起居室典型材料的火灾温度场实验研究

就建筑火灾发生频率较高的起居室为研究对象,主要对该类住宅中的一些常见和使用广泛的典型家具及装修材料,纸张（报纸）、多层胶合板以及软垫分别进行了火灾燃烧实验,对火场中重要参数温度场进行了测试与分析。对由典型装修材料组成的单室,既起居室火灾进行了全尺寸火灾实验,目的是掌握起居室内火灾的发生发展、燃烧过程和火灾蔓延特点。研究表明,住宅火灾中聚合材料、人工填充泡沫等人造材料的热释放速率最大,最高可达305kW,是火灾前期起居室升温的主要热源;全尺寸火灾实验过程中火焰蔓延较快,扩展幅度较大,蔓延过程中多股火焰交叉处温度可达250％左右,容易造成火势火场传播,同时释放出大量深色烟气,火场能见度极低。全尺寸起居室实验表明,短短3min27s内火场温度达到850℃。     

两种水源的水质及其混凝效果对比

针对一年中长江原水和黄浦江原水的水质情况,进行了两种原水几种水质指标的对比分析,混凝沉淀后两种原水氨氮和CODMn的达标情况对比,以及不同水温对于两大原水浊度、氨氮和CODMn混凝效果的影响。结果表明,黄浦江原水的浊度、氨氮和CODMn一般比长江原水高,pH比长江原水低,经过混凝沉淀处理后长江原水氨氮和CODMn的达标率比黄浦江原水高,两种原水的浊度、氨氮和CODMn的去除率随水温的升高有增大的趋势,若两种原水进行混合,为保证其处理后水质达标,则黄浦江和长江原水的配比最好不能超过2∶8。     

膜法处理低温低浊水技术综述

低温低浊水的处理是给水处理的一个难点.分析了常规混凝方法难处理低温低浊水的原因,介绍和比较了膜处理低温低浊水的4种方法.研究结果表明,膜法出水水质好、稳定,采用低压膜直接过滤降低能耗,节省药剂投加费用;混凝-超滤工艺中加入粉末活性炭后可增加溶解性有机物的去除,膜生物反应器能有效去除氨氮.膜法处理低温低浊水对浊度和有机物的去除明显好于传统工艺,能提供水质良好的饮用水,是低温低浊水处理的发展方向.     

"双高"产品名录的制定与农药行业环境保护

论述了<"高污染、高环境风险"产品名录>(以下简称"双高"产品名录)制定的背景、依据与原则,以及演化过程,重点介绍了农药行业"双高"产品名录制定的意义、进展,以及对农药行业发展的影响等.     

LQZ型气力输送系统在电厂除灰中的应用

介绍了气力输送系统在电厂660MW机组除灰中的应用,并对飞灰特性,以及除灰系统设计、关键技术运用、运行情况、设备维护和故障处理等问题进行了分析论述。     

环境类高等职业教育产学研用合作机制研究

环境类高等职业教育具有鲜明的非行业背景和人才需求领域广泛而应用岗位相对集中的特殊性。在对国内部分环境类高职院校和环境类高职专业就产学研用合作机制及运行模式实地调研的基础上,对现存的环境类高职院校产学研用合作模式进行了深入分析,提出了"依托政府,实施‘双轨并行’工学结合"的产学研用合作机制与运行模式。     

Identifying 120 years of decline in ecosystem structure and maturity of Great South Bay, New York using the Ecopath modelling approach

Mass balanced models yield valuable information regarding ecological function and delivery of ecosystem services, but often rely on data collected well before many species were reduced to fractions of their original abundance. Lagoonal systems, such as Great South Bay (GSB), NY, sit on the interface of terrestrial and marine ecosystems and are prone to anthropogenic stressors but proximity to land also makes the presence of data regarding historic populations and structure more likely. To quantify over a century of ecosystem change, Ecopath models were developed for GSB at each of four time periods where commercial and scientific data exist: 1880s, 1930s, 1980s and 2000s. The results indicated that the GSB has experienced a decline in ecosystem maturity, loss of top keystone predators, a decline in connectivity to the ocean though the reduction of migratory species and increasing dominance of low trophic level organisms. These changes undermine the delivery of ecosystem services, increase conflicts over limited resources and suggest that present day restoration targets fail to recognize appropriate baselines. We discuss the role of stochastic events, which result in state changes that could be defined as regime shifts, and ecosystem connectivity to the long-term stability of lagoonal systems.     

Integrating soil carbon cycling with that of nitrogen and phosphorus in the watershed model SWAT: Theory and model testing

In this paper we describe and test a sub-model that integrates the cycling of carbon (C), nitrogen (N) and phosphorus (P) in the Soil Water Assessment Tool (SWAT) watershed model. The core of the sub-model is a multi-layer, one-pool soil organic carbon (S_C) algorithm, in which the decomposition rate of S_C and input rate to S_C (through decomposition and humification of residues) depend on the current size of S_C. The organic N and P fluxes are coupled to that of C and depend on the available mineral N and P, and the C:N and N:P ratios of the decomposing pools. Tillage explicitly affects the soil organic matter turnover rate through tool-specific coefficients. Unlike most models, the turnover of soil organic matter does not follow first order kinetics. Each soil layer has a specific maximum capacity to accumulate C or C saturation (S_x) that depends on texture and controls the turnover rate. It is shown in an analytical solution that S_x is a parameter with major influence in the model C dynamics. Testing with a 65-yr data set from the dryland wheat growing region in Oregon shows that the model adequately simulates the S_C dynamics in the topsoil (top 0.3 m) for three different treatments. Three key model parameters, the optimal decomposition and humification rates and a factor controlling the effect of soil moisture and temperature on the decomposition rate, showed low uncertainty as determined by generalized likelihood uncertainty estimation. Nonetheless, the parameter set that provided accurate simulations in the topsoil tended to overestimate S_C in the subsoil, suggesting that a mechanism that expresses at depth might not be represented in the current sub-model structure. The explicit integration of C, N, and P fluxes allows for a more cohesive simulation of nutrient cycling in the SWAT model. The sub-model has to be tested in forestland and rangeland in addition to agricultural land, and in diverse soils with extreme properties such high or low pH, an organic horizon, or volcanic soils.     

耐高温酵母高浓度发酵生产燃料乙醇工艺优化

采用两水平部分因子设计(23Fractional Factorial),选取发酵温度、接种量、初始糖浓度为自变量考察因素,以最终发酵乙醇浓度和9 h生物量浓度为响应值,考察耐高温高浓度酵母的燃料乙醇发酵能力,并对实验数据进行二次模型变异分析(Ahalysis of variance,ANOVA),建立了三元二次方程数学...     

温度和氮素输入对青藏高原三种高寒草地土壤碳矿化的影响

选取了海北高寒草甸、那曲高寒草原和当雄高寒湿地3种典型高寒草地生态系统类型为研究对象,采集了表层0~10 cm土壤,在实验室内进行可控温度下的碳矿化培养实验。结果表明,青藏高原土壤碳矿化在不同高寒草地类型间存在显著差异（P≤0.05）。在较低的温度下,高寒湿地土壤的碳矿化速率显著低于高寒草甸土壤,而温度在15℃左右时,高寒湿地土的碳矿化速率略高于高寒草甸土壤,当温度处于较高的水平时（〉20℃）,高寒湿地土壤碳矿化速率远高于高寒草甸土壤,高寒湿地土壤碳矿化的Q10显著大于高寒草甸。无论是低温还是较高的温度,高寒草原土壤碳矿化速率最低,数值范围也最窄。高寒草甸和高寒湿地土壤碳矿化均受温度的显著影响（P≤0.05）,其速率均跟温度呈现一级指数函数方程关系,而高寒草原土壤碳矿化速率与温度间未呈现明显的函数关系,但不同温度间的土壤碳矿化速率存在显著差异。氮素输入对高寒草甸和高寒湿地土壤碳矿化的影响不明显,但显著促进了高寒草原土壤碳矿化作用。