全文获取类型
收费全文 | 1109篇 |
免费 | 64篇 |
国内免费 | 113篇 |
专业分类
林业 | 37篇 |
农学 | 75篇 |
基础科学 | 20篇 |
436篇 | |
综合类 | 431篇 |
农作物 | 47篇 |
水产渔业 | 64篇 |
畜牧兽医 | 109篇 |
园艺 | 16篇 |
植物保护 | 51篇 |
出版年
2024年 | 15篇 |
2023年 | 27篇 |
2022年 | 47篇 |
2021年 | 41篇 |
2020年 | 37篇 |
2019年 | 45篇 |
2018年 | 45篇 |
2017年 | 60篇 |
2016年 | 56篇 |
2015年 | 54篇 |
2014年 | 60篇 |
2013年 | 88篇 |
2012年 | 108篇 |
2011年 | 87篇 |
2010年 | 58篇 |
2009年 | 51篇 |
2008年 | 55篇 |
2007年 | 67篇 |
2006年 | 43篇 |
2005年 | 56篇 |
2004年 | 35篇 |
2003年 | 22篇 |
2002年 | 17篇 |
2001年 | 24篇 |
2000年 | 12篇 |
1999年 | 8篇 |
1998年 | 14篇 |
1997年 | 7篇 |
1996年 | 9篇 |
1995年 | 10篇 |
1994年 | 5篇 |
1993年 | 4篇 |
1992年 | 1篇 |
1991年 | 3篇 |
1990年 | 3篇 |
1989年 | 2篇 |
1988年 | 2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1286条查询结果,搜索用时 15 毫秒
1.
2.
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
3.
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
4.
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
5.
Emissions of N2O were measured following addition of 15N‐labelled residues of tropical plant species [Vigna unguiculata (cowpea), Mucuna pruriens and Leucaena leucocephala] to a Ferric Luvisol from Ghana at a rate of 100 mg N/kg soil under controlled environment conditions. Residues were also applied in different ratio combinations with inorganic N fertilizer, at a total rate of 100 mg N/kg soil. N2O emissions were increased after addition of residues, and further increased with combined (ratio) applications of residues and inorganic N fertilizer. However, 15N‐N2O production was low and short‐lived in all treatments, suggesting that most of the measured N2O‐N was derived from the applied fertilizer or native soil mineral N pools. There was no consistent trend in magnitude of emissions with increasing proportion of inorganic fertilizer in the application. The positive interactive effect between residue‐ and fertilizer‐N sources was most pronounced in the 25:75 Leucaena:fertilizer and cowpea:fertilizer treatments where 1082 and 1130 mg N2O‐N/g residue were emitted over 30 days. N2O (loge) emission from all residue amended treatments was positively correlated with the residue C:N ratio, and negatively correlated with residue polyphenol content, polyphenol:N ratio and (lignin + polyphenol):N ratio, indicating the role of residue chemical composition in regulating emissions even when combined with inorganic fertilizer. The positive interactive effect in our treatments suggests that it is unlikely that combined applications of residues and inorganic fertilizer can lower N2O emissions unless the residue is of very low quality promoting strong immobilisation of soil mineral N. 相似文献
6.
A new type of inorganic anchoring material is developed as a substitution for anchoring adhesive to overcome some imperfections in the process of planting reinforcing steel bar.The mix proportion of the anchoring material is determined by experiments.The compressive strength,adhesive force to concrete,volume stability and anchoring force with steel bar are studied.The early strength of the anchoring inorganic material is quite high: for 1d up to 38.5MPa and 3d up to 60MPa.It is a good adhesive to concrete and the adhesive strength of 28d is about 2MPa.The anchoring material will have tiny volume expansion with the age,which is beneficial to enhancing the anchoring force.The essential component of the inorganic anchoring material is cement-based material,so some defects of the organic macromolecular material can be avoided,such as poor stability and requirement for vigorous construction conditions.Its characteristics in early strength,adhesive force to concrete and volume expansion can satisfy the requirement of the construction to the planting reinforcing steel bar and the loading force,thus it can be used as a substituting material for anchoring adhesive. 相似文献
7.
8.
为探究玉米高产和减少硝态氮残留的合理施肥模式,通过山西寿阳旱地春玉米田间试验和APSIM模型模拟,研究不同施肥类型和施氮量对春玉米产量、硝态氮残留量和氮肥利用率的影响。田间试验设置3个施肥类型主处理,包括化肥单施、有机无机肥配施(配施比例1∶1)和有机肥单施;7个施肥梯度副处理,分别为0、50、100、150、200、250、300 kg·hm-2,并利用2019—2021年试验站点数据对模型进行校准验证。结果表明:APSIM模型可以较好地模拟当地玉米产量和硝态氮残留量状况。各降水年型下,随氮肥施用量的增加,玉米产量先增加后减少,硝态氮残留量显著增加,氮肥利用率有所降低;相同施肥类型及施肥量下,丰水年的春玉米作物产量最高,硝态氮残留量最低,氮肥利用率最高;相同降水年型及施肥量下,有机无机肥配施方式的春玉米产量最高,硝态氮残留量居中,氮肥利用率最高。相较于化肥单施和有机肥单施方式,有机无机肥配施对于干旱地区玉米产量提升效果更好,其土壤硝态氮残留量对降水变化的敏感性相对较低,其氮肥利用率受降水影响也更小。综上,当施氮量介于148~168 kg·hm-2时,有机无机肥配施方式下土壤硝态氮残留量维持在阈值内,春玉米产量可达到理论产量的95%左右,适宜在研究区域推广应用。 相似文献
9.
有机无机氮肥配施下洛阳烟田土壤N2O排放特点及其控制因素 总被引:1,自引:0,他引:1
随着农田化肥使用量的逐年增加和土壤退化问题日趋严重,农田温室气体排放关注度持续提高,为研究旱作植烟土壤N_2O排放特征及影响机理,设置6个田间试验处理,分别为CK0(不施肥处理)、CK1(100%无机氮)、T1(50%无机氮+50%饼肥氮)、T2(50%无机氮+50%羊粪肥氮)、T3(25%无机氮+75%饼肥氮)、T4(25%无机氮+75%羊粪肥氮),各处理施氮量均为45 kg/hm2,烟田施用基肥后起142天内测量不同处理土壤N_2O排放通量、硝态氮、铵态氮含量、根层温度和含水率。结果表明:(1)基肥施入后的3~7天内,土壤N_2O排放通量进入高峰,无机肥处理和有机无机肥配施处理的高峰期分别可维持20,9天,追肥后3天再次出现排放峰并持续9天,随后伴随烟株的生长发育,烟地N_2O排放通量逐渐趋向稳定。(2)基肥施用后仅1个月内N_2O累积排放量可达到总排放量的27.4%~32.6%;处理间N_2O排放量和排放系数均表现为无机>有机+无机(1∶1)>有机+无机(3∶1),无机肥配施有机肥明显降低了肥料中氮素以N_2O形态的损失量;与无机肥相比,T1和T2烟叶产量分别增加9.44%和6.37%,T1、T2、T3和T4处理的N_2O排放强度有着不同程度的降低。(3)主成分分析结果显示,在不施肥烟地中0—5 cm土壤温度和含水率是N_2O排放通量主导因子,利用相关性分析此环境下温度和水分分别与N_2O排放通量间呈现显著和极显著正相关关系;施肥后土壤铵态氮含量和土壤含水率是烟地N_2O排放通量的主导因子且相关性分析均呈现极显著正相关关系。综上,旱地植烟土壤N_2O排放受氮肥种类影响较大,施肥后N_2O排放通量对土壤温度响应减弱,主要受土壤铵态氮含量和含水量的影响;在总氮量相同情况下,有机无机肥配施比例为1∶1时明显降低土壤N_2O排放并提高了产量,该比例饼肥和羊粪肥处理分别将烟地N_2O排放强度降低20.4%和23.7%。 相似文献
10.