全文获取类型
收费全文 | 8526篇 |
免费 | 1217篇 |
国内免费 | 5568篇 |
出版年
2024年 | 19篇 |
2023年 | 358篇 |
2022年 | 410篇 |
2021年 | 487篇 |
2020年 | 608篇 |
2019年 | 714篇 |
2018年 | 673篇 |
2017年 | 667篇 |
2016年 | 616篇 |
2015年 | 606篇 |
2014年 | 595篇 |
2013年 | 729篇 |
2012年 | 616篇 |
2011年 | 561篇 |
2010年 | 490篇 |
2009年 | 647篇 |
2008年 | 571篇 |
2007年 | 646篇 |
2006年 | 557篇 |
2005年 | 516篇 |
2004年 | 460篇 |
2003年 | 457篇 |
2002年 | 355篇 |
2001年 | 325篇 |
2000年 | 294篇 |
1999年 | 300篇 |
1998年 | 223篇 |
1997年 | 207篇 |
1996年 | 214篇 |
1995年 | 196篇 |
1994年 | 179篇 |
1993年 | 129篇 |
1992年 | 123篇 |
1991年 | 106篇 |
1990年 | 116篇 |
1989年 | 105篇 |
1988年 | 78篇 |
1987年 | 58篇 |
1986年 | 56篇 |
1985年 | 38篇 |
1984年 | 41篇 |
1983年 | 11篇 |
1982年 | 48篇 |
1981年 | 25篇 |
1980年 | 24篇 |
1979年 | 23篇 |
1978年 | 7篇 |
1975年 | 4篇 |
1973年 | 6篇 |
1958年 | 5篇 |
排序方式: 共有10000条查询结果,搜索用时 390 毫秒
51.
The effect of soil salinity and soil moisture on the growth and yield of maxipak wheat (Triticum aestivum L.) was studied in a lath-house experiment in whih, chloride-sulphate salt mixtures were used to artificially salinize a sandy loam soil from Al-Jadyriah Baghdad. Five soil salinity levels of ECe's equal to 1.7 (Control) 4.2, 5.8, 8.1, 9.4 and 11.0dSm–1 were prepared and used at 3 levels of available soil moisture depletion, namely, 25, 50, and 75% as determined by weight. Both growth (vegetative) and yield components were studied throughout the growing season.Results showed that increasing the soil salinity from 1.7 to 11.0 dSm–1, and decreasing the available soil water from 75 to 25% resulted in independent and significant decreases in Mazipak wheat growth and yield components at different stages of plant development. Root growth showed more sensitivity to both available soil water and soil salinity level than other components. It has been concluded that at soil salinity levels of more than 8.0 dSm–1, available soil water became a limiting factor on wheat growth and the maintenance of 75% of available soil water during the growth period is recommended to obtain satisfactory grain yield. 相似文献
52.
Victor Chude 《Plant and Soil》1988,112(2):293-295
The profile distribution of total and extractable B was determined in 16 Nigerian cacao-growing soil profiles formed from
different parent materials. Total B for all soils ranged from 8 to 54μgg−1 with a mean of 24μgg−1. The soils formed from sandstones in the rainforest zone contained higher amounts of total B than soils derived from basement
complex. Boron extractable in hot water, in 0.1% CaCl2, and in 1N NH4OAc varied from 0.13 to 1.38, 0.44 to 1.20 0.03 to 0.56μgg−1 respectively. The corresponding means were 0.66, 0.75 and 0.27μgg−1 B. Soils on metamorphic rocks gave the highest values. All extractable B values were related to organic matter while only
CaCl2-extractable B correlated with total B. Generally total and extractable B values were higher in the top soils than in the
subsoils. 相似文献
53.
The fate of sheep urine-N applied to an upland grass sward at four dates representing widely differing environmental conditions,
was followed in soil (0–20 cm) and in herbage. Urine was poured onto 1-m2 plots to simulate a single urination in August 1984 (warm and dry), May (cool), July and August 1985 (cool and wet) at rates
equivalent to 40–52 g N m−2.
The transformation of urine-N (61–69% urea-N) in soil over a 6–7 week period followed the same general pattern when applied
at different times during the season; rapid hydrolysis of urea, the appearance of large amounts of urine-N as ammonium in
soil extracts, and the appearance of nitrate about 14 days after application. The magnitude of “apparent” nitrification however
differed markedly with environmental conditions, being greatest in May 1985 when a maximum of 76% of the inorganic soil N
was in the form of nitrate. At all other application dates nitrate levels were relatively low. With the August 1984 application
soil inorganic N returned to control levels (given water only) after 31 days but considerable amounts remained in soil for
60–90 days with the other applications.
Weekly cuts to 3-cm indicated that increases in herbage dry matter and N yields in response to urine application were greatest
in absolute terms after the May 1985 application and continued for at least 70 days with all applications. Relative to control
plots the May application resulted in a 3-fold increase in herbage DM compared with corresponding values of 6-, 5-, and 7-fold
increases with the August 1984, July and August 1985 applications. Recovery of urine-N in herbage was poor averaging only
17% of that applied at different dates, while recovery in soil extracts was incomplete. The exact routes of loss (volatilisation,
leaching, denitrification or immobilisation) were not quantified but it is evident that substantial amounts of urine-N can
be lost from the soil-plant system under upland conditions. 相似文献
54.
应用电子探针对植物根际和根内营养元素微区分布的探讨 总被引:3,自引:0,他引:3
用电子探针可检测出玉米、大豆根际和根内含有Na,Mg,Al,Si,P,S,Cl,K,Ca,Ti,Fe,Cu和Zn 13种元素。这些元素在根际土壤、粘液层和根组织内的含量分布有一定的规律性。除Si,Al,Ca,Fe在根际土壤中峰值较高外,Ti仅在土壤中达到可检测量;S,Fe和Zn富集在粘液层,Mg,P,Cl只在根组织内才有较明显的峰。这些规律可作为区分根—土界面的参考指标。K含量在根内明显高于根际土壤,并由表皮层到中柱径向增加;Ca则与K不同,且受植物种类的影响。 相似文献
55.
Metabolism of nitric oxide and nitrous oxide during nitrification and denitrification in soil at different incubation conditions 总被引:1,自引:0,他引:1
Abstract NO production and consumption rates as well as N2 O accumulation rates were measured in a loamy cambisol which was incubated under different conditions (i.e. soil moisture content, addition of nitrogen fertilizer and/or glucose, aerobic or anaerobic gas phase). Inhibition of nitrification with acetylene allowed us to distinguish between nitrification and denitrification as sources of NO and N2 O. Under aerobic conditions untreated soil showed very low release of NO and N2 O but high consumption of NO. Fertilization with NH4 + or urea stimulated both NO and N2 O production by nitrification. Addition of glucose at high soil moisture contents led to increased N2 and N2 O production by denitrification, but not to increased NO production rates. Anaerobic conditions, however, stimulated both NO and N2 O production by denitrification. The production of NO and N2 O was further stimulated at low moisture contents and after addition of glucose or NO3 − . Anaerobic consumption of NO by denitrification followed Michaelis-Menten kinetics and was stimulated by addition of glucose and NO3 − . Aerobic consumption of NO followed first-order kinetics up to mixing ratios of at least 14 ppmv NO, was inhibited by autoclaving but not by acetylene, and decreased with increasing soil moisture content. The high NO-consumption activity and the effects of soil moisture on the apparent rates of anaerobic and aerobic production and consumption of NO suggest that diffusional constraints have an important influence on the release of NO, and may be a reason for the different behaviour of NO release vs N2 O release. 相似文献
56.
Toshiyuki Sato 《Ecological Research》1992,7(1):1-7
Gametophyte populations inAthyrium brevifrons were analysed with respect to population size and surviving area (%) of individual thalli in a transplant garden at Sapporo
during 5–26 April 1983, to study the safe-microsite for gametophyte establishment in nature. Spores dispersed in August 1982
germinated and grew into thalli of various widths (<10 mm); 10.3% of the thalli matured by early October 1982. Maturation
was attained by gametophytes of width 4–7 mm. The number of gametophytes gradually decreased with increasing width. By April
1983, 20.5% of total gametophytes were mature with a mode of 5–6 mm in width. The relative number of gametophytes with surviving
area of 2–20% increased and that of 85–100% decreased in accordance with collection days delayed until after snow-melt. Surviving
area (%) on gametophyte of all widths decreased with decreasing soil moisture contents. In particular, immature gametophytes
of 2–4 mm width showed a significant correlation (P<0.01) between soil moisture content and relative number of gametophytes with 0–20% surviving area and mean surviving area
(%) of every width of thalli. The spring desiccation might be a factor that reduces or limits gametophyte populations in nature. 相似文献
57.
Dicotyledonous plants subjected to Fe-deficiency stress can decrease pH in the rhizosphere by proton excretion and reduce ferric iron by an activated reduction system in the plasma membranes of the root or by reductants released from the roots. The efficiency by which these plants take up Fe may strongly depend on their cation-anion balance. This study presents results of two experiments conducted to evaluate the effect of K, growth stage and cultivar on ionic balance and Fe acquisition of peanut (Arachis hypogaea L.) plants.Potassium applications to the high calcareous soil (30.3% CaCO3) favoured proton release, but did not ameliorate plant Fe acquisition. At the earliest stages of plant growth, anion uptake exceeded cation uptake due to intensive N uptake. With time, a shift in the ionic balance was observed as a result of predominant cation uptake. It appears that the relationship between H/OH-ion release and Fe nutrition of peanut plants is actually a complex phenomenon under soil conditions and depends on some soil parameters, such as CaCO3 content. Even by enhanced H-ion release Fe nutrition of plants can be impaired if soil CaCO3 is too high. 相似文献
58.
Silicon accumulation and water uptake by wheat 总被引:2,自引:0,他引:2
Silicon (Si) content in cereal plants and soil-Si solubility may be used to estimate transpiration, assuming passive Si uptake. The hypothesis for passive-Si uptake by the transpiration stream was tested in wheat (Triticum aestivum cv. Stephens) grown on the irrigated Portneuf silt loam soil (Durixerollic calciorthid) near Twin Falls, Idaho. Treatments consisted of 5 levels of plant-available soil water ranging from 244 to 776 mm provided primarily by a line-source sprinkler irrigation system. Evapotranspiration was determined by the water-balance method and water uptake was calculated from evapotranspiration, shading, and duration of wet-surface soil. Water extraction occurred from the 0 to 150-cm zone in which equilibrium Si solubility (20°C) was 15 mg Si L–1 in the Ap and Bk (0–58 cm depth) and 23 mg Si L–1 in the Bkq (58–165 cm depth).At plant maturity, total Si uptake ranged from 10 to 32 g m–2, above-ground dry matter from 1200 to 2100 g m–2 and transpiration from 227 to 546 kg m–2. Silicon uptake was correlated with transpiration (Siup=–07+06T, r2=0.85) and dry matter yield with evapotranspiration (Y=119+303ET, r2=0.96). Actual Si uptake was 2.4 to 4.7 times that accounted for by passive uptake, supporting designation of wheat as a Si accumulator. The ratio of Si uptake to water uptake increased with soil moisture. The confirmation of active Si uptake precludes using Si uptake to estimate water use by wheat. 相似文献
59.
Air dry soil samples stored at room temperature for more than one and a half years, were used as inocula for actinorhizal plants. Seedlings of Colletia paradoxa, Discaria americana, D. articulata and D. trinervis (Rhamnaceae) cultivated in nitrogen-free nutrient solution, were inoculated by adding dry soil to the solution. All the soil samples tested were able to induce nodulation, showing the presence of infective propagules of Frankia. Healthy growth of nodulated plants suggested the occurrence of nitrogen fixation. 相似文献
60.
An inflatable minirhizotron system for root observations with improved soil/tube contact 总被引:3,自引:1,他引:2
Commonly used minirhizotrons consisting of a transparent tube inserted into the soil seldom attain good contact between the tube and the soil, which leads to root growth occurring in a gap rather than in the soil. A new system is described involving an inflatable flexible rubber wall, made from a modified motorcycle tube. Pressure ensures a proper tube/soil contact so that the environmental circumstances for root growth along the tube more closely correspond to those in the undisturbed soil. Before the endoscope slide is introduced into the minirhizotron for taking pictures, the inflatable tube is removed, so that there is no-often opaque-wall between the endoscope and the roots. This improves the picture quality and facilitates the analysis of root images. 相似文献