氮输入对纳帕海沼泽湿地土壤氨挥发和反硝化的影响

选取纳帕海常见湿地植物茭草（Zizania caduciflora）和水葱（Scirpus validus）]及其生长土壤为对象,通过培养实验,研究了3个不同氮输入水平[0g-m^2（对照,NO）、20g-m^2（N20）、40g-m^2。（N40）]对茭草和水葱湿地土壤氨挥发和反硝化的影响。结果表明：氮输入促进了茭草和水葱湿地土壤氨挥发化作用,增加了湿地土壤氨挥发的累积量。适量的氮输入对湿地土壤氨挥发促进显著。在培养前期适量氮输入下的氨挥发积累量高于高水平氮输入的,随着培养时间的延长,后期适量氮输入下的积累量明显下降;而高水半氮输入处理下氨挥发积累量的明显增加,适量氮输入下茭草氨挥发积累大于水葱。氮输入增强了菱草和水葱湿地土壤反硝化作用,加快了反硝化N2O的排放。适量的氮输入促进茭草反硝化作用和反硝化损失量增加明显,培养的前期的适量氮输入处理下的反硝化作用和反硝化N2O的排放增强不明显,随着培养时间的延长,高水平氮输入处理下的反硝化损失量越明显,并且水葱较茭草更为明显。后期适量氮输入下的反硝化损失速率和反硝化损失量高于高水平氮输入,适量氮输入较高水平氮输人促进明显,高水平的氮输入限制了反硝化损失,反硝化N2O的排放总量下降,土壤中氮富集增大。     

影响石油污染物挥发行为的因素

进行了4种不同石油制品在不同温度时的挥发试验,并对其挥发量与挥发时间的关系进行了模拟,试验结果表明,柴油和煤油的挥发量与挥发时间呈二次多项式关系,而90#汽油的挥发量与挥发时间呈对数关系,混合芳烃的挥发量与挥发时间呈线性关系。柴油经过不同程度的挥发后,其物理性质如粘度和比重发生了改变,其中柴油粘度随着挥发而增加,并且柴油的粘度与挥发质量分数有很好的正相关性,相关系数为0.988。     

土层中石油烃类污染物索氏抽提流程改进及回收氯仿资源化研究

通过对土层中石油烃类污染物索氏抽提流程的改进 ,实现蒸馏氯仿的回收与再利用。实验结果表明 ,用改进索氏抽提流程测的有机物含量与传统的流程相比 ,所减少的石油烃类物质损耗占总石油物质含量的 1 0 % ;同时 ,蒸馏回收的氯仿的 70 %可以重新用于索氏抽提 ,由此产生的误差小于 1 % ,不会影响残油微生物降解试验的分析精度 ,具有资源回收与保护环境的双重效应     

Mercury remediation potential of a mercury resistant strain Sphingopyxis sp. SE2 isolated from contaminated soil

A mercury resistant bacterial strain SE2 was isolated from contaminated soil.The 16 s rRNA gene sequencing confirms the strain as Sphingopyxis belongs to the Sphingomonadaceae family of the α-Proteobacteria group.The isolate showed high resistance to mercury with estimated concentrations of Hg that caused 50%reduction in growth(EC_(50)) of 5.97 and 6.22 mg/L and minimum inhibitory concentrations(MICs) of 32.19 and 34.95 mg/L in minimal and rich media,respectively.The qualitative detection of volatilized mercury and the presence of mercuric reductase enzyme proved that the strain SE2 can potentially remediate mercury.ICP-QQQ-MS analysis of the remaining mercury in experimental broths indicated that a maximum of 44%mercury was volatilized within 6 hr by live SE2 culture.Furthermore a small quantity(23%) of mercury was accumulated in live cell pellets.While no volatilization was caused by dead cells,sorption of mercury was confirmed.The mercuric reductase gene merA was amplified and sequenced.Homology was observed among the amino acid sequences of mercuric reductase enzyme of different organisms from a-Proteobacteria and ascomycota groups,     

我国半干旱区滴灌水肥一体化马铃薯田土壤NH3挥发特征和强度及影响因素

氨(NH₃)挥发是农业生态系统氮肥损失的重要途经,然而,北方干旱半干旱地区水肥耦合马铃薯田土壤NH₃挥发规律缺少数据支撑.该研究利用通气法田间原位观测我国西北滴灌水肥一体化和传统沟灌施肥马铃薯田水肥耦合土壤NH₃挥发特征,设置滴灌施肥500 kg·hm^-2(DDF)、滴灌施肥1000 kg·hm^-2(DGF)、滴灌不施肥(DCK)、沟灌施肥500 kg·hm^-2(FDF)、沟灌施肥1000 kg·hm^-2(FGF)、沟灌不施肥(FCK)6个处理.结果表明,NH₃挥发速率峰值出现在施用氮肥后1—2周,不同水肥处理土壤NH₃挥发存在显著差异(P<0.01).2018年DDF、DGF、DCK、FDF、FGF、FCK土壤NH₃累积挥发量分别为21.50、28.14、7.20、37.06、66.25、11.88 kg·hm^-2;2019年,分别为9.42、15.25、7.24、34.73、76.81、8.56 kg·hm^-2.2018年和2019年,沟灌FDF处理的NH₃挥发损失率分别是滴灌DDF处理的1.76倍和11.89倍;沟灌FGF处理分别是滴灌DGF的2.60倍和8.54倍.滴灌DGF处理NH₃挥发强度比滴灌DDF处理分别增加27.03%和52.94%,沟灌FGF处理比沟灌FDF处理分别增加76.04%和118.37%.随施肥量增加,传统沟灌马铃薯田土壤NH₃挥发损失率和NH₃挥发强度的增量高于滴灌水肥一体化模式.NH₃挥发速率与土壤体积含水量、NH₄⁺-N和NO₃^--N呈极显著相关(P<0.01).和传统沟灌比较,滴灌水肥一体化技术降低马铃薯田土壤NH₃挥发损失率,减轻NH₃挥发强度,提高马铃薯水肥利用率,减轻环境污染.     

Ammonia volatilization from a Chinese cabbage field under different nitrogen treatments in the Taihu Lake Basin, China

Ammonia(NH_3) volatilization is a major pathway of nitrogen(N) loss from soil-crop systems.As vegetable cultivation is one of the most important agricultural land uses worldwide,a deeper understanding of NH_3 volatilization is necessary in vegetable production systems.We therefore conducted a 3-year(2010–2012) field experiment to characterize NH_3 volatilization and evaluate the effect of different N fertilizer treatments on this process during the growth period of Chinese cabbage.Ammonia volatilization rate,rainfall,soil water content,p H,and soil NH_4~+were measured during the growth period.The results showed that NH_3 volatilization was significantly and positively correlated to topsoil p H and NH4+concentration.Climate factors and fertilization method also significantly affected NH_3 volatilization.Specifically,organic fertilizer(OF) increased NH_3 volatilization by 11.77%–18.46%,compared to conventional fertilizer(CF,urea),while organic–inorganic compound fertilizer(OIF) reduced NH_3 volatilization by 8.82%–12.67% compared to CF.Furthermore,slow-release fertilizers had significantly positive effects on controlling NH_3 volatilization,with a 60.73%–68.80% reduction for sulfur-coated urea(SCU),a 71.85%–78.97% reduction for biological Carbon Power~#174; urea(BCU),and a 77.66%–83.12% reduction for bulk-blend controlled-release fertilizer(BBCRF)relative to CF.This study provides much needed baseline information,which will help in fertilizer choice and management practices to reduce NH_3 volatilization and encourage the development of new strategies for vegetable planting.     

高炉洗气含氰废水除氰方法研究—气化分离与富集

本文用ＣＯ２气体气体化分离含氰废水中的氰，用乙醛等醛类吸收富集挥发出来的氰化氢而使氰以回收利用。气化分离除氰后，水中残余氰的浓度小于０．５ｐｐｍ。对醛类与ＨＣＮ反应的动力学和热力学性质的研究和吸收试验表明，乙醛等低分子醛能快速和完全地吸收气化分离出的ＨＣＮ，并得到α－羟基腈、羟基酸及其盐等系列产品。     

抑制剂对淹水土壤反硝化和氨挥发的影响

通过室内培养试验,设置3个硝化抑制剂双氰胺（DCD）（氮肥用量的2.5%（DCD1）、5.0%（DCD2）、7.5%（DCD3））,3个脲酶抑制剂氢醌（HQ）（氮肥用量的0.1%（HQ1）、0.3%（HQ2）、0.5%（HQ3））和3个硝化抑制剂DCD+脲酶抑制剂HQ联合施用（氮肥用量的2.5%+0.1%（HH1）、5.0%+0.3%（HH2）、7.5%+0.5%（HH3））试验处理,探讨抑制剂联合施用对淹水土壤反硝化和氨挥发过程及其环境因子的影响,并借助通径分析探讨环境因子对反硝化和氨挥发过程的影响程度,探求抑制剂、氮素转化过程及其环境因子之间定量影响关系.结果表明,单独施用硝化抑制剂DCD能显著减少反硝化速率,但是增加氨挥发损失.单独施用脲酶抑制剂HQ能不同程度减少氨挥发损失,但对反硝化作用效果不稳定.而联合施用DCD和HQ,尤其是HH2（5.0%的DCD+0.3%的HQ）联合施用可有效地同时抑制反硝化和氨挥发损失,相比CK,其反硝化和氨挥发速率分别减少31.3%和12.5%.通径分析发现,硝化抑制剂DCD和脲酶抑制HQ主要影响土体NO₃^--N和NH₄⁺-N浓度、上覆水体NH₄⁺-N和DON浓度,从而影响反硝化和氨挥发速率.     

垃圾焚烧飞灰热处理过程中Zn的挥发机理研究

试验在650~1350℃条件下探讨了温度和时间对飞灰中Zn的挥发率的影响,采用XAFs对飞灰及二次飞灰中Zn的赋存形态进行分析,运用吉布斯自由能理论推导了Zn的氯化反应途径,并开展了验证试验.结果表明：温度是影响Zn挥发的主要因素,其挥发趋势随温度先增加而后降低,在1000℃时挥发率达到最高,而时间对其挥发效果影响较小;Zn主要以氯化物形态挥发,从假设反应途径的吉布斯自由能理论计算及验证试验得出,热处理过程中Zn的氯化反应分两步进行,首先飞灰中氯化物与SiO₂反应生成Cl₂,而后与ZnO反应生成ZnCl₂,而小部分Cl₂可能与水蒸气反应形成HCl,再与ZnO反应生成ZnCl₂.     

A Relaxed Eddy Accumulation System for the Automated Measurement of Atmospheric Ammonia Fluxes

A continuous relaxed eddy accumulation system ispresented for the automated measurement of surface/atmosphere exchange fluxes of atmospheric ammonia (NH₃) at a single height. The new system features sampling by parallel plate denuder inlets, online chemical analysis using the conductivity cell of a commercially available NH₃ analyzer and online flux calculation. The effective detection limit of the system for air concentrations is 0.2 g m^-3 and it is estimated to resolve fluxes > ± 20 ng m^-2 s^-1, depending on the NH₃ concentration and turbulence. The performance of the system was tested in two measurement campaigns above agricultural grassland, in which it was compared with a 3-point continuous gradient system. During the first campaign, after urea application of 47 kg N ha^-1 in autumn, the REA system derived fluxes which were on average twice as large as the gradient fluxes, while concentrations agreed closely (on average within 4%). Possible reasons include differences in the footprint and an over-correction of the gradient flux in stable conditions. Due to wet and cold conditions, only 0.3% of the fertilizer N was volatilized as NH₃ during the first week. Results from the deployment of an improved system are presented for a summer day, 6 days after fertilization with calcium ammonium nitrate. The agreement of both concentrations (on average within 13%) and fluxes (26%) was very encouraging and similar to the agreement found between two state-of-the-art gradient systems with online analysis.