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991.
采用厌氧水解—好氧和单独好氧处理两种生化方法对蒽醌染整废水进行了平行对照试验。结果表明,厌氧水解—好氧处理方法可有效地提高该废水的可生化程度。当进水CODcr浓度为400mg/L、色度为800倍时,厌氧水解—好氧处理后出水CODcr可达120—170mg/L,CODcr去除率在63%以上,色度降低至150倍,明显优于单一好氧处理的出水水质。 相似文献
992.
催化电解法处理垃圾渗滤液的研究 总被引:23,自引:1,他引:23
对垃圾渗滤液的SBR处理出水进行了催化电解的正交实验研究。结果表明 ,其最佳工艺条件 :pH为 8,电极材料为RuO2 IrO2 TiO2 /Ti,电流密度为 1 0A/dm2 ,电极间距为 0 .5cm ,[Cl- 1 ]为 1 0 0 0 0mg/L ,SA /L为 50cm2 /L。在此条件下 ,电解 48min时 ,COD去除率达 82 .6 % ,电流效率为 31 .6 % ,耗电量为 32 .4kwh/t水。 相似文献
993.
Daizhou Zhang Guangyu Shi Yasunobu Iwasaka Min Hu Jiaye Zang 《Water, Air, & Soil Pollution: Focus》2005,5(3-6):261-276
Analysis of individual particles collected at Beijing in northern China revealed that particles abundant in calcium (Ca) always
constituted a large fraction of mineral particles in the urban atmosphere. The particles were characterized by cubic morphologies.
The major mineral element in the particles was Ca and few or no other mineral elements were detected. A large number of the
particles were in the range of diameter <1 μm, where common natural mineral particles were rarely detected. The contribution
of the Ca particles to the volume of total mineral particles greatly exceeded that of other mineral particles during non-dust-storm
periods and was comparable to that during dust-storm periods. Reagent film tests showed that particulate sulfate and nitrate
formation on the Ca particles was similar to that on common mineral particles. These results indicate that a large portion
of Ca in the atmospheric particulate matter in Beijing was from anthropogenic sources rather than from natural sources, and
the anthropogenic Ca particles acted as a significant medium for the formation of sulfate and nitrate. Similar particles were
also detected at Qingdao, a coastal city in northern China. Data of a dust storm event showed that Ca-abundant particles from
East China arrived there and moved out of the continent, similarly to Asian dust storm particles, suggesting possible contributions
of anthropogenic Ca even in Asian dust storm samples in the downstream areas. Therefore, Ca may not be a good indicator of
Asian dust from natural sources. However, the Ca particles, due to their unique shapes and elemental compositions, may provide
an indicator for the atmospheric dispersion of anthropogenic particulate matters in East Asia. 相似文献
994.
HPLC法测定复方甘草合剂中甘草苷的含量 总被引:2,自引:0,他引:2
建立HPLC法测定了复方甘草合剂中甘草苷的含量.以Shim-pack CLC-DOS 150mm×4.6mm(5μm)为分析柱,乙腈-0.5 醋酸(15∶85)为流动相,流速为1.0 ml·min-1,检测波长为276nm,采用外标法定量测定.结果表明,甘草苷在5~25μg·ml-1范围内呈良好的线性关系(r=0.9998);其高、中、低3个量的平均回收率分别为99.57%、99.41%、98.76%,RSD分别为0.46%、0.72%、0.69%(n=6).本方法简便可靠,重现性好,可作为复方甘草合剂质量控制方法. 相似文献
995.
石化企业的消防安全评价 总被引:12,自引:0,他引:12
本以“石油化工企业设计防火规范”等消防规范和德尔菲专家调查法为基础,尝试进行石化企业内自然厂的消防安全评价。评价中,固定消防设施部分以各生产装置和储运设施为单元,各装置、设施的权重在道化学公司火灾、爆炸危险指数法的基础上确定;移动消防力量部分和消防管理部分以厂为单元,各指标的权重由层次分析法确定。对于各指标的评价打分,本暂不给出明确的分级标准,而是在各项指标下设置若干检查要点,专家根据实际情况与相关法规条的符合程度进行打分。最终采用线性加权模型得出评价结果,并根据各指标的整改效果排序确定整改的重点。 相似文献
996.
采用SBR反应器建立了一套通过特定pH终值调控曝气停止点,以实现稳定部分亚硝化的策略,整个运行过程分为3个阶段,阶段Ⅰ启动亚硝化,阶段Ⅱ在稳定亚硝化的同时探索pH终值的设定规律,阶段Ⅲ采用pH终值设定规律实现稳定部分亚硝化,通过跨越夏、冬季(7~35℃)共148d的运行,考察SBR系统内有机物、氮素的转化规律,并分析不同温度(23、18、13℃)对部分亚硝化反应过程的影响.结果表明,在低DO(0.2~0.4mg/L)和MLSS为4000mg/L的条件下,控制pH终值为(7.73±0.02),使出水FA在0.5~1.2mg/L,可稳定部分亚硝化期间的出水NO2--N/NH4+-N值在1~1.4之间,出水亚硝积累率(NAR)维持在85%以上,有机物去除率在60%以上.比氨氧化速率、比亚硝态氮氧化速率、比COD去除速率均随温度下降而降低,但降低趋势较缓,且反应均能稳定完成. 相似文献
997.
998.
Guangshan Liu Sumei Liu Jing Zhang Yipu Huang Min Chen 《Water, Air, & Soil Pollution: Focus》2007,7(6):693-701
Sediment cores were collected from two sites (A2 and ZQ) in the Qingdao sea area of the Yellow Sea. Radionuclides 40K, 137Cs, 210Pb, 226Ra, 228Ra, 228Th, 234Th, and 238U in the cores were measured using HPGe γ spectrometry. The sedimentation rate of the A2 Core using 210Pbex and 137Cs was 0.665 cm yr−1, therefore this 32 cm long core represents a 48 year timespan leading to the sampling date in 2001. The mixing layer was
restricted to the upper 5 cm as determined from the profile of 234Th. The uniformity of the activity distributions of 40K and 238U throughout the A2 Core and the activity distributions of 226Ra, 228Ra and 228Th below the mixing layer suggested that no significant oceanographic event or change in sediment material source had occurred
during this timespan. The 210 Pb was in excess relative to 226Ra, but 226Ra was deficient with respect to 238U in the entire A2 Core, while excess 234Th and 228Th were apparent only in the surface 5 cm. Total organic matter (TOM) in Core A2 decreases with depth. The second core, taken
to a depth of 14 cm, was from Site ZQ, which is located near Zhanqiao, Qingdao. The variations of the nuclide activity ratios
in this core were similar to those in the A2 Core, i.e., the excess 210 Pb and 226Ra deficiency were consistent throughout the core but excess 228Th was only in the surface to a depth of 2 cm. The 40K activity in the ZQ Core fluctuated and showed no real trend with depth. The activities of 137Cs, 210Pb, 226Ra and 238U in the entire length of Core ZQ, and 228Ra and 228Th from 2 cm to the bottom, were comparable within the uncertainty of measured activity. 相似文献
999.
1000.
采用类UV/Fenton法对模拟三唑磷废水进行处理。在模拟废水中人工投加H2O2和Fe^3+试剂能产生类Fenton试剂,类Fenton试剂在光照条件过程中可以产生大量活性羟基.OH,能够很好地氧化降解废水中的有机化合物。本方法可以有效的处理低浓度的含三唑磷的废水,提供三唑磷农药水样的UV/Fenton催化氧化过程的一级动力学方程。 相似文献