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101.
Microbial reactions play an important role in regulating pore water chemistry as well as secondary mineral distribution in many subsurface systems and, therefore, may directly impact radionuclide migration in those systems. This paper presents a general modeling approach to couple microbial metabolism, redox chemistry, and radionuclide transport in a subsurface environment. To account for the likely achievement of quasi-steady state biomass accumulations in subsurface environments, a modification to the traditional microbial growth kinetic equation is proposed. The conditions for using biogeochemical models with or without an explicit representation of biomass growth are clarified. Based on the general approach proposed in this paper, the couplings of uranium reactions with biogeochemical processes are incorporated into computer code BIORXNTRN Version 2.0. The code is then used to simulate a subsurface contaminant migration scenario, in which a water flow containing both uranium and a complexing organic ligand is recharged into an oxic carbonate aquifer. The model simulation shows that Mn and Fe oxyhydroxides may vary significantly along a flow path. The simulation also shows that uranium(VI) can be reduced and therefore immobilized in the anoxic zone created by microbial degradation. 相似文献
102.
Kun Li Tingming Ye Wang Zhang Jianfeng Peng Yaohui Bai Weixiao Qi Huijuan Liu 《Frontiers of Environmental Science & Engineering》2022,16(2):17
103.
Yanfeng Yang Ruina Zhang Ziyang Lou 《Frontiers of Environmental Science & Engineering》2022,16(12):158
104.
Shuqin Liu Rui Wu Xi Yang Shuting Fang Zhangmin Xiang Shenghong Yang Gangfeng Ouyang 《Frontiers of Environmental Science & Engineering》2022,16(9):116
105.
Cho ST Tsai SH Ravindran A Selvam A Yang SS 《Environmental geochemistry and health》2008,30(3):255-272
To investigate the seasonal variations of microbial ecology in grassland of Tatachia forest, soil properties, microbial populations,
microbial biomass, and 16S rDNA clone library analysis were determined. The soil had temperatures 6.6–18.4°C, pH 3.6–5.1,
total organic carbon 1.11–10.68%, total nitrogen 0.18–0.78%, and C/N ratios 3.46–20.55. Each gram of dry soil contained bacteria,
actinomycetes, fungi, cellulolytic, phosphate-solubilizing microbes, and nitrogen-fixing microbes 4.54 × 104 to 3.79 × 107, 3.43 × 102 to 2.17 × 105, 5.74 × 103 to 3.76 × 106, 1.97 × 103 to 1.34 × 106, 8.49 × 102 to 5.59 × 105, and 3.86 × 102 to 3.75 × 105 CFU, respectively. Each gram of soil contained 117–2,482 μg of microbial biomass carbon, 23–216 μg of microbial biomass nitrogen
and 9–29 μg of DNA. The microbial populations, microbial biomass, and DNA decreased stepwise with the depth of soil, and they
had low values in winter seasons. The microbial populations, microbial biomass carbon, microbial biomass nitrogen, and DNA
at the BW2 horizon were 8.42–17.84, 19.26–64.40, 16.84–61.11, and 31.03–46.26% of those at the O horizon, respectively. When
analyzing 16S rDNA library, members of Proteobacteria, Acidobacteria, Actinobacteria, Bacteroidetes, Chloroflexi, Firmicutes,
candidate division TM1, candidate division TM7, Gammatimonadetes, and Verrucomicrobia were identified. Members of Proteobacteria
(44.4%) and Acidobacteria (33.3%) dominated the clone libraries. Within the phylum Proteobacteria, α-, β-, and γ-Proteobacteria
were most numerous, followed by δ-Proteobacteria. 相似文献
106.
以FeSO4、MgO和H2SO4为原料,制备了新型镁铁复合絮凝剂(PFMS),考察了PFMS的结构和Fe(Ⅲ)分布形态,为了考察自制PFMS、自制聚合硫酸铁(PFS)与工业PFS产品的絮凝性能差别,选择高岭土模拟浊度废水、直接耐晒黑G模拟染料废水和焦化废水生化出水,分别进行了去除浊度、色度和COD的絮凝实验.结果表明,Mg2+未参与聚合过程,但引入Mg2+提高了PFMS的稳定性.PFMS对浊度去除效果略高于自制PFS和工业PFS,余浊<5NTU;在碱性条件下,PFMS的脱色率、COD去除率高于自制PFS和工业PFS. 相似文献
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