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21.
铁锰复合氧化物/壳聚糖珠:一种环境友好型除磷吸附剂 总被引:3,自引:0,他引:3
采用两步法制备了一种环境友好型除磷基吸附剂——铁锰复合氧化物/壳聚糖珠(FMCB),对其进行了表征,并对其磷吸附行为进行了系统研究.表征结果表明,该吸附剂为多孔纤维结构,比表面积为248 m~2·g~(-1),孔容为0.37 m~3·g~(-1).吸附实验结果表明,FMCB对磷的吸附容量远高于纯的壳聚糖颗粒,且Langmuir模型能更好地拟合FMCB对磷的吸附,最大吸附量为13.3 mg·g~(-1)(pH 7.0);准二级动力学模型能更好地拟合FMCB对磷吸附的动力学实验数据;溶液pH对磷的吸附影响较大,随着pH的增大,磷的吸附量逐渐降低;共存的Ca~(2+)和Mg~(2+)对磷吸附略有促进,而共存阴离子对磷吸附具有抑制作用,影响大小顺序为:SiO_3~(2-)CO_3~(2-)SO_4~(2-)≥Cl~-.吸附磷后的FMCB可用NaOH溶液进行脱附再生,并可重复使用.在进水磷初始浓度为3 mg·L~(-1)条件下,吸附达到穿透时(出水磷浓度达0.5 mg·L~(-1)),可处理约800个柱体积的模拟含磷废水. 相似文献
22.
镧改性沸石活性覆盖控制重污染河道底泥溶解性磷酸盐和铵释放研究 总被引:4,自引:4,他引:0
通过实验考察了镧改性沸石对水中磷酸盐和铵的吸附性能,并探讨了低溶解氧情况下镧改性沸石覆盖控制底泥溶解性磷酸盐和铵态氮释放的效率.镧改性沸石对水中磷酸盐和铵的吸附动力学过程满足准二级动力学模型.镧改性沸石对水中磷酸盐的吸附平衡数据可以采用Langmuir等温吸附方程加以描述,对水中铵的吸附平衡数据可以采用Langmuir、Freundlich和Dubinin-Radushkevich(D-R)等温吸附方程加以描述.当pH 7时,镧改性沸石吸附水中磷酸盐的机制包括配位体交换、路易斯酸碱反应和静电吸引,吸附水中铵的机制是阳离子交换.镧改性沸石覆盖不仅可以有效地控制溶解性磷酸盐从底泥向上覆水的释放,而且可以明显降低铵态氮从底泥向上覆水迁移的速率.镧改性沸石覆盖量越多,控制底泥铵态氮释放的效果越好.镧改性沸石覆盖层吸附从底泥中释放出来的溶解性磷酸盐后主要以较为稳定的形态存在,低溶解氧情况下不容易重新释放出来.上述结果表明,镧改性沸石适合作为一种覆盖材料用于控制低溶解氧情况下溶解性磷酸盐和铵态氮从底泥向上覆水的释放. 相似文献
23.
WAHMO model was used to simulate the distribution of pollutants in Dalian Bay, China as to predict well as the growth and control of alga. The observed and predicted values of main pollutants showed a good trend at all study locations and the different between them can be ignored. Simulation results illustrated that phosphate was one of limited factors to control algal growth at the location near the sewage outfall, meanwhile, away from the sewage outfall, the synergy of ammonium nitrogen and phosphate was the limited factor. 相似文献
24.
氮磷肥料对HB-5菌株降解莠去津的促进作用及去毒效应的影响 总被引:1,自引:0,他引:1
以莠去津降解细菌HB-5为研究对象,进行了氮、磷肥单一及复合施肥对HB-5细菌降解土壤中莠去津的促进作用的研究,探讨了莠去津降解率与土壤中速效氮、速效磷含量之间的关系及莠去津降解过程中生态毒性的变化情况.莠去津在土壤中的残留采用高效液相色谱法进行测定;土壤中速效氮和速效磷分别采用碱解扩散法及0.5mol/L-NaHCO3浸提-钼锑抗比色法测定;土壤的生态毒性采用蚕豆根尖微核法进行测定.结果表明,在实验的前5d,不论氮、磷肥单一或复合施肥均能够明显促进HB-5对莠去津的降解,不同施肥条件下莠去津的降解速率依次为:氮、磷肥复合单施磷肥单施氮肥不施肥料对照;实验5d后,各处理中莠去津降解率没有显著差异(p0.05),均达到了95%以上.土壤中速效氮和速效磷含量随着莠去津的降解而呈现逐渐减少的趋势.土壤的生态毒性试验结果表明,莠去津经HB-5菌株降解后,土壤的生态毒性显著降低;各施肥处理土壤中莠去津的生态毒性均低于不施肥处理的土壤;实验的前5d,各处理土壤中生态毒性的大小依次为:氮、磷肥复合单施磷肥单施氮肥不施肥料对照.实验7d时,各处理土壤中莠去津的生态毒性均恢复到空白对照水平.氮磷肥料的施用不仅能促进HB-5菌株对土壤中莠去津的降解,而且能加速降低土壤的生态毒性,为莠去津污染土壤的快速修复提供了理论依据. 相似文献
25.
26.
27.
三峡库区悬移质泥沙对磷污染物的吸附解吸特性 总被引:3,自引:0,他引:3
就三峡库区悬移质泥沙对磷污染物的吸附解吸特性从野外同步监测和室内试验研究两个方面展开研究。选取长江干流、嘉陵江和乌江共7个监测断面于2002年和2003进行野外同步监测,测试结果表明:水中的悬移质泥沙对水中各种覆存形态的磷污染物浓度具有显著影响,单位重量泥沙对磷的吸附量与水体总泥沙含量、泥沙粒径有密切关系。采集寸滩断面泥沙对磷酸盐吸附解吸特性进行室内试验研究,并根据Langmuir吸附动力学方程对吸附解吸过程进行了拟合,发现吸附速率常数k随着泥沙粒径的增加而呈递增变化,而磷酸盐初始浓度对k值的影响并不明显,同时,磷酸盐解吸量随着泥沙浓度的增加和粒径的增加呈递减变化,k值随着泥沙粒径的增加而呈递增变化,泥沙浓度对k值的影响不明显。 相似文献
28.
Competition of three bloom-forming marine phytoplankton (diatom Skeletonema costatum, and dinoflagellates Prorocentrum
minimum and Alexandrium tamarense) was studied through a series of multispecies cultures with di erent nitrate (NaNO3) and
phosphate (NaH2PO4) levels and excess silicate to interpret red tide algae succession. S. costatum outgrew the other two dinoflagellates
in nitrate and phosphate replete cultures with 10 mol/L Na2SiO3. Under nitrate limited (8.82 mol/L NaNO3) conditions, the growth
of S. costatum was also dominant when phosphate concentrations were from 3.6 to 108 mol/L. Cell density of the two dinoflagellates
only increased slightly, to less than 400 and 600 cells/mL, respectively. Cell density of S. costatum decreased with time before day
12, and then increased to 4000 cells/mL (1.5 mg/L dry biomass) at NaNO3 concentrations between 88.2 and 882 mol/L with limited
phosphate (0.36 mol/L NaH2PO4) levels. In addition, P. minimum grew well with a maximal cell density of 1690–2100 cells/mL
(0.5–0.6 mg/L dry biomass). Although S. costatum initially grew fast, its cell density decreased quickly with time later in the growth
phase and the two dinoflagellates were dominant under the nitrate-limited and high nitrate conditions with limited phosphate. These
results indicated that the diatom was a poor competitor compared to the two dinoflagellates under limited phosphate; however, it grew
well under limited nitrate when growth of the dinoflagellates was near detection limits. 相似文献
29.
Removal of phosphate by Fe-coordinated amino-functionalized 3D mesoporous
silicates hybrid materials
Phosphate removal from aqueous waste streams is an important approach to control the eutrophication downstream bodies of water.
A Fe(III) coordinated amino-functionalized silicate adsorbent for phosphate adsorption was synthesized by a post-grafting and metal
cation incorporation process. The surface structure of the adsorbent was characterized by X-ray di raction, N2 adsoropion/desoprotion
technique, and Fourier transform infrared spectroscopy. The experimental results showed that the adsorption equilibrium data were well
fitted to the Langmuir equation. The maximum adsorption capacity of the modified silicate material was 51.8 mg/g. The kinetic data
from the adsorption of phosphate were fitted to pseudo second-order model. The phosphate adsorption was highly pH dependent and
the relatively high removal of phosphate fell within the pH range 3.0–6.0. The coexistence of other anions in solutions has an adverse
e ect on phosphate adsorption; a decrease in adsorption capacity followed the order of exogenous anions: F?? > SO2?? 4 > NO??3 > Cl??. In
addition, the adsorbed phosphate could be desorbed by NaOH solutions. This silicate adsorbent with a large adsorption capacity and
relatively high selectivity could be utilized for the removal of phosphate from aqueous waste streams or in aquatic environment. 相似文献
30.
Tao Zhang Qiucheng Li Lili Ding Hongqiang Ren Ke Xu Yonggang Wu Dong Sheng 《环境科学学报(英文版)》2011,23(6):881-890
Chemical precipitation to form magnesium ammonium phosphate (MAP) is an effective technology for recovering ammonium
nitrogen (NH4
+-N). In the present research, we investigated the thermodynamic modeling of the PHREEQC program for NH4
+-N
recovery to evaluate the effect of reaction factors on MAP precipitation. The case study of NH4
+-N recovery from coking wastewater
was conducted to provide a comparison. Response surface methodology (RSM) was applied to assist in understanding the relative
significance of reaction factors and the interactive effects of solution conditions. Thermodynamic modeling indicated that the saturation
index (SI) of MAP followed a polynomial function of pH. The SI of MAP increased logarithmically with the Mg2+/NH4
+ molar ratio
(Mg/N) and the initial NH4
+-N concentration (CN), respectively, while it decreased with an increase in Ca2+/NH4
+ and CO3
2??/NH4
+
molar ratios (Ca/N and CO3
2??/N), respectively. The trends for NH4
+-N removal at different pH and Mg/N levels were similar to the
thermodynamic modeling predictions. The RSM analysis indicated that the factors including pH, Mg/N, CN, Ca/N, (Mg/N) (CO3
2??/N),
(pH)2, (Mg/N)2, and (CN)2 were significant. Response surface plots were useful for understanding the interaction effects on NH4
+-N
recovery. 相似文献