全文获取类型
收费全文 | 2396篇 |
免费 | 285篇 |
国内免费 | 938篇 |
专业分类
安全科学 | 165篇 |
废物处理 | 102篇 |
环保管理 | 375篇 |
综合类 | 1842篇 |
基础理论 | 334篇 |
污染及防治 | 506篇 |
评价与监测 | 184篇 |
社会与环境 | 91篇 |
灾害及防治 | 20篇 |
出版年
2024年 | 11篇 |
2023年 | 70篇 |
2022年 | 112篇 |
2021年 | 119篇 |
2020年 | 118篇 |
2019年 | 121篇 |
2018年 | 119篇 |
2017年 | 116篇 |
2016年 | 127篇 |
2015年 | 125篇 |
2014年 | 129篇 |
2013年 | 191篇 |
2012年 | 198篇 |
2011年 | 180篇 |
2010年 | 148篇 |
2009年 | 193篇 |
2008年 | 142篇 |
2007年 | 166篇 |
2006年 | 180篇 |
2005年 | 130篇 |
2004年 | 138篇 |
2003年 | 121篇 |
2002年 | 99篇 |
2001年 | 111篇 |
2000年 | 86篇 |
1999年 | 55篇 |
1998年 | 63篇 |
1997年 | 58篇 |
1996年 | 30篇 |
1995年 | 28篇 |
1994年 | 18篇 |
1993年 | 23篇 |
1992年 | 22篇 |
1991年 | 10篇 |
1990年 | 9篇 |
1989年 | 5篇 |
1988年 | 1篇 |
1987年 | 8篇 |
1986年 | 5篇 |
1985年 | 6篇 |
1984年 | 2篇 |
1982年 | 6篇 |
1981年 | 5篇 |
1980年 | 6篇 |
1979年 | 4篇 |
1978年 | 2篇 |
1972年 | 3篇 |
排序方式: 共有3619条查询结果,搜索用时 11 毫秒
31.
Influence of temporally variable groundwater flow conditions on point measurements and contaminant mass flux estimations 总被引:2,自引:0,他引:2
Arno Rein Sebastian Bauer Peter Dietrich Christof Beyer 《Journal of contaminant hydrology》2009,108(3-4):118-133
Monitoring of contaminant concentrations, e.g., for the estimation of mass discharge or contaminant degradation rates, often is based on point measurements at observation wells. In addition to the problem, that point measurements may not be spatially representative, a further complication may arise due to the temporal dynamics of groundwater flow, which may cause a concentration measurement to be not temporally representative. This paper presents results from a numerical modeling study focusing on temporal variations of the groundwater flow direction. “Measurements” are obtained from point information representing observation wells installed along control planes using different well frequencies and configurations. Results of the scenario simulations show that temporally variable flow conditions can lead to significant temporal fluctuations of the concentration and thus are a substantial source of uncertainty for point measurements. Temporal variation of point concentration measurements may be as high as the average concentration determined, especially near the plume fringe, even when assuming a homogeneous distribution of the hydraulic conductivity. If a heterogeneous hydraulic conductivity field is present, the concentration variability due to a fluctuating groundwater flow direction varies significantly within the control plane and between the different realizations. Determination of contaminant mass fluxes is also influenced by the temporal variability of the concentration measurement, especially for large spacings of the observation wells. Passive dosimeter sampling is found to be appropriate for evaluating the stationarity of contaminant plumes as well as for estimating average concentrations over time when the plume has fully developed. Representative sampling has to be performed over several periods of groundwater flow fluctuation. For the determination of mass fluxes at heterogeneous sites, however, local fluxes, which may vary considerably along a control plane, have to be accounted for. Here, dosimeter sampling in combination with time integrated local water flux measurements can improve mass flux estimates under dynamic flow conditions. 相似文献
32.
Jessica T. Newlin Peggy A. Johnson 《Journal of the American Water Resources Association》2009,45(5):1197-1208
Abstract: An adaptive management framework is applied to the problem of identifying mitigation measures for sediment deposition near bridge crossings in small streams in the Northern Tier region of northern Pennsylvania. The presence of the rigid bridge infrastructure introduces a challenge for applying adaptive management practices, because the integrity of the bridge structure itself has to be maintained regardless of the mitigation practices used in the stream channel near the bridge. In an effort to overcome the unacceptable risk that field‐scale adaptive management experiments present to rigid bridge infrastructure, an adaptive management approach for laboratory‐scale experimentation of mitigation methods at bridge crossings in the Northern Tier region is presented as a way to decrease the level of uncertainty about channel response to mitigation measures and increase the rate of learning about the effectiveness of these measures. Four cycles of adaptive management experiments are discussed to demonstrate that this approach results in fast and efficient learning about channel response to mitigation methods for the given conditions. The value of monitoring and of assessment of monitored data in the overall efficiency of the adaptive management approach is highlighted. Assessment of what was learned in the adaptive management experiment cycles presented here leads to new directions to continually improve management policies and practices in stream channels at bridge crossings in the Northern Tier region. The adaptive management process, rather than continuing with a normally risk‐averse management approach, results in opportunities for learning new information about a system’s response. 相似文献
33.
34.
The dispersion of pollutants from naturally ventilated underground parking garages has been studied in a boundary layer wind tunnel. Two idealized model setups have been analysed, one was simulating pollutant dispersion around an isolated rectangular building and one was representing dispersion in a finite array of idealized building blocks. Flow and dispersion close to modelled ground level emission sources was measured. The results illustrate the complexity of the flow around buildings and provide insight in pollutant transport from ground level sources located directly on building surfaces. As a result, areas critical with respect to high pollutant concentrations could be visualized. Particularly, the results show high concentration gradients on the surface of the buildings equipped with modelled emission sources. Inside the boundary layers on the building walls, a significant amount of pollutants is transported to upwind locations on the surface of the building. The paper documents the potential of physical modelling to be used for the simulation and measurement of dispersion close to emission sources and within complex building arrangements. 相似文献
35.
This paper examines the importance of the correlation between hydraulic conductivity (K) and degradation rate constant (k) during the transport of reactive contaminants in heterogeneous aquifers. We simulated reactive transport in an ensemble of two-dimensional heterogeneous aquifers. Two sets of transport simulations were conducted: one in which a perfect positive correlation was assumed between ln(K) and ln(k), and one in which a perfect negative correlation was assumed. We found that the sign of the correlation has important consequences for the contaminant transport. Qualitatively, a negative correlation leads to significantly more pronounced "fingering" of the contaminant plume than does a positive correlation, with potentially important consequences for downgradient receptors. Quantitatively, the expected behavior (as quantified by the contaminant mass remaining in the aquifer) is statistically different between the positive and negative cases: on average, more contaminant mass persists when K and k are negatively correlated. Also, the negative correlation leads to more variability between realizations of the ensemble, whereas a positive correlation induces relatively little variability between realizations. We discuss the implications of these findings for the management of contaminated aquifers. 相似文献
36.
Schröder P Scheer CE Diekmann F Stampfl A 《Environmental science and pollution research international》2007,14(2):114-122
Background, Aim and Scope
Numerous herbicides and xenobiotic organic pollutants are detoxified in plants to glutathione conjugates. Following this enzyme
catalyzed reaction, xenobiotic GS-conjugates are thought to be compartmentalized in the vacuole of plant cells. In the present
study, evidence is presented for long range transport of these conjugates in plants, rather than storage in the vacuole. To
our knowledge this is the first report about the unidirectional long range transport of xenobiotic conjugates in plants and
the exudation of a glutathione conjugate from the root tips. This could mean that plants possess an excretion system for unwanted
compounds which give them similar advantages as animals.
Materials and Methods:
Barley plants (Hordeum vulgare L. cv. Cherie) were grown in Petri dishes soaked with tap water in the greenhouse.
- Fluorescence Microscopy. Monobromo- and Monochlorobimane, two model xenobiotics that are conjugated rapidly in plant cells
with glutathione, hereby forming fluorescent metabolites, were used as markers for our experiments. Their transport in the
root could be followed sensitively with very good temporal and spatial resolution. Roots of barley seedlings were cut under
water and the end at which xenobiotics were applied was fixed in an aperture with a thin latex foil and transferred into a
drop of water on a cover slide. The cover slide was fixed in a measuring chamber on the stage of an inverse fluorescence microscope
(Zeiss Axiovert 100).
- Spectrometric enzyme assay. Glutathione S-transferase (GST) activity was determined in the protein extracts following established
methods. Aliquots of the enzyme extract were incubated with 1-chloro-2,4-dinitrobenzene (CDNB), or monochlorobimane. Controls
lacking enzyme or GSH were measured.
- Pitman chamber experiments. Ten days old barley plants or detached roots were inserted into special incubation chambers, either
complete with tips or decapitated, as well as 10 days old barley plants without root tips. Compartment A was filled with a
transport medium and GSH conjugate or L-cysteine conjugate. Compartments B and C contained sugar free media. Samples were
taken from the root tip containing compartment C and the amount of conjugate transported was determined spectro-photometrically.
Results:
The transport in roots is unidirectional towards the root tips and leads to exsudation of the conjugates at rates between
20 and 200 nmol min-1. The microscopic studies have been complemented by transport studies in small root chambers and spectroscopic
quantification of dinitrobenzene-conjugates. The latter experiments confirm the microscopic studies. Furthermore it was shown
that glutathione conjugates are transported at higher rates than cysteine conjugates, despite of their higher molecular weights.
This observation points to the existence of glutathione specific carriers and a specific role of glutathione in the root.
Discussion:
It can be assumed that long distance transport of glutathione conjugates within the plant proceeds like GSH or amino acid
transport in both, phloem and xylem. The high velocity of this translocation of the GS-X is indicative of an active transport.
For free glutathione, a rapid transport-system is essential because an accumulation of GSH in the root tip inhibits further
uptake of sulfur. Taking into account that all described MRP transporters and also the GSH plasmalemma ATPases have side activities
for glutathione derivatives and conjugates, co-transport of these xenobiotic metabolites seems credible.
- On the other hand, when GS-B was applied to the root tips from the outside, no significant uptake was observed. Thus it can
be concluded that only those conjugates can be transported in the xylem which are formed inside the root apex. Having left
the root once, there seems to be no return into the root vessels, probably because of a lack of inward directed transporters.
Conclusions:
Plants seem to possess the capability to store glutathione conjugates in the vacuole, but under certain conditions, these
metabolites might also undergo long range transport, predominantly into the plant root. The transport seems dependent on specific
carriers and is unidirectional, this means that xenobiotic conjugates from the rhizosphere are not taken up again. The exudation
of xenobiotic metabolites offers an opportunity to avoid the accumulation of such compounds in the plant.
Recommendations and Perspectives:
The role of glutathione and glutathione related metabolites in the rhizosphere has not been studied in any detail, and only
scattered data are available on interactions between the plant root and rhizosphere bacteria that encounter such conjugates.
The final fate of these compounds in the root zone has also not been addressed so far. It will be interesting to study effects
of the exuded metabolites on the biology of rhizosphere bacteria and fungi. 相似文献
37.
Gerosa G Marzuoli R Desotgiu R Bussotti F Ballarin-Denti A 《Environmental pollution (Barking, Essex : 1987)》2008,152(2):274-284
An Open-Top Chambers experiment on Fagus sylvatica and Quercus robur seedlings was conducted in order to compare the performance of an exposure-based (AOT40) and a flux-based approaches in predicting the appearance of ozone visible injuries on leaves. Three different ozone treatments (charcoal-filtered; non-filtered; and open plots) and two soil moisture treatments (watered and non-watered plots) were performed. A Jarvisian stomatal conductance model was drawn up and parameterised for both species and typical South Alpine environmental conditions, thus allowing the calculation of ozone stomatal fluxes for every treatment. A critical ozone flux level for the onset of leaf visible injury in beech was clearly identified between 32.6 and 33.6 mmolO3 m(-2). In contrast, it was not possible to identify an exposure critical level using the AOT40 index. Water stress delayed the onset of the leaf visible injuries, but the flux-based approach was able to take it into account accurately. 相似文献
38.
The practice of contaminant transport and remediation has shown significant progress in recent years. However, despite the
significant progress made, remediation efforts are often delayed by extremely long breakthrough curve tails that render efforts
to bring the level of contaminants below the regulatory standards inefficient. One hypothesis is that these long tails are
due to the reservoir-like slow diffusive processes in soil micropore zones. This study compares the effects of micropores
at macroscopic and microscopic levels and establishes a link between these approaches for validation and calibration purposes.
The link between macroscopic and microscopic levels is established through comparisons and testing of the two models while
incorporating appropriate scale and boundary effects. Despite the differences in conceptual approaches and simulation time,
the two approaches rendered meaningful results. The link helps forecast the effects of micropore zone transport processes
in the subsurface efficiently and thus allows development of numerical tools that could contribute towards more efficient
remediation design. 相似文献
39.
Inverse modeling of multicomponent reactive transport through single and dual porosity media 总被引:3,自引:0,他引:3
Compacted bentonite is foreseen as buffer material for high-level radioactive waste in deep geological repositories because it provides hydraulic isolation, chemical stability, and radionuclide sorption. A wide range of laboratory tests were performed within the framework of FEBEX (Full-scale Engineered Barrier EXperiment) project to characterize buffer properties and develop numerical models for FEBEX bentonite. Here we present inverse single and dual-continuum multicomponent reactive transport models of a long-term permeation test performed on a 2.5 cm long sample of FEBEX bentonite. Initial saline bentonite porewater was flushed with 5.5 pore volumes of fresh granitic water. Water flux and chemical composition of effluent waters were monitored during almost 4 years. The model accounts for solute advection and diffusion and geochemical reactions such as aqueous complexation, acid-base, cation exchange, protonation/deprotonation by surface complexation and dissolution/precipitation of calcite, chalcedony and gypsum. All of these processes are assumed at local equilibrium. Similar to previous studies of bentonite porewater chemistry on batch systems which attest the relevance of protonation/deprotonation on buffering pH, our results confirm that protonation/deprotonation is a key process in maintaining a stable pH under dynamic transport conditions. Breakthrough curves of reactive species are more sensitive to initial porewater concentration than to effective diffusion coefficient. Optimum estimates of initial porewater chemistry of saturated compacted FEBEX bentonite are obtained by solving the inverse problem of multicomponent reactive transport. While the single-continuum model reproduces the trends of measured data for most chemical species, it fails to match properly the long tails of most breakthrough curves. Such limitation is overcome by resorting to a dual-continuum reactive transport model. 相似文献
40.
Identification of key parameters controlling dissolved oxygen migration and attenuation in fractured crystalline rocks 总被引:1,自引:0,他引:1
In the crystalline rocks of the Canadian Shield, geochemical conditions are currently reducing at depths of 500-1000 m. However, during future glacial periods, altered hydrologic conditions could potentially result in enhanced recharge of glacial melt water containing a relatively high concentration of dissolved oxygen (O2). It is therefore of interest to investigate the physical and geochemical processes, including naturally-occurring redox reactions, that may control O2 ingress. In this study, the reactive transport code MIN3P is used in combination with 2k factorial analyses to identify the most important parameters controlling oxygen migration and attenuation in fractured crystalline rocks. Scenarios considered are based on simplified conceptual models that include a single vertical fracture, or a fracture zone, contained within a rock matrix that extends from the ground surface to a depth of 500 m. Consistent with field observations, Fe(II)-bearing minerals are present in the fractures (i.e. chlorite) and the rock matrix (biotite and small quantities of pyrite). For the parameter ranges investigated, results indicate that for the single fracture case, the most influential factors controlling dissolved O2 ingress are flow velocity in the fracture, fracture aperture, and the biotite reaction rate in the rock matrix. The most important parameters for the fracture zone simulations are flow velocity in the individual fractures, pO2 in the recharge water, biotite reaction rate, and to a lesser degree the abundance and reactivity of chlorite in the fracture zone, and the fracture zone width. These parameters should therefore receive increased consideration during site characterization, and in the formulation of site-specific models intended to predict O2 behavior in crystalline rocks. 相似文献