全文获取类型
收费全文 | 7819篇 |
免费 | 334篇 |
国内免费 | 734篇 |
专业分类
林业 | 398篇 |
农学 | 596篇 |
基础科学 | 95篇 |
3455篇 | |
综合类 | 2349篇 |
农作物 | 520篇 |
水产渔业 | 140篇 |
畜牧兽医 | 971篇 |
园艺 | 160篇 |
植物保护 | 203篇 |
出版年
2024年 | 33篇 |
2023年 | 119篇 |
2022年 | 153篇 |
2021年 | 206篇 |
2020年 | 236篇 |
2019年 | 226篇 |
2018年 | 176篇 |
2017年 | 315篇 |
2016年 | 425篇 |
2015年 | 321篇 |
2014年 | 365篇 |
2013年 | 713篇 |
2012年 | 624篇 |
2011年 | 519篇 |
2010年 | 457篇 |
2009年 | 423篇 |
2008年 | 360篇 |
2007年 | 476篇 |
2006年 | 399篇 |
2005年 | 319篇 |
2004年 | 253篇 |
2003年 | 224篇 |
2002年 | 152篇 |
2001年 | 135篇 |
2000年 | 160篇 |
1999年 | 106篇 |
1998年 | 116篇 |
1997年 | 115篇 |
1996年 | 128篇 |
1995年 | 88篇 |
1994年 | 71篇 |
1993年 | 83篇 |
1992年 | 79篇 |
1991年 | 61篇 |
1990年 | 61篇 |
1989年 | 63篇 |
1988年 | 47篇 |
1987年 | 33篇 |
1986年 | 15篇 |
1985年 | 8篇 |
1984年 | 5篇 |
1983年 | 6篇 |
1982年 | 1篇 |
1981年 | 5篇 |
1979年 | 3篇 |
1976年 | 2篇 |
1975年 | 1篇 |
1956年 | 1篇 |
排序方式: 共有8887条查询结果,搜索用时 15 毫秒
61.
浅谈推算和预测宏观尺度土壤N_2O释放量的方法 总被引:8,自引:1,他引:8
土壤是N2 O的最主要释放源 .本文综述了根据局部地区土壤N2 O释放观察结果 ,推算和预测宏观尺度土壤甚至全球土壤N2 O释放通量变化和年释放量的方法 ,评述了各类方法的优缺点 ;并着重讨论了释放过程机理模型的应用 . 相似文献
62.
Ingrid K Thomsen Per SchjønningJørgen E Olesen Bent T Christensen 《Soil biology & biochemistry》2003,35(6):765-774
The turnover of native and applied C and N in undisturbed soil samples of different texture but similar mineralogical composition, origin and cropping history was evaluated at −10 kPa water potential. Cores of structurally intact soil with 108, 224 and 337 g clay kg−1 were horizontially sliced and 15N-labelled sheep faeces was placed between the two halves of the intact core. The cores together with unamended treatments were incubated in the dark at 20 °C and the evolution of CO2-C determined continuously for 177 d. Inorganic and microbial biomass N and 15N were determined periodically. Net nitrification was less in soil amended with faeces compared with unamended soil. When adjusted for the NO3-N present in soil before faeces was applied, net nitrification became negative indicating that NO3-N had been immobilized or denitrified. The soil most rich in clay nitrified least N and 15N. The amounts of N retained in the microbial biomass in unamended soils increased with clay content. A maximum of 13% of the faeces 15N was recovered in the microbial biomass in the amended soils. CO2-C evolution increased with clay content in amended and unamended soils. CO2-C evolution from the most sandy soil was reduced due to a low content of potentially mineralizable native soil C whereas the rate constant of C mineralization rate peaked in this soil. When the pool of potentially mineralizable native soil C was assumed proportional to volumetric water content, the three soils contained similar proportions of potentially mineralizable native soil C but the rate constant of C mineralization remained highest in the soil with least clay. Thus although a similar availability of water in the three soils was ensured by their identical matric potential, the actual volume of water seemed to determine the proportion of total C that was potentially mineralizable. The proportion of mineralizable C in the faeces was similar in the three soils (70% of total C), again with a higher rate constant of C mineralization in the soil with least clay. It is hypothesized that the pool of potentially mineralizable C and C rate constants fluctuate with the soil water content. 相似文献
63.
Fractal features of soil particle size distribution and the implication for indicating desertification 总被引:5,自引:0,他引:5
Some of the effects of land desertification on soil properties are manifested by the coarsening of the soil particlesize distribution (PSD) and the losses in organic C and nutrients. The changes and characteristics of PSD and selected chemical properties in soils at the 0-15 cm plough layer from different degrees of desertified croplands are analyzed in the semiarid Horqin Sandy Land, northern China. The fractal dimension of the PSD is emanated to characterize the patterns of PSD. The relationships between the fractal dimension of the PSD and selected soil properties are discussed. The results show that: (1) in the transformation from potential desertified cropland to extremely desertified cropland, the sand content at the 0-15 cm soil increased from 69% to 93%, organic C and total N contents decreased by 65% and 69%, respectively; (2) the fractal dimension of PSD ranged from 2.179 to 2.611, the more the contents of sand, the lower the fractal dimension and the higher the desertified degree of farmland. In the desertification process within the studied area, the mean fractal dimension decreased from 2.555 for the potential desertified soils to 2.298 for extremely desertified soils; (3) there existed considerable linear relationships between fractal dimension and soil properties. It was shown that fractal dimensions of PSD are useful parameters able to monitor soil degradation and to estimate the degree of soil desertification. 相似文献
64.
65.
66.
控释氮肥对水稻的增产效应及提高肥料利用率的研究 总被引:86,自引:13,他引:86
符建荣 《植物营养与肥料学报》2001,7(2):145-152
田间试验在日本山形县鹤冈市进行 ,探讨了树脂包膜类控释氮肥基施与尿素、硫铵分次施肥对单季稻的增产效应 ;应用15N示踪法研究了不同施肥处理水稻的吸氮模式及肥料利用率。结果表明 ,移栽稻以尿素与控释氮肥 (LPS-100)按 1∶1混合基施产量最高 ,分别比尿素和硫铵分次施肥增产23.6%和9.2% ;直播稻以LP-100基施产量最高 ,分别增产 9.2%和4.0% ;控释肥基施 ,水稻自移栽 (或直播 )至幼穗分化期吸氮量明显高于尿素或硫铵分次施肥。15N示踪研究表明 ,最高分蘖前水稻从尿素和硫铵基肥中吸收的氮素只占基肥氮总吸收量的 33%~ 45% ,水稻从基肥中吸收氮素可延续至抽穗期 ,而从LP-100中吸氮可持续至收获期。15N示踪法测得的氮素总回收率 ,以尿素处理最高 ,硫铵和LP-100接近 ;差减法测得的氮素总回收率以LP-100为最高 ,尿素 /LPS-100、尿素、硫铵三者接近 ;基肥的氮素回收率以LP-100硫铵 尿素。尿素 /LPS-100和LP-100一次基施 ,氮素生理效率和农学效率明显高于尿素和硫铵 ,是高产的主要原因 相似文献
67.
Soil enzymes are linked to microbial functions and nutrient cycling in forest ecosystems and are considered sensitive to soil
disturbances. We investigated the effects of severe soil compaction and whole-tree harvesting plus forest floor removal (referred
to as FFR below, compared with stem-only harvesting) on available N, microbial biomass C (MBC), microbial biomass N (MBN),
and microbial biomass P (MBP), and dehydrogenase, protease, and phosphatase activities in the forest floor and 0–10 cm mineral
soil in a boreal aspen (Populus tremuloides Michx.) forest soil near Dawson Creek, British Columbia, Canada. In the forest floor, no soil compaction effects were observed
for any of the soil microbial or enzyme activity parameters measured. In the mineral soil, compaction reduced available N,
MBP, and acid phosphatase by 53, 47, and 48%, respectively, when forest floor was intact, and protease and alkaline phosphatase
activities by 28 and 27%, respectively, regardless of FFR. Forest floor removal reduced available P, MBC, MBN, and protease
and alkaline phosphatase activities by 38, 46, 49, 25, and 45%, respectively, regardless of soil compaction, and available
N, MBP, and acid phosphatase activity by 52, 50, and 39%, respectively, in the noncompacted soil. Neither soil compaction
nor FFR affected dehydrogenase activities. Reductions in microbial biomass and protease and phosphatase activities after compaction
and FFR likely led to the reduced N and P availabilities in the soil. Our results indicate that microbial biomass and enzyme
activities were sensitive to soil compaction and FFR and that such disturbances had negative consequences for forest soil
N and P cycling and fertility. 相似文献
68.
不同施氮量对水稻氮素吸收与分配的影响 总被引:24,自引:8,他引:24
运用15N示踪法研究了不同施氮量对两个品种水稻(4007和武运粳15)干物质积累量与其对15N吸收及分配的影响。结果表明,当施氮量超过N 150 kg/hm2时, 两个品种水稻子粒产量均不再显著增加。4007在4个施氮量下(N 100,150,200和 250 kg/hm2)分别比无氮区增产22.3%,36.9%,43.2%和38.1%;武运粳15分别增产10.6%,18.8%,27.1%和21.5%。同一施氮量下,4007子粒中15N累积量显著高于武运粳15,但茎叶和根中没有差异。增加施氮量降低了15N在水稻子粒中的分配比例,但提高了茎叶中15N的分配比例。15N在根中的分配比例不受施氮量和品种的影响。研究结果还表明,同一施氮量下,4007对肥料氮的总体利用率要比武运粳15高3~6个百分点。 相似文献
69.
灌溉策略及氮肥施用对设施番茄产量及氮素利用的影响 总被引:7,自引:0,他引:7
以传统水肥管理为对照,根据根层氮素实时监控技术与氮素供应目标值指标,对秋冬季设施番茄生育期进行氮肥追施优化管理,同时结合小管出流的方式比较研究采用每次灌溉至田间持水量及固定灌额两种策略对设施番茄产量及氮素追施调控的影响。结果表明,传统灌溉方式下,优化氮素处理保证了番茄产量,与传统氮肥处理相比,追施的氮肥数量减少了48%;在番茄的主要生育时期内,采用每次灌溉至田间持水量及固定灌额处理的灌溉量分别比传统灌溉处理减少46%和30%;采用同样指标所推荐的氮肥追施数量也分别减少14%和10%,明显减少土壤–蔬菜体系中氮素的表观损失,减轻了由于过量施氮而对环境造成的影响。 相似文献
70.
Mohammad I. Khalil Muhammad S. Rahman Urs Schmidhalter Hans‐Werner Olfs 《植物养料与土壤学杂志》2007,170(2):210-218
A 90‐day laboratory incubation study was carried out using six contrasting subtropical soils (calcareous, peat, saline, noncalcareous, terrace, and acid sulfate) from Bangladesh. A control treatment without nitrogen (N) application was compared with treatments where urea, ammonium sulfate (AS), and ammonium nitrate (AN) were applied at a rate of 100 mg N (kg soil)–1. To study the effect of N fertilizers on soil carbon (C) turnover, the CO2‐C flux was determined at nine sampling dates during the incubation, and the total loss of soil carbon (TC) was calculated. Nitrogen turnover was characterized by measuring net nitrogen mineralization (NNM) and net nitrification (NN). Simple and stepwise multiple regressions were calculated between CO2‐C flux, TC, NNM, and NN on the one hand and selected soil properties (organic C, total N, C : N ratio, CEC, pH, clay and sand content) on the other hand. In general, CO2‐C fluxes were clearly higher during the first 2 weeks of the incubation compared to the later phases. Soils with high pH and/or indigenous C displayed the highest CO2‐C flux. However, soils having low C levels (i.e., calcareous and terrace soils) displayed a large relative TC loss (up to 22.3%) and the added N–induced TC loss from these soils reached a maximum of 10.6%. Loss of TC differed depending on the N treatments (urea > AS > AN >> control). Significantly higher NNM was found in the acidic soils (terrace and acid sulfate). On average, NNM after urea application was higher than for AS and AN (80.3 vs. 71.9 and 70.9 N (kg soil)–1, respectively). However, specific interactions between N‐fertilizer form and soil type have to be taken into consideration. High pH soils displayed larger NN (75.9–98.1 mg N (kg soil)–1) than low pH soils. Averaged over the six soils, NN after application of urea and AS (83.3 and 82.2 mg N (kg soil)–1, respectively) was significantly higher than after application of AN (60.6 mg N (kg soil)–1). Significant relationships were found between total CO2 flux and certain soil properties (organic C, total N, CEC, clay and sand content). The most important soil property for NNM as well as NN was soil pH, showing a correlation coefficient of –0.33** and 0.45***, respectively. The results indicate that application of urea to acidic soils and AS to high‐pH soils could be an effective measure to improve the availability of added N for crop uptake. 相似文献