烟气NO氧化催化剂Cu-V/Ti-PILCs的制备及其硫水稳定性

采用等体积浸渍法制备了以钛交联粘土为载体,Cu与V氧化物为活性组分的烟气NO氧化催化剂(Cu-v/Ti-PILCs),并考察了各种制备条件下催化剂的活性及稳定性.结果显示,当V水/V丙酮 =1∶2,负载4%CuO和2%V2O5,并在500℃煅烧时制得的Cu-V/Ti-PILCs催化剂,在NO浓度为350 mg/m3,O...     

脱硝催化剂孔结构及其脱硝特性的研究

选择性催化还原脱硝技术(SCR)所采用的催化剂多数为多孔介质,其内部孔隙有助于提高催化剂的反应活性。文中采用浸渍负载法,通过改变制备温度制备出不同孔结构的催化剂样品,采用N2吸附法对其孔结构进行测定和分析,并对不同孔结构的催化剂样品进行了脱硝实验。研究表明:煅烧及干燥温度对催化剂孔结构有很大的影响,比表面积越大,其催化剂内的孔分布宽度越窄,平均孔径越小;在活性温度范围(360～390℃)内,脱硝过程中主要是属于化学反应过程控制,脱硝效果随着比表面积的增大而增强;在非活性温度范围内,脱硝过程同时受到气体扩散过程及化学反应过程控制。     

尿素为还原剂燃煤烟气脱硝技术的研究与应用

尿素由于运输、储存安全性较高,作为还原剂进行脱硝备受关注。从工艺原理、系统组成和工程应用等方面,对尿素制氨选择性催化还原技术（SCR）、选择性非催化还原技术（SNCR）和尿素法三种脱硝方法进行了综述。分析了不同技术运用过程存在的问题,并提出解决措施。     

MFC强化同步短程硝化反硝化工艺的启动

微生物燃料电池(MFC)可在阴极实现反硝化、短程反硝化和同步硝化反硝化并产生电能,但在MFC阴极实现同步短程硝化反硝化的研究尚未见到报道。为了探讨MFC阴极同步短程硝化反硝化工艺的性能,将双室曝气阴极MFC与A/O脱氮工艺结合处理人工模拟低碳氮比废水。通过静置运行15 d使得MFC阴极室亚硝态氮得以积累,氨氧化菌得以富集。随即改为连续运行后第21天成功启动同步短程硝化反硝化MFC;阴极出水氨氮浓度为0.3 mg/L,亚硝态氮浓度为15.9 mg/L,硝态氮浓度为0.6 mg/L,亚硝化率达到95%以上,阴极电极自养反硝化去除率达到50%以上,COD去除率达到85%以上。结果表明,将MFC与同步短程硝化反硝化工艺结合,通过阴极室中氧气得电子获得高p H,可以强化同步短程硝化反硝化工艺,完成生物脱氮的同时回收电能,并具有减少外加碱度的优势。     

γ-Al2O3负载多金属复合催化剂选择性催化还原烟气脱硝

以γ-Al₂O₃作为载体,先后负载CeO₂,MnC₂O₄,Fe（NO₃）₃,CrO₃,Ni（NO₃）₂,NH₄VO₃等多种金属组分制备γ-Al₂O₃负载多金属复合催化剂,并用于模拟烟气的选择性催化还原脱硝。通过SEM和XRD技术对催化剂进行了表征。表征结果显示：Fe,Mn,Cr的添加能增加催化剂的低温催化活性、提高催化剂的N₂选择性;γ-Al₂O₃对活性金属氧化物的负载效果良好。实验结果表明：各金属化合物的最佳加入量为 w（MnC₂O₄·2H₂O）=20%,w（Fe（NO₃）₃·9H₂O）=15%,w（CrO₃）=10%,w（Ni（NO₃）₂·6H₂O）=5%,w（NH₄VO₃）=10%,w（CeO₂）=5%,w（γ-Al₂O₃）=35%;以在最佳正交实验条件下制得的γ-Al₂O₃负载多金属复合物为催化剂,在脱硝反应温度为205 ℃的条件下,NO转化率为96.7%;γ-Al₂O₃负载多金属复合催化剂经5次重复使用,NO转化率仍可稳定在94%左右。     

SOIL CHANGES CAUSED BY MUNICIPAL WASTEWATER APPLICATIONS IN EASTERN SOUTH DAKOTA1

ABSTRACT: Wastewater from a municipal treatment plant was applied in rapid infiltration basins for four years to determine a poorly drained soils effectiveness in removing influent N and P and the soil changes that might limit their removal. About half the total PO₄-P lost from the influent was sorbed in the upper 91 cm of the soil and the other half was sorbed by the soil below the perforated pipe, which was used to drain the basins and collect the effluent for analysis. Drying of the basin soils converted more sorbed PO₄-P to Ca phosphates but the total sorbed was about the same. The in. fluent N decreased, probably by volatilization, because the two basins with surface soil lost soil N rather than gained soil N. The soil total Ca, Mg, and K contents did not change significantly but Na increased slightly. Changes in the physical characteristics of the soils were slight and would have little effect on the longevity of a rapid infiltration basin.     

嘉兴电厂2×300MW机组脱硝方案的对比分析

根据嘉兴电厂的实际情况，在对6种主流脱硝工艺进行技术经济分析的基础上，结合电厂近期和远期的NOx控制目标，对各种脱硝工艺的组合进行研究，推荐了可行的脱硝方案，为工程的实施提供了可靠的技术依据。     

低NOx燃烧技术

介绍了锅炉燃烧中降低NOx的主要措施和几种国内外主要低NOx燃烧技术的脱硝原理.发展低NOx燃烧技术,对环境保护具有重大意义.     

DIN Retention‐Transport Through Four Hydrologically Connected Zones in a Headwater Catchment of the Upper Mississippi River1

Abstract: Dissolved inorganic nitrogen (DIN) retention‐transport through a headwater catchment was synthesized from studies encompassing four distinct hydrologic zones of the Shingobee River Headwaters near the origin of the Mississippi River. The hydrologic zones included: (1) hillslope ground water (ridge to bankside riparian); (2) alluvial riparian ground water; (3) ground water discharged through subchannel sediments (hyporheic zone); and (4) channel surface water. During subsurface hillslope transport through Zone 1, DIN, primarily nitrate, decreased from ～3 mg‐N/l to <0.1 mg‐N/l. Ambient seasonal nitrate:chloride ratios in hillslope flow paths indicated both dilution and biotic processing caused nitrate loss. Biologically available organic carbon controlled biotic nitrate retention during hillslope transport. In the alluvial riparian zone (Zone 2) biologically available organic carbon controlled nitrate depletion although processing of both ambient and amended nitrate was faster during the summer than winter. In the hyporheic zone (Zone 3) and stream surface water (Zone 4) DIN retention was primarily controlled by temperature. Perfusion core studies using hyporheic sediment indicated sufficient organic carbon in bed sediments to retain ground water DIN via coupled nitrification‐denitrification. Numerical simulations of seasonal hyporheic sediment nitrification‐denitrification rates from perfusion cores adequately predicted surface water ammonium but not nitrate when compared to 5 years of monthly field data (1989‐93). Mass balance studies in stream surface water indicated proportionally higher summer than winter N retention. Watershed DIN retention was effective during summer under the current land use of intermittently grazed pasture. However, more intensive land use such as row crop agriculture would decrease nitrate retention efficiency and increase loads to surface water. Understanding DIN retention capacity throughout the system, including special channel features such as sloughs, wetlands and floodplains that provide surface water‐ground water connectivity, will be required to develop effective nitrate management strategies.     

THE FATE OF NITRATE IN LAKE SEDIMENT COLUMNS1

ABSTRACT: To investigate the magnitude of denitrification and assimilatory nitrate reduction as these reactions relate to the fate of nitrate reaching sediments via groundwater seepage, undisturbed core samples of sediments (40 cm length) from two lakes (Mendota and Tomahawk) were leached from the bottom (at 1.4 cm/day) with a solution of ¹⁵N-nitrate (10 mg N/liter). The sediment columns were fitted with Pt electrodes to measure the oxidation-reduction (Eh) potential. While leaching removed considerable ammonium-N and soluble organic N, essentially no ¹⁵N had passed through the columns by 50 days. The Eh readings indicated that denitrification was occurring in the lower portions of the columns. The ¹⁵N distribution of the sediment N after 50 days showed that about 15 to 26% of the added nitrate-N was converted to organic N and ammonium-N. The data show that denitrification can be a significant N sink in seepage lakes.