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991.
Sara Sánchez-Moreno Sean Smukler Howard Ferris Anthony T. O’Geen Louise E. Jackson 《Biology and Fertility of Soils》2008,44(5):727-744
The aim of this paper was to assess biodiversity among different habitats of an organic farm and the relationships between
some soil properties, nematode taxonomic diversity, and soil food web condition. Eight habitats were studied in the farm:
ponds, ditches, a riparian corridor, hedgerows, and four agricultural fields (mustard, oats, fallow, and legumes). The undisturbed
riparian corridor had higher soil and concentrations, and potentially mineralizable N and higher abundances of bacterivore nematodes and longer food webs. Canonical
correlation analysis showed associations between habitats and nematode trophic groups: predatory and bacterial-feeding nematodes
in the riparian corridor and hedgerows, omnivore nematodes in the ponds and ditches, and fungal-feeding nematodes in the legume
field. Soil chemical and physical properties mirrored the aboveground farm patterns and were more similar among habitats that
were or had been cultivated, compared to the riparian corridor. Soil food web indices, based on functional analysis of nematode
faunal composition, reflected the aboveground landscape heterogeneity. Discriminant analysis indicated that soil food web
indices separated the two most disturbed habitats (ponds and tailwater ditches) from the two least disturbed habitats (the
riparian corridor and hedgerows). The indices correlated with soil functioning as inferred by soil properties. Abundance of
nematode taxa was not associated with aboveground landscape patterns. The complexity of the soil food web may have been influenced
by (1) environmental factors that differed between years, (2) different time periods since disturbance in the various habitats,
and (3) movement of nutrients and organisms by water flow between habitats in the farmscale. 相似文献
992.
Saman Bowatte Russell Tillman Andrew Carran Allan Gillingham David Scotter 《Biology and Fertility of Soils》2008,44(6):805-813
This paper explored the potential of application of in situ ion exchange resin membrane (IEM) technique for assessing soil
nitrogen (N) availability and spatial distribution in New Zealand grazed pastures. Field and incubation experiments conducted
to test the technique proved IEM technique to be a useful approach to monitoring the continuous changes in soil mineral N
in pasture soils. The field testing showed that the IEM technique reflects both differences in pool size and mineral N flux,
while 2-M KCl extraction reflects only pool size at the sampling. Testing the effects of residence time, temperature, soil
inorganic N content, and soil water content through diffusion modeling offers further support for using IEM to explore the
complex dynamics of nitrogen availability in pasture soils. 相似文献
993.
Experimental snowpack reduction alters organic matter and net N mineralization potential of soil macroaggregates in a northern hardwood forest 总被引:1,自引:0,他引:1
J. Megan Steinweg Melany C. Fisk Benjamin McAlexander Peter M. Groffman Janet P. Hardy 《Biology and Fertility of Soils》2008,45(1):1-10
Climate change is predicted to reduce or delay annual wintertime snow pack formation in the forests of the northeastern US.
Any delay in snowpack formation could increase soil freezing in winter and, thereby, alter soil characteristics and processes.
We examined the hypothesis that delayed snowpack would disrupt soil structure and change organic matter bioavailability in
an experimental snow removal study at the Hubbard Brook Experimental Forest (HBEF), NH, USA. Pairs of reference and snow removal
treatment plots were studied in four different sites at HBEF. Snow was removed from November–January of two winters, inducing
soil freezing throughout both winters. Size class distribution and organic matter concentration and content of aggregates,
and carbon and nitrogen mineralization potential of size fractions were quantified for surface mineral soils in the spring
of both years immediately after snowmelt. In the first year of sampling, the only significant effect of snow removal was an
increase in the smallest (<53 μm) size fraction of mineral soil. In the second year, snow removal increased organic matter
concentrations of macroaggregate (250–2,000 μm) and microaggregate (53–250 μm) size fractions. This change corresponded to
an increase in net N mineralization potential and the ratio of N to C mineralized in the macroaggregate fraction, but there
were no effects of snow removal on C mineralization. We propose that soil freezing increases the movement of organic matter
from organic to mineral soil horizons and increases the N content of mineralizable substrates in mineral soil following years
with delayed snowpack formation. 相似文献
994.
Sarah J. Kemmitt David Wright Daniel V. Murphy David L. Jones 《Biology and Fertility of Soils》2008,44(7):933-941
Dissolved organic nitrogen (DON) and in particular free amino acids represent a key pool in the terrestrial soil C and N cycle.
The factors controlling the rate of turnover of this pool in soil, however, remain poorly understood. We investigated the
factors regulating the rate of amino acid turnover at different depths (up to 1.2 m) in five low-input, acid soil profiles.
Within the root zone (0–60 cm), amino acids constituted 8% of the DON and represented only a small fraction of plant available
N. In all the soil profiles, the rate of amino acid mineralisation decreased progressively with depth. The average half-life
of the exogenously added amino acids in the soil was 5.8 h in topsoils (0–10 cm), falling to 20 h at a depth of 50 cm and
to 33 h at 100 cm. Generally, the rate of amino acid mineralisation correlated positively with total soil C and N, soil microbial
activity (basal soil respiration rate) and soil content. The relatively rapid rates of microbial amino acid assimilation in subsoils below the root zone (>60 cm) indicate
that long-term transport of amino acids (e.g. from soil to freshwaters) will be low. Based upon the C-to-N ratio of the amino
acid substrate and the microbial C assimilation efficiency, we estimate that approximately 40–60% of the amino acid-N will
be excreted as . In conclusion, the rapid rate of free amino acid turnover and their low concentration in soil solution indicate that the
formation of inorganic N ( and ) in soil is limited primarily by the rate of free amino acid appearance in soil and not by the rate of amino acid mineralisation. 相似文献
995.
Moses F. A. Maliro David McNeil Bob Redden James F. Kollmorgen Chris Pittock 《Genetic Resources and Crop Evolution》2008,55(1):53-63
Six hundred accessions of chickpea (Cicer arietinum L.) landraces and its wild relatives from 28 different countries, available at Australian Temperate and Field Crops Collection
(ATFCC) were screened for tolerance to salt under greenhouse conditions using three sampling strategies; (1) random sampling
of 200 accessions from different countries, (2) restricted random sampling of 200 accessions from geographical regions with
salinity problems and high diversity (Middle East and West & South Asia) and (3) as for strategy 1 but with a reduced representation
of accessions from the geographical regions used in strategy 2. Degree of salt tolerance was based on necrosis scores and
shoot biomass reduction relative to unstressed controls at harvest after subjecting stressed plants to salt treatment from
21 to 42 days after sowing. There was a wide variation in salinity tolerance determined by both measures. For sampling strategies
1, 2 and 3 respectively; 24, 28 and 14% of accessions were salt tolerant. Accessions from the middle east and south Asian
(regions with salinity problem, a long history of chickpea cultivation and high diversity) gave a higher probability (P < 0.01) of getting salt tolerant accessions. 相似文献
996.
997.
Evaluation of genetic diversity of bread wheat landraces from Pakistan by AFLP and implications for a future collection strategy 总被引:1,自引:0,他引:1
Ryoko Hirano Akira Kikuchi Makoto Kawase Kazuo N. Watanabe 《Genetic Resources and Crop Evolution》2008,55(7):1007-1015
We used amplified-fragment-length polymorphism (AFLP) markers to evaluate genetic variation in a set of bread wheat (Triticum aestivum L.) landraces and improved materials. Landraces collected from different geographic and agro-ecological zones in Pakistan
in 1987, 1989 and 1991 were separated into two groups based on their geographic origins: northern (Himalaya) and south-western
(Balochistan) Pakistan. Six AFLP primer combinations detected 453 AFLP markers in the 43 landrace accessions and four high-yield
varieties (HYVs). Of these, 225 (49.67%) were rare (shared with < 5% of all accessions). Among these rare alleles, 23 (10.22%)
were common in the Himalaya (shared with > 10% of accessions collected there) but were not found in Balochistan. We conclude
that there is a higher probability of collecting rare alleles at overall, but which are in contrast locally common ones in
the Himalayan region. Gene diversity was 0.17 in the Himalayan group and 0.15 in the Balochistan group. Considerable genetic
variability was found in both groups. Accessions from different agro-ecological zones were indistinguishable by cluster analysis,
indicating intensive seed trading within the country. Cluster analysis indicated that the landraces and the HYVs are genetically
distinct; suggesting that genetic erosion of wheat landraces has been unlikely taken in place. This study provides an example
of how analysis of existing materials and data, can serve as a basis for future collection planning and conservation policies. 相似文献
998.
R. Ortiz José Crossa Jorge Franco Ricardo Sevilla Juan Burgueño 《Genetic Resources and Crop Evolution》2008,55(1):151-162
The maize of Latin America, with its enormous diversity, has played an important role in the development of modern maize cultivars of the American continent. Peruvian highland maize shows a high degree of variation stemming from its history of cultivation by Andean farmers. Multivariate statistical methods for classifying accessions have become powerful tools for classifying genetic resources conservation and the formation of core subsets. This study has two objectives: (1) to use a numerical classification strategy for classifying eight Peruvian highland races of maize based on six vegetative traits evaluated in two years and (2) to compare this classification with the existing racial classification. The numerical classification maintained the main structure of the eight races, but reclassified parts of the races into new groups (Gi). The new groups are more separated and well defined with a decreasing accession within group × environment interaction. Most of the accessions from G1 are from Cusco Gigante, all of the accessions from G3 (except one) are from Confite Morocho, and all of the accessions from G7 are from Chullpi. Group G2 has four accessions from Huayleño and four accessions from Paro, whereas G4 has four accessions from Huayleño and five accessions from San Geronimo. Group G5 has accessions from four races, and G6 and G8 formed small groups with two and one accession each, respectively. These groups can be used for forming core subsets for the purpose of germplasm enhancement and assembling gene pools for further breeding. 相似文献
999.
For the selection of donors with valuable characteristics for breeding, 39 thyme accessions were evaluated in three years
according to a staggered schedule. The criteria investigated were: winter hardiness, beginning of flowering, growth height,
yield of the dry herb, content of essential oil, composition of the essential oil, DNA content of cell nuclei and number of
chromosomes. The most strongly varying traits between the populations were the yield of dry herb, the content of essential
oil and the content of volatile phenols with coefficients of variation (CV) between CV 40% and 50%. The largest variation
within a population was detected for the yield of dry herb (CV 25–46%) and the content of essential oil (CV 17–48%). The homogeneity
of the populations was different. The minimal average coefficient of variation of all traits (CV 19%) was determined in the
population of the cultivar ‘Varico II’ and in a population from Lithuania. The ploidy level of T. vulgaris was diploid (2n = 30). 相似文献
1000.
Ashutosh Mukherjee Satyesh Chandra Roy S. De Bera Hong-En Jiang Xiao Li Cheng-Sen Li Subir Bera 《Genetic Resources and Crop Evolution》2008,55(4):481-485
Hemp (Cannabis sativa L.) cultivation and utilization is an ancient practice to human civilization. There are some controversies on the origin
and subsequent spread of this species. Ancient plant DNA has proven to be a powerful tool to solve phylogenetic problems.
In this study, ancient DNA was extracted from an archaeological specimen of Cannabis sativa associated with archaeological human remains from China. Ribosomal and Cannabis specific chloroplast DNA regions were PCR amplified. Sequencing of a species-specific region and subsequent comparison with
published sequences were performed. Successful amplification, sequencing and sequence comparison with published data suggested
the presence of hemp specific DNA in the archeological specimen. The role of Humulus japonicus Sieb. et Zucc. in the evolution of Cannabis is also indicated. The identification of ancient DNA of 2500 years old C. sativa sample showed that C. sativa races might have been introduced into China from the European–Siberian center of diversity. 相似文献