11篇 |
植物保护 | 47篇 |
出版年
2024年 | 12篇 |
2023年 | 31篇 |
2022年 | 54篇 |
2021年 | 49篇 |
2020年 | 44篇 |
2019年 | 48篇 |
2018年 | 53篇 |
2017年 | 64篇 |
2016年 | 59篇 |
2015年 | 60篇 |
2014年 | 66篇 |
2013年 | 95篇 |
2012年 | 129篇 |
2011年 | 97篇 |
2010年 | 74篇 |
2009年 | 68篇 |
2008年 | 68篇 |
2007年 | 67篇 |
2006年 | 56篇 |
2005年 | 58篇 |
2004年 | 40篇 |
2003年 | 24篇 |
2002年 | 24篇 |
2001年 | 27篇 |
2000年 | 17篇 |
1999年 | 15篇 |
1998年 | 17篇 |
1997年 | 11篇 |
1996年 | 9篇 |
1995年 | 14篇 |
1994年 | 7篇 |
1993年 | 5篇 |
1992年 | 6篇 |
1991年 | 6篇 |
1990年 | 5篇 |
1989年 | 1篇 |
1988年 | 1篇 |
1987年 | 1篇 |
1986年 | 2篇 |
1985年 | 1篇 |
1982年 | 1篇 |
1980年 | 2篇 |
1974年 | 1篇 |
排序方式: 共有1489条查询结果,搜索用时 640 毫秒
1.
2.
长期施肥处理对双季晚稻叶绿素荧光特征及籽粒产量的影响 总被引:2,自引:0,他引:2
HOU Hong-Qian LIN Hong-Xin LIU Xiu-Mei JI Jian-Hua LIU Yi-Ren LAN Xian-Jin LYU Zhen-Zhen ZHOH Wei-Jun 《作物学报》2020,46(2):280-289
研究施肥模式对水稻叶绿素含量及荧光参数的调节作用,对提高水稻光能利用效率及籽粒产量具有重要意义。本研究以水稻品种赣929为试验材料,比较长期定位施磷钾肥(PK)、施氮磷钾肥(NPK)、等养分条件下70%氮磷钾肥配合施用30%有机肥(70F+30M)、50%氮磷钾肥配合施用50%有机肥(50F+50M)、30%氮磷钾肥配合施用70%有机肥(30F+70M)条件下水稻叶绿素荧光参数和产量变化特征。结果表明,水稻旗叶叶绿素含量从齐穗期到成熟期呈下降趋势,且表现为30F+70M50F+50M70F+30MNPKPK。水稻叶绿素荧光参数Fv/Fm随水稻生育期的推进呈降低趋势,其中PK处理Fv/Fm值最低,而施氮处理比不施氮处理Fv/Fm值增加了2.85%~4.18%。叶绿素荧光参数qL、ΦPSII在NPK处理中表现为齐穗期较高, 20 d之后显著降低;在50F+50M、30F+70M处理中表现为齐穗期较低, 20 d以后显著增加;在PK处理、70F+30M处理中一直处于较高水平。NPQ变化趋势与qL基本相反。ETR-PAR光响应曲线拟合结果表明, 70F+30M处理ETRmax、?和Ek值在齐穗期和20 d后值均最高。综合看来,等养分条件下配施30%有机肥具有最优的叶绿素荧光指标组合及籽粒产量;而配施超过50%有机肥由于前期热耗散增大使得用于光合作用的光能份额减少,而施用氮磷钾肥处理则由于后期的衰老使得光能利用效率下降。 相似文献
3.
Abstract To evaluate the suitability of angling groundbaits as a fish feed and the potential for nutrient loss, the macronutrient digestibility of four groundbaits was investigated in carp, Cyprinus carpio L., using a sieving method of faeces collection and chromic oxide. Apparent digestibility coefficients (ADCs) of protein and lipids were >80% for all angling baits. ADCs of nitrogen-free extracts and phosphorus (P) differed significantly between the test diets, probably because of divergent feed compositions and ingredient treatments. The generally high digestibility estimates indicated that fish feeding on angling groundbait will benefit from this food source. The differences in nutrient digestibility suggested that type of groundbait and ingredient used will have a major effect on potential eutrophication and fish production caused by groundbaiting. The principle of groundbaits to protect the environment should be to minimise the P-content of the groundaits and maximising P-digestibility and P-retention efficiency. 相似文献
4.
5.
6.
7.
黄河口生态恢复工程对湿地土壤不同形态无机硫动态变化的影响 总被引:1,自引:0,他引:1
选择黄河口生态恢复前后的未恢复区(R0)、2007年恢复区(R2007)和2002年恢复区(R2002)的芦苇湿地为研究对象,探讨了生态恢复工程对生长季湿地土壤无机硫形态变化的影响。结果表明,生态恢复工程不同程度地改变了湿地土壤中各形态无机硫含量。相对于R0,R2002和R2007土壤中的水溶性硫(H2O—S)含量分别降低46.7%和44.7%,吸附性硫(Adsorbed—S)和盐酸可溶性硫(HCl—Soluble—S)含量分别增加0.4%,116.0%和50.1%,29.1%,而盐酸挥发性硫(HCl—Volatile—S)含量在R2002下降8.0%,在R2007增加19.7%。不同恢复阶段湿地土壤中各形态无机硫含量在生长季呈不同的变化特征,这一方面与不同湿地植物生长节律以及地上与地下之间的硫养分供给关系密切相关;另一方面则与不同生态补水方式导致的环境因子,尤其是pH、EC和氮养分的变化有关。随着恢复年限的增加,湿地土壤的总无机硫(TIS)含量以及其占全硫(TS)含量的比例均呈降低趋势。湿地土壤的TIS储量整体随恢复年限的增加而降低,而这种降低主要取决于H2O—S、Adsorbed—S和HCl—Soluble—S的贡献,且以H2O—S占优(78%~80%)。研究发现,随着黄河口湿地的逐渐恢复以及每年冬季芦苇收割活动的进行,恢复湿地土壤中的无机硫养分逐渐趋于缺乏状态,长期来看将不利于维持湿地的稳定与健康。 相似文献
8.
Gemma A. Miller Robert M. Rees Bryan S. Griffiths Joanna M. Cloy 《Soil Use and Management》2020,36(2):285-298
Agricultural soils are important sources of greenhouse gases (GHGs). Soil properties and environmental factors have complex interactions which influence the dynamics of these GHG fluxes. Four arable and five grassland soils which represent the range of soil textures and climatic conditions of the main agricultural areas in the UK were incubated at two different moisture contents (50 or 80% water holding capacity) and with or without inorganic fertiliser application (70 kg N ha−1 ammonium nitrate) over 22 days. Emissions of N2O, CO2 and CH4 were measured twice per week by headspace gas sampling, and cumulative fluxes were calculated. Multiple regression modelling was carried out to determine which factors (soil mineral N, organic carbon and total nitrogen contents, C:N ratios, clay contents and pH) that best explained the variation in GHG fluxes. Clay, mineral N and soil C contents were found to be the most important explanatory variables controlling GHG fluxes in this study. However, none of the measured variables explained a significant amount of variation in CO2 fluxes from the arable soils. The results were generally consistent with previously published work. However, N2O emissions from the two Scottish soils were substantially more sensitive to inorganic N fertiliser application at 80% water holding capacity than the other soils, with the N2O emissions being up to 107 times higher than the other studied soils. 相似文献
9.
Abir Dey Brahma Swaroop Dwivedi Ranjan Bhattacharyya Siba Prasad Datta Mahesh Chand Meena Raj K. Jat Raj Kumar Gupta Mangi Lal Jat Vinod Kumar Singh Debarup Das Ravi G. Singh 《Soil Use and Management》2020,36(3):429-438
Increasing soil carbon (C) in arable soils is an important strategy to achieve sustainable yields and mitigate climate change. We investigated changes in soil organic and inorganic carbon (SOC and SIC) under conservation agriculture (CA) in a calcareous soil of the eastern Indo-Gangetic Plains of India. The treatments were as follows: conventional-till rice and wheat (CT-CT), CT rice and zero-till wheat (CT-ZT), ZT direct seeded rice (DSR) and CT wheat (ZT-CT), ZTDSR and ZT wheat without crop residue retention (ZT-ZT), ZT-ZT with residue (ZT-ZT+R), and DSR and wheat both on permanent beds with residue (PB-PB+R). The ZT-ZT+R had the highest total SOC in both 0–15 and 15–30 cm soil layers (20% and 40% higher (p < .05) than CT-CT, respectively), whereas total SIC decreased by 11% and 15% in the respective layers under ZT-ZT+R compared with CT-CT. Non-labile SOC was the largest pool, followed by very labile, labile and less labile SOC. The benefits of ZT and residue retention were greatest for very labile SOC, which showed a significant (p < .05) increase (~50%) under ZT-ZT+R compared with CT-CT. The ZT-ZT+R sequestered ~2 Mg ha−1 total SOC in the 0–15 cm soil layer in 6 years, where CT registered significant losses. Thus, the adoption of CA should be recommended in calcareous soils, for C sequestration, and also as a reclamation technique. 相似文献
10.
Siwei Shi Qingzhong Zhang Yilai Lou Zhangliu Du Qian Wang Ning Hu Yidong Wang Anna Gunina Jiqing Song 《Soil Use and Management》2021,37(1):95-103
Biochar addition can expand soil organic carbon (SOC) stock and has potential ability in mitigating climate change. Also, some incubation experiments have shown that biochar can increase soil inorganic carbon (SIC) contents. However, there is no direct evidence for this from the field experiment. In order to make up the sparseness of available data resulting from the long‐term effect of biochar amendment on soil carbon fractions, here we detected the contents and stocks of the bulk SIC and SOC fractions based on a 10‐year field experiment of consecutive biochar application in Shandong Province, China. There are three biochar treatments as no‐biochar (control), and biochar application at 4.5 Mg ha?1 year?1 (B4.5) and 9.0 Mg ha?1 year?1 (B9.0), respectively. The results showed that biochar application significantly enhanced SIC content (3.2%–24.3%), >53 μm particulate organic carbon content (POC, 38.2%–166.2%) and total soil organic carbon content (15.8%–82.2%), compared with the no‐biochar control. However, <53 μm silt–clay‐associated organic carbon (SCOC) content was significantly decreased (14%–27%) under the B9.0 treatment. Our study provides the direct field evidence that SIC contributed to carbon sequestration after the biochar application, and indicates that the applied biochar was allocated mainly in POC fraction. Further, the decreased SCOC and increased microbial biomass carbon contents observed in field suggest that the biochar application might exert a positive priming effect on native soil organic carbon. 相似文献