全文获取类型
收费全文 | 853篇 |
免费 | 49篇 |
国内免费 | 81篇 |
专业分类
林业 | 78篇 |
农学 | 64篇 |
基础科学 | 27篇 |
348篇 | |
综合类 | 290篇 |
农作物 | 42篇 |
水产渔业 | 49篇 |
畜牧兽医 | 48篇 |
园艺 | 20篇 |
植物保护 | 17篇 |
出版年
2024年 | 10篇 |
2023年 | 20篇 |
2022年 | 21篇 |
2021年 | 30篇 |
2020年 | 30篇 |
2019年 | 31篇 |
2018年 | 18篇 |
2017年 | 37篇 |
2016年 | 41篇 |
2015年 | 34篇 |
2014年 | 51篇 |
2013年 | 37篇 |
2012年 | 64篇 |
2011年 | 55篇 |
2010年 | 62篇 |
2009年 | 47篇 |
2008年 | 56篇 |
2007年 | 60篇 |
2006年 | 36篇 |
2005年 | 40篇 |
2004年 | 23篇 |
2003年 | 30篇 |
2002年 | 12篇 |
2001年 | 15篇 |
2000年 | 22篇 |
1999年 | 11篇 |
1998年 | 11篇 |
1997年 | 11篇 |
1996年 | 12篇 |
1995年 | 6篇 |
1994年 | 4篇 |
1993年 | 8篇 |
1992年 | 9篇 |
1991年 | 8篇 |
1990年 | 6篇 |
1989年 | 5篇 |
1988年 | 5篇 |
1987年 | 3篇 |
1981年 | 1篇 |
1977年 | 1篇 |
排序方式: 共有983条查询结果,搜索用时 796 毫秒
21.
鸡粪对芸豆土壤有机碳氧化稳定性与碳库管理指数的影响 总被引:5,自引:0,他引:5
为探讨鸡粪与化肥不同比例配施对芸豆/玉米轮作土壤有机碳氧化稳定性及碳库管理指数的影响,通过2009—2014年大田试验,研究了N100(尿素提供100%的氮)、M10N90(鸡粪和尿素分别提供10%和90%的氮)、M30N70(鸡粪和尿素分别提供30%和70%的氮)和M50N50(鸡粪和尿素各提供50%的氮)等不同施肥处理对芸豆/玉米轮作土壤有机碳(TOC)、微生物量碳(MBC)、易氧化碳(ROC)含量及有机碳氧化稳定性与碳库管理指数(CPMI)的影响。结果表明,M_(10)N_(90)、M30N70和M50N50处理的TOC含量分别比N100处理提高5.21%、12.74%和19.87%;M_(30)N_(70)处理的MBC、ROC含量和CPMI均最高,并显著高于其他处理,其中ROC含量分别较N100、M10N90和M50N50处理提高54.03%、16.50%和10.43%,CPMI分别提高75.10、30.75和27.94;但M30N70处理的有机碳氧化稳定系数显著低于其他处理,并较N100处理下降35.95%。此外,该处理能显著提高芸豆产量,明显改善品质,且影响效果明显优于其他处理。相关性分析表明,芸豆产量、维生素C含量与MBC、ROC、有机碳氧化稳定系数和CPMI之间有极显著或显著的相关性,各指标间具有紧密的内在联系。综合分析认为,在芸豆/玉米轮作种植中配施鸡粪措施有利于提高土壤质量,增强土壤供肥性能,并促进芸豆的高产优质生长,其中鸡粪氮与尿素氮以3∶7比例搭配的作用效果最佳。 相似文献
22.
Influence of inorganic fertilizers and organic amendments on soil organic matter and soil microbial properties under tropical conditions 总被引:33,自引:0,他引:33
Soil organic matter level, mineralizable C and N, microbial biomass C and dehydrogenase, urease and alkaline phosphatase
activities were studied in soils from a field experiment under a pearl millet-wheat cropping sequence receiving inorganic
fertilizers and a combination of inorganic fertilizers and organic amendments for the last 11 years. The amounts of soil organic
matter and mineralizable C and N increased with the application of inorganic fertilizers. However, there were greater increases
of these parameters when farmyard manure, wheat straw or Sesbania bispinosa green manure was applied along with inorganic fertilizers. Microbial biomass C increased from 147 mg kg–1 soil in unfertilized soil to 423 mg kg–1 soil in soil amended with wheat straw and inorganic fertilizers. The urease and alkaline phosphatase activities of soils
increased significantly with a combination of inorganic fertilizers and organic amendments. The results indicate that soil
organic matter level and soil microbial activities, vital for the nutrient turnover and long-term productivity of the soil,
are enhanced by use of organic amendments along with inorganic fertilizers.
Received: 6 May 1998 相似文献
23.
24.
Phosphate-solubilizing microorganisms associated with the rhizosphere of mangroves in a semiarid coastal lagoon 总被引:14,自引:0,他引:14
P. Vazquez G. Holguin M. E. Puente A. Lopez-Cortes Y. Bashan 《Biology and Fertility of Soils》2000,30(5-6):460-468
The phosphate-solubilizing potential of the rhizosphere microbial community in mangroves was demonstrated when culture media
supplemented with insoluble, tribasic calcium phosphate, and incubated with roots of black (Avicennia germinans L.) and white [Laguncularia racemosa (L.) Gaertn.] mangrove became transparent after a few days of incubation. Thirteen phosphate-solubilizing bacterial strains
were isolated from the rhizosphere of both species of mangroves: Bacillus amyloliquefaciens, Bacillus licheniformis, Bacillus atrophaeus, Paenibacillus macerans, Vibrio proteolyticus, Xanthobacter agilis, Enterobacter aerogenes, Enterobacter taylorae, Enterobacter asburiae, Kluyvera cryocrescens, Pseudomonas stutzeri, and Chryseomonas luteola. One bacterial isolate could not be identified. The rhizosphere of black mangroves also yielded the fungus Aspergillus niger. The phosphate-solubilizing activity of the isolates was first qualitatively evaluated by the formation of halos (clear zones)
around the colonies growing on solid medium containing tribasic calcium phosphate as a sole phosphorus source. Spectrophotometric
quantification of phosphate solubilization showed that all bacterial species and A. niger solubilized insoluble phosphate well in a liquid medium, and that V. proteolyticus was the most active solubilizing species among the bacteria. Gas chromatographic analyses of cell-free spent culture medium
from the various bacteria demonstrated the presence of 11 identified, and several unidentified, volatile and nonvolatile organic
acids. Those most commonly produced by different species were lactic, succinic, isovaleric, isobutyric, and acetic acids.
Most of the bacterial species produced more than one organic acid whereas A. niger produced only succinic acid. We propose the production of organic acids by these mangrove rhizosphere microorganisms as a
possible mechanism involved in the solubilization of insoluble calcium phosphate.
Received: 21 April 1999 相似文献
25.
利用盆栽试验研究了几种人工合成磷源在轻粘质潮土根际和本体土壤中的形态转化及配施不同形态氮肥对其形态转化的影响 ,结果表明 ,作物耗竭引起根际所有形态无机磷不同程度的下降。施入土壤的DCP(CaHPO4 ·2H2 O)、OCP(Ca8(PO4 ) 6 )、Al P(AlPO4 ·nH2 O)等大部分转化为其它形态无机磷 ,而Fe P(FePO4 ·nH2 O)和FA(Ca10 (PO4 ) 6 F2 )大部分以自身形态存在 ,尤其是FA很少向其它形态转化 ,根际条件促进了它们向其它无机磷形态的转化。Al P和FA等的形态转化明显受氮肥形态的影响 ,Al P配施NO- 3 N下 ,绝大部分转化为磷灰石 ,NH 4 N配施下促进了FA向其它形态的转化 ,在所有的磷源处理中 ,根际和本体磷酸铁都有显著地增加 ,NH 4 N和CO(NH2 ) 2 处理下存在磷酸铁的根际累积 ;其次是磷酸二钙和磷酸铝也有明显地增加 ,二者存在根际的亏缺。不同磷源的形态转化规律与其有效性大小相一致。 相似文献
26.
低丘红壤有机碳库的密度及变异 总被引:19,自引:4,他引:19
在中国科学院红壤生态实验站,采样分析了不同利用方式下土壤有机C 库的密度及其变异。结果表明,低丘红壤有机C 的密度0 ~ 20cm为(2.09 0.69) kg/m2,0 ~ 100 cm为(5.01 1.46) kg/m2; 全N密度0 ~ 20 cm为(0.20 0.07) kg/m2, 0 ~ 100 cm为(0.59 0.14) kg/m2。从裸地到稀疏荒草地,0 ~ 20 cm和0 ~ 100 cm土壤有机C 密度可以提高1.0 kg/m2和1.7 kg/m2;而从稀疏荒草地到人工林地或园地,0 ~ 20 cm和0 ~ 100 cm土壤有机C 密度可以提高0.7 kg/m2和0.9 kg/m2;稀疏荒草地如果开垦利用为水田,经长期培肥达到高度熟化,则0 ~ 20 cm和0 ~ 100 cm土壤有机C 密度可以提高2.3 kg/m2和4.4 kg/m2。即使不同类型的人工林地和园地之间,0 ~ 20 cm和0 ~ 100 cm土壤有机C 的密度差异也可达到1.0 kg/m2和3.5 kg/m2。不同地形部位之间0 ~ 20 cm和0 ~ 100 cm土壤有机C 密度差异达到1.3 kg/m2和2.9 kg/m2,全N密度差异达0.1 kg/m2和0.3 kg/m2;不同肥力水平之间0 ~ 20 cm和0 ~ 100 cm土壤有机C 密度差异达到1.5 ~ 2.2 kg/m2和2.8 ~ 4.1 kg/m2,全N密度差异达0.07 ~ 0.11 kg/m2和0.20 ~ 0.23 kg/m2; 强烈侵蚀可以降低0 ~ 20 cm和0 ~ 100 cm土壤有机C 密度1.4 kg/m2和2.2 kg/m2。因此,通过调整土地利用方式,可以提高土壤有机C 库密度,增 相似文献
27.
在北京郊区中壤质潮土上设置田间试验。结果表明:花椰菜获最大产量的氮供应量为300kghm-2。生育期花椰菜主要吸收表层(0~30cm)土壤中的无机氮,对下层(30~60cm)土壤无机氮(Nmin)的利用随氮供应量的增加而减少。不同生育期0~60cm土层中无机氮(Nmin)含量均随氮供应量增加而增加,但施肥后土壤中最高无机氮(Nmin)含量出现的时间随氮供应量增加而延迟。花椰菜生育期土壤有机氮矿化速率随生长期延长而增加,平均达N1.3kghm-2d-1,相当于各处理总吸氮量的47.5%~89.2%。试验后0~30cm及30~60cm土层无机氮(Nmin)含量随氮供应量增加而明显增加,但60~90cm土层无机氮(Nmin)受氮供应的影响不明显。花椰菜当季氮肥利用率及氮素利用率随施氮量增加而降低,最佳产量时的氮肥利用率及氮素利用率分别为36.5%和50.8%。土壤-花椰菜体系氮素表观损失量随氮施用水平的增加而明显增加,但其占总氮供应(肥料氮+播前土壤氮)的比例受氮供应的影响不明显,大致为20%。 相似文献
28.
Stabilization mechanisms of organic matter in four temperate soils: Development and application of a conceptual model 总被引:2,自引:0,他引:2
Margit von Lützow Ingrid Kögel‐Knabner Bernard Ludwig Egbert Matzner Heinz Flessa Klemens Ekschmitt Georg Guggenberger Bernd Marschner Karsten Kalbitz 《植物养料与土壤学杂志》2008,171(1):111-124
Based on recent findings in the literature, we developed a process‐oriented conceptual model that integrates all three process groups of organic matter (OM) stabilization in soils namely (1) selective preservation of recalcitrant compounds, (2) spatial inaccessibility to decomposer organisms, and (3) interactions of OM with minerals and metal ions. The model concept relates the diverse stabilization mechanisms to active, intermediate, and passive pools. The formation of the passive pool is regarded as hierarchical structured co‐action of various processes that are active under specific pedogenetic conditions. To evaluate the model, we used data of pool sizes and turnover times of soil OM fractions from horizons of two acid forest and two agricultural soils. Selective preservation of recalcitrant compounds is relevant in the active pool and particularly in soil horizons with high C contents. Biogenic aggregation preserves OM in the intermediate pool and is limited to topsoil horizons. Spatial inaccessibility due to the occlusion of OM in clay microstructures and due to the formation of hydrophobic surfaces stabilizes OM in the passive pool. If present, charcoal contributes to the passive pool mainly in topsoil horizons. The importance of organo‐mineral interactions for OM stabilization in the passive pool is well‐known and increases with soil depth. Hydrophobicity is particularly relevant in acid soils and in soils with considerable inputs of charcoal. We conclude that the stabilization potentials of soils are site‐ and horizon‐specific. Furthermore, management affects key stabilization mechanisms. Tillage increases the importance of organo‐mineral interactions for OM stabilization, and in Ap horizons with high microbial activity and C turnover, organo‐mineral interactions can contribute to OM stabilization in the intermediate pool. The application of our model showed that we need a better understanding of processes causing spatial inaccessibility of OM to decomposers in the passive pool. 相似文献
29.
30.
The effects of organic manure, mineral fertilizer (NPK), and P-deficiency fertilization (NK) on the individual biomass of young wheat plants, arbuscular mycorrhizal (AM) colonization in wheat root systems, population sizes of soil organic phosphorus mineralizing bacteria (OPMB) and inorganic phosphate solubilizing bacteria (IPSB) as well as soil P-mineralization and -solubilization potential were investigated in a long-term (18-year) fertilizer experiment. The experiment included five treatments: organic manure, an equal mixture of organic manure and mineral fertilizer, fertilizer NPK, fertilizer NK, and the control (without fertilization). Plant biomass, population sizes of soil OPMB and IPSB were greatly increased (P<0.05) by the application of organic manure and slightly increased by the balanced application of mineral fertilizer, while undiminished AM colonization in wheat root system was only observed in the case of the NK treatment. Compared to balanced fertilization, P-deficiency fertilization resulted in a significant increase (P<0.05) of OPMB-specific mineralization potential (soil P-mineralization potential per OPMB cell) and highest IPSB-specific solubilization potential (soil P-solubilization potential per IPSB cell), suggesting that OPMB and IPSB are likely more metabolically active in P-deficiency fertilized soils after long-term fertilizer management, and mycorrhizal plants are more dependent on AM in P-poor soils than in P-fertilized soils. Our results also showed the different effects of mineral fertilizer versus organic manure on soil P-mineralization and -solubilization potentials, as well as specific potentials of OPMB and IPSB in arable soils. 相似文献