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81.
Ghoramara Island is located ca. 150 km south of Kolkata, Bay of Bengal, India, in the Sundarban Delta complex. This sparsely
populated island is suffering from severe coastal erosion and areal reduction for the last three decades, which results in
the loss of major areas on the northwest coast. Both numerous households and a significant area of agricultural land and coastal
stretches for fish drying have been lost. This has rendered thousands of people homeless as ‘environmental refugess’. In the
present paper an attempt is made to study the erosion and accretion process through time series analysis using a GIS technique.
Also, a study of remedial measures to protect the island using a ‘bio-engineering’ technique is reported in this paper. It
has been shown that, in the absence of protection measures, the eastern shore will merge with the Indian mainland during the
next 25 years, while the western part will be completely washed off. 相似文献
82.
The Patagonian coast is considered a relatively pristine environment. However, studies conducted along coastal Patagonia have
showed hydrocarbon pollution mostly concentrated at ports that have fishing, oil loading, general merchant, and/or tourist
activities. A high value of total aliphatic hydrocarbons (TAH) was found at the Rawson fishing port (741 μg/g dw). In other
ports with and without petroleum-related activities, hydrocarbon values were approximately 100 μg/g dw. The highest values
for TAH and total aromatic hydrocarbons (TArH) were found in Faro Aristizábal, north of San Jorge gulf (1304 and 737 μg/g
dw, respectively). This is very likely the result of petroleum-related activities at the Comodoro Rivadavia, Caleta Cordova,
and Caleta Olivia ports located within this gulf. In other coastal areas away from potential anthropogenic sources, hydrocarbon
values were less than 2 and 3 μg/g dw for TAH and TArH, respectively. This review of published and unpublished information
suggests that ports are important oil pollution sources in the Patagonian coast. More detailed studies are needed to evaluate
the area affected by port activities, to understand the mechanisms of hydrocarbon distribution in surrounding environments,
and to assess bioaccumulation in marine organisms. Despite that some regulations exist to control oil pollution derived from
port and docked vessel activities, new and stricter management guidelines should be implemented. 相似文献
83.
海洋气溶胶对沿海地区降水组成的贡献 总被引:2,自引:0,他引:2
以青岛地区为对象,对沿海地区大气气溶海洋因子对降水组成的贡献,进行了研究分析。结果表明,1)夏季受海洋影响要比冬季明显得多;(2)降水中主要的碱性物质,不论是夏季或冬季,99%来自大陆气溶胶,海洋的影响可忽略;(3)海洋影响的程度和离海边的距离有关,离海愈远,受海洋影响就愈小,离海愈近,受其影响就愈大。 相似文献
84.
盐城海岸湿地资源环境压力与生态调控响应 总被引:21,自引:0,他引:21
江苏盐城海岸湿地拥有以保护丹顶鹤和麋鹿为特色的两个国家级自然保护区。然而强烈的人类活动贯穿于海岸湿地发育的每一个阶段,包括湿地围垦、资源酷取滥采以及环境污染等,使得该区资源环境面临的压力不断增大。通过对其资源环境特征、人口经济发展压力、湿地不合理开发利用压力以及水资源污染压力的分析,进而利用生态调控设计相应的政策措施响应方案,包括生态规划与设计---科学的生态功能区划,调整若干原缓冲区中生物多样性热点区为核心区;生态工程---生境更新与调整,建立人工湿地生态工程、芦苇生态工程、生态旅游等生态示范区;生态系统管理与能力建设---社区共管,与周围社区居民建立有效的伙伴关系。 相似文献
85.
S. J. Ursic 《Journal of the American Water Resources Association》1991,27(2):303-315
ABSTRACT: Hydrologic responses to logging with skidders and responses to logging with a cable yarder are compared. After a 23-year calibration with an undisturbed control catchment, mixed stands of shortleaf pine (Pinus echinata Mill.) and hardwoods were clearfelled on two small catchments in the hilly Coastal Plain of north Mississippi and observed for five years. Runoff increased 370 mm (skidded) and 116 mm (yarded) during the first year with 1876 mm of rainfall, and 234 mm (skidded) and 228 mm (yarded) during the second year when 1388 mm of precipitation equaled the calibration mean. Sediment concentrations for the yarded catchment during the first two years averaged 641 and 1,629 mg L?1, respectively, and yields were 6,502 and 12,086 kg ha?1. Compared to calibration means of 74 mg L?1 and 142 kg ha?1, these extreme values can be attributed largely to transport of sediment stored in the channel and to erosion of subsurface flow paths, which was exacerbated by high flow volumes. During the first year, the concentration (231 mg L?1) and yield (2,827 kg ha?1) for the control catchment also exceeded the calibration means. However, concentrations (134 mg L?1) and yields (1,806 kg ha?1) for the skidded catchment were about 40 percent lower than for the control catchment during the first year, and were higher than those for the control only during the second year. Because deep percolation was limited and because rainfall was unusually high, increases in flows and sediment concentrations and yields probably approximate maximum responses to clearcut harvesting in the uplands of the southern Coastal Plain. 相似文献
86.
The threat of man-induced global change on the nations of the South Asian seas region varies from place to place because of
differences in exposure to monsoons and stoms, differences in local tectonics and subsidence, and variations in air and sea
climates. Because several nations are involved, some having subsistence budgets, and given the cost of deriving independently
a comprehensive response to global change, the similarities and differences between national settings must be identified soon.
These comparisons will form the basis for local response strategies: the similarities provide a basis for responses similar
to that of other nations and the differences provide for local adaptation. That climate change on the South Asian coastal
region will have an impact is certain: its economics, environment, and coastal land uses are dominated to a certain extent
by this marine influence. The extent of these impacts, however, is uncertain. Accompanying global change will be changes in
sea level, differences in storm climate, and altered precipitation patterns; science cannot define today what pattern these
changes will take. Because global change is inevitable—although its magnitude, timing, and geographic distribution are unknown—the
South Asian seas region should begin the appropriate research and planning studies to set forth a reasoned response to global
change, for implementation when scientific evidence for global change is more quantitative. 相似文献
87.
We inventoried wetland impoundments in the Louisiana, USA, coastal zone from the late 1900s to 1985. Historically, impoundment
of wetlands for reclamation resulted in direct wetland loss after levees (dikes) failed and the impounded area was permanently
flooded, reverting not to wetland, but to open-water habitat. A current management approach is to surround wetlands by levees
and water control structures, a practice termed semi-impoundment marsh management. The purpose of this semi-impoundment is
to retard saltwater intrusion and reduce water level fluctuations in an attempt to reduce wetland loss, which is a serious
problem in coastal Louisiana. In order to quantify the total impounded area, we used historic data and high-altitude infrared
photography to map coastal impoundments. Our goal was to produce a documented inventory of wetlands intentionally impounded
by levees in the coastal zone of Louisiana in order to provide a benchmark for further research.
We inventoried 370,658 ha within the coastal zone that had been intentionally impounded before 1985. This area is equal to
about 30% of the total wetland area in the coastal zone. Of that total area, approximately 12% (43,000 ha) is no longer impounded
(i.e., failed impoundments; levees no longer exist or only remnants remain). Of the 328,000 ha still impounded, about 65%
(214,000 ha) is developed (agriculture, aquaculture, urban and industrial development, and contained spoil). The remaining
35% (114,000 ha) of impoundments are in an undeveloped state (wetland or openwater habitat). In December 1985, approximately
50% (78,000 ha) of the undeveloped and failed impoundments were open-water habitat. This inventory will allow researchers
to monitor future change in land-water ratios that occur within impounded wetlands and thus to assess the utility of coastal
wetland management using impoundments. 相似文献
88.
A. Jarernpornnipat O. Pedersen K. R. Jensen S. Boromthanarat S. Vongvisessomjai P. Choncheanchob 《Journal of Coastal Conservation》2003,9(2):135-146
Bandon Bay (Surat Thani Province) is one of the most productive coastal areas in southern Thailand. The Tapi River and 18
channels are the main sources of freshwater, nutrients, organic matter and sediment to the bay and the loading of freshwater
and nutrients provide essential support for the production of phytoplankton in the estuarine ecosystem. Bandon Bay is important
as natural spawning, nursery and feeding grounds for shellfish such as oysters, blood cockles, green mussels, short-necked
clams, mud crabs and shrimps, and the estuary also serves as an excellent area for mariculturing of shellfish. In fact, oysters
and blood cockles cultured in Bandon Bay are now being exported worldwide. However, Bandon Bay is also a textbook example
of overexploitation of coastal resources in the tropics including all the derived changes in the estuarial ecosystem with
severe socio-economic consequences. Hence, there is an urgent need for setting up an integrated management plant for a sustainable
use of shellfish resources in Bandon Bay. The present study attempts to integrate water quality simulation results, socio-economic
data and information on existing shellfish resource use in the process of proposing a set of sustainable management strategies
for shellfish resources in Bandon Bay. These strategies involve: (1) using water quality modeling to monitor ecological and
environmental changes in shellfish culture beds and their natural habitats in the process of setting up a master plan for
management of waste water discharge into Bandon Bay; (2) zoning of shellfish mariculture in the coastal area in order to solve
conflicts between resource users; (3) setting up a clear system for taxation of mariculture where the revenue may be used
for (4) setting up and managing mangrove strips as filters of pollution and sediment around Bandon Bay; and finally (5) it
is suggested to form a committee with members representing all relevant stakeholders plus the local government in order to
work on resolving the existing and potential future conflicts over resource usage in Bandon Bay. This methodology may be seen
as an important contribution towards a Bandon Bay sustainable management approach, based on the principles of integrated coastal
zone management because it is science-based and takes into consideration the needs and perceptions of people involved in coastal
resource extraction. 相似文献
89.
Aušrinė Armaitienė Vadim L. Boldyrev Ramūnas Povilanskas Julius Taminskas 《Journal of Coastal Conservation》2007,11(1):13-22
The varied and very dynamic landscape with a high biological diversity is a distinctive feature of the Curonian spit at the
regional scale. Throughout the 20th century the main morphodynamic trend in the littoral of the Curonian spit was shoreline
grading on the lagoon side, whereas on the marine side the increasing erosion at the foot of the spit, and increasing accretion
at the head of the spit prevailed. The results of a discriminant analysis (Wilkes’ λ = 0.001626 and F = 29.267 when p < 0.001) show that sites with prevailing erosion, accretion and sediment input from the drifting dunes form regular inter-related
spatial structures in the littoral with distinctive resulting discontinuities of the sediment drift along the lagoon coast.
Dune littoral cells are characterized by Aeolian sediment input and distribution ‘down-drift’, (usually northwards) from the
source. The most likely changes in the current development trends of the lagoon shore zone of the Curonian spit are related
to expected climate changes and further slowing down of the dune drift. The probability of storms and ice-drift events, and
their impact on coasts is expected to increase as a result of climate change. The dune advance will gradually slow down, and
with it, the sand input to the coastal zone will decline. In this paper, we define integrated shoreline management as a system
of long-term shoreline management measures, which is based on a littoral cell approach and aimed at harmonizing human activity
in the coastal zone with the natural development of the shoreline. We propose an integrated management program for the lagoon
shoreline of the Curonian spit, which is site-specific for each littoral cell as a coastal management unit. Drifting dunes
and seaside beaches are the natural amenities, which are best known and best appreciated on the Curonian spit by 49% of the
respondents representing the total Lithuanian population. A responsible tourism development should be considered as the key
means for proper appreciation of the drifting dunes and natural coasts by society, which means to acknowledge and cherish
the aesthetic and conservation values of dune and coastal landscapes of the Curonian spit as a World Heritage Site. There
are at least two pre-conditions for this: (1) to provide visitors with sufficient information about diverse values and functions
of the Curonian dunes and coasts within a broader regional and global heritage conservation context; (2) to enable tourists
to enjoy the most impressive dune and coastal landscapes at close range. In this paper we propose to encourage active dune
tourism, to reintroduce grazing into the Curonian dune areas, to restore and to preserve the most impressive landscapes of
the highest white drifting dunes by bringing the blown out sand from the leeward foot of the dunes back to the crest artificially. 相似文献
90.
The coastal city of Tel Aviv was founded at the beginning of the 20th century. The number of its inhabitants and its water consumption increased rapidly. This study analyses a 15-year record (1934-1948) of pre-industrial development of groundwater chemistry in the urban area. Archive data on concentrations of major ions, dissolved gases (CO2 and O2), organic matter, and pH were available for each half-year during the period of 1934-1948. The major factors causing changes in the chemistry of groundwater flowing in three sandy sub-aquifers have been seawater encroachment due to overpumping, and infiltration of effluents from pit-latrine collectors. Influence of these factors decreases with depth. Landward-penetrating seawater passed through clayey coastal sediments, interbedded among sands and calcareous sandstones, and spread into the Kurkar Group aquifer. This has led to exchange of sodium (dominant in seawater) with calcium adsorbed on clay particles, enriching groundwater with calcium. Intensity of cation exchange decreases inland and with depth. Infiltration of pit-latrine effluents has introduced large amounts of ammonium into the unsaturated zone. Its rapid oxidation in unsaturated sediments has caused massive nitrate production, accompanied by pore-water acidification. This process induces dissolution of vadose carbonate, resulting in enrichment of groundwater recharge in calcium. Anthropogenically induced dissolution of calcite in the unsaturated zone has been the major factor for the increase of Ca2+ concentration in groundwater, accounting for about 80% of this increase. In the interface zone, an additional 20% of calcium has been supplied by cation exchange. Owing to pH increase caused by denitrification in the aquifer, Ca(2+)-rich waters supersaturated with calcite could be formed, especially in the capillary fringe of the uppermost sub-aquifer, which could induce calcite precipitation and ultimately lead to the cementation of sandy aquifers. Urban development has caused drastic changes in the gas content in the unsaturated zone and in groundwater. Carbon dioxide was intensively generated by nitrification-denitrification processes, by hydration of urea, to a lesser degree by oxidation of organic matter, and probably by anoxic biodegradation of organics. Between 1934 and 1948, concentrations of CO2 in unsaturated sediment air rose from 3.2% to 7.6%. In the unsaturated zone, oxygen consumption for oxidation of ammonium and organic matter lowered O2 concentrations in sediment air to unusually low values of 3.9-12.9%. Nitrification in the urban unsaturated zone could thus serve as a pump, sucking in atmospheric oxygen at a rate of about 0.3-0.5 g m-2 day-1. The extreme concentrations of CO2 and O2 in unsaturated sediments have been preserved due to production and consumption of gas under conditions of diminishing areas open to the atmosphere, uncovered by buildings and by roads. 相似文献