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281.
Zusammenfassung  Nach wie vor findet der Faktor Zeit in den Umweltwissenschaften zu wenig Beachtung. Langfristige Beobachtungen und Me?reihen in der ?kologischen Forschung, wie sie für die Bewertung und Prognosen von Umweltzust?nden und-entwicklunger, unabdingbar w?ren, scheinen die Ausnahme zu sein. Besonders komplexe ?kosysteme, wie terrestrische oder marine Systeme, kennzeichnen sich auch durch l?ngere natürliche Eigenzeiten, die deshalb bei ihrer Erforschung berücksichtigt werden mü?ten. In diesem Zusammenhang soll verdeutlicht werden, welche Rolle zeitliche Parameter speziell in der terrestrischen ?kosystemforschung spielen. Zu diesem Zweck wurde eine Datenbank konzipiert, die Hauptcharakteristika von ?kosystemaren Analysen aufnehmen kann. Forschungsberichte verschiedener ?kosystemforschungszentren wurden zur Aufnahme in die Datenbank bearbeitet. Gezielte Abfragen auf den Datenpool erm?glichen dann eine Auswertung hinsichtlich der zeitlichen Ausrichtung bestimmter Untersuchungen. Dabei stellte sich — neben einer teilweisen Ungleichheit der Zeitskalen von Experiment und Realit?t — u.a. heraus, da? l?ngerfristige Untersuchungen ?u?erst selten durchgeführt werden. So vielf?ltig die Gründe für dieses Defizit auch sein m?gen, sie k?nnen nicht von der Forderung nach st?rkerer Berücksichtigung von langzeitlichen Beobachtungen ablenken, will die ?kosystemforschung die an sie gestellten Aufgaben erfüllen.   相似文献   
282.
A method is presented for determining production and consumption rates of .OH radicals produced photochemically in natural surface waters. It is based on the determination of the kinetics by which the concentration of a specified trace compound decreases during irradiation. In samples from Lake Greifensee (Switzerland) low production rates for .OH limit its possible effects. In addition, fast consumptions by the natural dissolved organic solutes and by the bicarbonate protect organic micropollutants from oxidation by .OH. Neither direct nor indirect H2O2 photolysis was a significant source of .OH in the lakewater studied lacking iron, whereas nitrate photolysis could have been a source. Comparison with reaction kinetic formulations allows generalizations for other types of waters.  相似文献   
283.
A program to fit theoretically modelled uptake and clearance periods of the bioconcentration of chemicals to experimental data using a programmable pocket calculator with thermal printer is reported. The bioconcentration factor (BCF) is calculated from the ratio of uptake and clearance rate constants. Because of the impossibility to linearize the kinetic equations an iterative nonlinear GAUSS-NEWTON least-squares fit has been applied for the pocket calculator programm ACCUTI-59, which calculates from a set of start parameters the best values for uptake and clearance rate constants, BCF, and the standard errors as well as the sum of squared deviations. A listing of the program is given.  相似文献   
284.
Zusammenfassung  Eine Zusammenstellung der Ozon-Me?werte der Luftme?stationnetze in Hessen und NRW ergab für die Jahresmittelwerte von 1990–1998 im Durchschnitt eine schwache Abnahme der Ozonkonzentrationen. Dabei lagen die Jahresmittelwerte der Ozonkonzentrationen über Waldstationen doppelt so hoch wie über Stadtstationen. Die Ozonkonzentrationen verhalten sich im regionalen Vergleich umgekehrt proportional zur Verkehrsdichte. In der Zahl der überschreitungen der gesetzlich festgelegten Grenzwerte von ≥180 μg Ozon/m3 pro Jahr lagen die Waldstationen mit dem 2–3 fachen Wert über den Stadtstationen. Lediglich die j?hrlichen Maximalwerte der stündlich gemessenen Ozonwerte n?hern sich einander. Die hohen Ozonwerte über den Waldstationen stehen im Zusammenhang mit den niedrigen Konzentrationen von NOx. Nachts reduziert sich das Ozon über den Waldstationen durch Rückreaktion mit vergleichsweise geringen Konzentrationen von NO nur bis ca. 50%, w?hrend der Ozongehalt über Stadtstationen bis nahe Null absinkt. Dieser Vorgang über den Stadtstationen wird auch durch Photolyse des in hohen Konzentrationen vorliegenden NO2 und die dadurch erfolgende erh?hte Bildung von Ozon w?hrend des Tages nicht wieder kompensiert. Für die hier dargestellten Ergebnisse gibt es prinzipiell keine Unterschiede zwischen den Ozonverh?ltnissen in Hessen und NRW.   相似文献   
285.
Goal, Scope and Background Ethoxyresorufin-O-deethylase (EROD) is a well-accepted marker for biological effects in fish and is, therefore, part of numerous monitoring programmes. EROD activity was measured in livers of dab (Limanda limanda) from the German Bight (North Sea) from 1995 to 2003. The aim of the present long-term study was (a) time trend monitoring of EROD activity of dab from the German Bight and (b) to elucidate the needs for a successful application of EROD activity as an early warning system. Methods. EROD activities were determined fluorimetrically in dab liver microsomes, using resorufin as an external standard. The limit of detection (LD) and the limit of quantification (LQ) were calculated. Results were referred to protein concentrations. Results and Discussion. EROD activities of 610 female dab caught in different seasons between January 1995 and August 2003 were analyzed individually. Activities varied from 〈 LD to 1768 pmol/(min mg protein) and showed an annual cycle as well as significant differences between the years. Highest EROD activities were observed in early summer and lowest activities during the winter period. In autumn 2002, significantly elevated EROD activities were detected, possibly related to effects of the River Elbe flood event. Two scenarios with different EROD baseline data are presented to discuss the prerequisites for the use of EROD as a monitoring tool. The comparison of these scenarios underlines the importance of appropriate season-specific baseline data. Conclusion. The use of EROD as an early warning tool for contaminant effects in dab in the German Bight has different prospects during the year, because, due to the high background variability, elevated EROD activities are less easy to detect in spring/summer than during the remaining times of the year. Recommendation and Outlook. The availability of site-specific data on the EROD baseline level, its random variation and its annual cycle is a necessary prerequisite for monitoring. If monitoring is to be carried out only for a limited time period of the year, a season with low background variability in EROD activity (autumn) should be chosen to avoid the need for a compensation of the temperature-triggered shift in sexual cycles and the resulting changes in EROD activity.  相似文献   
286.
287.
Summary The response of the starling to sugar solutions was investigated as this species, which eats sweet fruits, does not prefer sugar solutions according to the literature.In choice tests using two identical fountains, moderate preference for higher concentrations (0.5 M and 1 M) of glucose and fructose to water was demonstrated. The same concentrations of sucrose were rejected. Lower concentrations (0.25 M and less) of all three sugars were neither preferred nor rejected. In choice tests using two differently coloured fountains the subjects did not generally respond more sensitively to sugar solutions. In learning experiments with differently coloured fountains the starlings developed very marked preferences for 0.5 M glucose and 0.5 M fructose and a corresponding rejection of 0.5 M sucrose in the course of 1–2 days. In a learning experiment with dentical fountains they also developed a pronounced preference; the preference values obtained, however, are higher if secondary cues such as the colour of the fountain or its position are available. In short time tests immediate responses to sugar solutions could not be demonstrated.The rejection of sucrose is attributed to illness-induced aversion learning, the learned preference for glucose and fructose to the preference according to gain in energy per unit of time as postulated by the optimal foraging theory. Taste sensations play, if any, only a minor role. The learning mechanisms operating in the experiments could be employed by the starling for the selection of fruits.  相似文献   
288.
289.
Hochwasser 2002     
In August 2002, highly contaminated areas in the region of Bitterfeld, e.g. the floodplain of the creek Spittelwasser, as well as the adjacent regions of Jeßnitz and Raguhn, were submerged by the river Mulde. An input of mobilized contaminated sediments in residential areas was the matter of concern. The objective of the present study was to estimate the pollutants load on the basis of chemical and biological data and identify the sources of pollutants. Deposited sludge and flood water samples were assessed on the basis of biological and chemical analyses and in comparison with administrative reference values. The pollution of the investigated sites was rather heterogeneous. At several sites, tolerance limits of the German Klärschlammverordnung or the Bundesbodenschutzverordnung were clearly exceeded, e.g. for Pb, As and HCH. Organic extracts exhibited significant effects in several biotests. This may be relevant with respect to direct particle uptake via ingestion or respiration. Pollution patterns for heavy metals as well as for organic pollutants differed significantly from the pattern found in the Spittelwasser flood plain before the inundation, which is in contrast to the initial hypothesis of a possible transport of contaminated Spittelwasser sediments into residential areas. Interestingly, a correlation of chemical load and the overall biological effect could be shown. From the viewpoint of the precautionary principle, the identification of the compounds exerting toxic effects and of the respective pollutant sources would be desirable.  相似文献   
290.
The combination of remote sensing methods like Doppler lidar and FTIR allows remote determination of mass fluxes of gases. Doppler lidar measures the three-dimensional wind vector in the vicinity of diffuse sources, or the velocity of air in a chimney plume if an industrial complex is monitored. FTIR is a multicomponent remote sensing method for gas concentrations. The Fourier transformation of an interferogram of a Michelson interferometer within a FTIR system converts the recorded intensity (function of optical path length) to a spectral signal (function of wavenumber). Both information, velocity and concentration, give the mass fluxes of the tracer (gas). A first test was performed at Munich-Nord power station with FTIR and cw-Doppler lidar. Fluxes of CO2, CO, NO, and HCl were determined. The results are in good agreement with the fluxes measured byin situ instruments of the power station. The method can be used to control industrial complexes from an outside observation site.  相似文献   
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