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81.
广东省下庄和南雄铀矿区周围大气环境氡浓度调查 总被引:7,自引:2,他引:5
对广东省下庄和南雄两个铀矿区的大气氡环境地球化学进行了研究.矿区废渣和坑道口释放出来的氡气对周围大气形成了氡污染,特别是在矿区周围1~2km范围内的污染严重.但是空气中的氡污染随着离矿区的距离增大而迅速减弱.矿区周围居民室内氡的浓度高,是广东省室内氡浓度平均值的7~8倍左右.在进行调查的29个居室中,有9个(31%)居室内氡浓度超过美国环境保护局制定的0.15Bq/L室内氡浓度的上限值.居室中氡浓度的升高,除了受矿区释放出来的氡污染外,还因为本地区属高本底辐射区,房基下的土壤、岩石和建筑材料中的铀、镭等放射性元素的含量高,其放射性衰变产生的氡释放出来进入室内. 相似文献
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O.C. Lind B. Salbu L. Skipperud K. Janssens J. Jaroszewicz W. De Nolf 《Journal of environmental radioactivity》2009
A combination of synchrotron radiation based X-ray microscopic techniques (μ-XRF, μ-XANES, μ-XRD) applied on single depleted uranium (DU) particles and semi-bulk leaching experiments has been employed to link the potential bioavailability of DU particles to site-specific particle characteristics. The oxidation states and crystallographic forms of U in DU particles have been determined for individual particles isolated from selected samples collected at different sites in Kosovo and Kuwait that were contaminated by DU ammunition during the 1999 Balkan conflict and the 1991 Gulf war. Furthermore, small soil or sand samples heavily contaminated with DU particles were subjected to simulated gastrointestinal fluid (0.16 M HCl) extractions. Characteristics of DU particles in Kosovo soils collected in 2000 and in Kuwait soils collected in 2002 varied significantly depending on the release scenario and to some extent on weathering conditions. Oxidized U (+6) was determined in large, fragile and bright yellow DU particles released during fire at a DU ammunition storage facility and crystalline phases such as schoepite (UO3·2.25H2O), dehydrated schoepite (UO3·0.75H2O) and metaschoepite (UO3·2.0H2O) were identified. As expected, these DU particles were rapidly dissolved in 0.16 M HCl (84 ± 3% extracted after 2 h) indicating a high degree of potential mobility and bioavailability. In contrast, the 2 h extraction of samples contaminated with DU particles originating either from corrosion of unspent DU penetrators or from impacted DU ammunition appeared to be much slower (20–30%) as uranium was less oxidized (+4 to +6). Crystalline phases such as UO2, UC and metallic U or U–Ti alloy were determined in impacted DU particles from Kosovo and Kuwait, while the UO2,34 phase, only determined in particles from Kosovo, could reflect a more corrosive environment. Although the results are based on a limited number of DU particles, they indicate that the structure and extractability of DU particles released from similar sources (metallic U penetrators) will depend on the release scenarios (fire, impact) and to some extent environmental conditions. However, most of the DU particles (73–96%) in all investigated samples were dissolved in 0.16 M HCl after one week indicating that a majority of the DU material is bioaccessible. 相似文献
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85.
共存离子对地浸废水中铀生物沉淀过程的影响 总被引:1,自引:0,他引:1
采用硫酸盐还原菌生物(还原)沉淀法消除地浸废水中的放射性铀污染,研究了共污染离子Cu(II)、Zn(II)、Fe(III)和SO42-分别对铀生物沉淀过程的影响。序批式实验结果表明,初始Cu(II)浓度低于10mg/L或Zn(II)浓度低于20mg/L时对铀生物沉淀过程影响不大,当Cu(II)浓度超过15mg/L或Zn(II)浓度超过25mg/L时,该过程会因重金属的生物毒性作用受到完全抑制。在含有Fe(III)的氧化环境中,铀生物沉淀过程与Fe(III)还原过程同时进行,但铀沉淀速度相对减慢。初始SO42-浓度低于4000mg/L时对铀生物沉淀过程影响很小,超过5000mg/L时会产生明显的抑制作用,且抑制作用随着SO42-浓度的上升而加强。 相似文献
86.
乌江流域石灰土中铀等元素形态与铀活性 总被引:1,自引:0,他引:1
以中国西南乌江流域石灰土为例,运用逐级提取(Sequential Extraction,SEE)技术,并结合化学成分和相关参数数据,研究了石灰土中铀(U)等元素的形态,并在此基础上探讨了石灰土中U的活动性及释放潜力,旨在增进对U等元素生物地球化学循环的了解,同时也为流域U污染防治提供科学依据。研究结果表明:①石灰土中Mn主要存在于锰(氢)氧化物中,Ca主要存在于碳酸盐和硅酸盐矿物中,P主要存在于硅酸盐矿物和有机质中,U主要赋存于硅酸盐等残留部分中,其次赋存于有机质结合部分和碳酸盐矿物中;②石灰土剖面中活动态U所占的比例为10%~30%,平均17%,说明石灰土中的部分U在酸性和氧化-还原界面等条件下具有一定的迁移活性,即在上述条件下,石灰土中的部分U可释放进入周围水体或植物中;③石灰土中U的潜在释放量为036~150 g/t,平均U潜在释放量为076 g/t,因此,在酸雨和侵蚀等作用下,石灰土U释放可显著提高乌江河水U通量。 相似文献
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Ralph L. Seiler 《Journal of the American Water Resources Association》1996,32(6):1233-1245
ABSTRACT: From 1986 to 1993, the National Irrigation Water-Quality Program (NIWQP) of the U.S. Department of the Interior studied whether contamination was induced by irrigation drainage in 26 areas of the Western United States. In 1992, a study to evaluate and synthesize data collected during these 26 investigations began. Selenium, boron, and molybdenum are the trace elements and DDT the pesticide most commonly found in surface water at concentrations exceeding chronic criteria for the protection of aquatic life. In six of the areas, the median selenium concentration exceeded the criterion. Aquatic-life criteria have not been developed for uranium, but the median uranium concentration exceeded the proposed Maximum Contaminant Level for drinking water in seven areas. A principal components analysis indicates that severity of selenium contamination is not related to the severity of contamination by boron, molybdenum, and arsenic. Arsenic, boron, molybdenum, and selenium concentrations are nearly the same in both filtered and unfiltered samples, which indicates that contaminant concentrations in filtered samples can be directly compared with biological-effects data developed using unfiltered samples. At a given site, selenium concentrations in surface water can change by an order of magnitude during the course of a year and from one year to another. 相似文献
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