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1.
生态足迹影响因子的定量分析   总被引:2,自引:0,他引:2  
人口的膨胀和人类工业化进程的加剧,使得人类向自然界获取越来越多的资源,同时向环境源源不断的输入废弃物,已经严重超过了自然生态系统的供给能力和环境容量,生态环境日益恶化,水土流失、草场退化、植被消亡、生物多样性锐减、全球变暖等情况已经严重到难以遏制的地步,危及到人类自身的生存。在和平与发展成为世界两大主题的今天,人们越来越关注可持续发展的问题。在现有资料的基础上,利用主成分分析方法,定量地讨论了中国各省(区市)1999年生态足迹大小与其影响因子间的关系。结果表明,生态足迹的大小是各省(区市)的大中型企业个数、全社会固定生产投资等众多因子共同作用的结果,其中总人口和GDP是生态足迹大小的主要影响因子,其因子载荷量分别达到了0.940和0.913。值得一提的是非农业人口与生态足迹的相关系数超过了农业人口,这说明由于消费模式和生活水平等的差异,非农业人口对生态足迹的影响大于农业人口对生态足迹的影响。在此基础上建立了生态足迹影响因子的多元线性回归模型,以期为生态足迹在进行区域可持续发展评价的方法上提供新的思路。  相似文献   
2.
Diadromous fish often enter freshwater directly from seawater via fish ladders or channels built in estuarine dams. The oxygen consumption rates (OCR) of glass eel, Anguilla japonica, were determined using an automatic intermittent flow respirometer under various salinity and temperature regimes to physiologically explain this direct movement. The endogenous rhythm of the OCR in wild glass eels, freshly collected from estuaries, was nearly synchronous with the tidal pattern at the estuarine collection site. When the salinity was changed from 20 psu (12°C) at a constant temperature to that of freshwater, the OCR of the glass eels decreased by 21.6±7.0% (mean ± SD) (P<0.05), showing a dampened rhythm for about 48 h. After this period of impediment, the glass eels resumed normal metabolic activity. Direct migration from seawater to freshwater under constant temperature would result in a severe physiological stress for these glass eels for about two days. When the glass eels were exposed to a cyclic change in water temperature of 2°C 26 h−1, as they encounter in estuaries, and then were introduced to freshwater abruptly, the OCR rhythm corresponded to the cyclic changes in water temperature after exposure to freshwater. Under these conditions, the mean OCR of the glass eels had a small difference before and after exposure to freshwater. These data explained how glass eels can directly move from sea water into the freshwater without any apparent metabolic stress in the estuaries showing cyclic change in water temperature (Δt=2°C).  相似文献   
3.
罗欢  陈秀洪  吴琼  罗娜  黄徐 《自然资源学报》2020,35(12):3018-3028
随着点源污染逐步得到有效控制,面源与截排溢流污染对水环境的胁迫日益突出。基于土地遥感数据、城市排水管网等资料,构建流域—海湾一体化水环境模型,探讨深圳湾流域面源与截排溢流污染特征及其对水环境的影响,研究表明:(1)雨季COD、NH3-N和TP单位面积面源与截排溢流污染负荷分别为17.21 t/km2与10.21 t/km2、0.17 t/km2与0.69 t/km2、0.04 t/km2与0.07 t/km2;(2)面源与截排溢流污染时间上主要集中于大雨及以上等级降水较多的5月和8月,空间上主要分布在截排工程集中、下垫面面积较大且坡度较陡的深圳河、大沙河和新洲河流域;(3)面源与截排溢流水体COD、NH3-N和TP浓度可达地表水V类标准的3.7倍、18.2倍和8.5倍;(4)雨季COD、NH3-N和TP浓度高于旱季的区域分别超过深圳湾总面积的40%、60%和65%。  相似文献   
4.
Water-uptakes of pure sodium carbonate(Na_2CO_3),pure β-alanine and internally mixedβ-alanine/Na_2CO_3 aerosol particles with different mole ratios are first monitored using attenuated total reflectance Fourier transform infrared spectroscopy(ATR-FTIR) technique.For pure Na_2CO_3 aerosol particles,combining the absorptions at 877 and 1422 cm-1 with abrupt water loss shows the efflorescence relative humidity(ERH) of 62.9%–51.9%.Upon humidifying,solid Na_2CO_3 firstly absorbs water to from Na_2CO_3·H2 O crystal at 72.0% RH and then deliquesces at 84.5% RH(DRH).As for pure β-alanine particles,the crystallization takes place in the range of 42.4%–33.2% RH and becomes droplets at ~ 88.2% RH.When β-alanine is mixed with Na_2CO_3 at various mole ratios,it shows no efflorescence of Na_2CO_3 whenβ-alanine to Na_2CO_3 mole ratio(OIR) is 2:1.For 1:1 and 1:2 β-alanine/Na_2CO_3 aerosols,the ERHs of Na_2CO_3 are 51.8%–42.3% and 57.1%–42.3%,respectively.While β-alanine crystal appears from 62.7% RH for 2:1 and 59.4% RH for both 1:1 and 1:2 particles and lasts to driest state.On hydration,the DRH is 44.7%–75.2% for Na_2CO_3 with the OIR of 1:1 and 44.7%–69.0%for 1:2 mixture,and those of β-alanine are 74.8% for 2:1 mixture and 68.9% for two others.After the first dehumidification–humidification,all the water contents decrease despite of constituent fraction.And at ~ 92% RH,the remaining water contents are 92%,89% and 82%at ~ 92% RH,corresponding to OIR of 2:1,1:1 and 1:2 mixed system,respectively.  相似文献   
5.
In this work, a series of Cu-ZSM-5 catalysts with different SiO2/Al2O3 ratios (25, 50, 100 and 200) were synthesized and investigated in n-butylamine catalytic degradation. The n-butylamine can be completely catalytic degradation at 350°C over all Cu-ZSM-5 catalysts. Moreover, Cu-ZSM-5 (25) exhibited the highest selectivity to N2, exceeding 90% at 350°C. These samples were investigated in detail by several characterizations to illuminate the dependence of the catalytic performance on redox properties, Cu species, and acidity. The characterization results proved that the redox properties and chemisorption oxygen primarily affect n-butylamine conversion. N2 selectivity was impacted by the Brønsted acidity and the isolated Cu2+ species. Meanwhile, the surface acid sites over Cu-ZSM-5 catalysts could influence the formation of Cu species. Furthermore, in situ diffuse reflectance infrared Fourier transform spectra was adopted to explore the reaction mechanism. The Cu-ZSM-5 catalysts are the most prospective catalysts for nitrogen-containing volatile organic compounds removal, and the results in this study could provide new insights into catalysts design for VOC catalytic oxidation.  相似文献   
6.
As a novel alternative to traditional perfluoroalkyl substances (PFASs), including perfluorooctanoic acid (PFOA) and perfluorooctane sulfonate (PFOS), hexafluoroproplyene oxide trimer acid (HFPO-TA) has been detected worldwide in surface water. Moreover, recent researches have demonstrated that HFPO-TA has stronger bioaccumulation potential and higher hepatotoxicity than PFOA. To treat these contaminants e.g. PFOA and PFOS, some photochemical techniques by adding exogenous substances had been reported. However, there is still no report for the behavior of HFPO-TA itself under direct UV irradiation. The current study investigated the photo-transformation of HFPO-TA under UV irradiation in aqueous solution. After 72 hr photoreaction, 75% degradation ratio and 25% defluorination ratio were achieved under ambient condition. Reducing active species, i.e., hydrated electrons and active hydrogen atoms, generated from water splitting played dominant roles in degradation of HFPO-TA, which was confirmed by different effects of reaction atmospheres and quenching experiments. A possible degradation pathway was proposed based on the products identification and theoretical calculations. In general, HFPO-TA would be transformed into shorter-chain PFASs, including hexafluoropropylene oxide dimer acid (HFPO-DA), perfluoropropionic acid (PFA) and trifluoroacetate (TFA). This research provides basic information for HFPO-TA photodegradation process and is essential to develop novel remediation techniques for HFPO-TA and other alternatives with similar structures.  相似文献   
7.
为探究"稀土王国"江西省赣南地区离子型稀土矿对周边水体环境的影响,以离子型稀土矿分布密集区定南县濂江月子河流域和龙迳河龙头流域为研究对象,综合分析研究区特征污染物ρ(NH4+-N)空间分布特征,采用相关性分析和主成分分析揭示其主要污染来源及影响因素.结果表明:①离子型稀土矿停产整顿半年后,濂江月子河流域和龙迳河龙头流域ρ(NH4+-N)超过1.00和2.00 mg/L的采样点分别达72%和68%;pH范围为2.95~7.66,平均值分别为6.23和5.53,水体总体上偏酸性;ρ(TN)、ρ(NH4+-N)、EC与ρ(NO3--N)变异系数较大,均介于0.80~1.50之间.②相关性分析结果显示,ρ(NH4+-N)与ρ(TN)、EC均呈极显著正相关(P < 0.01);ρ(NH4+-N)与pH呈显著负相关(P < 0.05).③流经稀土尾矿区的水体中ρ(NH4+-N)随距离增加呈现明显的空间梯度分布特征,即距稀土矿区边界200 m处水体中ρ(NH4+-N)最高(12.20~200.00 mg/L),其次为1.15 km内(3.69~11.80 mg/L)及3.5 km以上水体(0.80~1.51 mg/L),矿区周边未受到采矿活动影响的水体中ρ(NH4+-N)最低(0.03~0.15 mg/L).④PCA结果表明,2条河流的主要环境影响因子为ρ(TN)、ρ(NH4+-N)、pH和EC,主要受到周边稀土矿山尾矿的强烈影响.研究显示,离子型稀土矿原位浸矿开采停产半年后,重点小流域水体中ρ(NH4+-N)高概率超标的现状仍然存在,受稀土开采活动影响较大.建议进一步开展重点小流域NH4+-N剩余"库容"精算和矿山周边地表水定期监测.   相似文献   
8.
9.
刘瑀  刘宇馨  米雪娇  李娜  王海霞 《海洋环境科学》2020,39(2):283-287, 314
为了研究溢油对海岸潮间带重要的大型绿藻孔石莼(Ulva Pertusa)的影响,本文探究了在180#燃料油的原油分散液(WAF)胁迫下,孔石莼的生长速率、叶绿素a以及碳氮稳定同位素的变化。在低WAF浓度(1.43 mg/L、2.87 mg/L和4.30 mg/L)胁迫下,对孔石莼的生长具有促进作用,生长速率均高于对照组,同时叶绿素a和碳氮稳定同位素均呈现上升的趋势;而高浓度WAF(5.72 mg/L和7.17 mg/L)会抑制藻类生长,导致生长速率低于对照组,而叶绿素a含量却高于对照组,孔石莼的δ15N和δ13C相比对照组偏负。对于孔石莼来说,C、N稳定同位素变化的趋势比叶绿素a更明显,这表明在溢油胁迫下,孔石莼的C、N稳定同位素能够更好更快速地评价溢油胁迫毒性大小,因此可以作为海洋环境监测和评价的一种新手段。  相似文献   
10.
液相色谱法测定环境空气中酞酸酯类   总被引:1,自引:0,他引:1  
制作了半挥发性有机物中流量采样装置,使用超细玻璃纤维滤膜采样,反相液相色谱法测定环境空气中酞酸酯类,并对样品净化方式、目标化合物在气相和颗粒物上的分布规律及采样器的捕集效率进行了试验.方法在0.50 mg/L~50.0 mg/L之间线性关系良好,当浓缩体积为1.0 mL、采样体积为144 m3时,目标化合物的检出限为0.4×10-3 μg/m3~6.0×10-3 μg/m3;当采样体积为6 m3时,检出限为0.008 μg/m3~0.145 μg/m3.  相似文献   
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