全文获取类型
收费全文 | 323篇 |
免费 | 40篇 |
国内免费 | 108篇 |
专业分类
测绘学 | 2篇 |
大气科学 | 4篇 |
地球物理 | 23篇 |
地质学 | 44篇 |
海洋学 | 303篇 |
天文学 | 2篇 |
综合类 | 77篇 |
自然地理 | 16篇 |
出版年
2024年 | 1篇 |
2023年 | 5篇 |
2022年 | 20篇 |
2021年 | 10篇 |
2020年 | 15篇 |
2019年 | 4篇 |
2018年 | 7篇 |
2017年 | 14篇 |
2016年 | 14篇 |
2015年 | 17篇 |
2014年 | 29篇 |
2013年 | 40篇 |
2012年 | 28篇 |
2011年 | 20篇 |
2010年 | 14篇 |
2009年 | 21篇 |
2008年 | 29篇 |
2007年 | 16篇 |
2006年 | 22篇 |
2005年 | 24篇 |
2004年 | 22篇 |
2003年 | 15篇 |
2002年 | 12篇 |
2001年 | 8篇 |
2000年 | 7篇 |
1999年 | 6篇 |
1998年 | 10篇 |
1997年 | 18篇 |
1996年 | 3篇 |
1995年 | 6篇 |
1994年 | 3篇 |
1993年 | 2篇 |
1992年 | 2篇 |
1991年 | 1篇 |
1990年 | 2篇 |
1989年 | 2篇 |
1988年 | 1篇 |
1986年 | 1篇 |
排序方式: 共有471条查询结果,搜索用时 203 毫秒
111.
Simrad EM12 backscatter strength data of the Southwest Indian Ridge (SWIR), between 57°E and 70°E, are used to reveal the along-axis segmentation of this super slow-spreading ridge. The backscatter properties of different geologic domains, like bathymetric highs and oblique basins within the rift valley, are characterized using 66 small test sites. We show that backscatter strength is higher on bathymetric swells, corresponding to segment centres, and lower in deep oblique basins corresponding to axial non-transform discontinuities and fracture zones. This contrast between segment centres and discontinuities is produced by both a thicker sediment cover and less frequent volcanic eruptions at segment ends. Using the model of Mitchell (1993), sediments have been estimated to be 2 to 5 m thicker in these areas than at segment centres. The distribution of the seamounts within the rift valley is controlling the long-wavelength variations of the mean backscatter strength calculated along the axis. Lower densities of seamounts and thicker sediments are producing lower and heterogeneous reflectivity levels in the deepest part of the axial valley floor between 61°45′E and 63°45′E. We propose that cooler mantle temperatures inducing construction of fewer volcanoes occur beneath this part of the ridge. The mean backscatter strength along the SWIR axis decreases dramatically toward the Rodrigues Triple Junction suggesting that volcanic production is reduced between 68°20′E and 69°20′E and that the transition from amagmatic tectonic deformation at the triple junction to new seafloor spreading occurs between 69°20′E and 70°E. 相似文献
112.
Sediment trapping and bypassing characteristics of a stable tidal inlet at Kaohsiung Harbor, Taiwan 总被引:2,自引:0,他引:2
Around the artificially stabilized tidal inlet that connects Kaohsiung Harbor to Taiwan Straight, 203 surficial samples of the sea floor were taken from the nearshore, in the outer harbor, and portions of the inner harbor. The bathymetry of the same area was also surveyed. The sand fraction in each sample was analyzed for the grain-size composition with a custom-built rapid sediment analyzer. A total of twenty-one size-classes were used in the analysis. Three hypothetical sediment sources were assumed to have influenced the spatial grain-size patterns in the study area: the northward and southward littoral drifts, and the sediments exported from the harbor. After reducing the influence of each hypothetical sediment source separately, the data were analyzed using empirical orthogonal (eigen) function (EOF) analysis. The results indicate that the northward long-term littoral drift is the dominant direction of sediment transport in the nearshore of the study area. A conceptual model for four different sediment trapping and bypassing patterns are proposed. (1) Excess bypass (or net outflux): this bypass pattern is characterized by the export of fine-grained sediments (mud and size classes in the very fine sand fraction) from the interior of the harbor. (2) Partial bypass (or partial trapping): this bypass pattern is represented by the size-classes in fine sand fraction. The amount of these grain sizes entering the outer harbor through the inlet is more than the amount exiting at the inlet mouth, resulting in the retention of a portion of these grain sizes. (3) Total bypass (or zero trapping): grain sizes that exhibit this bypass pattern do not come near the mouth of the inlet. These grain sizes include medium and coarse sand fractions. (4) Lag deposits: this group includes the size classes in the very coarse sand fraction, which are largely concentrated in the scour pit immediately seaward of the inlet mouth. In general, surficial sediment grain-size patterns represent a time-averaged response of the substrate to the transport processes over the time scale of at least two seasons. The differential associations of grain-size groups with various topographic features in the study area suggest morpho-textural relationships exist between the sea floor topography and grain size distribution patterns. 相似文献
113.
从鳕鱼碎肉中提取水解蛋白 总被引:15,自引:0,他引:15
用蛋白酶水解法从鳕鱼加工废弃物-鳕鱼碎肉中提取水解蛋白。鳕鱼碎肉经枯草杆菌AS1.398中性蛋白酶240IU/ml,pH7.0,50℃下水解2h;再经黄曲霉IFFI2342(蛋白酶活力2000IU/g)1.5%(w/v),50℃,pH6.0下水解6h以脱苦味。水解液经真空浓缩后喷雾干燥得水解蛋白粉。该制品易溶于水,无苦味,有海鲜味。其氨基酸组成合理,是优良的蛋白质制品。 相似文献
114.
Abstract. Combined effects of temperature, salinity, and metal enrichment (Zn, Mn, Co) on the growth rate and chemical composition of Fucus vesiculosus L. were studied in culture. Factorial combinations of two temperatures and three salinities were used. The results indicated that the accumulation of Zn and Mn into algal tissue was enhanced by dilution of the media, whereas Co accumulation exhibited maxima at the medium salinity. Zn accumulation was enhanced by temperature, while the opposite was true for Mn and Co.
In the presence of metals the usual dilution-induced changes in growth activity and chemical composition of Fucus plants were altered, while responses to the temperature factor remained unchanged. In diluted media, growth activity and mannitol content decreased along with a simultaneous increase of protein content. In the presence of Zn and Mn the mannitol content exhibited peaks at the medium salinity; in the presence of Co the dilution-induced pattern remained unchanged. Salinity-induced changes in growth and protein content were altered in the presence of metals. Maxima in growth rates were found at the medium salinity. Growth was higher in extremely diluted media than in scawater, indicating an inversion of responses to the salinity factor. Both the growth rate and mannitol content were lowest under the influence of Zn. 相似文献
In the presence of metals the usual dilution-induced changes in growth activity and chemical composition of Fucus plants were altered, while responses to the temperature factor remained unchanged. In diluted media, growth activity and mannitol content decreased along with a simultaneous increase of protein content. In the presence of Zn and Mn the mannitol content exhibited peaks at the medium salinity; in the presence of Co the dilution-induced pattern remained unchanged. Salinity-induced changes in growth and protein content were altered in the presence of metals. Maxima in growth rates were found at the medium salinity. Growth was higher in extremely diluted media than in scawater, indicating an inversion of responses to the salinity factor. Both the growth rate and mannitol content were lowest under the influence of Zn. 相似文献
115.
116.
117.
1 Introduction T he light-harvesting com plex (LH C ) com posedofphotosynthesis pigm ents and associated proteins arelocated on the thylakoid m em brane of chloroplast inhigherplants and algae. T he capture oflightenergy isthe first step in photosynthesis and is largely accom -plished by the pigm entprotein com plexes. To m axi-m ize the capture of light energy under various envi-ronm entalconditions, the LH C s w ith differentchro-m ophore com positions have evolved in differentpho-tosynth… 相似文献
118.
为更好地了解海带病烂的发生机制,针对褐藻酸降解菌埃氏交替单胞菌(Altermonas espejiana)菌株A1的生长及产酶条件进行了初步研究,并用不同浓度的菌液对健康海带进行了感染试验,测定了其体内可溶性蛋白质和可溶性糖含量的变化。结果表明,该菌株生长和产酶的最适条件为:20℃,0.5%~0.6%褐藻酸钠,pH=7,5,氮源为(NH4)2S04,培养时间72h。此外,感染菌株A1后,海带体内可溶性蛋白质和可溶性糖的含量均增加,且随着感染菌液浓度的升高,海带体内可溶性蛋白质含量升高,而可溶性糖含量先升高后降低。 相似文献
119.
120.