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241.
以盘塘红壤实验区为例,在阐明湘北环湖低丘红壤区土壤形成、类型及特性的基础上,提出了综合开发利用该区土壤资源的措施和途径。 相似文献
242.
Forrest E. Dierberg 《Environmental management》1992,16(3):371-380
Following a period of prolonged drought or intentional lake level drawdown, large littoral areas that once contained submersed
aquatic vegetation (SAV) are reinundated when lake levels rise. A complete assessment of the contribution made by decomposing
SAV to the in-lake phosphorus (P) concentration is important in both the management of Lake Okeechobee and understanding basic
P processes. The P contribution to the open waters of Lake Okeechobee from a rapid inundation of exposed SAV was calculated
by four methods: cores of field-desiccated SAV, cores of lab-desiccated SAV in the presence and absence of sediments, in situ
decomposition, and sequential macrophyte harvesting. P releases, given such an episodic event, were similar among the four
methods, ranging from 116±48 to 384±528 mg/m2 in the absence of sediment. When SAV is in contact with sediment, which is the realistic field situation, the amount of P
released was four times less (30±14 mg/m2) than in the absence of sediment. The calculated P releases would result in total P concentration increases in the lake from
2 to 15 μg/liter (upper 95% CI=2–25 μg/liter) in the absence of sediment; only 1 μg/liter increase was predicted when SAV
released P in contact with sediment. Thus it is unlikely that a significant rise in total P concentrations in the limnetic
zone of the lake would occur from the export of P released during the desiccation of SAV in the littoral-marsh zone during
a drawdown. 相似文献
243.
F. Douglas Shields 《Journal of the American Water Resources Association》1991,27(3):527-536
ABSTRACT: Stability of vegetated and bare riprap revetments along a Sacramento River reach during the flood of record was assessed. Revetment damages resulting from the flood were identified using records provided by the U.S. Army Corps of Engineers and verified by contacts with local interests. Vegetation on revetments along a 35.6-mile reach was mapped using inspection records and stereo interpretation of aerial phoths taken shortly before and after the flood. A follow-up field inspection was conducted in September 1989. Revetment age, material, bank curvature, vegetation, and damage were mapped from a boat. Mapping results from both 1986 and 1989 were placed in a data base. About 70 percent of the bank line of the study reach was revetted. About two-thirds of the revetment was cobble; one-third was quarry stone. Revetment vegetation varied from none to large (> 50-inch diameter) cotton-woods. About 10 percent of the revetted bank line supported some type of woody vegetation. Damage rates for revetments supporting woody vegetation tended to be lower than for unvegetated revetments of the same age located on banks of similar curvature. Chisquared tests indicated damage rates were greater for older (pre-1950 construction) revetments, but were unable to detect differences based on vegetation or bank curvature. Research is needed to generate design criteria and construction techniques to allow routine use of woody plants in bank protection structures. 相似文献
244.
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
245.
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
246.
本文论证了中国海域基底与邻区古构造演化关系,中朝地台与京畿地块以北对应。中下扬子台拗东延为朝南古拗陷,东南地槽系连接本州地槽系,华夏地块经东海接日本“南方大陆”,华夏和印支地块隶属于南海—东海地台的边缘地块。 相似文献
247.
248.
249.
断裂带工程边坡地质条件复杂,稳定性差,治理工程失效事例已日益引起人们关注,本文以滇中某高速公路在断裂带中的边坡为实例,分析了断裂带边坡变形的原因、治理措施和治理对策。 相似文献
250.