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121.
Jens Havskov Sørensen Alix Rasmussen Thomas Ellermann Erik Lyck 《Atmospheric environment (Oxford, England : 1994)》1998,32(24):101
During the first European Tracer Experiment (ETEX) tracer gas was released from a site in Brittany, France, and subsequently observed over a range of 2000 km. Hourly measurements were taken at the National Environmental Research Institute (NERI) located at Risø, Denmark, using two measurement techniques. At this location, the observed concentration time series shows a double-peak structure occurring between two and three days after the release. By using the Danish Emergency Response Model of the Atmosphere (DERMA), which is developed at the Danish Meteorological Institute (DMI), simulations of the dispersion of the tracer gas have been performed. Using numerical weather-prediction data from the European Centre for Medium-Range Weather Forecast (ECMWF) by DERMA, the arrival time of the tracer is quite well predicted, so also is the duration of the passage of the plume, but the double-peak structure is not reproduced. However, using higher-resolution data from the DMI version of the HIgh Resolution Limited Area Model (DMI-HIRLAM), DERMA reproduces the observed structure very well. The double-peak structure is caused by the influence of a mesoscale anti-cyclonic eddy on the tracer gas plume about one day earlier. 相似文献
122.
123.
Peter F. Ffolliott D. Phillip Guertin William D. Rasmussen 《Environmental management》1988,12(6):809-814
Recurrent fire has played a dominant role in the ecology of southwestern ponderosa pine forests. To assess the benefits or losses of fire in these forests, a computer simulation model, called BURN, considers vegetation (mortality, regeneration, and production of herbaceous vegetation), wildlife (populations and habitats), and hydrology (streamflow and water quality). In the formulation of the model, graphical representations (time-trend response curves) of increases or losses (compared to an unburned control) after the occurrence of fire are converted to fixedterm annual ratios, and then annuities for the simulation components. Annuity values higher than 1.0 indicate benefits, while annuity values lower than 1.0 indicate losses. Studies in southwestern ponderosa pine forests utilized in the development of BURN are described briefly. 相似文献
124.
Culbertson JA Prins JM Grimsrud EP Rasmussen RA Khalil MA Shearer MJ 《Chemosphere》2004,55(8):1109-1119
The concentrations of CF(3)-containing compounds in archived air samples collected at Cape Meares, Oregon, from 1978 to 1997, at Point Barrow, Alaska, from 1995 to 1998, and at Palmer Station, Antarctica, from 1991 to 1997, were determined by high resolution gas chromatography and high resolution mass spectrometry. The CF(3)-containing compounds measured by this method and discussed here are: the perfluorinated compound, C(3)F(8) (FC 218); four perhalogenated compounds, CF(3)Cl (CFC 13), CF(3)CF(2)Cl (CFC 115), CF(3)CFCl(2) (CFC 114a), and CF(3)Br (Halon 1301); and three hydrofluorocompounds, CF(3)H (HFC 23), CF(3)CH(3) (HFC 143a), and CF(3)CH(2)F (HFC 134a). For four of these compounds, very few measurements have been previously reported. The atmospheric concentrations of all of the CF(3)-containing compounds continuously increased in time over the sample collection periods. From these data, the annual rates of emission into the atmosphere have been estimated. The emission rates fall into one of three distinct categories. The annual emission rates of C(3)F(8), CF(3)H, CF(3)CH(3), and CF(3)CH(2)F have continuously increased over the last two decades. That of CF(3)CFCl(2) has decreased continuously. Emission rates for CF(3)Cl, CF(3)CF(2)Cl, and CF(3)Br reached maximum levels in the late 1980s, and have been decreasing in the 1990s. The emission rates of C(3)F(8), CF(3)CH(3) and CF(3)CH(2)F were nearly zero 20 years ago but have increased rapidly during the last decade. 相似文献
125.
Stine Aakre Ilona Banaszak Reinhard Mechler Dirk Rübbelke Anita Wreford Harvir Kalirai 《Mitigation and Adaptation Strategies for Global Change》2010,15(7):721-736
Increasing losses from weather related extreme events coupled with limited coping capacity suggest a need for strong adaptation
commitments, of which public sector responses to adjustments to actual and expected climate stimuli are key. The European
Commission has started to address this need in the emerging European Union (EU) climate adaptation strategy; yet, a specific
rationale for adaptation interventions has not clearly been identified, and the economic case for adaptation to extremes remains
vague. Basing the diagnosis on economic welfare theory and an empirical analysis of the current EU and member states’ roles
in managing disaster risk, we discuss how and where the public sector may intervene for managing climate variability and change.
We restrict our analysis to financial disaster management, a domain of adaptation intervention, which is of key concern for
the EU adaptation strategy. We analyse three areas of public sector interventions, supporting national insurance systems,
providing compensation to the affected post event as well as intergovernmental loss sharing through the EU solidarity fund,
according to the three government functions of allocation, distribution, and stabilization suggested by welfare theory, and
suggest room for improvement. 相似文献
126.
Pil Uthaug Rasmussen Katrine Uhrbrand Mette Damkj r Bartels Helle Neustrup Dorina Gabriela Karottki Ute B ltmann Anne Mette Madsen 《Frontiers of Environmental Science & Engineering》2021,15(3):41