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1.
对50例冠心病和50例随机做平板运动试验(TET)者作频域心电图(FCG)对比分析探讨FCG对冠心病的诊断价值。结果表明:单纯根据FCG异常诊断冠心病有较高假阳性(65.22%)。如将FCG的阳性指标作综合判断,虽然敏感性降低(88.00%降至70.00%)。假阳性都明显降低(65.22%降至26.00%)。认为TET的特异性较FCG高。若两者均为阴性,则冠心病可能性很小。  相似文献   
2.
从某鸡场发病鸡中分离出一株细菌,经过病原的分离培养、生化鉴定试验、动物回归试验等实验室方法,初步鉴定为副鸡嗜血杆菌。通过药敏试验筛选敏感药物,对该病的防治起到了积极的效果。  相似文献   
3.
该研究揭示了类开菲尔粒发酵乳酸度受发酵条件影响的主次顺序分别为时间、温度、接种量;乙酸、乳酸含量受发酵条件影响的主次顺序分别为温度、时间、接种量;甲酸含量受发酵条件影响的主次顺序分别为温度、接种量、时间。1:10接种、37℃条件下发酵16小时产酸量较高.  相似文献   
4.
以‘秦美’猕猴桃为试材,分离纯化在贮藏过程中引起腐烂的主要病原真菌。采用形态学观察及核糖体rDNA-ITS(Internal transcribed spacer)区序列分析法进行鉴定。结果表明:从腐烂猕猴桃中共分离出5株致病菌,对ITS区序列测序结果经GenBank数据库BLAST比对,A的ITS序列与Trichothecium roseum(EU552162.1)同一分支,支持率达100%;B的ITS序列与Fusarium tricinctum(AB587078.1)同一分支,支持率达99%;C的ITS序列与Penicillium expansum(AF330635.1)同一分支,支持率达99%;D的ITS序列与Colletotrichum boninense(KF819619.1)同一分支,支持率达99%;E的ITS序列与Botrytis elliptica(KJ638600.1)同一分支,支持率达100%。由形态学及ITS区序列分析,构建系统发育树,最终鉴定A为粉红聚端孢(Trichothecium roseum),B为镰刀菌属(Fusarium tricinctum),C为扩展青霉(Penicillium expansum),D为炭疽病菌(Colletotrichum boninense),E为灰葡萄孢(Botrytis cinerea)。5种病原真菌中灰葡萄孢为主要致病菌。  相似文献   
5.
植物转基因技术开辟了作物遗传改良的新途径。近年来,随着植物反应器技术的多元化发展以及日趋成熟,以玉米为分子工厂合成一些高价值产品成为研究热点。笔者就以玉米为植物反应器,用其生产糖类、必需氨基酸、不饱和脂肪酸、维生素、微量元素、生物酶、疫苗、抗体等各种高价值分子代谢物进行了综述,以期为中国分子农业领域的研究与应用提供参考。  相似文献   
6.
水稻插秧时,均匀、定位、定量及可靠施肥是保证秧苗均匀吸收肥料、均匀生长的必要因素,侧深施肥技术的应用给出了水稻生产过程中科学合理的施肥方法,以上问题有了明显改善,但水田机械施肥时肥料易受潮粘结堵塞带来了新的难题。为此,设计了一种电动螺旋施肥装置,并对该技术的优越性进行了分析。该装置通过控制器来调节直流电机转速,驱动软轴强制排肥,不但实现了施肥量的无极调节,且传动简单节省了空间,解决了水稻插秧侧深施肥过程中肥料受潮粘结堵塞开沟器的问题,提高了肥料排施作业质量和效果。样机试验表明:该机具有施肥均匀、性能先进及安全可靠等特点。该项新技术及装置技术关键突破后,解决了水稻插秧侧深施肥作业堵塞问题,可为水稻插秧侧深施肥技术的研究提供参考。  相似文献   
7.
During the last decade a new pattern of Hg pollution has been discerned, mostly in Scandinavia and North America. Fish from low productive lakes, even in remote areas, have been found to have a high Hg content. This pollution problem cannot be connected to single Hg discharges but is due to more widespread air pollution and long-range transport of pollutants. A large number of waters are affected and the problem is of a regional character. The national limits for Hg in fish are exceeded in a large number of lakes. In Sweden alone, it has been estimated that the total number of lakes exceeding the blacklisting limit of 1 mg Hg kg-1 in 1-kg pike is about 10 000. The content of Hg in fish has markedly increased in a large part of Sweden, exceeding the estimate background level by about a factor of 2 to 6. Only in the northernmost part of the country is the content in fish close to natural values. There is, however, a large variation of Hg content in fish within the same region, which is basically due to natural conditions such as the geological and hydrological properties of the drainage area. Higher concentrations in fish are mostly found in smaller lakes and in waters with a higher content of humic matter. Since only a small percentage of the total flow of Hg through a lake basin is transferred into the biological system, the bioavailability and the accumulation pattern of Hg in the food web is of importance for the Hg concentrations in top predators like pike. Especially, the transfer of Hg to low trophic levels seems to be a very important factor in determining the concentration in the food web. The fluxes of biomass through the fish community appear to be dominated by fluxes in the pelagic food web. The Hg in the lake water is therefore probably more important as a secondary source of Hg in pike than is the sediment via the benthic food chain. Different remedy actions to reduce Hg in fish have been tested. Improvements have been obtained by measures designed to reduce the transport of Hg to the lakes from the catchment area, eg. wetland liming and drainage area liming, to reduce the Hg flow via the pelagic nutrient chains, eg. intensive fishing, and to reduce the biologically available proportion of the total lake dose of Hg, eg. lake liming with different types of lime and additions of selenium. The length of time necessary before the remedy gives result is a central question, due to the long half-time of Hg in pike. In general it has been possible to reduce the Hg content in perch by 20 to 30% two years after treatments like lake liming, wetland liming, drainage area liming and intensive fishing. Selenium treatment is also effective, but before this method can be recommended, dosing problems and questions concerning the effects of selenium on other species must be evaluated. Regardless how essential these kind of remedial measures may be in a short-term perspective, the only satisfactory long-term alternative is to minimize the Hg contamination in air, soil and water. Internationally, the major sources of Hg emissions to the atmosphere are chlor-alkali factories, waste incineration plants, coal and peat combustion units and metal smelter industries. In the combustion processes without flue gas cleaning systems, probably about 20 to 60% of the Hg is emitted in divalent forms. In Sweden, large amounts of Hg were emitted to the atmosphere during the 50s and 60s, mainly from chlor-alkali plants and from metal production. In those years, the discharges from point sources were about 20 to 30 t yr 1. Since the end of the 60s, the emission of Hg has been reduced dramatically due to better emission control legislation, improved technology, and reduction of polluting industrial production. At present, the annual emissions of Hg to air are about 3.5 t from point sources in Sweden. In air, more than 95% of Hg is present as the elemental Hg form, HgO0. The remaining non-elemental (oxidized) form is partly associated to particles with a high wash-out ratio, and therefore more easily deposited to soils and surface waters by precipitation. The total Hg concentration in air is normally in the range 1 to 4 ng m-3. In oceanic regions in the southern hemisphere, the concentration is generally about 1 ng m?3, while the corresponding figure for the northern hemisphere is about 2 ng m-3. In remote continental regions, the concentrations are mainly about 2 to 4 ng m?3. In precipitation, Hg concentrations are generally found in the range 1 to 100 ng L?1. In the Nordic countries, yearly mean values in rural areas are about 20 to 40 ng L?1 in the southern and central parts, and about 10 ng L?1 in the northern part. Accordingly, wet deposition is about 20 (10 to 35) g km?2 yr?1 in southern Scandinavia and 5 (2 to 7) in the northern part. Calculations of Hg deposition based on forest moss mapping techniques give similar values. The general pattern of atmospheric deposition of Hg with decreasing values from the southwest part of the country towards the north, strongly suggests that the deposition over Sweden is dominated by sources in other European countries. This conclusion is supported by analyses of air parcel back trajectories and findings of significant covariations between Hg and other long range transported pollutants in the precipitation. Apart from the long range transport of anthropogenic Hg, the deposition over Sweden may also be affected by an oxidation of elemental Hg in the atmosphere. Atmospheric Hg deposited on podzolic soils, the most common type of forest soil in Sweden, is effectively bound in the humus-rich upper parts of the forest soil. In the Tiveden area in southern Sweden, about 75 to 80% of the yearly deposition is retained in the humus layer, chemically bound to S or Se atoms in the humic structure. The amount of Hg found in the B horizon of the soils is probably only slightly influenced by anthropogenic emissions. In the deeper layers of the soil, hardly any accumulation of Hg takes place. The dominating horizontal flow in the soils takes place in the uppermost soil layers (0 to 20 cm) during periods of high precipitation and high groun water level in the soils. The yearly transport of Hg within the soils has been calculated to be about 5 to 6 g km?2. The specific transport of total Hg from the soil system to running waters and lakes in Sweden is about 1 to 6 g km?2 yr1. The transport of Hg is closely related to the transport of humic matter in the water. The main factors influencing the Hg content and the transport of Hg in run-off waters from soils are therefore the Hg content in soils, the transport of humic matter from the soils and the humus content of the water. Other factors, for example acidification of soils and waters, are of secondary importance. Large peatlands and major lake basins in the catchment area reduce the out-transport of Hg from such areas. About 25 to 75% of the total load of Hg of lakes in southern and central Sweden originates from run-off from the catchment area. In lakes where the total load is high, the transport from run-off is the dominating pathway. The total Hg concentrations in soil solution are usually in the range 1 to 50, in ground water 0.5 to 15 and in run-off and lake water 2 to 12 ng L?1, respectively. The variation is largely due to differences in the humus content of the waters. In deep ground water with a low content of humic substances, the Hg concentration is usually below 1 ng L?1. The present amount and concentrations of Hg in the mor layer of forest soils are affected by the total anthropogenic emissions of Hg to the atmosphere, mainly during this century. Especially in the southern part of Sweden and in the central part along the Bothnian coast, the concentrations in the mor layer are markedly high. In southern areas the anthropogenic part of the total Hg content is about 70 to 90%. Here, the increased content in these soils is mainly caused by long-range transport and emissions from other European countries, while high level areas in the central parts are markedly affected by local historical emissions, mainly from the chlor-alkali industry. When comparing the input/output fluxes to watersheds it is evident that the present atmospheric deposition is much higher than the output via run-off waters, on average about 3 to 10 times higher, with the highest ration in the southern parts of Sweden. Obviously, Hg is accumulating in forest soils in Sweden at the present atmospheric deposition rate and, accordingly, the concentrations in forest soils are still increasing despite the fact that the emissions of Hg have drastically been reduced in Sweden during the last decades. The increased content of Hg in forest soils may have an effect on the organisms and the biological processes in the soils. Hg is by far the most toxic metal to microorganisms. In some regions in Sweden, the content of Hg in soils is already today at a level that has been proposed as a critical concentration. To obtain a general decrease in the Hg content in fish and in forest soils, the atmospheric deposition of Hg has to be reduced. The critical atmospheric load of Hg can be defined as the load where the input to the forest soils is less than the output and, consequently, where the Hg content in the top soil layers and the transport of Hg to the surface waters start to decrease. A reduction by about 80% of the present atmospheric wet deposition has to be obtained to reach the critical load for Scandinavia.  相似文献   
8.
研究了无胁迫和NaCl胁迫条件下,同基因型二倍体葡萄4个脯氨酸累积变异系和对照系愈伤组织的过氧化氢酶(CAT)和超氧物歧化酶(SOD)活性。结果表明,在无胁迫条件下,葡萄脯氨酸累积变异系的CAT和SOD活性显著高于对照系,4个变异系的CAT活性分别是对照的2.41,2.30,2.29和2.13倍,SOD活性分别是对照的4.51,3.69,3.84和3.72倍。在一定浓度NaCl胁迫下,对照系和变异系的CAT和SOD活性都有一定的增加,变异系的CAT和SOD活性仍高于对照系。脯氨酸累积变异系CAT和SOD活性高是其对NaCl胁迫具有较强抗性的可能原因之一  相似文献   
9.
Journal of Crop Science and Biotechnology - In this research, we investigated genetic diversity of 21 rice genotypes (Oryza sativa L.) assessed using 38 decamer RAPD primers. A total of 405 bands...  相似文献   
10.
 由(Xanthomonas campestris pv.glycines)所致大豆斑疹病病斑隆起成疱。盆栽大豆感病品种(Chippewa和Horosoy)和它们的抗病品系在二片真叶展开2/3时,用高压喷雾接种(Xanthomonas campestris pv.glycines),接种后的第3、6、9天分别取样;样本分二种处理分别在扫描电镜、透射电镜和普通光学显微镜下观察病斑形成过程.接种后3天,肉眼可见褪绿斑时,病斑部分的表皮细胞和薄壁细胞组织已开始膨大,病斑部分稍有隆起.第6天,肉眼能见疱斑时,表皮细胞和薄壁细胞膨大明显,少数细胞开始破裂.第9天病斑开始变褐,电镜下可见疱斑完全破裂,表皮细胞和薄壁细胞膨大数倍于正常细胞,且细胞破裂,大量细菌溢出。同时可以看到大豆斑疹病细菌在发病初期是在细胞间隙中存活和繁殖的,在表皮细胞和薄壁细胞破裂后进入细胞内,最后完全破坏细胞.从电镜切片中也可以看到疱斑形成主要是由于细胞体积增大所致.抗病品种只有褪绿斑,渐变褐,肉眼看不见疱斑,但在电镜下可见得下表皮稍隆起,有少数细菌存在于细胞间隙,未见有细菌溢出现象。  相似文献   
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