甲氰菊酯在土壤中的降解与移动性

采用模拟试验和田间试验相结合的方法,研究了甲氰菊酯在南方菜地土壤中的降解和移动.得出了一些基本数据,为甲氰菊酯在菜地(旱地)生态中的安全使用,提出了合理的评价.     

BOD微生物传感器的研究

本实验从活性污泥中分离筛选出一株对广泛底物具有外源呼吸的假单胞菌(Pseudomonas sp.A_4)。用该种菌株制成的BOD微生物传感器可在15min内完成一个样品BOD的测定。该法与传统方法有较好的相关性,可连续使用六周以上。     

旅游踩踏对土壤微生物生物量碳、氮、磷的影响

为了探明旅游活动对张家界国家森林公园土壤微生物活性及多样性的影响,保护土壤生态平衡及合理开发自然保护区提供理论依据,进行了旅游踩踏对土壤微生物生物量碳、氮、磷的影响研究.结果表明,在所设的3个试验区中,0～5cm土壤层的微生物生物量碳、磷受到旅游踩踏的影响最严重,5～15cm土壤层的微生物生物量碳、磷受到旅游踩踏的影响较严重,而15～25cm土壤层的微生物生物量碳、磷受到旅游踩踏的影响最轻,旅游踩踏对所设3个试验区中3个层次土壤的微生物生物量碳、磷的影响均达到了显著水平(p＜0.05).从旅游踩踏对3个土壤层的微生物生物量氮的影响程度来看,0～5cm土壤层的微生物生物量氮受到的影响最严重,5～15cm土壤层的微生物生物量氮受到的影响较严重,而15～25cm土壤层的微生物生物量氮受到的影响最轻,背景区与缓冲区15～25cm土壤层的微生物生物量氮差异没有达到显著水平.说明张家界国家森林公园土壤微生物遭到了旅游踩踏的破坏,抵御外界干扰的能力已受到了旅游踩踏的破坏.     

Solid phase extraction of methomyl and thiodicarb from environmental water with an activated carbon cartridge and their determination by HPLC

ＩｎｔｒｏｄｕｃｔｉｏｎＢｏｔｈｍｅｔｈｏｍｙｌａｎｄｔｈｉｏｄｉｃａｒｂａｒｅＮｍｅｔｈｙｌｃａｒｂｍａｔｅｐｅｓｔｉｃｉｄｅｓ.Ｍｅｔｈｏｍｙｌｉｓｅｆｆｅｃｔｉｖｅｏｎａｗｉｄｅｒａｎｇｅｏｆｉｎｓｅｃｔｓａｓａｎｏｖｉｃｉｄｅ,ｌａｒｖｉｃｉｄ...     

气相连通罐组群罐燃爆风险定量评估技术研究

炼化企业气相连通罐组存在群罐重大火灾风险,需要采取系统评估、层层设防的思路进行防控。采用HALOPA技术,结合中国石化风险矩阵标准,建立基于风险的气相连通罐组重大燃爆风险控制准则、不同罐容的事故后果等级划分标准、各类保护措施的风险消减因子和燃爆事件可能性评估方法以及相关重要设计要求。案例分析表明,VOCs气相连通罐组群罐燃爆风险定量评估方法可对群罐火灾风险进行快速量化评估,可用于气相连通罐组的风险评估和工程安全设计。     

利用粉煤灰制备高纯超细氧化铝粉体的研究

利用粉煤灰为原料制备高纯超细氧化铝粉体。给出了采用硅酸二钙晶相转变自粉化、高效分散剂———碳化法从粉煤灰中制备氧化铝方法的工艺路线 ,确定了从粉煤灰制备高纯超细氧化铝粉体的最佳工艺条件 ,为粉煤灰的高价值利用开辟了一条新途径     

阴极极化对金属电极表面微生物膜的影响

阴极极化对不锈钢表面微生物膜的附着有一定的影响,通过 荧光显微镜记数和细菌双染色方法(AO+PI),对在不同电位下极 化过的不锈钢表面进行了观察,同时做了对比实验。实验证明在一 定的范围内(-800mV~-1000mV),阴极极化对微生物向洁净金属 表面的附着有一定的抑制作用,但是对已经附着的微生物膜不能 够起到脱除或完全杀灭作用,只能杀死靠近金属表面的微生物。通 过模拟膜实验,从侧面证明了只有微生物膜附着而无生物活性时, 钝性金属的开路电位不会发生正移。     

Determination and discussion hydraulic retention time in membrane bioreactor system

Based on the microorganism kinetic model, the formula for computing hydraulic retention time in a membrane bioreactor system (MBR) is derived. With considering HRT as an evaluation index a combinational approach was used to discuss factors which have an effect on MBR. As a result, the influencing factors were listed in order from strength to weakness as: maximum specific removal rate K, saturation constant Ks, maintenance coefficient m, maximum specific growth rate ,ua and observed yield coefficient Yobs. Moreover, the formula was simplified, whose parameters were experimentally determined in petrochemical wastewater treatment. The simplified formula is θ= 1.1( 1/β -1)(Kｓ S)/KXo , for oetroehemical wastewater treatment K and Ko eaualed 0.185 and 154.2, resoectively.     

循环流化床锅炉床温控制方法

就目前电厂循环流化床锅炉运行中存在的床温波动问题，讨论了导致床温波动的因素，并针对性地提出了控制床温的一些措施。     

Characterisation of Organic Matter and Carbon Cycling in Rehabilitated Lignite-rich Mine Soils

Open-cast lignite mining in the Lusatian mining district resulted in rehabilitated mine soils containing up to four organic matter types: (1) recent plant litter, (2) lignite deposited by mining activity, (3) carbonaceous ash particles deposited during amelioration of the lignite-containing parent substrate and (4) airborne carbonaceous particles deposited during contamination. The influence of lignite-derived carbon types on the organic matter development and their role in the soil carbon cycle was unknown. This paper presents the findings obtained during a six year project concerning the impact of lignite on soil organic matter composition and the biogeochemical functioning of the ecosystem. The organic matter development after rehabilitation was followed in a chronosequence of rehabilitated mine soils afforested in 1966, 1981 and 1987. A differentiation of the organic matter types and an evaluation of their role within the ecosystem was achieved by the use of ¹⁴C activity measurements, ¹³C CPMAS NMR spectroscopy and wet chemical analysis of plant litter compounds. The results showed that the amount and degree of decomposition of the recent organic matter derived from plant material of the 30 year old mine soil was similar to natural uncontaminated forest soil which suggests complete rehabilitation of the ecosystem. The decomposition and humification processes were not influenced by the presence of lignite. On the other hand it was shown that lignite, which was thought to be recalcitrant because of its chemical structure, was part of the carbon cycle in these soils. This demonstrates the need to elucidate further the stabilisation mechanisms of organic matter in soils.