人工湿地不同基质对氨氮的吸附特性研究

过量氮是引发水体富营养化的重要原因之一,氮的去除是控制水体富营养化的关键,其中人工湿地中基质对氨氮的去除是人工湿地处理污水的重要途径。通过基质氨氮吸附动力学、等温吸附以及基质饱和吸附后氨氮解吸实验,研究沸石、红泥、水洗砂、炉渣4种人工湿地基质净化氨氮的效果,评价其饱和吸附后氨氮解吸可能造成的二次污染风险及基质去除氨氮的主要途径。结果表明：4种基质对氨氮的吸附量顺序依次为沸石〉红泥〉炉渣〉水洗砂;沸石去除氨氮的途径以离子交换为主,物理吸附作用很小;炉渣的离子交换作用和物理吸附作用效果相当。从氨氮的解吸率来看,沸石的解吸率最小,红泥次之,炉渣和水洗砂的解吸率较大。综合评价,沸石更适合作为人工湿地污水去除氨氮的基质。     

天然斜发沸石的氨氮改性吸附与化学再生

本文采用改性与化学再生方法,探索天然斜发沸石对氨氮吸附的最佳改性及化学再生条件.无机盐改性、热改性、有机改性试验结果表明,最佳改性方法为无机盐NaCl法,改性沸石吸附量较天然沸石提升了近20%,最佳NaCl浓度为1 mol·L~(-1);热改性法不能显著提高沸石的氨氮吸附容量,相反高温会破坏其结构;十二烷基苯磺酸钠改性法可以使改性沸石在其表面形成了新的阳离子吸附点,使其吸附性能提升;而十六烷基三甲基溴化铵改性沸石表面形成的是阴离子吸附点,对带正电的NH_4~+会产生排斥,导致其吸铵性能下降.化学再生试验表明,KCl溶液对铵饱和沸石的再生效果最显著,适宜再生浓度为0.1—0.2 mol·L~(-1).经KCl再生后的沸石再次通过NaCl改性,可延长沸石使用周期以及提高再生沸石的吸附能力.     

人工湿地磷吸附饱和基质的化学再生研究

长期处理了生活污水后的人工湿地基质对磷素的吸附会达到饱和,通过化学浸提方法,研究了2种无机酸（盐酸和硫酸）,酸和碱（盐酸和氢氧化钠溶液）对饱和吸附磷基质的释磷效果以及再生后基质吸附磷效果。结果表明：盐酸和硫酸对基质释磷的差异性不大,硫酸的释磷效果略好于盐酸,对3种基质的释磷效果几乎都大于80%;碱对砂和煤渣释磷效果好,对高炉渣释磷效果差,但经碱再生后的高炉渣、砂基质对磷素的吸收率极高,磷素初始浓度在1～50mg·L-1范围内时,吸收率在95.18%～99.04%范围内,对基质的再生能力好,而经碱再生后的煤渣基质对磷素的吸收率却很低,吸收率不超过21.14%。     

沸石生物联合吸附再生工艺及铵沸石再生

简述了沸石生物联合吸附再生的工艺原理,重点讨论吸附了NH 4的沸石粉的生物再生.结果表明,沸石和液相之间的NH 4是一种动态的离子交换平衡,污水的电导率对吸附了NH 4的沸石粉的NH 4解吸量有明显的影响;污水中阳离子对吸附了NH 4的沸石粉的再生率可达40%-50%,在微生物的硝化作用下可达94%.沸石生物联合吸附再生工艺中,吸附了NH 4的沸石粉的再生是"化学再生"和"生物再生"相结合的过程,生物硝化作用促进了沸石相中NH 4的解吸.     

改性斜发沸石在水处理中的应用

斜发沸石钠改性后能明显提高对Cu2 ,Pb2 ,Cd2 等重金属离子的交换能力,交换顺序为Cu2 ＞Pb2 ＞Cd2 ,对Cu2 -Pb2 和Cd2 -Pb2 混合体系有较好的分离效果.斜发沸石经铁活化后吸附水中F-的能力明显改善,吸附容量从57.0mg·kg-1提高到420.5mg·kg-1,吸附行为能满足Frendlich等温方程,是吸热过程,属异种电荷吸附方式和阴离子交换方式共存的化学吸附.斜发沸石经微波磷改性后,沸石骨架上的P原子能部分取代Si和Al原子形成Si-O-P 结构,具有阴离子交换能力,对水中As(Ⅲ)的吸附能力明显提高,吸附为放热过程,吸附机理为沸石骨架配位阴离子与水中As(Ⅲ)阴离子交换过程.     

生物炭基质潮汐流人工湿地处理生活污水性能

潮汐流人工湿地是一种新型的污水处理技术,作为人工湿地的重要组成部分,基质的合理选择能够直接影响人工湿地的运行效果。以鸡粪生物炭和玉米秸秆生物炭为基质分别建立潮汐流人工湿地来处理生活污水,并以石灰石基质人工湿地作为对照,考察不同淹没/排水比(8 h/4 h和4 h/8 h)下人工湿地对生活污水中各项污染物的去除性能。研究结果表明:生物炭基质人工湿地对COD、BOD、NH4~+-N、TN和PO4~(3-)-P的去除效率均高于石灰石基质人工湿地,且玉米秸秆生物炭基质人丁湿地对各项污染物的去除效果最好,各项污染物去除率分别为(73.6%±2.9%,COD)、(84.8%±6.1%,BOD5)、(84.2%±3.2%,NH4~+-N)、(45.3%±2.2%,TN)和(84.6%±2.8%,PO4~(3-)-P);当淹没/排水比由8 h/4 h改为4 h/8 h时,除PO4~(3-)-P的去除率基本不变外,各组人工湿地对生活污水COD、BOD、NH4~+-N和TN的去除率均有不同程度的升高,且玉米秸秆生物炭基质人工湿地对各项污染物的去除效果最好,各项污染物去除率分别为(80.5%±5.2%,COD)、(92.1%±5.1%,BOD5)、(90.3%±3.2%,NH4~+-N)、(60.3%±2.2%,TN)和(84.7%±1.5%,PO4~(3-)-P);生物炭基质人工湿地对NH4~+-N的去除途径主要为物理吸附和微生物硝化作用,且微生物硝化作用占主导,对PO4~(3-)-P的去除途径主要为物理吸附和微生物好氧吸磷作用,且微生物好氧吸磷作用占主导;生物炭基质中的微生物量要高于石灰石基质,且上层基质的微生物量高于下层基质;在微生物群落中,Clostridiaceae和Nitrosomonadaceae菌群分别承担有机物和NH4~+-N的主要去除,其在生物炭基质中的相对丰富度均高于石灰石基质。     

NaCl改性人造沸石去除废水中氨氮的性能及其影响因素

采用NaCl溶液对人造沸石进行改性处理,考察NaCl溶液浓度对改性效果的影响.通过表面特征分析、静态吸附试验及吸附等温分析,进一步比较了人造沸石和改性人造沸石对氨氮的吸附去除性能.由X射线衍射(XRD)分析可知,沸石经改性后表面变粗糙,同时出现NaCl晶体特征衍射峰.试验结果表明,1.0 mol·L-1NaCl溶液对人造沸石的改性效果最佳;在沸石用量为1.0 g(50 mL废水)、氨氮浓度为10 mol·L-1、反应时间为40 min、反应温度为25℃和pH值为6.52条件下,改性人造沸石对氨氮的吸附效果最佳,去除率为96.02％.Langmuir和Freundlich吸附等温方程均可较好地拟合2种沸石对氨氮的吸附过程.改性人造沸石对氨氮的吸附饱和容量(21.46 mg·g-1)远大于人造沸石(9.03 mg·g-1).     

粘土改性条件的研究Ⅱ.沸石的改性

考察了改性沸石的CTMAB加入量、CTMAB溶液浓度和吸附时间对CTMAB吸附量的影响 .测得沸石对CTMAB的饱和吸附容量为 6 5 0 0± 1 0 0mg·1 0 0g- 1沸石 ,明显高于改性膨润土的饱和吸附量 ,吸附符合Langmuir吸附特征 . 2 5℃时 ,当CTMAB的加入量为沸石饱和吸附容量的 1 1— 1 2倍 ,CTMAB溶液浓度≥ 1 6mg·ml- 1,吸附时间超过 6h时 ,沸石基本达到饱和吸附 .考察了有机沸石对于水中BTEX的去除效果 .并对沸石和膨润土的性质进行了比较 .     

基质对于人工湿地净化磷素潜能的探讨

综述了不同基质对于人工湿地净化磷素的潜能的研究结果。总结了不同基质对磷素的理论最大吸附量以及基质在人工湿地运行中对磷素净化能力,探讨了影响基质对磷素吸附性能的几个主要因素,并对今后在人工湿地基质类型的选择方面提出了展望。     

镧-四氧化三铁-沸石复合材料制备及去除水中磷酸盐和铵

采用La3+、Fe~(2+)、Fe3+和粉末状天然沸石制备了一种镧-Fe_3O_4-沸石复合材料,通过批量吸附实验考察了该复合材料对水中磷酸盐和铵的吸附作用.结果表明,镧-Fe_3O_4-沸石复合材料对水中磷酸盐和铵的单位吸附量随吸附剂投加量的增加而降低,对磷酸盐和铵的去除率随吸附剂投加量的增加而增加.当溶液pH值由6逐渐增加到11时,镧-Fe_3O_4-沸石复合材料对水中磷酸盐和铵的吸附能力逐渐下降.镧-Fe_3O_4-沸石复合材料对水中磷酸盐的吸附平衡数据可以采用Langmuir、Freundlich和Dubinin-Redushkevich(D-R)等温吸附模型加以拟合,对铵的吸附平衡数据可以采用Langmuir和D-R等温吸附模型加以拟合.根据Langmuir模型计算得到的镧-Fe_3O_4-沸石复合材料对水中磷酸盐和铵的最大单位吸附量分别为12.9 mg·g~(-1)(以磷计)和6.99 mg·g~(-1)(以铵计).镧-Fe_3O_4-沸石复合材料对水中磷酸盐和铵的吸附动力学过程可以采用准二级动力学方程加以描述.升高反应温度增强了镧-Fe_3O_4-沸石复合材料对水中磷酸盐和铵的吸附.溶液存在的氯离子、硫酸根离子和碳酸氢根离子对镧-Fe_3O_4-沸石复合材料吸附磷无负面影响.溶液存在的钾离子对镧-Fe_3O_4-沸石复合材料吸附铵的负面影响最大,其次为钠离子,钙离子的负面影响最小.1 mol·L~(-1)NaOH溶液可以使50%左右吸附到吸附剂上的磷酸盐解吸下来.1 mol·L~(-1)NaCl溶液可以使98%左右吸附到吸附剂上的铵解吸下来.当溶液pH值为7时,镧-Fe_3O_4-沸石复合材料对磷酸盐的吸附机制主要是配位体交换作用.镧-Fe_3O_4-沸石复合材料对铵的吸附机制主要是阳离子交换作用.     

Enhanced nitrogen removal reliability and efficiency in integrated constructed wetland microcosms using zeolite

The purpose of this study is to reduce the seasonal fluctuation and enhance the efficiency of nitrogen removal in vertical flow-horizontal subsurface flow (VF-HSF) constructed wetlands. Two sets of VF-HSF constructed wetlands were built, VF1-HSF1 and VF2-HSF2, and a zeolite section was placed in VF2. The results showed that VF2-HSF2 compared to VF1-HSF1 was not only a more reliable nitrogen removal method, but also enhanced the nitrogen removal efficiency by 50%. The average apparent rate of nitrogen removal in VF2-HSF2 reached to 2.52 gN·m^-3·d^-1, which doubled the rate in VF1-HSF1. Plant uptake and organic nitrogen sediment accounted for 12% and 6% of the total nitrogen removal in VF1-HSF1, respectively, and 10% and 4% in VF2-HSF2, respectively. Biologic nitrogen removal was the dominant mechanism, which accounted for 79% and 87% of the total nitrogen removal in VF1-HSF1 and VF2-HSF2, respectively. Ammonia adsorbed by zeolite during the cold seasons was desorbed, and then nitrified in warm seasons, which resulted in a bioregeneration efficiency of 91%. Zeolite in VF was capable of transferring ammonia from cold seasons to warm seasons as well as enhancing nitrification, which was accompanied by high potential denitrification in HSF that reinforced the efficiency and relieved seasonal fluctuation of nitrogen removal in VF-HSF.     

天然沸石对农田退水中氨氮的去除

利用静态吸附实验研究了沸石颗粒大小、氨氮初始浓度、接触时间及Na+离子浓度等因素对天然白银沸石去除模拟黄灌区农田退水中氨氮(NH4+-N)效果的影响,同时研究了吸附等温线特征,并考察了其吸附机理.研究结果表明,沸石颗粒大小、接触时间及NH4+和Na+初始浓度对NH4+-N交换容量都会产生一定影响;根据复相关系数(R2),NH4+-N的吸附等温线更符合三参数等温线模型;而对于两参数等温线模型,Langmuir模型比Freundlich模型能更好地描述NH4+-N在天然沸石上的离子交换过程;NH4+-N吸附实验数据与Elovich模型拟合最好(R2≥0.9766).研究结果表明了天然白银沸石是一种适合NH4+-N去除的离子交换剂,可用于黄灌区农田退水中NH4+-N的去除.     

Enhanced nitrogen removal and microbial analysis in partially saturated constructed wetland for treating anaerobically digested swine wastewater

Anaerobically digested swine wastewater was treated by a novel constructed wetland. Tidal operation was better for total nitrogen removal than intermittent flow. Mechanism of nitrogen removal by biozeolite-based constructed wetland was discussed. Simultaneous nitrification and denitrification were determined in zeolite layer. Nitrogen removal of wastewater containing high-strength ammonium by the constructed wetlands (CWs) has been paid much attention. In this study, the ability of a partially saturated CW to treat anaerobically-digested decentralized swine wastewater under varying operating parameters from summer to winter was investigated. The partially saturated CW achieved better NH₄⁺-N and TN removal by tidal flow than intermittent flow. With surface loading rates of 0.108, 0.027, and 0.029 kg/(m²·d) for COD, NH₄⁺-N, and TN, the partially saturated CW by tidal operation achieved corresponding removal efficiencies of 85.94%, 61.20%, and 57.41%, respectively, even at 10°C. When the rapid-adsorption of NH₄⁺-N and the bioregeneration of zeolites reached dynamically stable, the simultaneous nitrification and denitrification in the aerobic zeolite layer was observed and accounted for 58.82% of the total denitrification of CW. The results of Illumina high-throughput sequencing also indicated that nitrifiers (Nitrospira and Rhizomicrobium) and denitrifiers (Rhodanobacter and Thauera) simultaneously existed in the zeolite layer. The dominant existence of versatile organic degraders and nitrifiers/denitrifiers in the zeolite layer was related to the removal of most COD and nitrogen in this zone. The contribution of the possible nitrogen removal pathways in the CW was as follows: nitrification-denitrification (86.55%)>substrate adsorption (11.70%)>plant uptake (1.15%)>microbial assimilation (0.60%).     

A novel polyacrylonitrile–zeolite nanocomposite to clean Cs and Sr from radioactive waste

Radioactive wastes containing Cs⁺ and Sr²⁺ are among the most dangerous environmental pollutants. Therefore, removing Cs⁺ and Sr²⁺ from environmental media is needed. Removal can be done by nanocrystalline ion exchangers. Nanocrystalline ion exchangers are studied in depth for the treatment of nuclear wastes because these exchangers have high exchange capacity and fast kinetics. However, operating the columns of these exchangers is very difficult. This issue may be overcome by the preparation and use of nanocomposites. Here, we prepared a novel polyacrylonitrile–zeolite nanocomposite for the removal of Cs⁺ and Sr²⁺ in a fixed-bed column operation. We studied the effect of influent flow rate, nanocomposite bed height and initial concentrations. Experimental data were analysed using the Thomas model and the bed-depth service time model. The results reveal that total adsorbed ion and bed capacity increased with increasing initial ions concentration and bed height; and decreased with increasing influent flow rate. The maximum bed capacity was 0.085 meq/g for Cs⁺ and 0.128 meq/g for Sr²⁺. The critical bed height (Z ₀) was 4.35 cm for Cs⁺ and 2.89 cm for Sr²⁺. These findings demonstrate that the new nanocomposite is suitable for removal of Cs⁺ and Sr²⁺.     

土壤水分胁迫对花生籽仁矿质元素含量的影响

选用我国北方地区近年来选育或推广应用的29个花生品种（系）,采用全生育期内人工控水盆栽试验,设置正常供水（控制整个生育期土壤含水量为田间持水量的75%~80%）和中度干旱胁迫（控制土壤含水量为田间持水量的45%~50%）2个水分处理。收获后分析籽仁中铁、锌、锰、铝、镉等微量元素和钙、镁、钾、磷、氮等主要矿物质元素含量。结果表明,花生籽仁中铅、铬含量极低,未能检测出;品种间各微量和其他矿质元素含量均存在明显差异,微量元素中,铝平均含量最高,锰含量最低,铁和锌含量居中。干旱使花生籽仁中除铝之外的铁、锌、镉、锰微量元素含量显著增加,尤其是铁,其含量是浇水条件下的2.9倍,其次是镉,为浇水条件下的2.4倍,锌也达1.6倍;但干旱使籽仁中钙、镁含量降低,氮、磷、钾3元素的变化不大,两处理间差异不明显;两处理中除锌元素外其余矿质元素含量间的相关系数间均呈显著或极显著相关关系,镁、锰和镉三元素间的相关系数最大,均在0.95以上,钙次之,磷最小。表明土壤干旱可提高花生籽仁中铁、锌、镉、锰微量元素含量,且微量矿质元素协同效应明显;土壤湿润降低花生籽仁中磷、钾元素与其他矿质元素间的相关关系。     

A model of macroinvertebrate trophic structure and oxygen demand in freshwater wetlands

We present a model of macroinvertebrate trophic structure, detrital cycling, and dissolved oxygen (DO) dynamics in shallow freshwater wetlands with varying allochthonous subsidies. The model is based on field data of primary and secondary production in municipal wastewater-fed and river-fed constructed wetlands in central Ohio, USA. State variables for primary production include macrophyte, periphyton, and metaphyton biomass. Macroinvertebrate biomass is segregated by functional feeding group and includes collectors, scrapers, shredders, and predators. Model simulations demonstrate the association of water column dissolved oxygen, primary production, allochthonous organic matter, and the structure of the macroinvertebrate community. The quality and quantity of allochthonous carbon is shown to have considerable importance, not only as a food source but also as an oxygen sink. Allochthonous carbon equivalent to 5% of autochthonous production increases the macroinvertebrate standing crop by 4–17%, depending on particle size. A large allochthonous subsidy also reduces the simulated average diel dissolved oxygen and increases the percentage of hypoxia-tolerant macroinvertebrates. Simulations show both the heterotrophic response and the changes in community structure brought about by an allochthonous subsidy.     

天然沸石床处理受污染景观水体的试验

采用天然沸石滤床对富营养化景观湖水进行净化试验,结果表明,天然沸石滤床能有效地净化受污染的湖水,CODCr、氨氮、总磷和浊度的去除率分别为35.8%、95.0%、66.7%和78.0%,沸石能有效地去除水中的氨氮,其作用机理包括离子交换和生物硝化两种作用。     

盐碱地农-渔开发对土壤环境的影响

在东北苏打盐碱地进行了稻-鱼-苇-蒲开发试验,并探讨了该模式对盐碱土壤环境的影响。结果表明,开发后土壤有机质含量增加96.8%(平均值,以下同),盐分含量下降43.6%,全量和速效N、P、K质量分数分别增加142.8%和188.2%;阳离子交换量、盐基总量分别增加8.21%及27.71%;土壤腐殖质以富里酸为主,w(HA)/w(FA)比值提高36.15%;养鱼稻田的土壤微生物总量明显高于未养鱼田(P<0.01);优势种为放线菌。土壤酶活性进一步加强。系统废水的盐分质量浓度降至1.0 g/L左右,碱浓度低于水源(7.0~10.0 mmol/L)。该模式不会造成土壤次生盐碱化。