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81.
钼对小白菜叶绿素和抗坏血酸含量以及硝酸盐累积的影响   总被引:7,自引:0,他引:7  
研究了钼对盆栽小白菜叶绿素、抗坏血酸含量以及硝酸盐累积的影响。试验分为3组,对照组(CK),未施钼;试验1组(Mo1)施钼0.15mg/kg;试验2组(Mo2)施钼0.30mg/kg。盆栽3周后对小白菜取样,分别测定其硝酸盐、叶绿素和抗坏血酸的含量。结果表明,随着施钼量的增加,小白菜中硝酸盐的含量显著降低,叶绿素显著增加,且各组间差异极显著(p<0.01)。与CK相比,施钼后小白菜中抗坏血酸含量的增加幅度更大,其中Mo1组和Mo2组与对照组间差异极显著(p<0.01),而Mo1组和Mo2组之间差异显著(p<0.05)。钼可以显著改善小白菜的品质,有效防止其硝酸盐的累积。  相似文献   
82.
K. Reinink 《Euphytica》1991,54(1):83-92
Summary The genetics of nitrate content in butterhead lettuce (Lactuca sativa L.) was studied using the mean values of five parental genotypes and several generations obtained from crosses between them. One high nitrate parental genotype was chosen and four low nitrate ones. A diallel analysis showed additive genetic effects to be the major source of variation in generation means. Estimates of additive genetic effects differed significantly between experiments, indicating genotype x experiment interactions. Effects of dominance were relatively small. The size and direction of dominance varied between experiments. Reciprocal differences were of very limited size and also varied between experiments. The inheritance of nitrate content in lettuce fitted the additive-dominance genetic model.  相似文献   
83.
过量施用磷肥和有机肥对土壤磷渗漏的影响   总被引:5,自引:0,他引:5  
采用土柱培养的模拟试验方法,研究在不同磷水平土壤上大量施用磷肥和有机肥对土壤测试磷、土壤磷渗漏的影响及机理。结果表明,不同磷水平土壤施用磷肥和有机肥后,土壤CaCl2-P、Olsen-P和土壤渗漏液中可溶性磷均显著增加;单位量磷肥或有机肥所增加土壤各形态磷量随土壤磷水平的增加而增大;随着磷肥和有机肥用量的增加,单位量磷肥或有机肥所增加各形态磷量也逐渐增大,差异均达到显著和极显著水平;施用磷肥和有机肥土壤磷的最大吸磷量(Qm)和土壤磷吸持指数(PSI)逐渐减少,土壤磷的吸附饱和度(DPS)逐渐增加;单位量磷肥或有机肥所增加的土壤磷的吸附饱和度随着土壤磷水平的增加而增加。随磷肥和有机肥用量的增加,不同磷水平土壤磷的吸附饱和度逐渐增加、土壤磷的吸持指数下降、土壤磷的渗漏量逐渐增大;土壤磷渗漏量与土壤测试磷呈显著正相关;单位量磷肥或有机肥所增加的土壤测试磷随着磷肥或有机肥用量以及土壤磷水平的增加而增加。  相似文献   
84.
【目的】通过水肥管理达到减少温室土壤硝态氮残留、维持土壤质量的目的,探求温室土壤硝态氮残留与水肥用量的关系。【方法】在滴灌施肥条件下,以灌水量和氮、磷、钾及有机肥用量为试验因素,根据当地日光温室番茄长季节栽培实际中的水肥用量,设计各试验因子的水肥水平,采用五元二次通用旋转组合设计进行试验。拉秧后测定耕层土壤硝态氮量,建立土壤硝态氮量与水肥因子间的数学模型,据此分析了各单因子效应及二因素的耦合效应。【结果】施氮量对土壤硝态氮残留量影响最大,施磷量、灌水量和施钾量次之,有机肥用量最小。当其他因子为0水平时,土壤硝态氮残留量随氮肥用量的增多而增加,随施磷量呈开口向上的抛物线变化,随灌水量、施钾量以及有机肥用量呈开口向下的抛物线变化。灌水量及氮、磷、钾和有机肥用量对土壤硝态氮残留产生的影响程度随其他因子的水平而变,存在明显交互作用。模型寻优显示:灌水量455.1~471.5 mm,施氮量532.3~586.5 kg/hm2,施磷量420.8~466.4 kg/hm2,施钾量646.1~723.5 kg/hm2,有机肥用量25.6~27.9 t/hm2,耕层土壤硝态氮量可维持在100~150 mg/kg的较低水平。【结论】温室菜地土壤硝态氮残留量相对较大,可以通过优化水肥用量来减少土壤硝态氮的残留,故在滴灌施肥条件下仍需严格控制水肥用量。  相似文献   
85.
Quantification of the interactive effects of nitrogen (N) and water on nitrate (NO3) loss provides an important insight for more effective N and water management. The goal of this study was to evaluate the effect of different irrigation and nitrogen fertilizer levels on nitrate-nitrogen (NO3-N) leaching in a silage maize field. The experiment included four irrigation levels (0.7, 0.85, 1.0, and 1.13 of soil moisture depletion, SMD) and three N fertilization levels (0, 142, and 189 kg N ha−1), with three replications. Ceramic suction cups were used to extract soil solution at 30 and 60 cm soil depths for all 36 experimental plots. Soil NO3-N content of 0-30 and 30-60-cm layers were evaluated at planting and harvest maturity. Total N uptake (NU) by the crop was also determined. Maximum NO3-N leaching out of the 60-cm soil layer was 8.43 kg N ha−1, for the 142 kg N ha−1 and over irrigation (1.13 SMD) treatment. The minimum and maximum seasonal average NO3 concentration at the 60 cm depth was 46 and 138 mg l−1, respectively. Based on our findings, it is possible to control NO3 leaching out of the root zone during the growing season with a proper combination of irrigation and fertilizer management.  相似文献   
86.
研究了在饲料中添加稀土壳聚糖螯合盐(RECC)对水产颗粒饲料性能的影响。根据鲫(Carassiusauratus)鱼苗的营养需求配制4种类型的RECC试验日粮,即1号饲料(0.00%)、2号饲料(0.08%)、3号饲料(0.16%)和4号饲料(024%)。测定4种饲料的粉化率和溶失率。结果显示,添加稀土壳聚糖螯合盐后可以降低饲料的 粉化率,饲料中添加0.16%的稀土壳聚糖螯合盐效果尤其明显(P<0.01);在饲料中添加RECC可以显著降低饲料的溶失率(P<0.05),并可以提高和改善水产颗粒饲料的性能。  相似文献   
87.
The use of cattle manure (CM) for fertilization presents challenges for optimizing nitrogen (N) use. Our work aimed to assess N efficiencies, in a 6‐year experiment with three biennial rotations of four crops: oat–sorghum (first year) and ryegrass–maize (second year) in a rainfed humid Mediterranean area of Spain. Fertilization treatments included the following: control (no N), 250 kg mineral N ha?1 year?1 (250MN), three CM rates (supplying 170, 250 and 500 kg N ha?1 year?1) and four treatments where the two lowest CM rates were complemented with either 80 or 160 kg mineral N ha?1 year?1. Treatments were distributed randomly in each of three blocks. Maximum dry‐matter yield (~44–49 t ha?1 rotation?1) was achieved in the third rotation, and only the control and the 170CM yielded significantly less. Within the limitations of the EU Nitrate Directive, the N steady state supply of 170CM always requires a complement of mineral N (80 kg N ha?1) to maximize N agronomic efficiency. The maximum N‐fertilizer replacement value (250CM vs. 250MN) was 0·67, without significant differences between the two treatments in other N‐related efficiency indexes, which indicates that plants took advantage of residual‐N effects. Nitrogen losses by leaching in the 250CM treatment were around 5–7% of the N applied. This reinforces the sustainability of manure recycling in long cropping seasons.  相似文献   
88.
以郑单958和鲁单981为研究对象,进行水培分根试验,在正常供水和水分胁迫条件下,分别以均匀低浓度硝酸盐处理主根和种子根(LPR-LSR)、局部高浓度硝酸盐处理主根(HPR-LSR)和局部高浓度硝酸盐处理种子根(LPR-HSR),测定分析根系形态、生物量以及氮含量。结果表明:与氮低效鲁单981相比,氮高效郑单958具有较高的主根根长、根表面积、根系生物量、地上部生物量和氮累积量。水分胁迫条件下,郑单958和鲁单981的主根的根长、根表面积、根体积、地上部生物量和氮累积量总体上均低于正常水分条件。玉米主根和种子根对局部高浓度硝酸盐的反应存在差异。与均匀低浓度硝酸盐处理相比,局部高浓度硝酸盐处理促进正常水分条件下主根和种子根根系的生长,尤其是根长和根系表面积;在正常水分条件下,主根根长和根系表面积增加幅度范围为6.8%~27.3%和1.9%~21.9%,除HPR-LSR处理条件下的郑单958外,种子根根长和根系表面积增加幅度范围为30.4%~92.7%和10.5%~135.1%;在水分胁迫条件下,主根根长和表面积增加幅度范围为24.6%~152.9%和62.1%~229.9%,然而种子根根长降低了10.0%~29.9%,表明水分胁迫会影响种子根对高浓度硝酸盐的响应。除水分胁迫条件下LPR-HSR处理外,局部高浓度处理可同时增加两侧根系的生物量和氮累积量。无论是正常供水还是水分胁迫,与LPR-LSR处理相比,局部高浓度硝酸盐供应均能够增加地上部生物量以及氮累积量,在LPR-HSR处理条件下,增加幅度范围分别在35.0% ~107.9%和162.9%~291.1%,在HPR-LSR处理条件下分别为56.7%~109.4%和204.1%~377.0%,HPR-LSR处理条件下增加幅度较大,表明在氮素非均匀分布环境中,当主根处于高浓度硝酸盐区域时将会更显著促进生物量的增加和氮累积。  相似文献   
89.
Although preference for NH4+, NO3? or a combination of the two often differs among species, we know little about the responses of invasive plants to different inorganic N forms. Furthermore, many studies have suggested that an increase in N availability may facilitate further invasions. However, most of these studies predicted the positive feedback without considering the preference for N forms of invasive plants. Therefore, we cultivated four common invasive species (Mikania micrantha, Ipomoea cairica, Wedelia trilobata and Bidens pilosa) in South China with hydroponic media containing different forms of N (i.e. NO3?, NH4NO3 and NH4+) at equimolar concentrations. Our results showed that the N forms significantly affected the growth, biomass allocation and physiological traits of the plants. All four invasive plants supplied with NO3? alone had better performance and greater allocation to root biomass than did plants that were supplied with NH4+ alone. Moreover, the photosynthetic rate, pigment content and photosystem II activity of plants supplied with NO3? or NH4NO3 were significantly higher than those of plants supplied with NH4+alone. The results suggested that all four invasive plants preferred NO3? rather than NH4+, and changes in NO3? played an important role in furthering the invasions of these plants than did changes in NH4+. Our results implied that decreasing NO3? may be a useful tool for controlling and managing invasive plants preferring NO3?. In addition, this study highlighted the importance of considering plant N form preference to better understand plant invasions.  相似文献   
90.
生物炭对砂壤土氮素淋失的影响试验研究   总被引:2,自引:0,他引:2  
通过室内土柱模拟试验,研究了生物炭对砂壤土的p H值、电导率及氮素淋失的影响。试验设5个生物炭添加比例,分别为0(CK)、1%(T1)、2%(T2)、4%(T3)、6%(T4)。结果表明,p H值和电导率均随生物炭添加比例的增加呈逐渐升高的趋势,其中,各处理砂壤土的电导率较CK分别提高了2.79%、10.88%、11.30%、12.50%。土壤淋溶液中氮素随生物炭添加比例的增加,呈逐渐减小趋势,氮素累积淋溶量也逐渐减小。各处理淋溶液中氮素的淋失总量较CK分别降低了2.89%、7.41%、9.50%和12.25%。研究表明,生物炭能够有效改变砂壤土的理化性质,降低氮素的淋失量,降低地下水面源污染的风险。  相似文献   
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