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651.
从孤岛油田石油污染土壤中分离到一株高效石油降解菌,命名为SKD-1。该菌株菌落表面湿润光滑、边缘整齐、圆形、不透明、乳黄色,能够利用葡萄糖和淀粉作为其生长的碳源和能源,其最适生长环境为碱性(pH8-10),在分别以正十六烷烃和原油为惟一碳源,温度为30℃,摇床(180r/min)培养的条件下,菌株SKD-1的降解率分别为66.1%和36.9%。16SrRNA基因序列分析表明,菌株SKD-1与不动杆菌AcinetobactercalcoaceticusSY-1同源性达99%。结合菌株SKD.1菌落形态、理化性质以及系统发育分析,可以鉴定菌株SKD-1属于不动杆菌属(Acinetobactersp.),序列登录号为AB774229。 相似文献
652.
653.
Triclosan is an antimicrobial agent, an endocrine disrupting compound, and an emerging contaminant in the environment. This is the first study investigating triclosan biodegradation potential of four oxygenase-expressing bacteria: Rhodococcus jostii RHA1, Mycobacterium vaccae JOB5, Rhodococcus ruber ENV425, and Burkholderia xenovorans LB400. B. xenovorans LB400 and R. ruber ENV425 were unable to degrade triclosan. Propane-grown M. vaccae JOB5 can completely degrade triclosan (5 mg L−1). R. jostii RHA1 grown on biphenyl, propane, and LB medium with dicyclopropylketone (DCPK), an alkane monooxygenase inducer, was able to degrade the added triclosan (5 mg L−1) to different extents. Incomplete degradation of triclosan by RHA1 is probably due to triclosan product toxicity. The highest triclosan transformation capacity (Tc, defined as the amount of triclosan degraded/the number of cells inactivated; 5.63 × 10−3 ng triclosan/16S rRNA gene copies) was observed for biphenyl-grown RHA1 and the lowest Tc (0.20 × 10−3 ng-triclosan/16S rRNA gene copies) was observed for propane-grown RHA1. No triclosan degradation metabolites were detected during triclosan degradation by propane- and LB + DCPK-grown RHA1. When using biphenyl-grown RHA1 for degradation, four chlorinated metabolites (2,4-dichlorophenol, monohydroxy-triclosan, dihydroxy-triclosan, and 2-chlorohydroquinone (a new triclosan metabolite)) were detected. Based on the detected metabolites, a meta-cleavage pathway was proposed for triclosan degradation. 相似文献
654.
Erin K. Cameron Inês S. Martins Patrick Lavelle Jérôme Mathieu Leho Tedersoo Mohammad Bahram Felix Gottschall Carlos A. Guerra Jes Hines Guillaume Patoine Julia Siebert Marten Winter Simone Cesarz Olga Ferlian Holger Kreft Thomas E. Lovejoy Luca Montanarella Alberto Orgiazzi Henrique M. Pereira Helen R. P. Phillips Josef Settele Diana H. Wall Nico Eisenhauer 《Conservation biology》2019,33(5):1187-1192
Human activities are accelerating global biodiversity change and have resulted in severely threatened ecosystem services. A large proportion of terrestrial biodiversity is harbored by soil, but soil biodiversity has been omitted from many global biodiversity assessments and conservation actions, and understanding of global patterns of soil biodiversity remains limited. In particular, the extent to which hotspots and coldspots of aboveground and soil biodiversity overlap is not clear. We examined global patterns of these overlaps by mapping indices of aboveground (mammals, birds, amphibians, vascular plants) and soil (bacteria, fungi, macrofauna) biodiversity that we created using previously published data on species richness. Areas of mismatch between aboveground and soil biodiversity covered 27% of Earth's terrestrial surface. The temperate broadleaf and mixed forests biome had the highest proportion of grid cells with high aboveground biodiversity but low soil biodiversity, whereas the boreal and tundra biomes had intermediate soil biodiversity but low aboveground biodiversity. While more data on soil biodiversity are needed, both to cover geographic gaps and to include additional taxa, our results suggest that protecting aboveground biodiversity may not sufficiently reduce threats to soil biodiversity. Given the functional importance of soil biodiversity and the role of soils in human well-being, soil biodiversity should be considered further in policy agendas and conservation actions by adapting management practices to sustain soil biodiversity and considering soil biodiversity when designing protected areas. 相似文献
655.
Jun Li Wentao Li Gan Luo Yan Li Aimin Li 《Frontiers of Environmental Science & Engineering》2019,13(1):6
656.
Yao Zhang Yayi Wang Yuan Yan Haicheng Han Min Wu 《Frontiers of Environmental Science & Engineering》2019,13(1):7
657.
Virender K. Sharma Xin Yu Thomas J. McDonald Chetan Jinadatha Dionysios D. Dionysiou Mingbao Feng 《Frontiers of Environmental Science & Engineering》2019,13(3):37
658.
从培养基配方、菌种来源、激活时间、菌液用量以及检测方式等几个方面对脱氢酶快速毒性检测法进行了改进,确定了整个体系的操作方法。并用HgCl2和NaN3验证了改进后方法的可行性。结果表明,以天然地表水作为菌种来源,转接培养1次后,混合细菌的脱氢酶活性的稳定性便可达到实验要求。样品液与菌液按照6∶1的比例混合效果较好。混合体系在37℃恒温培养箱中激活50min以上细菌可完全活化,最终检测可用普通分光光度计进行。改进后的方法解决了原方法菌液失活过快,实验稳定性较差的问题,同时克服了检测仪器难以购买的问题,使这一方法得以在普通实验室实现。 相似文献
659.
660.
海洋石油降解酵母的分离鉴定与降解特性 总被引:1,自引:0,他引:1
以原油为唯一碳源,采用富集培养、平板涂布分离、平板划线纯化及摇瓶复筛等方法,从表层海水或海泥中分离得到2株具有较强石油降解能力的菌株SYB-5和SYB-2. 根据菌落及菌体形态、生理生化特征和分子生物学分析、鉴定显示,SYB-5为季也蒙毕赤酵母(Meyerozyma guilliermondii/Pichia guilliermondii),SYB-2为长孢洛德酵母(Lodderomyces elongisporus). 对2株酵母菌的石油降解性能的研究结果表明,SYB-5和SYB-2以原油组分作为碳源,以(NH4)2SO4和(NH4)3PO4作为氮源,在ρ(NaCl)为30g/L、氧气充足的条件下,生长的最适温度分别为36和32℃,pH均为7.0. 在最适生长条件下,培养5d后的原油降解率分别达到45.8%和34.4%. 当2株菌混合培养时,培养5d的原油降解率可提高到53.9%,培养8d时达到56.4%,说明2株菌利用原油作碳源生长时具有协同作用. 相似文献