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821.
Lars Håkanson 《Environmental Modeling and Assessment》2003,8(4):275-283
This work exemplifies how a given lake (Lake Huljesjön, Sweden) would likely respond to changes in pH-values and to liming (a standard measure against anthropogenic acidification). The basic questions are: How would a liming influence pH? How long would the changes last? How would the changes influence the structure and function of lake ecosystems? The work uses a comprehensive lake ecosystem model, LakeWeb, which accounts for production, biomasses, predation, abiotic/biotic interactions of nine key functional groups of organisms, phytoplankton, bacterioplankton, two types of zooplankton (herbivorous and predatory), two types of fish (prey and predatory), zoobenthos, macrophytes and benthic algae. LakeWeb is a dynamic model and gives weekly variations. It has been critically tested using empirical data and regressions from many lakes. Those tests are not presented here but have shown that the model can capture typical functional and structural patterns in lakes very well. This gives credibility to the results presented in this work, which would be very costly to obtain in the traditional manner by extensive field studies in one or a few lakes. This work presents for the first time predictions at the ecosystem level of how functional groups of organisms (and not individual species) are likely to respond to acidification and liming. Two existing dynamic models, one for liming, the other for Hg-concentrations in fish, have been added to the LakeWeb-model. These two models have previously been tested and proven to yield good predictions. The results presented here indicate that there are several probable changes in the structure and function of the lake foodweb related to acidification and liming. The predicted changes in macrophyte cover will influence the predation pressure on fish, and thereby the fish biomass. Reductions in primary production at low pH-values will cause reductions in fish biomass. There are several interesting compensatory effects between factors that increase fish biomass and factors that tend to decrease the biomass. Such matters can be handled quantitatively by the LakeWeb-model. 相似文献
822.
40多年来秦皇岛市气候发生了明显的变化,致使农业气象灾害增加:第一,冬暖、倒春寒、春末高温等灾害频次增多,冬季低温冻害频次和程度减少;第二,冬旱、春旱、秋旱、秋冬连旱、冬春连旱增多,伏旱次数明显减少,盛夏洪涝频次减少;第三,低温连阴雨、高温干旱、干热风等灾害在频次和程度上均发生明显变化。因此,秦皇岛农业生产防灾减灾的重点和方法也适当调整。 相似文献
823.
824.
825.
成都市区植被变化的遥感动态监测 总被引:4,自引:1,他引:4
利用1987年和2000年的TM影像,对成都市区植被动态变化进行了分析.首先, 利用1:25万数字地形图对2000年的TM影像进行几何校正,并将1987年的TM影像与其配准.其次,利用TM影像的第四和第三波段计算植被指数,根据植被指数提取植被.第三,对成都市区1987~2000年的植被进行了动态变化分析.研究表明,1987~2000年成都市区植被有增有减,但总的趋势是减少:增加部分集中在老城区,是人工绿化的结果;减少部分主要集中在市区西北和西南的面状区域以及因城市道路扩展而占用的线状区域,这是城市化的必然结果. 相似文献
826.
Duane A. Wells Paul F. Doyle 《Journal of the American Water Resources Association》2004,40(2):477-483
ABSTRACT: Snow course surveys in late winter provide stream‐flow forecasters with their best information for making water supply and flood forecasts for the subsequent spring and summer runoff period in mountainous regions of western North America. Snow survey data analyses are generally based on a 30‐year “normal” period. It is well documented that forest cover changes over time will affect snow accumulation on the ground within forests. This paper seeks to determine if forest cover changes over decades at long term snow courses decrease measured peak snow water equivalent (SWE) enough to affect runoff prediction. Annual peak SWE records were analyzed at four snow courses in two different forest types having at least 25 years of snowpack data to detect any decreases in SWE due to forest growth. No statistically significant decreases in annual peak SWE over time were found at any of these four snow courses. The wide range of annual winter precipitation and correspondingly highly variable peak snowpack accumulation, as well as many other weather and site variables, masked any minor trends in the data. 相似文献
827.
James W. Hornbeck 《Journal of the American Water Resources Association》1975,11(6):1257-1260
ABSTRACT: Experimental cuttings on two small, hardwood-forested watersheds in New England showed that annual streamflow can be increased as much as 41 percent. Most of the increase occurred in summer and early autumn when additional streamflow is most needed. Revegetation caused the annual increases to nearly disappear within 4 years after complete forest clearing. 相似文献
828.
陕西未来50年区域旱涝气候预测研究 总被引:7,自引:0,他引:7
用陕西省近526a的旱涝等级资料,根据超低频气候振动理论和尺度对应原理,通过旱涝气候对天体物理、太阳活动等周期,特别是ENSO对天体物理显著敏感的周期响应关系的物理统计分析,选取周期概率显著的周期,进行外延叠加集成预测,给出了未来50a陕西省不同区域旱涝趋势的预测结果. 相似文献
829.
The physical properties of corn starch loose-fill were examined at various relative humidities (r.h.). After 48 h of storage at both 25 and 50% r.h., only a slight change in the dimension and physical properties of the corn starch loose-fill was apparent. A wet environment (75% r.h. for 48 h), however, caused significant shrinkage and the loss of physical properties. The tensile properties, particularly tensile modulus, sharply increased, while the resilience gradually decreased with storage time. Amorphous X-ray diffraction patterns of corn starch loose-fills were transformed into crystalline patterns due to aging at 75% r.h. after 48 h. These changes were attributed to the structural relaxation, which was accelerated by moisture gain. The T
g of corn starch loose-fill decreased with increasing the moisture content in expanded starch. Our proposed model based on Avrami equation was able to describe the time-dependent recrystallization of corn starch by modifying the time-dependent tensile modulus. The growth parameter (n) and time constant (k) for the recrystallization process of corn starch loose-fill were about 3.2 and 8.87 × 10–18 s–1, respectively. If the growth parameter of 3.2 is considered, spherulitic growth of crystallization occurred in the corn starch loose-fill in the wet environment. 相似文献
830.
以四川大竹拱桥坝锶矿床为例,探讨了开放构造系低温矿床可能具有的某些重要特征。指出了低温矿床的矿石矿物组合及围岩蚀变简单;矿床具隐蔽垂向分带;成矿作用发生于浅成环境;浅层大气降水与深层建造水的混合导致了矿质的沉淀。 相似文献