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Seepage from Hg mine wastes and calcines contains high concentrations of mercury (Hg). Hg pollution is a major environmental
problem in areas with abandoned mercury mines and retorting units. This study evaluates factors, especially the hydrological and
sedimentary variables, governing temporal and spatial variation in levels and state of mercury in streams impacted by Hg contaminated
runo . Samples were taken during di erent flow regimes in theWanshan Hg mining area in Guizhou Province, China. In its headwaters
the sampled streams/rivers pass by several mine wastes and calcines with high concentration of Hg. Seepage causes serious Hg
contamination to the downstream area. Concentrations of Hg in water samples showed significant seasonal variations. Periods of
higher flow showed high concentrations of total Hg (THg) in water due to more particles being re-suspended and transported. The
concentrations of major anions (e.g., Cl??, F??, NO3?? and SO4
2??) were lower during higher flow due to dilution. Due to both sedimentation
of particles and dilution from tributaries the concentration of THg decreased from 2100 ng/L to background levels (< 50 ng/L) within
10 km distance downstream. Sedimentation is the main reason for the fast decrease of the concentration, it accounts for 69% and 60%
for higher flow and lower flow regimes respectively in the upper part of the stream. Speciation calculation of the dissolved Hg fraction
(DHg) (using Visual MINTEQ) showed that Hg(OH)2 associated with dissolved organic matter is the main form of Hg in dissolved
phase in surface waters in Wanshan (over 95%). 相似文献
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聚β羟基烷酸盐(PHA)以其较好的生物相容性、可生物降解性和再生性成为最有前途的生物高分子材料.本文基于甘油作为基质在饱食-饥饿模式下富集合成PHA的混培物,以乙酸、丙酸、丁酸、乳酸和葡萄糖作为基质考察混培物合成PHA的基质广谱性,结果表明乳酸和乙酸作为基质时PHA的产率系数较高;使用不同比例乙酸/丙酸混合基质时,PHA产量随着乙酸含量的增加而增大,乙酸/丙酸为3∶1时PHA产量最高.通过活性污泥同时贮存与生长模型模拟与线性回归两种方法证实,在单一基质或乙酸/丙酸混合基质情况下,PHA合成速率与OUR存在线性关系,因此,基于在线OUR测量数据可以实时估计PHA合成量. 相似文献
108.
采用搅拌流动法研究了酸性水钠锰矿及水羟锰矿2种δ-MnO2矿物氧化As(Ⅲ)的动力学过程,构建了可用于多相体系的搅拌-流动氧化还原反应动力学模型.经过As吸附量的校正后,该模型对酸性水钠锰矿及水羟锰矿氧化As(Ⅲ)动力学数据拟合度分别为0.980和0.951,模型拟合得到pH 7时2种矿物单位比表面上氧化As(Ⅲ)的初始反应速率常数k分别为0.131,0.014min-1·m-2.相比而言,该速率常数明显高于批量法得到的表观速率常数kobs,0.021,0.001min-1?m-2更接近真实的化学动力学参数.搅拌流动法与批量法得到的不同矿物的速率常数大小趋势一致,即尽管酸性水钠锰矿对As(Ⅲ)的氧化率低于水羟锰矿,单位比表面上酸性水钠锰矿氧化As(Ⅲ)初始反应速率却远高于水羟锰矿.反应过程分析表明,反应初始阶段,As(Ⅲ)的吸附为主要限速步骤;而随着反应的进行,矿物表面反应位点逐渐钝化或减少,反应位点数量成为限速步骤. 相似文献
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Mengnjo J. Wirmvem Takeshi Oh Wilson Y. Fantong Samuel N. Ayonghe Jonathan N. Hogarh Justice Y. Suil Asobo Nkengmatia E. Asaah Seigo Ooki Gregory Tanyileke Joseph V. Hell 《环境科学学报(英文版)》2014,26(4):801-809
Rainwater characteristics can reveal emissions from various anthropogenic and natural sources into the atmosphere. The physico-chemical characteristics of 44 monthly rainfall events (collected between January and December 2012) from 4 weather stations (Bamenda, Ndop plain, Ndawara and Kumbo) in the Bamenda Highlands (BH) were investigated. The purpose was to determine the sources of chemical species, their seasonal inputs and suitability of the rainwater for drinking. The mean pH of 5 indicated the slightly acidic nature of the rainwater. Average total dissolved solids (TDS) were low (6.7 mg/L), characteristic of unpolluted atmospheric moisture/air. Major ion concentrations (mg/L) were low and in the order K+ 〉 Ca2+ 〉 Mg2~ 〉 Na+ for cations and NO3 〉〉 HCO3 〉 SO] 〉 CI- 〉 PO3- 〉 F- for anions. The average rainwater in the area was mixed Ca-Mg-SO4-CI water type. The CI-/Na+ ratio (1.04) was comparable to that of seawater (1.16), an indication that N a+ and CI originated mainly from marine (Atlantic Ocean) aerosols. High enrichments of Ca2+, Mg2+ and SO2- to Na+ ratios relative to seawater ratios (constituting 44% of the total ions) demonstrated their terrigenous origin, mainly from Saharan and Sahelian arid dusts. The K+/Na+ ratio (2.24), which was similar to tropical vegetation ash (2.38), and NO3 was essentially from biomass burning. Light (〈 100 mm) pre-monsoon and post-monsoon convective rains were enriched in major ions than the heavy (〉 100 mm) monsoon rains, indicating a high contribution of major ions during the low convective showers. Despite the acidic nature, the TDS and major ion concentrations classified the rainwater as potable based on the WHO guidelines. 相似文献
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桂江主要离子及溶解无机碳的生物地球化学过程 总被引:18,自引:9,他引:9
河流水体的化学组成记录了流域内各种自然过程与人类活动的信息.对西江一级支流桂江化学径流的分析结果表明,桂江水体的离子组成主要受碳酸盐岩化学风化过程的控制,CO2是这一过程的主要侵蚀介质;H2SO4对碳酸盐岩的风化影响桂江河水的化学组成.大气沉降、人类活动、碳酸盐岩和硅酸盐岩化学风化对桂江水体贡献的溶解物质分别占总溶解物质的2.7%、6.3%、72.8%和18.2%.河流溶解无机碳(DIC)的稳定同位素组成(δ13CDIC)揭示桂江河水中的DIC明显被浮游植物的光合作用所利用.浮游植物初级生产力对桂江颗粒有机碳(POC)的贡献达22.3%~30.9%,这表明岩石风化来源的DIC经浮游植物的光合作用转化为有机碳,并在迁移过程中部分沉积水体底部,进而形成埋藏有机碳. 相似文献