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611.
The mercury removals by existing pollution control devices in four coal-fired power plants of China were carried out based on a measurement method with the aluminum matrix sorbent. 相似文献
612.
Heterogeneous oxidation of gas-phase Hg0 by nano-Fe2O3 was investigated on a fixed bed reactor, and the e ects of oxygen
concentration, bed temperature, water vapour concentration and particle size have been discussed. The results showed that Hg0 could
be oxidized by active oxygen atom on the surface of nano-Fe2O3 as well as lattice oxygen in nano-Fe2O3. Among the factors that
a ect Hg0 oxidation by nano-Fe2O3, bed temperature plays an important role. More than 40% of total mercury was oxidized at 300°C,
however, the test temperature at 400°C could cause sintering of nano-catalyst, which led to a lower e ciency of Hg0 oxidation. The
increase of oxygen concentration could promote mercury oxidation and led to higher Hg0 oxidation e ciency. No obvious mercury
oxidation was detected in the pure N2 atmosphere, which indicates that oxygen is required in the gas stream for mercury oxidation. The
presence of water vapour showed di erent e ects on mercury oxidation depending on its concentration. The lower content of water
vapour could promote mercury oxidation, while the higher content of water vapour inhibits mercury oxidation. 相似文献
613.
TGM measurements on board ships have proved to provide valuable complementary information to measurements by a ground based monitoring network. During the third China Arctic Research Expedition (from July 11 to September 24, 2008), TGM concentrations over the marine boundary layer along the cruise path were in-situ measured using an automatic mercury vapor analyzer. Here we firstly reported the results in Japan Sea, North Western Pacific Ocean and Bering Sea, where there are rare reports. The value ranged between 0.30 and 6.02 ng/m3 with an average of (1.52 ± 0.68) ng/m3, being slightly lower than the background value of Northern Hemisphere (1.7 ng/m3). Notably TGM showed considerably spatial and temporal variation. Geographically, the average value of TGM in Bering Sea was higher than those observed in Japan Sea and North Western Pacific Ocean. In the north of Japan Sea TGM levels were found to be lower than 0.5 ng/m3 during forward cruise and displayed obviously diurnal cycle, indicating potential oxidation of gaseous mercury in the atmosphere. The pronounced episode was recorded as well. Enhanced levels of TGM were observed in the coastal regions of southern Japan Sea during backward cruise due primarily to air masses transported from the adjacent mainland reflecting the contribution from anthropogenic sources. When ship returned back and passed through Kamchatka Peninsula TGM increased by the potential contamination from volcano emissions. 相似文献
614.
Two ornithogenic sediment cores, which have a time span of 1000 years and are influenced by red-footed booby (Sula sula), were collected from Dongdao Islands, South China Sea. The determined mercury concentrations of the two cores show similar and substantial fluctuations during the past millennium, and the fluctuations are most likely caused by the changes in mercury level of the ocean environment and in anthropogenic Hg emission. For the past 500 years, the mercury concentration in the red-footed booby excrement has a striking association with global anthropogenic mercury emission. The mercury concentration increased rapidly after AD 1600 in corresponding to beginning of the unparalleled gold and silver mining in South Central America that left a large volume of anthropogenic mercury pollution. Since the Industrial Revolution, the mercury level has increased at a fast pace, very likely caused by modern coal combustion, chlor-alkali and oil refining industries. The comparison of mercury profiles from different places on earth suggested that anthropogenic mercury pollution after the Industrial Revolution is more severe in Northern Hemisphere than in Antarctica. 相似文献
615.
Leaf litterfall plays an important role in transporting atmospheric mercury to soil in forests area. 相似文献
616.
617.
618.
通过在氧化钙中加入氧化性物质三氯化铁,制成混合型吸附剂在固定床中分别在20℃,80℃,140℃的实验条件下,进行吸附反应。实验结果为单纯的氧化钙吸附剂在20℃,80℃,140℃下对汞蒸汽的穿透率分别为80%,85%,90%,穿透平衡时间在25分钟左右,随着温度的升高穿透率越高吸附效率越低,温度升高不利于吸附反应,而混合型吸附剂中含三氯化铁为5%的吸附剂,在20℃,80℃,140℃下,对汞蒸汽的平衡穿透率分别60%,40%,30%,吸附效率比单独的氧化钙吸附剂有大幅度提高,除了进行物理吸附还发生了化学吸附,温度的升高有利于吸附反应的进行,平衡穿透时间提高到50分钟左右。 相似文献
619.
采用RA-915^+型汞分析仪对海水中的总汞进行了测试。进行了线性关系、检出限、准确度、精密度、回收率等实验。实验结果表明,本方法检出限0.00002mg/L,在0—40000Pg范围内线性良好。本方法操作简单,灵敏度高,结果准确。 相似文献
620.
文章研究了粉煤灰在热处理过程中汞的逸出规律,通过改变焙烧温度、焙烧时间和通气流量等条件,利用安大略水法,对逸出的零价汞(Hg0)和二价汞(Hg2+)以及总汞的含量进行了测定。结果表明:在加热温度达到400℃时,飞灰中的可挥发汞已基本完全释放,逸出量大约为0.2μg/g。当加热温度升高到600~1 000℃之间时,零价汞含量明显降低,而二价汞含量明显升高,可以观察到较为明显的零价汞氧化为二价汞的现象。汞的逸出量与氧化程度主要与加热温度有关,而加热时间与通气量的影响相对较小。在1 000℃,加热时间30 min,通气量0.5 L/min的条件下,可挥发汞将完全逸出并有部分零价汞被氧化。结合上述研究结果,在对粉煤灰进行加热处理时,需要对其中汞的二次释放现象加以重视并采取相应的控制措施。 相似文献