湿热预处理餐厨垃圾的盐分研究

对于盐分的研究是以通过湿热法餐厨垃圾制作适宜益生菌生长基质为目标.研究选取益生菌生长的主要限制因素-盐分进行研究,确定降低盐分浓度的工艺条件.实验通过选取一定温度、加水量和反应时间条件,在高温高压反应釜中反应.研究发现,全盐适宜温度为100℃或140℃,水溶性氯离子和水溶性钠离子适宜温度为50℃;三种离子适宜加水量均为80%;三种离子适宜的反应时间为15 min.研究为餐厨垃圾制作成适宜益生菌生长的工艺奠定了基础,较深入地研究了盐分在预处理过程中的变化情况和趋势.     

Effect of cooling rate and laser process parameters on additive manufactured Fe–Ti–C metal matrix composites microstructure and carbide morphology

In this paper, laser additive manufacturing (LAM) of Fe–TiC composite coating on AISI 1030 carbon steel is investigated using a numerical and experimental method. In order to have a desired result using LAM, it is crucial to understand the effects of the process parameters’ values on the TiC morphology and microstructure. For this purpose, the LAM process is numerically simulated in order to calculate cooling rate and peak temperature. Experimental data and numerical results are in good agreement in terms of the phase development. Results show that cooling rate plays a crucial role in phase transformation in the clad, however, final microstructure strongly depends on the cooling rate and powder's chemical composition. Two main carbide morphologies (i.e. dendritic and particulate) are studied and relevant cooling rates are detected. Based on this paper and developed map, it is possible to control the cooling rate in order to achieve specific carbide morphologies in the clad. In this study, scanning electron microscopy (SEM) and energy dispersive spectroscopy (EDS) are used to characterize clads’ microstructure.     

基于修正A值法估算西安市大气环境容量研究

采用以单箱模型法为基础的A值法对西安市大气容量进行估算,并将干沉降、湿沉降和化学转化三个消除过程引入模型测算中,借鉴国内外对于大气常规污染物的清除系数的科学研究成果,对研究区域的SO2、NO2、PM10及PM2.5等4项常规污染物的环境容量进行估算。结果表明,执行2012年新的环境质量标准下,西安市SO2、NO2、PM10及PM2.5大气环境容量分别为13.86×104吨/年,9.24×104吨/年、1.62×105吨/年及8.09×104吨/年。     

氮添加对生长季寒温带针叶林土壤有效氮和酸化的影响

基于低剂量、多形态的N添加控制实验,以大兴安岭寒温带针叶林为研究对象,通过长期持续的原位增N处理,测定了2010年、2012年和2013年生长季初期(5月)和生长旺季(8月)0~10 cm土壤有效氮(NH+4-N和NO-3-N)含量以及土壤p H值.结果表明,生长季初期和生长旺季土壤有效氮均以NH+4-N为主,NO-3-N含量较低,其中NH+4-N含量占无机氮含量的96%以上.随着增N时间的延长,同生长旺季相比,增N对生长季初期0~10 cm土壤NH+4-N影响较为明显,且主要受施N类型影响.与此相反,生长旺季0~10 cm土壤NO-3-N含量高于生长季初期.N输入对生长季初期和生长旺季土壤NO-3-N影响较为明显,且低N处理更倾向于促进0~10 cm土壤NO-3-N的富集.随着时间的延长,土壤NH+4-N和NO-3-N对增N的响应都由前期的不显著向后期的显著转变.增N对生长季初期和生长旺季0~10 cm土壤p H值影响显著,其中低N处理的土壤和生长旺季阶段土壤p H值相对较低.随着增N时间的延长,土壤p H值对增N的响应也由前期的不显著向后期的显著转变.长期持续的增N处理已经使大兴安岭寒温带针叶林0~10 cm土壤产生了明显的酸化.     

Dry deposition of PM10 over the Yellow Sea during Asian dust events from 2001 to 2007

Dry deposition velocities and fluxes of PM10during Asian dust events over the Yellow Sea from 2001 to 2007 were investigated using observation data in Qingdao, China and Jeju, Korea. The dry deposition velocities of PM10 during dust events over the Yellow Sea ranged from 0.19 to 8.17 cm/sec, with an average of 3.38 cm/sec. Dry deposition fluxes of PM10during dust events over the Yellow Sea were in the range of 68.5–2647.1 mg/(m2·day), with an average of 545.4 mg/(m2·day), which is 2–10 times higher than those reported by other studies for both dust and non-dust periods. It was estimated that 2.6 × 1011–48.7 × 1011g dust particles deposit to the Yellow Sea during dust events through dry deposition every year. Compared with the results in previous studies, it was found that the dry deposition of PM10over the Yellow Sea during dust events in the years with high frequency of dust could account for a large or overwhelming fraction of the annual total dry deposition. Backward air mass trajectory analysis showed that dust events influenced Jeju mainly originated from the desert regions located in Mongolia and Inner Mongolia, China. There were 119 backward trajectories influenced both Qingdao and Jeju during 15 dust events from 2001 to 2007, accounting for 61.3% of the total trajectories of 194, indicating that Qingdao and Jeju were usually on the same pathway of dust transport downwind from source areas.     

硫氮沉降下西北荒漠煤矿区周边土壤性质的变化特点

近年来中国大部分区域大气硫、氮沉降速率趋于平稳甚至下降,但西北地区煤炭行业的快速发展使得硫、氮沉降速率加快.燃煤电厂作为酸前体物的主要排放源之一,在其周围开展硫、氮沉降效应研究,可为合理评价煤矿区大气污染物控制措施的实施效果提供数据支撑.该文以宁东能源化工基地3个燃煤电厂为采样点,研究了电厂周围土壤化学和生物学性质的变...     

Preparation and characterization of Fe2O3-CeO2-TiO2/γ-Al2O3 catalyst for degradation dye wastewater

In order to develop a catalyst with high activity for catalytic wet oxidation （CWO） process at room temperature and atmospheric pressure, Fe2O3-CeO2-TiO2/γ-Al2O3 catalyst was prepared by consecutive impregnation method and the prepared parameters were optimized. The structure of the catalyst was characterized by BET, XRF, SEM and XPS technologies, and the actual wastewater was used to investigate the catalytic activity of Fe2O3-CeO2-TiO2/γ-Al2O3 in CWO process. The experimental results showed that the prepared catalyst exhibited good catalytic activity when the doping amount of Ti was 1.0 wt% （the weight ratio of Ti to carriers）, and the middle product, Fe2O3-CeO2-TiO2/γ-Al2O3, was calcined in 450℃ for 2 h. The CWO experiment for treating actual dye wastewater indicated that the COD, color and TOC of actual wastewater were decreased by 62.23%, 50.12% and 41.26% in 3 h, respectively, and the ratio of BOD5/COD was increased from 0.19 to 0.30.     

Distribution of Al-, Fe- and Mn-pools and their correlation in soils from two acid deposition small catchments in Hunan, China

Distribution of Al-, Fe- and Mn-pools was investigated in five forest soil profiles (consisting of four horizons) in each of two Hunan catchments (BLT and LKS) where acid deposition has been considered critical. Al- and Fe-pools were higher in BLT than those in LKS, but Mn-pools much lower in BLT. Mn-pools vary from topsoils to bottom soils, but there are different trends for different Mn speciation. Al- and Fe-pools, except amorphous Fe_ox, were positively correlated to contents of soil organic matter (OM) showed by the loss on ignition in the two catchments. Accumulation of Al- and Fe-pools may occur in the area where soil organic matter was enriched (e.g. in top soil and rhizosphere soil). However, no direct correlation is observed between Mn and OM. Acidic atmospheric deposition may affect transforming among speciations of Al-, Fe- and Mn-pools and leaching of soil Al, Fe and Mn through formation of soluble organo-metal dissolved Al which was potentially toxic, increased. There were significant correlations between Al-pools complexes or change of oxidation–reduction conditions. Mn_ex (exchangeable Mn) and Mn_ox (amorphous and organic Mn) were highly linearly correlation with soil pH values at LKS but at BLT. Under acid deposition, the availability of the nutrient Fe increased with the amount of dissolved Al, which was potentially toxic, in the two catchments. There are no significant correlations between Al_ex (exchangeable Al) and Mn_ex, Fe_ex (exchangeable Fe) and Mn_ex in this work, indicating potentially toxic Mn increase seldom accompanying with Al increase in the two catchments.     

碳酸盐体系天然水体多指标酸化模型

本文以碳酸盐体系为基础提出适于区域环境水体酸化敏感性多指标评价模型,利用该模型结合各评价指标的标准化体系可进行大尺度范围水体酸化敏感性评价。     

PREDICTING EROSION AND DEPOSITION ON A STRIPMINED AND RECLAIMED AREA1

ABSTRACT A rill-interrill erosion model was applied to a mined and reclaimed area. Soil loss from the interrill areas was estimated by the Universal Soil Loss Equation (USLE). The model considers the fate and ultimate disposition of the sediment from interrill areas along with the fate and destination of soil materials detached by the rill flow. The net sediment loss was predicted by comparing, for a given flow, the amounts of eroded soil to rill transport capacity. When applied to a selected stripmined and reclaimed site the model displayed the location of contributing areas and the amount of erosion and deposition. The predicted areal distribution of erosion and deposition was compared to measured data. Agreement between the predicted and measured values was within 25 percent.