全文获取类型
收费全文 | 110篇 |
免费 | 2篇 |
专业分类
测绘学 | 7篇 |
大气科学 | 22篇 |
地球物理 | 34篇 |
地质学 | 24篇 |
海洋学 | 13篇 |
天文学 | 5篇 |
自然地理 | 7篇 |
出版年
2023年 | 1篇 |
2020年 | 3篇 |
2019年 | 1篇 |
2018年 | 1篇 |
2016年 | 2篇 |
2015年 | 5篇 |
2014年 | 6篇 |
2013年 | 5篇 |
2012年 | 6篇 |
2011年 | 11篇 |
2010年 | 4篇 |
2009年 | 7篇 |
2008年 | 6篇 |
2007年 | 7篇 |
2006年 | 7篇 |
2005年 | 1篇 |
2004年 | 7篇 |
2003年 | 4篇 |
2002年 | 5篇 |
2000年 | 2篇 |
1999年 | 2篇 |
1989年 | 1篇 |
1986年 | 2篇 |
1985年 | 1篇 |
1982年 | 1篇 |
1980年 | 1篇 |
1977年 | 1篇 |
1976年 | 1篇 |
1975年 | 2篇 |
1972年 | 2篇 |
1962年 | 1篇 |
1961年 | 2篇 |
1960年 | 2篇 |
1959年 | 1篇 |
1956年 | 1篇 |
排序方式: 共有112条查询结果,搜索用时 15 毫秒
71.
Arno Rein Steffen Popp Steffen Zacharias Carsten Leven Martin Bittens Peter Dietrich 《Environmental Earth Sciences》2011,63(6):1239-1249
The present work focuses on approaches for the characterization of subsurface contamination, which need to be reliable and
cost-effective, particularly for extended and remote areas aimed at being redeveloped. Requirements are discussed with respect
to specific conditions at megasites, in order to enable site valorization. In a case study, two approaches are compared, comprising
(1) conventional site investigation based on historical surveys and concentration measurements at monitoring wells installed
in areas suspected of being polluted and (2) the use of direct push (DP) methods covering the complete area. The DP investigation
provided information on the contamination distribution and yielded also important information on hydraulic conditions. Statistical
analysis of the results applying indicator kriging revealed that the conventional approach is markedly risky when decision-making
relies solely on historical and sparse data. The DP campaign remarkably reduced the uncertainty concerning the estimated occurrence
of polluted groundwater at the whole site. Furthermore, monitoring measurements are analyzed showing the possible importance
of temporal variability. Taking economical consideration into account, DP-based groundwater screening is recommended to obtain
either first or complementary information on the entire site. Based on these data, also locations for a long-term monitoring
could be selected if temporal variability is assumed relevant. 相似文献
72.
Acoustic seabed classification is a useful tool for monitoring marine benthic habitats over broad-scales (>1 km2) and meso-scales (10 m2–1 km2). Its utility in this context was evaluated using two approaches: by describing natural changes in the temporal distribution of marine biotopes across the broad-scale (4 km2), and by attempting to detect specific experimentally-induced changes to kelp-dominated biotopes across the meso-scale (100 m2). For the first approach, acoustic backscatter mosaics were constructed using sidescan sonar and multibeam echosounder data collected from Church Bay (Rathlin Island, Northern Ireland) in 1999, 2008 and 2009. The mosaics were manually segmented into acoustic facies, which were ground-truthed using a drop-video camera. Biotopes were classified from the video by multivariate exploratory analysis and cross-tabulated with the acoustic facies, showing a positive correlation. These results were integrated with bathymetric data to map the distribution of seven unique biotopes in Church Bay. Kappa analysis showed the biotope distribution was highly similar between the biotope maps, possibly due to the stability of bedforms shaped by the tidal regime around Rathlin Island. The greatest biotope change in this approach was represented by seasonal and annual changes in the growth of the seagrass, Zostera marina. In the second approach, sidescan sonar data were collected before and after the removal of 100 m2 of kelp from three sites. Comparison of the data revealed no differences between the high-resolution backscatter imagery. It is concluded that acoustic seabed classification can be used to monitor change over broad- and meso-scales but not necessarily for all biotopes; its success depends on the type of acoustic system employed and the biological characteristics of the target biotope. 相似文献
73.
Robert Marchant Hermann Behling Juan‐Carlos Berrio Antoine Cleef Joost Duivenvoorden Henry Hooghiemstra Peter Kuhry Bert Melief Elisabeth Schreve‐Brinkman Bas Van Geel Thomas Van der Hammen Guido Van Reenen Michael Wille 《第四纪科学杂志》2002,17(2):113-129
Colombian biomes are reconstructed at 45 sites from the modern period extending to the Last Glacial Maximum (LGM). The basis for our reconstruction is pollen data assigned to plant functional types and biomes at six 3000‐yr intervals. A reconstruction of modern biomes is used to check the treatment of the modern pollen data set against a map of potential vegetation. This allows the biomes reconstructed at past periods to be assessed relative to the modern situation. This process also provides a check on the a priori assignment of pollen taxa to plant functional types and biomes. For the majority of the sites, the pollen data accurately reflect the potential vegetation, even though much of the original vegetation has been transformed by agricultural practices. At 18 000 14C yr BP, a generally cool and dry environment is reflected in biome, assignments of cold mixed forests, cool evergreen forests and cool grassland–shrub; the latter extending to lower altitudes than presently recorded. This signal is strongly recorded at 15 000 and 12 000 14C yr BP, the vegetation at these times also reflecting a relatively cool and dry environment. At 9000 14C yr BP there is a shift to biomes thought to result from slightly cooler environmental conditions. This trend is reversed by 6000 14C yr BP; most sites, within a range of different environmental settings, recording a shift to more xeric biome types. There is an expansion of steppe and cool mixed‐forest biomes, replacing tropical dry forest and cool grassland–shrub biomes, respectively. These changes in biome assignments from the modern situation can be interpreted as a biotic response to mid‐Holocene climatic aridity. At 3000 14C yr BP the shift is mainly to biomes characteristic of slightly more mesic environmental conditions. There are a number of sites that do not change biome assignment relative to the modern reconstruction, although the affinities that these sites have to a specific biome do change. These ‘anomalies’ are interpreted on a site‐by‐site basis. Spatially constant, but differential response of the vegetation to climatic shifts are related to changes in moisture sources and the importance of edaphic controls on the vegetation. The Late Quaternary reconstruction of large‐scale vegetation dynamics in Colombia allows an understanding of the environmental controls on these to be developed. In particular, shifts in the character of the main climatic systems that influence Colombian vegetation are described. Copyright © 2002 John Wiley & Sons, Ltd. 相似文献
74.
Rowin J. van Lanen Menne C. Kosian Bert J. Groenewoudt Esther Jansma 《Geoarchaeology》2015,30(3):200-222
This study focuses on reconstructing landscape prerequisites for Roman and early‐medieval routes in the Netherlands. We applied spatial modeling to modern and paleogeographical landscape data in order to determine geographical obstacles for possible translocation in ca. A.D. 100 and 800 via land and water. Network‐friction values were calculated to produce a spatial model of possible movement corridors and to enable the integration of archaeological data. Results show that in geographically dynamic lowland regions such as the current Netherlands, landscape units such as water, peat, and levees must have had a high impact on route orientation. The lower parts of the western Netherlands were almost inaccessible by land, implying that its inhabitants largely must have depended on rivers and streams for transportation. In Dutch coastal and river areas, the landscape changed drastically between A.D. 100 and 800, the largest changes occurring along the coast. 相似文献
75.
76.
Göran Björk Leif G. Anderson Martin Jakobsson Dennis Antony Björn Eriksson Patrick B. Eriksson Benjamin Hell Sofia Hjalmarsson Timothy Janzen Sara Jutterström Johanna Linders Ludvig Löwemark Christian Marcussen K. Anders Olsson Bert Rudels Emma Sellén Morten Sølvsten 《Deep Sea Research Part I: Oceanographic Research Papers》2010,57(4):577-586
The LOMROG 2007 expedition targeted the previously unexplored southern part of the Lomonosov Ridge north of Greenland together with a section from the Morris Jesup Rise to Gakkel Ridge. The oceanographic data show that Canadian Basin Deep Water (CBDW) passes the Lomonosov Ridge in the area of the Intra Basin close to the North Pole and then continues along the ridge towards Greenland and further along its northernmost continental slope. The CBDW is clearly evident as a salinity maximum and oxygen minimum at a depth of about 2000 m. The cross-slope sections at the Amundsen Basin side of the Lomonosov Ridge and further south at the Morris Jesup Rise show a sharp frontal structure higher up in the water column between Makarov Basin water and Amundsen Basin water. The frontal structure continues upward into the Atlantic Water up to a depth of about 300 m. The observed water mass division at levels well above the ridge crest indicates a strong topographic steering of the flow and that different water masses tend to pass the ridge guided by ridge-crossing isobaths at local topographic heights and depressions. A rough scaling analysis shows that the extremely steep and sharply turning bathymetry of the Morris Jesup Rise may force the boundary current to separate and generate deep eddies. 相似文献
77.
78.
Subsurface sediments of tidal flats and the marine deep biosphere share several features. Although on different scales in
time and space, geochemical profiles and microbial successions follow the same trends. Microbial activities are governed by
the availability of electron acceptors and the quality of electron donors. Two deep-biosphere sites and a shallow site from
a German North Sea tidal flat were exemplarily chosen to compare geochemical settings and microbiological features. At all
sites, microbial abundance was elevated at sulfate–methane transition zones. The known discrepancy between cultivation-based
and molecular diversity assessments is observed, but similar microbial community compositions are found with each of the approaches
at deep and shallow sites. These findings lead to the conclusion that we are presently unable to draw a cutting line between
the shallow and the deep subsurface. Rather, there appears to exist only one “subsurface biosphere” with gradual differences.
Therefore, tidal flats serve as an excellent model to perform microbiological experiments and to test novel techniques before
applying them to much deeper and older samples.
Responsible editor: Meinhard Simon 相似文献
79.
Valle Raidla Kalle Kirsimäe Rein Vaikmäe Argo Jõeleht Enn Karro Andres Marandi Lehte Savitskaja 《Chemical Geology》2009,258(3-4):219-231
The shallowly buried marginal part of the Cambrian–Vendian confined aquifer system of the Baltic Basin is characterised by fresh and low δ18O composition water, whereas the deeply settled parts of the aquifer are characterized by typical Na–Ca–Cl basinal brines. Spatial variation in water geochemistry and stable isotope composition suggests mixing origin of the diluted water of three end-members—glacial melt water of the Weichselian Ice Age (115 000–10 000 BP), Na–Ca–Cl composition basin brine and modern meteoric water. The mixing has occurred in two stages. First, the intrusion and mixing of isotopically depleted glacial waters with basinal brines occurred during the Pleistocene glacial periods when the subglacial melt-water with high hydraulic gradient penetrated into the aquifer. The second stage of mixing takes place nowadays by intrusion of meteoric waters. The freshened water at the northern margin of the basin has acquired a partial equilibrium with the weakly cemented rock matrix of the aquifer. 相似文献
80.
Yengkhom Kesorjit Singh Bert De Waele Subrata Karmakar Sunayana Sarkar Tapas Kumar Biswal 《Precambrian Research》2010
Granulites are developed in various tectonic settings and during different geological periods, and have been used for continental correlation within supercontinent models. In this context the Balaram-Kui-Surpagla-Kengora granulites of the South Delhi Terrane of the Aravalli Mobile Belt of northwestern India are significant. The granulites occur as shear zone bounded lensoidal bodies within low-grade rocks of the South Delhi Terrane and comprise pelitic and calcareous granulites, a gabbro-norite-basic granulite suite and multiple phases of granites of the Ambaji suite. The granulites have undergone three major phases of folding and shearing. The F1 and F2 folds are coaxial along NE-SW axis, and F3 folds are developed across the former along NW-SE axis. Thus, various types of interference patterns are produced. The granulite facies metamorphism is marked by a spinel–cordierite–garnet–sillimanite–quartz assemblage with melt phase and is synkinematic to the F1 phase of folding. The peak thermobarometric condition is set at ≥850 °C and 5.5–6.8 kb. The granulites have been exhumed through thrusting along multiple ductile shear zones during syn- to post-F2 folding. Late-stage shearing has produced cataclasites and pseudotachylites. Sensitive High Resolution Ion MicroProbe (SHRIMP) U–Pb dating of zircon from pelitic granulites and synkinematically emplaced granites indicate that: (1) the sedimentary succession of the South Delhi Terrane was deposited between 1240 and 860 Ma with detritus derived from magmatic sources with ages between 1620 and 1240 Ma; (2) folding and granulite metamorphism have taken place between ca. 860 and 800 Ma, and exhumation at around ca. 800–760 Ma; and (3) the last phase of granitic activity occurred at ca. 759 Ma. This shows, for the first time, that the granulites of the South Delhi Terrane are much younger than those of the Sandmata Granulite Complex of the northern part of the Aravalli Mobile Belt, the Saussar granulites of the Central India Mobile Belt and the Eastern Ghats Mobile Belt. Instead, they show similarities to the Neoproterozoic granulites of the Circum Indian Orogens that include the East African Orogen (East Africa and Madagascar), the Southern Granulite Terrane of India and much of Sri Lanka. We suggest that the South Delhi Basin probably marks a trace of the proto-Mozambique Ocean in NW India within Gondwana, that closed when the Marwar Craton, arc fragments (Bemarivo Belt in Madagascar and the Seychelles) and components of the Arabian-Nubian Shield collided with the Aravalli-Bundelkhand Protocontinent at ca. 850–750 Ma. 相似文献