Is The Ca + K + Mg/Al Ratio in the Soil Solution a Predictive Tool for Estimating Forest Damage?

The ratio between (Ca +K +Mg) and Al in nutrientsolution has been suggested as a predictive tool forestimating tree growth disturbance. However, the ratiois unspecific in the sense that it is based on severalelements which are all essential for plant growth;each of these may be growth-limiting. Furthermore,aluminium retards growth at higher concentrations. Itis therefore difficult to give causal and objectivebiological explanations for possible growthdisturbances. The importance of the proportion ofbase-cations to N, at a fixed base-cation/Al ratio, isevaluated with regard to growth of Picea abies.The uptake of elements was found to be selective;nutrients were taken up while most Al remained insolution. Biomass partitioning to the roots increasedafter aluminium addition with low proportions of basecations to nitrogen. We conclude that the low growthrates depend on nutrient limitation in thesetreatments. Low growth rates in the high proportionexperiments may be explained by high internal Alconcentrations. The results strongly suggest thatgrowth rate is not correlated with the ratio in therooting medium and question the validity of usingratios as predictive tools for estimating forestdamage. We suggest that growth limitation of Picea abies in the field may depend on lowproportions of base cations to nitrate. It istherefore important to know the nutritional status ofthe plant material in relation to the growth potentialand environmental limitation to be able to predict andestimate forest damage.     

缺氧环境下硫酸盐还原对反硝化过程影响的特性试验研究

对缺氧环境下硫酸盐还原对反硝化脱氮过程影响进行了试验研究。试验结果表明和单纯的热力学和动力学分析不同,在硫酸盐和硝酸盐同时存在的生物脱氮体系中,具备着反硝化和硫酸盐还原同时进行的环境条件。缺氧环境下硫酸盐还原过程影响了反硝化脱氮效果和反硝化历程,即硫酸盐初始浓度越高,硝氮的去除率越低,当硫酸盐浓度从0mg/L增加到2000mg/L时,脱氮效率从100%降低到81.4%,脱氮速率从6.428mg/L.min降低到4.04mg/L.min,并且发现在硫酸盐影响下的反硝化过程出现了氨氮积累的现象。本研究结果对富含硫酸盐的有机废水生物处理有指导意义。     

总磷测定中温度浓度时间对显色的影响

对钼酸铵分光光度法测定水质中总磷时温度、浓度、时间与显色反应的规律进行了研究,给出了吸光度对温度、浓度和显色时间的变化曲线,和不同温度下的标准曲线的线性相关性,指出了不同温度时,吸光度随时间的变化。从而得到了达到最大显色所需要的时间,以指导标准曲线的绘制,提高样品测定精度。     

曝气生物滤池内的自养反硝化作用

采用多孔介质——火山岩为载体的上向流曝气生物滤池(BAF),研究了限制供氧条件下,无有机碳源时反应器的硝化反硝化特性.结果表明,在 10～30℃范围内,20℃为临界点,低于20℃时,硝化速率缓慢;高于 20℃后,硝化速率加快.温度从 20℃升高到 30℃,硝化速率增长仅为10%,这一特性与悬浮生长反应器内温度对硝化速率的影响完全不同.此外,稳定运行的 BAF 内存在大量氮流失现象,分析认为,限制供氧和无有机碳源时,生物膜内发生了以 Anammox反应为主的自养反硝化作用,大量的氮以 N₂的形式流失.     

粉煤灰合成沸石同步脱氨除磷特性的研究

利用粉煤灰合成沸石,研究其在同步去除氮、磷方面的特性.合成沸石对氨氮和磷酸盐的吸附净化均随时间增加而变化,但均在24h后基本达到平衡.随合成沸石投加量的增加,同步去除污水中氮磷的效果越好,但在投加量为8 g·L^-1以上时去除率的增加明显放慢.在pH为7～9时氨氮去除率最高(约60%),超过此pH范围时去除率降低.在pH 7～9范围磷去除率达最低(约为85%),超过此pH范围时去除率增加(最高达到近100%).合成沸石对氨氮的吸附为放热反应,对磷的吸附为吸热反应.不同阳离子饱和的合成沸石对氨氮的吸附顺序依次为:Al>Mg>Ca>Na>Fe,对磷的吸附顺序则为:Al>Fe>Ca>Mg>Na.合成沸石的氨氮吸附机理为阳离子交换作用,对磷的去除除化学沉淀作用外尚有吸附机制.     

曝气生物滤池快速启动和活性保持性能研究

研究了两级曝气生物滤池处理生活污水时各级的快速启动和在低负荷下活性保持的能力,考察了出水中主要污染物和生物滤池内生物量随时间的变化情况。结果表明,碳氧化生物滤池从低负荷恢复时,所需要的时间与活性保持时的负荷大小有关,负荷越小,所需要的时间越长。在极端情况下,恢复时间接近一次完全启动的时间,因此碳氧化生物滤池的低负荷维持并没有太大的实际意义。而硝化生物滤池在低负荷下活性保持良好,重新启动仅需要完全启动1/10的时间,这就有可能以低成本实现硝化生物滤池的活性保持。     

沉淀分离富集-分光光度法测定海水中痕量活性磷酸盐

十六烷基三甲基溴化铵(cetyltrimethylammonium bromide,CTAB)可与磷钼蓝(phosphomolybdenum blue,PMB)生成水难溶的PMB-CTAB离子缔合物沉淀,从而分离富集水溶液中的PMB。该沉淀易溶于硫酸乙醇溶液,溶液在700 nm有强吸收,基于此建立了沉淀分离富集-分光光度法测定海水中痕量活性磷酸盐的新方法。对溶剂酸度、试剂用量、反应时间与温度等实验参数进行了优化选择,并考察了盐度对测定结果的影响。实验结果表明,PMB可被CTAB有效地定量沉淀;盐度在15~45范围内,对测定结果无影响。在优化的实验条件下,以盐度为35的人工海水为基底,做空白加P标实验,方法的线性范围为0.30~8.00μg/L,平均回收率为95.0%,方法检测限为0.10μg/L。对实际海水中痕量活性磷酸盐进行测定,相对标准偏差(RSD)为4.4%~7.1%,与广泛采用的MAGIC法比较,置信度为99%时结果无显著差异。新方法具有消耗试样体积少、测定速度快等优点。     

Biological conversion pathways of sulfate reduction ammonium oxidation in anammox consortia

• The SRAO phenomena tended to occur only under certain conditions. • High amount of biomass and non-anaerobic condition is requirement for SRAO. • Anammox bacteria cannot oxidize ammonium with sulfate as electron acceptor. • AOB and AnAOB are mainly responsible for ammonium conversion. • Heterotrophic sulfate reduction mainly contributed to sulfate conversion. For over two decades, sulfate reduction with ammonium oxidation (SRAO) had been reported from laboratory experiments. SRAO was considered an autotrophic process mediated by anammox bacteria, in which ammonium as electron donor was oxidized by the electron acceptor sulfate. This process had been attributed to observed transformations of nitrogenous and sulfurous compounds in natural environments. Results obtained differed largely for the conversion mole ratios (ammonium/sulfate), and even the intermediate and final products of sulfate reduction. Thus, the hypothesis of biological conversion pathways of ammonium and sulfate in anammox consortia is implausible. In this study, continuous reactor experiments (with working volume of 3.8L) and batch tests were conducted under normal anaerobic (0.2≤DO<0.5 mg/L) / strict anaerobic (DO<0.2 mg/L) conditions with different biomass proportions to verify the SRAO phenomena and identify possible pathways behind substrate conversion. Key findings were that SRAO occurred only in cases of high amounts of inoculant biomass under normal anaerobic condition, while absent under strict anaerobic conditions for same anammox consortia. Mass balance and stoichiometry were checked based on experimental results and the thermodynamics proposed by previous studies were critically discussed. Thus anammox bacteria do not possess the ability to oxidize ammonium with sulfate as electron acceptor and the assumed SRAO could, in fact, be a combination of aerobic ammonium oxidation, anammox and heterotrophic sulfate reduction processes.     

钼酸铵生产废液的综合治理

钼酸铵生产过程中产生的酸性废液,经中和,过滤,滤渣热碱浸取、滤液蒸发浓缩等步骤,可回收废液中的７９％的钼,并获得ＮＨ４ＮＯ３、ＮＨ４Ｃｌ混合液体肥料。     

利用白云石石灰去除与回收污泥厌氧消化液中氮和磷

以白云石石灰为实验材料去除与回收污泥厌氧消化液中的氮磷,通过小试实验研究不同投药固液比S/L、初始pH值、反应温度、搅拌速度及反应时间对去除与回收氮磷效果的影响。实验结果表明,在最佳投药固液比S/L为300mg/L,最佳初始pH值范围为8.5~9.5,反应温度为25.0℃,搅拌速度为150 r/min,反应时间为24 h条件下,氨氮(NH+4-N)和磷(PO3-4-P)的去除率分别为37.26%和89.60%。利用X射线衍射仪(XRD)、扫描电镜(SEM)对沉淀产物进行了表征,通过分析可知沉淀产物中含有磷酸铵镁(MAP),可实现废水中氮磷经济有效的回收。