全文获取类型
收费全文 | 103篇 |
免费 | 4篇 |
专业分类
测绘学 | 1篇 |
大气科学 | 1篇 |
地球物理 | 19篇 |
地质学 | 38篇 |
海洋学 | 11篇 |
天文学 | 24篇 |
自然地理 | 13篇 |
出版年
2021年 | 3篇 |
2020年 | 4篇 |
2019年 | 3篇 |
2018年 | 4篇 |
2017年 | 2篇 |
2016年 | 2篇 |
2015年 | 3篇 |
2014年 | 2篇 |
2013年 | 7篇 |
2012年 | 6篇 |
2011年 | 1篇 |
2010年 | 4篇 |
2009年 | 5篇 |
2008年 | 5篇 |
2007年 | 2篇 |
2006年 | 8篇 |
2005年 | 4篇 |
2004年 | 4篇 |
2003年 | 3篇 |
2002年 | 3篇 |
2001年 | 2篇 |
2000年 | 1篇 |
1999年 | 1篇 |
1998年 | 3篇 |
1996年 | 1篇 |
1992年 | 2篇 |
1991年 | 2篇 |
1990年 | 1篇 |
1987年 | 2篇 |
1986年 | 2篇 |
1985年 | 1篇 |
1984年 | 1篇 |
1983年 | 3篇 |
1982年 | 2篇 |
1981年 | 1篇 |
1979年 | 1篇 |
1978年 | 1篇 |
1977年 | 2篇 |
1975年 | 2篇 |
1973年 | 1篇 |
排序方式: 共有107条查询结果,搜索用时 718 毫秒
71.
Frances Tang 《Solar physics》1978,60(1):119-122
H flare patches usually do not occur in sunspot umbrae. Presented here are cases of a type of umbral flare in which the flare patch originated in, and was confined to, the p spot umbra. All are H subflares. Two of the four flares were accompanied by type III radio bursts. The simplicity and similarity of the magnetic fields of these regions were striking. 相似文献
72.
Primary production in the Northern San Francisco Estuary (SFE) has been declining despite heavy loading of anthropogenic nutrients. The inorganic nitrogen (N) loading comes primarily from municipal wastewater treatment plant (WTP) discharge as ammonium (NH(4)). This study investigated the consequences for river and estuarine phytoplankton of the daily discharge of 15 metric tons NH(4)-N into the Sacramento River that feeds the SFE. Consistent patterns of nutrients and phytoplankton responses were observed during two 150-km transects made in spring 2009. Phytoplankton N productivity shifted from NO(3) use upstream of the WTP to productivity based entirely upon NH(4) downstream. Phytoplankton NH(4) uptake declined downstream of the WTP as NH(4) concentrations increased, suggesting NH(4) inhibition. The reduced total N uptake downstream of the WTP was accompanied by a 60% decline in primary production. These findings indicate that increased anthropogenic NH(4) may decrease estuarine primary production and increase export of NH(4) to the coastal ocean. 相似文献
73.
The purpose of this study was to develop an interpretive groundwater‐flow model to assess the impacts that planned forest restoration treatments and anticipated climate change will have on large regional, deep (>400 m), semi‐arid aquifers. Simulations were conducted to examine how tree basal area reductions impact groundwater recharge from historic conditions to 2099. Novel spatial analyses were conducted to determine areas and rates of potential increases in groundwater recharge. Changes in recharge were applied to the model by identifying zones of basal area reduction from planned forest restoration treatments and applying recharge‐change factors to these zones. Over a 10‐year period of forest restoration treatment, a 2.8% increase in recharge to one adjacent groundwater basin (the Verde Valley sub‐basin) was estimated, compared to conditions that existed from 2000 to 2005. However, this increase in recharge was assumed to quickly decline after treatment due to regrowth of vegetation and forest underbrush and their associated increased evapotranspiration. Furthermore, simulated increases in groundwater recharge were masked by decreases in water levels, stream baseflow, and groundwater storage resulting from surface water diversions and groundwater pumping. These results indicate that there is an imbalance between water supply and demand in this regional, semi‐arid aquifer. Current water management practices may not be sustainable into the far future and comprehensive action should be taken to minimize this water budget imbalance. 相似文献
74.
Sam?Broom-FendleyEmail authorView authors OrcID profile Frances?Wall Baruch?Spiro Clemens?V.?Ullmann 《Contributions to Mineralogy and Petrology》2017,172(11-12):96
Carbonatites host some of the largest and highest grade rare earth element (REE) deposits but the composition and source of their REE-mineralising fluids remains enigmatic. Using C, O and 87Sr/86Sr isotope data together with major and trace element compositions for the REE-rich Kangankunde carbonatite (Malawi), we show that the commonly observed, dark brown, Fe-rich carbonatite that hosts REE minerals in many carbonatites is decoupled from the REE mineral assemblage. REE-rich ferroan dolomite carbonatites, containing 8–15 wt% REE2O3, comprise assemblages of monazite-(Ce), strontianite and baryte forming hexagonal pseudomorphs after probable burbankite. The 87Sr/86Sr values (0.70302–0.70307) affirm a carbonatitic origin for these pseudomorph-forming fluids. Carbon and oxygen isotope ratios of strontianite, representing the REE mineral assemblage, indicate equilibrium between these assemblages and a carbonatite-derived, deuteric fluid between 250 and 400 °C (δ18O + 3 to + 5‰VSMOW and δ13C ? 3.5 to ? 3.2‰VPDB). In contrast, dolomite in the same samples has similar δ13C values but much higher δ18O, corresponding to increasing degrees of exchange with low-temperature fluids (< 125 °C), causing exsolution of Fe oxides resulting in the dark colour of these rocks. REE-rich quartz rocks, which occur outside of the intrusion, have similar δ18O and 87Sr/86Sr to those of the main complex, indicating both are carbonatite-derived and, locally, REE mineralisation can extend up to 1.5 km away from the intrusion. Early, REE-poor apatite-bearing dolomite carbonatite (beforsite: δ18O + 7.7 to + 10.3‰ and δ13C ?5.2 to ?6.0‰; 87Sr/86Sr 0.70296–0.70298) is not directly linked with the REE mineralisation. 相似文献
75.
Community mapping is a relatively new tool with considerable potential in giving practical effect at the local level to sustainable development rhetoric. As a repository of socially constructed knowledge, it has considerable value in democratizing information both in terms of what is recorded and public access to it, in a manner that facilitates more meaningful participation of non-experts in planning and advocacy processes. Focusing on a community mapping project in Galway, Ireland, this research paper explores how the city's municipal authority is employing community mapping not just to record and promote the city's social, environmental, economic and cultural assets but also as a practical tool to bolster public participation in policy-making and to improve local communities' trust in the municipal authority, thereby shaping sustainability practices through enhanced governance. 相似文献
76.
Ika Paul-Pont Patrice Gonzalez Florence Jude Line Bourrasseau Frances Haynes Christine Paillard 《Marine pollution bulletin》2010,60(4):515-118
The present study evaluated the interactive effects of cadmium contamination and pathogenic organisms (trematodes Himasthla elongata and bacteria Vibrio tapetis) singularly and in combination during 7 days on the bivalve Cerastoderma edule. Some defense-related activities were analyzed such as genetic expression, metallothionein and immune responses. Trematode metacercarial infection, similar whatever the treatment, induced the strongest responses of immune parameters. Particularly, the interaction between cadmium and parasite exposures induced unusual responses on gene expression and immune responses. No effect of bacterial challenge appeared on bivalve responses, nevertheless a strong mortality of V. tapetis infected cockles occured between 7 and 14 days. Cadmium bioaccumulation was significantly modulated by both pathogenic organisms. Furthermore, an antagonistic effect of trematodes and bacteria was shown on metal bioaccumulation of co-infected cockles. These results highlighted the importance of considering the multiplicity of perturbation sources in coastal ecosystems to assess the health status of organisms. 相似文献
77.
Seanpaul La Selle Bruce M. Richmond Bruce E. Jaffe Alan R. Nelson Frances R. Griswold Maria E. M. Arcos Catherine Chagué James M. Bishop Piero Bellanova Haunani H. Kane Brent D. Lunghino Guy Gelfenbaum 《Sedimentology》2020,67(3):1249-1273
Over the past 200 years of written records, the Hawaiian Islands have experienced tens of tsunamis generated by earthquakes in the subduction zones of the Pacific ‘Ring of Fire’ (for example, Alaska–Aleutian, Kuril–Kamchatka, Chile and Japan). Mapping and dating anomalous beds of sand and silt deposited by tsunamis in low-lying areas along Pacific coasts, even those distant from subduction zones, is critical for assessing tsunami hazard throughout the Pacific basin. This study searched for evidence of tsunami inundation using stratigraphic and sedimentological analyses of potential tsunami deposits beneath present and former Hawaiian wetlands, coastal lagoons, and river floodplains. Coastal wetland sites on the islands of Hawai΄i, Maui, O΄ahu and Kaua΄i were selected based on historical tsunami runup, numerical inundation modelling, proximity to sandy source sediments, degree of historical wetland disturbance, and breadth of prior geological and archaeological investigations. Sand beds containing marine calcareous sediment within peaty and/or muddy wetland deposits on the north and north-eastern shores of Kaua΄i, O΄ahu and Hawai΄i were interpreted as tsunami deposits. At some sites, deposits of the 1946 and 1957 Aleutian tsunamis are analogues for deeper, older probable tsunami deposits. Radiocarbon-based age models date sand beds from three sites to ca 700 to 500 cal yr bp , which overlaps ages for tsunami deposits in the eastern Aleutian Islands that record a local subduction zone earthquake. The overlapping modelled ages for tsunami deposits at the study sites support a plausible correlation with an eastern Aleutian earthquake source for a large prehistoric tsunami in the Hawaiian Islands. 相似文献
78.
Temporal variability of dimethylsulfide and dimethylsulfoniopropionate in the Sargasso Sea 总被引:1,自引:0,他引:1
John W. H. Dacey Frances A. Howse Anthony F. Michaels Stuart G. Wakeham 《Deep Sea Research Part I: Oceanographic Research Papers》1998,45(12):2085-2104
Vertical profiles of dimethylsulfide (DMS) and β-dimethylsulfoniopropionate, particulate (pDMSP) and dissolved (dDMSP), were measured biweekly in the upper 140 m of the Sargasso Sea (32°10′N, 64°30′W) during 1992 and 1993. DMS and pDMSP showed strong, but different, seasonal patterns; no distinct intra-annual pattern was observed for dDMSP. During winter, concentrations of DMS were generally less than 1 nmol l−1 at all depths, dDMSP was less than 3 nmol l−1 and pDMSP was less than 8 nmol l−1. In spring, concentrations of both dDMSP and pDMSP rose, on a few occasions up to 20 nmol l−1 in the dissolved pool and up to 27 nmol l−1 in the particulate pool. These increases, due to blooms of DMSP-containing phytoplankton, resulted in only minor increases in DMS concentrations (up to 4 nmol l−1). Throughout the summer, the concentrations of DMS continued to increase, reaching a maximum in August of 12 nmol l−1 (at 30 m depth). There was no concomitant summer increase in dDMSP or pDMSP. The differences among the seasonal patterns of DMS, dDMSP, and pDMSP suggest that the physical and biological processes involved in the cycling of DMS change with the seasons. There is a correlation between the concentration of DMS and temperature in this data set, as required by some of the climate feedback models that have been suggested for DMS. A full understanding of the underlying processes controlling DMS is required to determine if the temperature-DMS pattern is of significance in the context of global climate change. 相似文献
79.
Wang Zhengui Chai Fei Dugdale Richard Liu Qianqian Xue Huijie Wilkerson Frances Chao Yi Zhang Yinglong Zhang Hongchun 《Ocean Dynamics》2020,70(8):1169-1186
Ocean Dynamics - San Francisco Bay (SFB) is a complex ecosystem that has been heavily impacted by human activities. It has experienced strong year-to-year variations in physical, chemical, and... 相似文献
80.
A carbon,nitrogen, and sulfur elemental and isotopic study in dated sediment cores from the Louisiana Shelf 总被引:2,自引:0,他引:2
Robert J. Rosenbauer Peter W. Swarzenski Carol Kendall William H. Orem Frances D. Hostettler Mark E. Rollog 《Geo-Marine Letters》2009,29(6):415-429
Three sediment cores were collected off the Mississippi River delta on the Louisiana Shelf at sites that are variably influenced
by recurring, summer-time water-column hypoxia and fluvial loadings. The cores, with established chronology, were analyzed
for their respective carbon, nitrogen, and sulfur elemental and isotopic composition to examine variable organic matter inputs,
and to assess the sediment record for possible evidence of hypoxic events. Sediment from site MRJ03-3, which is located close
to the Mississippi Canyon and generally not influenced by summer-time hypoxia, is typical of marine sediment in that it contains
mostly marine algae and fine-grained material from the erosion of terrestrial C4 plants. Sediment from site MRJ03-2, located
closer to the mouth of the Mississippi River and at the periphery of the hypoxic zone (annual recurrence of summer-time hypoxia
>50%), is similar in composition to core MRJ03-3, but exhibits more isotopic and elemental variability down-core, suggesting
that this site is more directly influenced by river discharge. Site MRJ03-5 is located in an area of recurring hypoxia (annual
recurrence >75%), and is isotopically and elementally distinct from the other two cores. The carbon and nitrogen isotopic
composition of this core prior to 1960 is similar to average particulate organic matter from the lower Mississippi River,
and approaches the composition of C3 plants. This site likely receives a greater input of local terrestrial organic matter
to the sediment. After 1960 and to the present, a gradual shift to higher values of δ13C and δ15N and lower C:N ratios suggests that algal input to these shelf sediments increased as a result of increased productivity
and hypoxia. The values of C:S and δ34S reflect site-specific processes that may be influenced by the higher likelihood of recurring seasonal hypoxia. In particular,
the temporal variations in the C:S and δ34S down-core are likely caused by changes in the rate of sulfate reduction, and hence the degree of hypoxia in the overlying
water column. Based principally on the down-core C:N and C:S ratios and δ13C and δ34S profiles, sites MRJ03-3 and MRJ03-2 generally reflect more marine organic matter inputs, while site MRJ03-5 appears to be
more influenced by terrestrial deposition. 相似文献