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211.
This work reports the results of one year's sampling of aquatic macroinver-brates in various streams with different salinity gradients. The study area was the headwaters of the rivers Guadaíra and Guadalete, located in the same geographical area in south-western Spain. The most interesting feature of the Guadaíra basin is the natural salinity of its waters due to the abundance of gypsum in its headwaters. Lithologically, the headwaters of the Guadalete basin flow over marls, clay, sandstone and limestone. Salinity values in most streams do not reach 1 mS cm–1. At least at the levels of salinity found in the Guadaíra basin headwaters, the existence of a well-structured community of macroinvertebrates can be claimed. Of the groups studied, Diptera and Coleoptera showed the highest species richness, being distributed preferentially at the ends of the conductivity spectrum. Groups including taxa inhabiting waters of low salinty and taxa inhabiting waters with high salinity could be reliable indicators of salinity. 相似文献
212.
R. Zander G. Roland L. Delbouille A. Sauval C. B. Farmer R. H. Norton 《Journal of Atmospheric Chemistry》1987,5(4):395-404
The integrated column amount of hydrogen chloride has been monitored above the International Scientific Station of the Jungfraujoch (Switzerland) during the last 8 years. The results deduced from solar absorption measurements near 3.42 m indicate a secular trend equivalent to (0.75±0.2) % increase per year since 1978, superimposed on a significant short-term variability which can be partly attributed to the tropospheric component of the total HCl burden. Based on an intensified set of measurements carried out over the last three years, a seasonal component in the total content of HCl has been established for the first time, showing a minimum occuring in early winter and a maximum during the spring. 相似文献
213.
214.
Daniel Markewitz Ricardo de O. Figueiredo Eric A. Davidson 《Journal of Geochemical Exploration》2006,88(1-3):214
The objective of this study was to investigate the role of dissolved CO2 (H2CO3*) as a mechanism of cation removal from surface soils under secondary land uses in the tropics. Soil leachate columns were prepared with 0–10 cm soils from mature and secondary forest, and managed pastures, and extracted with H2CO3* from deionized water equilibrated with 0%, 0.5%, 1%, and 10% CO2 (g). Extraction of soil cations slowed over time following an exponential form for the cumulative data. The rate of cation concentration decline varied as a function of CO2 concentration with the 10% solution resulting in a greater percent decline with extraction volume. Potassium removal from the exchange sites of all soils and for all solutions was nearly complete ranging from 85% to 97% while removals of Mg (31% to 71%) and Ca (12% to 42%) were lower. The asymptotic patterns of cation loss observed in this study suggest that H2CO3* acid-driven losses of cations may become self-limiting over time. Other stronger acids from atmospheric deposition or organic sources may serve to perpetuate cation removal, and re-forestation on these cleared lands would certainly re-distribute cations from soils to vegetation. 相似文献
215.
高岭土中全硫量快速测定方法 总被引:13,自引:1,他引:13
采用碳酸钠一氧化镁半熔融一氯化钡滴定法测定高岭土中的硫含量。试样用碱性熔荆半熔,熔块以水浸取,将转化为硫酸盐后的滤液,以玫瑰红酸钠为指示剂,在pH为5.5.7.0的条件下,用氯化钡标准溶液进行滴定。测定结果的RSD=2.47%(n=5),加标回收率为95.2%-100.3%。改进后的方法已用于高岭土中全硫量的测定,结果与国标重量法相符。 相似文献
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218.
Shelley D. Crausbay James M. Russell Douglas W. Schnurrenberger 《Journal of Paleolimnology》2006,35(3):641-659
Lithostratigraphic analyses of a sub-annually laminated core from Ranu Lamongan, a maar lake on the island of Java, document
considerable changes in the lake’s chemistry and water balance over the past ca. 800 calendar years. Composition of the dark
(clastics) and light (diatoms and/or calcium carbonate minerals) couplets suggests that these laminations form in response
to seasonal changes in rainfall and water-column overturn in the lake. Calcium carbonate is not continuous in the core, and
when it occurs it varies, sometimes abruptly, in carbonate phase and elemental composition (low Mg-calcite Mg-calcite, and
aragonite). A significant correlation between Mg/Ca changes and δ18O variations in authigenic calcium carbonate suggest the basin is highly sensitive to hydrologic variation. Lithologic data
suggest calcium carbonate precipitates and thus records hydrologic conditions during the dry season – a season in which rainfall
anomalies are highly correlated with the phase of ENSO. Our carbonate-based record of Mg/Ca shows variability in evaporative
concentration on a quasi-seasonal frequency for the past ca. 800 years. Our record shows two multi-decadal periods of drought
– ca. 1275–1325 and ca. 1450–1650 CE – the latter of which was especially strong and/or prolonged. Our record also shows a
possible change in drought frequency at around 1650 CE, in which periods of calcium carbonate precipitation and Mg/Ca change
shifted from multi-decadal to interannual variability. Given the strong correlations between modern-day drought in East Java
and ENSO variability, our drought record may indicate a regime shift in the behavior of the ENSO system about 350 years ago.
Finally, comparisons between our record and others suggest that variation in ENSO on centennial and sub-centennial scales
is not strongly associated with changes in the global mean climate state. 相似文献
219.
氯离子守恒法确定土壤生态蓄水量 总被引:1,自引:0,他引:1
通过实验测得降水及土壤水的氯离子浓度,依据化学守恒原理,即降水与包气带土壤水中氯离子的质量守恒关系,计算出长春市丘陵、台地、阶地3类不同地貌区土壤一年内所得水量,该水量为土壤生态蓄水量。将土壤生态蓄水量与土壤的田间持水量、作物的生态需水量进行对比分析,评述了三者之间的关系。阐明土壤生态蓄水量不仅能客观反映土壤中的水分含量情况,也能对植被生态需水量的满足情况给予客观评价。 相似文献
220.