全文获取类型
收费全文 | 25803篇 |
免费 | 419篇 |
国内免费 | 1432篇 |
专业分类
测绘学 | 1527篇 |
大气科学 | 2157篇 |
地球物理 | 4823篇 |
地质学 | 12398篇 |
海洋学 | 1369篇 |
天文学 | 1672篇 |
综合类 | 2276篇 |
自然地理 | 1432篇 |
出版年
2024年 | 16篇 |
2023年 | 51篇 |
2022年 | 89篇 |
2021年 | 91篇 |
2020年 | 84篇 |
2019年 | 92篇 |
2018年 | 4859篇 |
2017年 | 4121篇 |
2016年 | 2655篇 |
2015年 | 331篇 |
2014年 | 176篇 |
2013年 | 112篇 |
2012年 | 1098篇 |
2011年 | 2814篇 |
2010年 | 2105篇 |
2009年 | 2397篇 |
2008年 | 1970篇 |
2007年 | 2429篇 |
2006年 | 119篇 |
2005年 | 254篇 |
2004年 | 463篇 |
2003年 | 471篇 |
2002年 | 307篇 |
2001年 | 96篇 |
2000年 | 106篇 |
1999年 | 62篇 |
1998年 | 66篇 |
1997年 | 36篇 |
1996年 | 26篇 |
1995年 | 29篇 |
1994年 | 24篇 |
1993年 | 14篇 |
1992年 | 7篇 |
1991年 | 2篇 |
1990年 | 5篇 |
1989年 | 3篇 |
1988年 | 4篇 |
1987年 | 7篇 |
1986年 | 1篇 |
1985年 | 2篇 |
1984年 | 3篇 |
1983年 | 1篇 |
1982年 | 2篇 |
1981年 | 24篇 |
1980年 | 20篇 |
1977年 | 2篇 |
1976年 | 7篇 |
1958年 | 1篇 |
排序方式: 共有10000条查询结果,搜索用时 15 毫秒
951.
Sachiko Oguma Tsuneo Ono Akira Kusaka Hiromi Kasai Yasuhiro Kawasaki Tomonori Azumaya 《Journal of Oceanography》2008,64(4):525-539
In this study we used two stable isotopes, δ13C and δ18O, for water mass classification in the coastal region off eastern Hokkaido. δ13C* values, which were corrected for the biological effect, and δ
18O values up to 300 m depth suggested that the isotopic character of the onshore and offshore water in the southern Okhotsk
Sea, the Nemuro Strait and the western North Pacific could be explained by the mixing of three source waters: the Oyashio
water (OYW), Soya Warm Current water (SWCW) and East Sakhalin Current water (ESCW). In summer, δ
13C*-δ
18O plots indicated mixing between SWCW from the southern Okhotsk Sea and OYW in the Pacific coast of southeastern Hokkaido,
while temperature-salinity plots of the onshore water showed minimal difference from the offshore OYW. In winter, on the other
hand, the mixed water of ESCW and OYW (or SWCW) appeared in the Pacific coastal region, distributed as cold, low salinity
onshore water. Finally, we estimated mixing ratios of OYW, SWCW and ESCW in the coastal region of western North Pacific using
their mean values of δ
13C* and δ
18O as endmembers. These results suggest seasonal and yearly changes of water mass combination en route from the southern Okhotsk
Sea to the western North Pacific. 相似文献
952.
Takafumi Hirata 《Journal of Oceanography》2008,64(4):561-566
An irradiance inversion model to estimate the in situ absorption coefficient of seawater has been developed for the Ultraviolet-A (UVA) wavelength domain. Input parameters are
sun angle and the up-and downward planar irradiances measured for at least two depths. The present method does not require
seawater to be sampled, and is a discrete wavelength method which returns the absorption coefficient at a given wavelength
from the irradiances measured at that wavelength without assuming a spectral shape of any optical properties a priori. Comparison between the model results and spectrophotometric measurements shows that the model is practically useful when
cloud cover in the atmosphere is ≤ 50%. According to the present method, measurements of the irradiances enable simultaneous
observation of the in situ underwater UVA radiation level and the absorption capacity of bulk seawater using a radiometer. 相似文献
953.
Michiel A. F. Knaapen 《Geo-Marine Letters》2009,29(1):17-24
Sandbanks, the largest of bed patterns in shallow sandy seas, pose a potential risk to shipping. They are also valuable elements
of natural coastal protection, dissipating the energy of waves. In the Southern Bight of the North Sea, several sandbank areas
have been reported in the literature. However, based on an objective crest–trough analysis of the bathymetry of the Dutch
continental shelf, the present study shows that sandbanks are more widespread than commonly considered. These banks are relatively
low, presumably explaining why they have not been documented before. This widespread occurrence of sandbanks in the North
Sea is in agreement with theoretical predictions based on stability analysis techniques. The possible interference between
large-scale human activity and low-amplitude open-shelf ridges implies that one should be careful not to overlook these patterns
if none should appear in a preliminary (visual) assessment. The only part of the Southern Bight in which no ridges can be
seen is a circular area with a diameter of about 50 km near the mouth of the river Rhine. Here, freshwater outflow affects
the direction of tidal ellipses and residual flow, and suppresses the formation of open ridges. 相似文献
954.
Christian J. Noll Timothy M. Dellapenna Andrea Gilkinson Randall W. Davis 《Geo-Marine Letters》2009,29(1):1-16
Surficial sediment distribution within Simpson Bay is a function of antecedent bedrock and recently deposited glacial geology,
as well as active physical processes both within Simpson Bay and Prince William Sound (PWS). Simpson Bay is a turbid, outwash
fjord located in northeastern PWS, Alaska. Freshwater from heavy precipitation, and the melting of high alpine glaciers enter
the bay through bay head rivers and small shoreline creeks. The catchment has a high watershed/basin surface area ratio (∼8:1),
and easily erodible bedrock that contribute to high sediment loads. The system can be divided into three discrete basins,
each with specific morphologic and circulatory characters. Side scan sonar, swath bathymetry, and seismic profiles reveal
that bathymetric highs are areas of outcropping glacial surfaces. High backscatter coupled with surface grab samples reveal
these surfaces to be composed of coarse sediment and bedrock outcrops. Bathymetric lows are areas of low backscatter, and
grab samples reveal these areas to be ponded deposits of organic-rich estuarine muds. The data provide evidence of terminal
morainal bank systems, and glacial grounding line deposits at the mouth of the bay and rocky outcrops were identified as subsurface
extensions of aerial rocky promontories. Radioisotope analyses of short cores reveal that the bay has an average accumulation
rate of approx. 0.5 cm year−1, but that this varies in function of the watershed/basin surface area ratios of the different basins. The interaction of
tidal currents and sediment source drives sediment distribution in Simpson Bay. Hydrographic data reveal high spatial variability
in surface and bottom currents throughout the bay. Subsurface currents are tide dominated, but generally weak (5–20 cm s−1), while faster currents are found along shorelines, outcrops, and bathymetric highs. Bathymetric data reveal steep slopes
with little to no modern sediment throughout the bay, suggesting lack of deposition due to tidal currents. 相似文献
955.
956.
Pockmarks in the inner Oslofjord,Norway 总被引:5,自引:3,他引:2
Multibeam bathymetric surveys of the Inner Oslofjord, Norway have revealed a high density of pockmarks in the 179-km2 inner fjord area, which contains over 500 pockmarks of varying size, typically 20–50 m in diameter and 2–10 m deep. These
pockmarks have been investigated with a variety of techniques, including acoustic subbottom profiling, sedimentological and
geochemical analyses of cores, remotely operated vehicle observation, and morphometry. Both the distribution and shapes of
the pockmarks suggest that they are related to structures in the bedrock underlying relatively thin (<50 m) unconsolidated
glacial and postglacial sediments. The data provide no direct indication of a particular mode of pockmark formation, but release
of large amounts of biogenic, shallow methane seems unlikely. Several lines of evidence point to a continuous process of pockmark
formation followed by inactivity, with some pockmarks recently active whereas others have been inactive for a considerable
time. Some pockmarks are characterised by coarse sediment in their centres. The density, variety and easy access make this
pockmark field an ideal model area for pockmark research.
John S. Gray is deceased. 相似文献
957.
Organized bacterial assemblies in manganese nodules: evidence for a role of S-layers in metal deposition 总被引:1,自引:0,他引:1
Xiaohong Wang Heinz C. Schröder Ute Schloßmacher Werner E. G. Müller 《Geo-Marine Letters》2009,29(2):85-91
Polymetallic/ferro-manganese nodules (Mn-nodules) reach sizes of up to 10 cm in diameter and are abundantly found on the seabed.
To date, the origin of Mn-nodules remains unclear, and both abiogenic and biogenic origins have been proposed. In search of
evidence for a contribution of microbial processes to the formation of Mn-nodules, we analyzed those spherical nodules which
contain a concentrically banded texture in their interior. The Mn-nodules were collected at a depth of 5,152 m from the Clarion-Clipperton
Zone. Our high-resolution scanning electron microscopy analyses reveal first published evidence that endolithic microorganisms
exist and are arranged in a highly organized manner on plane mineral surfaces within the nodules. These microorganisms are
adorned on their surfaces with S-layers, which are indicative for bacteria. Moreover, the data suggest that these S-layers
are the crystallization seeds for the mineralization process. We conclude that the mineral material of the Mn-nodule has a
biogenic origin, and hope that these data will contribute to the development of biotechnological approaches to concentrate
metals from seawater using bacteria in bioreactors. 相似文献
958.
James Flocks Michael D. Miner David C. Twichell Dawn L. Lavoie Jack Kindinger 《Geo-Marine Letters》2009,29(6):359-378
The barrier-island systems of the Mississippi River Delta plain are currently undergoing some of the highest rates of shoreline
retreat in North America (~20 m/year). Effective management of this coastal area requires an understanding of the processes
involved in shoreline erosion and measures that can be enacted to reduce loss. The dominant stratigraphy of the delta plain
is fluvial mud (silts and clays), delivered in suspension via a series of shallow-water delta lobes that prograded across
the shelf throughout the Holocene. Abandonment of a delta lobe through avulsion leads to rapid land subsidence through compaction
within the muddy framework. As the deltaic headland subsides below sea level, the marine environment transgresses the bays
and wetlands, reworking the available sands into transgressive barrier shorelines. This natural process is further complicated
by numerous factors: (1) global sea-level rise; (2) reduced sediment load within the Mississippi River; (3) diversion of the
sediment load away from the barrier shorelines to the deep shelf; (4) storm-induced erosion; and (5) human alteration of the
littoral process through the construction of hardened shorelines, canals, and other activities. This suite of factors has
led to the deterioration of the barrier-island systems that protect interior wetlands and human infrastructure from normal
wave activity and periodic storm impact. Interior wetland loss results in an increased tidal prism and inlet cross-sectional
areas, and expanding ebb-tidal deltas, which removes sand from the littoral processes through diversion and sequestration.
Shoreface erosion of the deltaic headlands does not provide sufficient sand to balance the loss, resulting in thinning and
dislocation of the islands. Abatement measures include replenishing lost sediment with similar material, excavated from discrete
sandy deposits within the muddy delta plain. These sand bodies were deposited by the same cyclical processes that formed the
barrier islands, and understanding these processes is necessary to characterize their location, extent, and resource potential.
In this paper we demonstrate the dominant fluvial and marine-transgressive depositional processes that occur on the inner
shelf, and identify the preservation and resource potential of fluvio-deltaic deposits for coastal management in Louisiana. 相似文献
959.
Rare earth elements (REEs) of 91 fine-grained bottom sediment samples from five major rivers in Korea (the Han, Keum, and
Yeongsan) and China (the Changjiang and Huanghe) were studied to investigate their potential as source indicator for Yellow
Sea shelf sediments, this being the first synthetic report on REE trends for bottom sediments of these rivers. The results
show distinct differences in REE contents and their upper continental crust (UCC)-normalized patterns: compared to heavy rare
earth elements (HREEs), light rare earth elements (LREEs) are highly enriched in Korean river sediments, in contrast to Chinese
river sediments that have a characteristic positive Eu anomaly. This phenomenon is observed also in primary source rocks within
the river catchments. This suggests that source rock composition is the primary control on the REE signatures of these river
sediments, due largely to variations in the levels of chlorite and monazite, which are more abundant in Korean bottom river
sediments. Systematic variations in ΣLREE/ΣHREE ratios, and in (La/Yb)–(Gd/Yb)UCC but also (La/Lu)–(La/Y)UCC and (La/Y)–(Gd/Lu)UCC relations have the greatest discriminatory power. These findings are consistent with, but considerably expand on the limited
datasets available to date for suspended sediments. Evidently, the REE fingerprints of these river sediments can serve as
a useful diagnostic tool for tracing the provenance of sediments in the Yellow Sea, and for reconstructing their dispersal
patterns and the circulation system of the modern shelf, as well as the paleoenvironmental record of this and adjoining marginal
seas. 相似文献
960.
Vinu Valsala 《Journal of Oceanography》2009,65(6):803-816
The spreading pathways of the Somali and Arabian coastal upwelled waters in the northern Indian Ocean are identified from
an ocean re-analysis data set of a single year using numerical passive tracers in a transport model. The Somali and Arabian
coastal upwelled waters are found to have entirely different spreading pathways in the northern Indian ocean. The former circulates
anticyclonically, is mixed vertically, and is advected to the eastern Indian Ocean along the north equatorial region; while
the later intrudes into the northern Arabian Sea, circulates anticyclonically and is advected to the south in the central
Arabian Sea and then to the eastern Indian Ocean. The seasonal surface mixing by strong monsoon winds and sheared currents
due to dominant eddies of the Somali region are found responsible for mixing 25% of Somali upwelled water with the subsurface
and affecting the resultant pathways. The effect of mixing is, however, found negligible in the case of Arabian coastal upwelled
water pathways. The seasonal reversal of circulation and eddy dominance during the southwest monsoon cause the Somali upwelled
water to spread over the northern Indian Ocean faster than the simultaneously upwelled Arabian coastal water. 相似文献