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This study analyzes the impacts of climate change on maize yields using an econometric model that incorporates climate, economic, and technology variables. The major finding is climate change will not universally cause negative impacts of maize yields in the United States and China. The results of a simulation of climate change on maize yields over the period 2008-2030 show that a combination of changes in temperature and precipitation can either bring positive or negative effects on maize yields. Furthermore, variation in regional climatic and economic conditions makes the impacts of climatic change on maize yields substantially different in different regions. In this research, the impacts of climate change on maize yields are not simply examined by climate factors. Economic and technology adaptation effects on maize yields are also incorporated. Thus, even with significant changes in climate conditions that alter the maize crop’s growing environment and affect crop yields, a decrease in maize supply due to a decrease in maize yields would lead to an increase in the maize price, which in turn would induce farmers to add more investments in production inputs to raise yields. Thus, the decrease in actual yields may not be as dramatic as predicted in only climate factor considered cases. In this research, findings gained from the study can be used for early-staged policymaking decisions and advanced problem prevention programs. To ensure the continuous increase in maize yields in the future, further studies and research, as well as efficient environmental policies and actions are required. 相似文献
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Ohne Zusammenfassung 相似文献
44.
F. Madec J. M. Gourreau C. Kaiser J. Le Dantec P. Vannier M. Aymard 《Comparative immunology, microbiology and infectious diseases》1985,8(3-4)
Une étude est mise en place dans un groupe de 16 élevages intensifs venant de connaitre une attaque grippale et pratiquant à la fois le naissage et l'engraissement dans la région de Bretagne (France). L'objet de cette étude est de mettre en évidence une activité du virus grippal au sein des élevages en dehors des vagues épidémiques. Dans chaque élevage, 2 lots de porcelets sont individuellement suivis depuis la phase d'allaitement jusqu'à l'abattage. Des contrôles sérologiques mensuels sont pratiqués en vue de suivre l'évolution des anticorps grippaux ainsi que ceux de la maladie d'Aujeszky. En outre des écouvillonnages nasaux et des prélèvements de poumons sont réalisés en vue de recherches virales. Ces travaux sont accompagnés par la collecte de renseignements épidémiologiques dans chacun des élevages. Les anticorps grippaux d'origine colostrale inhibant l'hémagglutination décroissent assez rapidement chez le porcelet. Par la suite une conversion sérologique est observée sur près de 10% des animaux suivis. Les animaux concernés appartiennent à 4 des 16 élevages. La séroconversion intervient généralement après 3 mois d'âge. Aucun isolement viral n'a pu être réalisé. Certaines conditions semblent associées à la persistance d'une activité virale comme la démographie déséquilibrée du troupeau de truies, la conduite en continu de la porcherie d'engraissement, la préexistence d'une pathologie respiratoire sévère. Une séroconversion Aujeszky est également observée dans 3 des 4 élevages concernés par l'activité du virus grippal. 相似文献
45.
Dissolved organic phosphorus and sulphur as influenced by sorptive interactions with mineral subsoil horizons 总被引:2,自引:0,他引:2
K. Kaiser 《European Journal of Soil Science》2001,52(3):489-493
This study tested the hypothesis that, like dissolved organic nitrogen (N), dissolved organic phosphorus (P) and sulphur (S) are more mobile in soil than is organic carbon (C). To do so, I compared the sorption of organic P and S to subsoil materials with that of organic C. Soil samples were equilibrated with water‐soluble organic matter from the forest floor at pH 4 and in the equilibrium solutions organic C, P, and S, and their distributions between the hydrophilic and hydrophobic fraction were determined. Sorption of C within the organic matter did not differ from that of P and S. However, the hydrophilic fraction contained the vast majority of P and S and sorbed far less than the hydrophobic fraction. So the overall retention of organic P and S was smaller than that of organic C. This result suggested that dissolved organic matter is more important in the loss of plant nutrients than in the release of C from soil. 相似文献
46.
About the sorption of dissolved organic matter to forest soils This investigation characterizes the major forest soils of the temperate climatic zones (leptosols, vertisols, cambisols, luvisols, podzols, stagnosols, gleysols) as sorbents for dissolved organic matter (DOM). Sorption isotherms were obtained for 135 soil horizons from 36 profiles. When solutions containing no DOC were added, the release of dissolved organic carbon (DOC) was highest for horizons rich in organic C (A and Bh horizons). In subsoil horizons DOC release was much lower. Most of the investigated top soils (A and E horizons) and Bh, Bg, and C horizons showed a weak DOC sorption. This was caused by low contents of sorbents (clay and sesquioxides) and/or high contents of organic C. Organic C seems to reduce the DOC sorption by occupying binding sites. Subsoils rich in clay and sesquioxides like Bs, Bt, and Bw horizons showed a strong retention of DOC. Under the aerobic conditions of the experiments, some of the subsoils of stagnosols and gleysols also showed a strong sorption of DOC. However, in sorption experiments conducted after an anaerobic incubation, the DOC sorption decreased significantly. 相似文献
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Kaiser J 《Science (New York, N.Y.)》2000,289(5478):371-372
The debate, finally, seemed to be settled. After an 18-month review, a panel of the National Academy of Sciences last week weighed in on the health risks of mercury, endorsing strict safety levels proposed by the Environmental Protection Agency in 1995. But already some scientists are contesting the panel's conclusions, and federal agencies are grappling with how to reconcile competing regulations. 相似文献
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