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11.
    
Soil and crop management practices may alter the quantity, quality, and placement of plant residues that influence soil C and N fractions. We examined the effects of two tillage practices [conventional till (CT) and no-till (NT)] and five crop rotations [continuous spring wheat (Triticum aestivum L.) (CW), spring wheat–fallow (W–F), spring wheat–lentil (Lens culinaris Medic.) (W–L), spring wheat–spring wheat–fallow (W–W–F), and spring wheat–pea (Pisum sativum L.)–fallow (W–P–F)] on transient land previously under 10 years of Conservation Reserve Program (CRP) planting on the amount of plant biomass (stems + leaves) returned to the soil from 1998 to 2003 and soil C and N fractions within the surface 20 cm in March 2004. A continued CRP planting was also included as another treatment for comparing soil C and N fractions. The C and N fractions included soil organic C (SOC), soil total N (STN), microbial biomass C and N (MBC and MBN), potential C and N mineralization (PCM and PNM), and NH4-N and NO3-N contents. A field experiment was conducted in a mixture of Scobey clay loam (fine-loamy, mixed, Aridic Argiborolls) and Kevin clay loam (fine, montmorillonitic, Aridic Argiborolls) in Havre, MT, USA. Plant biomass yield varied by crop rotation and year and mean annualized biomass was 45–50% higher in CW and W–F than in W–L. The SOC and PCM were not influenced by treatments. The MBC at 0–5 cm was 26% higher in W–W–F than in W–F. The STN and NO3-N at 5–20 cm and PNM at 0–5 cm were 17–1206% higher in CT with W–L than in other treatments. Similarly, MBN at 0–5 cm was higher in CT with W–L than in other treatments, except in CT with W–F and W–P–F. Reduction in the length of fallow period increased MBC and MBN but the presence of legumes, such as lentil and pea, in the crop rotation increased soil N fractions. Six years of tillage and crop rotation had minor influence on soil C and N storage between croplands and CRP planting but large differences in active soil C and N fractions.  相似文献   
12.
Agroforestry systems have the potential to increase sequestration of atmospheric carbon dioxide (CO2) as soil organic carbon (SOC) because of the increased rates of organic matter addition and retention. However, few studies have characterized the relative stability of sequestered SOC in soil. We characterized SOC storage in aggregate size and chemical stability classes to estimate the relative stability of SOC pools after the addition of Leucaena-KX2 pruning residues (mulch) from 2006 to 2008 in a shaded coffee agroforestry system in Hawaii. Soil samples were separated by microaggregate isolation, density flotation and dispersion, and acid hydrolysis, resulting in five distinct fractions that differed in relative stability: coarse particulate organic matter (POM), fine POM, microaggregate-protected POM, silt + clay hydrolyzable soil organic matter (SOM), and silt + clay non-hydrolyzable SOM. With mulch addition, the fine POM fraction increased. There was also a shift in the proportion of SOC to more stable silt + clay fractions. In the absence of mulch there was no significant change in SOC fractions. Given that the turnover time of SOC in silt + clay fractions is on the order of decades to centuries, the potential benefits of active shade management and mulching compensate for the loss of C sequestration in tree biomass from pollarding.  相似文献   
13.
全球变化背景下草地生态系统的退化及碳循环过程是生态学、地学、植物学和农学领域的研究热点之一。本文介绍了草地退化的概念、层次及退化现状,探讨了开垦、放牧、气候变化等人为因素和自然因素对内蒙古地区草地退化的驱动作用,重点分析了草地退化对碳循环过程的影响机制及退化草地恢复的固碳潜力,以期加深对草地生态系统退化及恢复过程中碳循环动态变化的理解。本文提出了内蒙古退化草地恢复过程中尚需解决的主要问题以及草业和畜牧业可持续发展的战略计划,以期为草地碳增汇方面的研究提供新的思路,并为决策者合理调整草地利用和保护布局提供理论基础。  相似文献   
14.
随着经济高速发展,高耗能、高污染的问题日益严重,通过绿色证券资源配置可以达到低碳、环保的目的。该文分析了绿色证券市场的资源配置模式,并对中国绿色证券市场的现状进行了分析;最后从上市条件、制度和立法等方面对提高绿色证券市场资源配置效率提出了具体的对策。  相似文献   
15.
在对区域性森林碳汇效益补偿机制的理论框架研究的基础上,以黑河地区森林碳汇效益补偿为例,采用森林碳密度法,并结合森林资源调查数据的有关统计结果,对该地区森林碳储量进行核算;然后采用按GDP总量配比方法,确定了森林碳汇效益的补偿标准。结果表明:截止到2007年,黑河林区森林总碳储量为3.50×106t,碳密度为178.97 t/km2,区域森林碳汇效果显著;黑河地区森林碳汇效益补偿费基准价(以万元GDP计)164.45元,截止2007年,全区应缴纳补偿费共计4.36×107元;黑河地区5×106元以上规模工业企业,截止2007年平均缴纳森林碳汇补偿费约4.356×105万元,其年度应缴纳费用仅为4 356元/a,征收森林碳汇补偿费对相关企业无显著影响,表明征收区域森林碳汇效益补偿费是可行的。  相似文献   
16.
    
A high level of biological degradation is usually observed in soils under semiarid climate where the low inputs of vegetal debris constraint the development of microbiota. Among vegetal inputs, cellulose and lignin are dominant substrates but their assimilation by the microbial community of semiarid soils is yet not understood. In the present study, 13C-labeled cellulose and 13C-labeled lignin (75 μg 13C g−1 soil) were added to two semiarid soils with different properties and degradation level. Abanilla soil is a bare, highly degraded soil without plant cover growing on it and a total organic C content of 5.0 g kg−1; Santomera soil is covered by plants (20% coverage) based on xerophytic shrubs and has a total organic C content of 12.0 g kg−1. The fate of added carbon was evaluated by analysis of the carbon isotope signature of bulk soil-derived carbon and extractable carbon fractions (water and sodium-pyrophosphate extracts). At long-term (120 days), we observed that the stability of cellulose- and lignin-derived carbon was dependent on their chemical nature. The contribution of lignin-derived carbon to the pool of humic substances was higher than that of cellulose. However, at short-term (30 days), the mineralization of the added substrates was more related to the degradation level of soils (i.e. microbial biomass). Stable isotope probing (SIP) of phospholipid fatty acids (PLFA-SIP) analysis revealed that just a minor part of the microbial community assimilated the carbon derived from cellulose and lignin. Moreover, the relative contribution of each microbial group to the assimilation of lignin-derived carbon was different in each soil.  相似文献   
17.
    
Measurements of the horizontal and vertical fluxes of energy and mass were taken at a crop canopy edge and downwind of it to examine the effects of inhomogeneity on surface-atmosphere exchange, for the ideal case of flat uniform terrain. Energy balance closure was also examined and the effects of the often-neglected advection terms on the energy budget were evaluated. The results show that neither vertical nor horizontal advection should be neglected for moderate distances downwind from heterogeneous boundaries, with the energy budget closure near the leading edge improved by more than 20% with the inclusion of the horizontal and vertical advection of latent and sensible heat. Significant mean advective horizontal and vertical flux divergences of water vapor and temperature were found even in typical daytime conditions. In stable conditions horizontal advection can be responsible for more than 15% of the scalar (water vapor) transport 136 canopy heights downwind of a change in water vapor source density and surface roughness.  相似文献   
18.
介绍了固碳思想产生的背景,在此基础上提出《土壤肥料学》教学过程中固碳思想融入与加强的必要性,并从提高教师专业素质,优化课程教学内容,丰富课程教学方法,注重实践能力培养等方面探讨了实现途径.  相似文献   
19.
A fraction of the C of residues incorporated into soil diffuses into the adjacent soil where it is eventually mineralised by microorganisms. Our aim was to quantify the contribution of this adjacent soil to the overall mineralisation of residue-C. For this, we incorporated two different residues labelled with 13C, with contrasting biochemical characteristics, namely mature wheat straw and young rye leaves, in soil cores. When 15% mineralisation of residue-C was measured for both residues, we separated a particulate fraction (the residues), the adjacent soil (4-5 mm thick) and a distant soil fraction, and incubated them separately for 5 h. We found that 76% of the mineralised wheat straw-C came from the particulate fraction and 23% from the soil adjacent to the residues. For rye leaves, 67% of the evolved CO2 came from the particulate fraction and 33% from the adjacent soil. It showed that the adjacent soil had a significant role in the mineralisation of carbon from the residues, even if the main source of residue-derived CO2 was the particulate fraction itself. The functional importance of the soil adjacent to the residues increased with the amount of soluble organic compounds that had been leached from the residue into the adjacent soil, suggesting a strong interaction between the initial quality of the crop residue and the resulting spatial heterogeneity of the decomposing microorganisms and C within the soil.  相似文献   
20.
    
It is well established that certain substrate additions to soils may accelerate or retard the mineralisation of soil organic matter. But up to now, research on these so called ‘priming effects’ was almost exclusively conducted with arable soils and with plant residues or glucose as additives. In this study, the effects of the uniformly 14C-labelled substrates fructose, alanine, oxalic acid and catechol on the mineralisation of soil organic carbon (SOC) from different horizons of two forest soils (Haplic Podzol and Dystric Cambisol) and one arable soil (Haplic Phaeozem) under maize and rye cultivation were investigated in incubation experiments for 26 days. Apart from the controls, all samples received substrate additions of 13.3 μg substrate-C mg−1 Corg. During the incubation, CO2-evolution was measured hourly and the amount of 14CO2 was determined at various time intervals. In almost all soils, priming effects were induced by one or several of the added substrates. The strongest positive priming effects were induced by fructose and alanine and occurred in the Bs horizon of the Haplic Podzol, where SOC mineralisation was nearly doubled. In the other soil samples, these substrates enhanced SOC mineralisation by +10 to +63%. Catechol additions generally reduced SOC mineralisation by −12 to −43% except in the EA horizon of the Haplic Podzol where SOC-borne CO2-evolution increased by +46%. Oxalic acid also induced negative as well as positive priming effects ranging from −24 to +82%. The data indicate that priming effects are ubiquitously occurring in surface and subsoil horizons of forest soils as well as in arable soils. Although a broad variety of soils was used within this study, relationships between soil properties and priming effects could not be ascertained. Therefore, a prediction on occurrence and magnitude of priming effects based on relatively easily measurable chemical and physical soil properties was not possible. Nevertheless, the data suggest that positive priming effects are most pronounced in forest soils that contain SOC of low biodegradability, where the added substrates may act as an important energy source for microbial metabolism.  相似文献   
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