交替冻融对东北地区典型土壤氮磷浓度的影响

研究了交替冻融对东北地区黑土、暗棕壤和水稻土中的全氮、有效氮、全磷和有效磷的影响。结果表明,经过15次交替冻融后,三种类型土壤的全氮浓度均未发生明显变化,说明在交替冻融过程中,硝化与反硝化共同作用并不明显。由于冻融作用增强土壤释水性和水分渗透性,经15次交替冻融后,黑土、暗棕壤和水稻土的有效氮浓度均有所升高,以水稻土最显著,上升了31.25%。三种土壤全磷浓度均在初次冻融后大幅增高,总体呈升高趋势,分析原因主要是冻融作用破坏了土壤团聚体,增加了与消化液反应的机会。经15次交替冻融后,黑土和水稻土的有效磷浓度分别上升17.72%和56.16%,暗棕壤的有效磷浓度下降35.19%,这说明交替冻融过程中土壤有效磷的变化不但取决于土壤的C/P,还受土地利用类型的影响,林地的有效磷浓度可能由于发生磷的净固定而降低。     

SBBR工艺处理有机农药废水的生产性试验

为了实现SBBR工艺处理有机农药废水在生产上的应用,选择有代表性的农药厂进行生产性试验。试验结果表明:COD、BOD5、SS、TP平均去除率分别为90.1%、91%、88.8%和94.7%,出水水质达到GB8978-1996《污水综合排放标准》中的二级标准,并且运行稳定、投资省。     

盐碱土壤基质人工湿地对低浓度氮磷废水的净化效果

采用实验室模拟研究了以盐碱土壤为基质的不同湿地植物人工湿地系统以及对水中低质量浓度氮和磷的去除效率。实验表明，芦苇系统、香蒲系统、车钱草系统和无植物系统均对水中低质量浓度的N具有净化效果。3种植物系统相比，香蒲系统的净化效果较其他二者较佳，芦苇系统与车钱草的净化效果相当；同时实验也表明4种湿地系统对低质量浓度的P不具有净化效果，随着水力停留时间的增加，系统中的P质量浓度反而会有所增加。     

不同施肥措施对棉田土壤磷细菌及磷转化强度的影响

研究了不同施肥措施对棉田土壤磷细菌的数量、分布、动态变化及磷转化强度的影响.结果表明,有机肥合理配施N、P、K肥能有效的促进磷细菌的生长发育,磷细菌数量及活性增加,从而增强磷的有效性,改善土壤的供磷性能,有利于棉花生长.     

The Influence of Mycorrhiza on Uranium and Phosphorus Uptake by Barley Plants from a Field-contaminated Soil (7 pp)

Background Recent studies indicated that arbuscular mycorrhizal fungi (AMF) play important roles in plant accumulation of uranium (U) from contaminated environments, but the impacts of fertilization practices on functioning of the symbiotic associations, which are crucial factors influencing plant nutrition and growth responses to mycorrhiza, have rarely been considered. Materials and Methods In a greenhouse experiment, a bald root barley mutant (brb) together with the wild type (wt) were used to test the role of root hairs and AMF in uranium (U) uptake by host plants from a U contaminated soil. Nil, 20 and 60 mg KH2PO4-P kg–1 soil were included to investigate the influences of phosphorus (P) fertilization on plant growth and accumulation of U. Results Dry matter yield of barley plants increased with increasing P additions and wt produced significantly higher dry weight than brb. Mycorrhiza markedly improved dry matter yield of both genotypes grown at nil P, whereas only brb responded positively to mycorrhiza at 20 mg P kg-1. At the highest P level, mycorrhiza resulted in growth depressions in both genotypes, except for the roots of wt. In general, plant P concentrations increased markedly with increasing P additions and in response to mycorrhiza. Mycorrhiza and P additions had no significant effects on shoot U concentrations. However, root U concentrations in both genotypes were significantly increased by mycorrhiza. On the other hand, shoot U contents increased with increasing P levels, while 20 mg P kg-1 stimulated, but 60 mg P kg-1 marginally affected the U accumulation in roots. Root length specific U uptake was moderately enhanced both by root hairs and strongly enhanced by mycorrhiza. Moreover, non-inoculated plants generally had higher shoot-root ratios of U content than the corresponding inoculated controls. Conclusion Our study shows that AMF and root hairs improves not only P acquisition but also the root uptake of U, and mycorrhiza generally decreases U translocation from plant root to shoot. Hence, mycorrhiza is of potential use in the phytostabilization of U contaminated environments. Perspectives The complex impacts of P on U accumulation by barley plants suggested that U behavior in mycorrhizosphere and translocation along the soil-fungi-plant continuum as affected by fertilization practices deserve extensive studies for optimizing the function of mycorrhizal associations for phytoremediation purposes.     

利用微拟球藻去除污水中氮磷及生产富油生物质

为探讨污水深度处理和同步获取产油微藻的可行性,建立光生物反应器,应用微拟球藻去除污水和中水中的氮磷,并分析不同浓度的Fe3+和Zn2+离子对微藻的生长和油脂积累的影响,从而在净化污水的同时培养微藻获得富油生物质。结果表明,该藻对污水氮磷具有较强的去除能力,可在13 d内,去除水体中96%的氨氮和94%的磷,同时化学需要氧量(COD)的去除率可达72.9%。在生活污水中培养至第16天,微藻的细胞密度可达4.55×106 cell/mL。Fe3+浓度对微拟球藻的生长具有显著影响(P6 cell/mL。该研究以中水和生活污水为基质培养微拟球藻,同时获取微藻油脂,为污水中氮磷的去除和能源的同步获取提供了新途径。     

废水除磷技术的研究与发展

目前 ,人们越来越重视污水除磷技术。本文介绍与评述了化学和生物两种除磷方式及其除磷机理和工艺 ,并着重介绍了生物除磷的现状、发展和研究动向     

组合骨料型百喜草植生混凝土去除氮磷

以6组90 d龄期的组合骨料型百喜草植生混凝土盆栽为研究对象,用配制溶液静态培养的方法,选择氨氮(NH3-N)、总氮(TN)和总磷(TP)为主要指标,考查沸石与钢渣、沸石与浮石两种组合骨料型的植生混凝土对污染物的去除效果。结果表明,各组NH3-N 1 d、7 d的去除率分别为13.0%~16.9%和45.7%~56.7%,1 d去除率约占7 d的30%。各组TN 1 d、7 d的去除率分别为9.0%~14.1%和25.6%~39.2%,1 d去除率约占7 d的30%。各组TP 1 d、7 d的去除率分别为22.0%~33.3%和57.3%~89.3%,1 d去除率约占7 d的40%。NO3--N、NO2--N含量很低,NO3--N浓度基本在0.50 mg/L以下,NO2--N浓度变化范围在0.10 mg/L以下。综合NH3-N、TN和TP去除效果,沸石与浮石按1:1~1:3混合的百喜草植生混凝土具有良好的脱氮除磷效果。     

原位洗脱技术对凉水河底泥中氮、磷释放特征的影响

为探讨新兴底泥原位修复技术—原位洗脱技术对城市河流凉水河底泥中氮、磷释放的抑制作用,于现场采集洗脱前后样品并设计室内静态模拟实验,分析了实验期间洗脱组和对照组上覆水中${{\rm{NH}}_4^ + }$-N、${{\rm{NO}}_3^ - }$-N、TN、${{\rm{PO}}_4^{3 - }}$-P、TP浓度和释放速率变化特征。结果表明：洗脱组释放第30天时,${{\rm{NH}}_4^ + }$-N由底泥向上覆水中平均释放速率(−6.51±0.32) mg·(m²·d)⁻¹,对应上覆水中${{\rm{NH}}_4^ + }$-N平均浓度为0.52 mg·L⁻¹,较对照组下降了89.4%;${{\rm{PO}}_4^{3 - }}$-P和TP平均释放速率较对照组降低了78.1%和83.0%,上覆水中TP平均浓度为0.22 mg·L⁻¹,较对照组下降了68.1%。原位洗脱技术对底泥中${{\rm{NH}}_4^ +} $-N、${{\rm{PO}}_4^{3 - }}$-P释放的抑制作用主要通过对有机氮、磷物质的削减和水-沉积物界面还原环境的改善来实现。     

水热+厌氧消化对污泥碳、氮、磷溶出的影响

研究了水热预处理和厌氧消化联合作用时温度对污泥中碳、氮、磷溶出的影响。结果表明:水热处理温度越高越有利于污泥中碳氮磷的溶出,当水热温度为200 ℃时,SCODCr的溶出率较原泥提高了5.9倍;氨氮和总氮的溶出率分别提高了7.2和8.7倍;磷酸根和总磷的溶出率分别提高了0.2和6.1倍。厌氧消化后污泥中碳磷浓度下降,而氮浓度上升。厌氧消化后累积产气量与水热温度有关:当温度为160 ℃时,最大累积产甲烷量为12 223 L/mg-CO D C H 4 (以每mg COD的产甲烷量计),较原泥提高了14.5倍。根据试验结果,提出了从水热和厌氧消化污泥中回收氮磷的策略,即水热处理污泥后可在污泥清液中投加镁源进行磷的回收,厌氧消化中溶出的氮可通过加入吸附材料进行吸附回收。在污泥中氮磷资源回收的同时,可通过水热过程提高污泥厌氧过程中累积产甲烷量。