磷在农田溪流中的动态变化

磷是水体富营养化的限制因子,河流系统是农业非点源污染物的主要运移通道,污染物在河流中的持留控制着污染物向受纳水体的输出.本次研究对象是巢湖流域一个长约1.8 km的农田源头溪流六岔河,河流由4个渠道型、1个水塘型和3个河口型断面构成,长度分别为1.3 km、0.15 km和0.36 km.在河流上设置9个监测点研究总磷、磷酸盐和悬浮物在六岔河中的持留空间特征,评价人为严重干扰下的农田溪流在农业非点源污染物运移中的生态功能.结果表明:总磷、磷酸盐、悬浮物在溪流中的持留和释放受溪流的渠道型、水塘型和河口型断面控制,水塘型和河口型断面是污染物持留的主要区域,总磷、磷酸盐和悬浮物在水塘型、河口型断面内的持留量分别占溪流持留量的58%、77%和58%;污染物在降雨-径流过程中的持留是溪流持留的主要部分,总磷、磷酸盐和悬浮物的持留分别占溪流持留量的96%、98%和93%;渠道型断面是溪流最主要的内在污染源,总磷、磷酸盐和悬浮物的释放分别占溪流释放量的93%、99%和94%;养分和悬浮物在渠道型断面中具有不同的持留特性,而位于水塘前的渠道型断面在基流和降雨-径流过程中均能有效地持留污染物.     

Winter Soil Respiration from Different Vegetation Patches in the Yellow River Delta, China

Vegetation type and density exhibited a considerable patchy distribution at very local scales in the Yellow River Delta, due to the spatial variation of soil salinity and water scarcity. We proposed that soil respiration is affected by the spatial variations in vegetation type and soil chemical properties and tested this hypothesis in three different vegetation patches (Phragmites australis, Suaeda heteroptera and bare soil) in winter (from November 2010 to April 2011). At diurnal scale, soil respiration all displayed single-peak curves and asymmetric patterns in the three vegetation patches; At seasonal scale, soil respiration all declined steadily until February, and then increased to a peak in next April. But, the magnitude of soil respiration showed significant differences among the three sites. Mean soil respiration rates in winter were 0.60, 0.45 and 0.17 μmol CO(2) m(-2) s(-1) for the Phragmites australis, Suaeda heteroptera and bare soil, respectively. The combined effect of soil temperature and soil moisture accounted for 58-68 % of the seasonal variation of winter soil respiration. The mean soil respiration revealed positive and linear correlations with total N, total N and SOC storages at 0-20 cm depth, and plant biomass among the three sites. We conclude that the patchy distribution of plant biomass and soil chemical properties (total C, total N and SOC) may affect decomposition rate of soil organic matter in winter, thereby leading to spatial variations in soil respiration.     

基于风险指数RI的选址评价在LNG储备库中的应用

研究基于风险指数RI的选址评价方法,确定评价方法的框架和程序,并将该评价方法用于某拟建LNG储备库的选址.结果表明,沸腾液体扩展蒸气爆炸在拟建LNG储备库可能发生的事故中的后果最严重.以沸腾液体扩展蒸汽爆炸的计算结果为依据,在GIS中对LNG储备库进行缓冲区分析,得到直观显示的事故影响区域和影响对象.计算拟建LNG储备库的选址风险并与可接受风险水平进行比较,确定选址的合理性且适当调整周边布局.研究表明,基于风险指数RI的选址评价方法对合理确定重大工程选址是切实可行的.     

风险积分参数RI在LPG站风险分析及评价中的应用

对液化石油气站选址风险进行定量分析,判断风险的可接受性,从而确定选址是否合理.拟建液化石油气站的F/N曲线未知,辨识液化石油气站可能发生的最严重事故,并应用风险积分参数确定液化石油气站的风险.经判断,液化石油气站可能发生的最严重事故为沸腾液体扩展蒸气爆炸(BLEVE),应用BLEVE火球模型对事故后果进行评价并确定事故影响范围,进而确定影响范围内的最大人数及事故发生频率,在此基础上对LPG站的风险积分参数进行计算.将计算结果与英国安全卫生执行局应用ALARP准则制定的风险可接受标准进行比较.结果表明,该液化石油气站的风险处于合理可接受区.采取一定风险减缓措施后,可考虑在此地点建设液化石油气站.     

有意违章行为动因分析与控制对策探讨

对有意违章行为的含义进行了界定,并对有意违章行为产生的动因进行了详细分析,提出了有意违章行为的动因主要包含违章行为与遵章行为满足生理心理需要作用的差值ΔXW 、违章行为会受到法规惩处的作用FW、违章行为可导致人身伤害的主观感觉的作用RW 3个方面.同时对3个方面的动因按弗鲁姆的激励理论进行了转化,给出了各自的含义说明.笔者按动因分析的结果,给出了控制有意违章行为的步骤和措施.     

PEM式臭氧消毒在地上游泳池水处理中的应用

采用臭氧法水处理系统对地上游泳池的循环水进行灭菌消毒,研究了臭氧用量、循环水流量和运行时间等因素对臭氧法灭菌效果的影响。结果表明,3组PEM臭氧发生器应用于21.2 m3的地上游泳池,在4 m3/h的循环水流量下运行12 h后,水中的细菌总数与大肠杆菌群数达到国家标准,去除率均在99%以上。与盐电解法水处理系统相比较,臭氧法水处理系统的优势在于:杀菌快速高效、出水水质的理化指标较好和运行费用低廉。     

一起钢质无缝气瓶爆炸事故技术分析

文章简要描述了一起消防气体灭火钢质气瓶爆炸事故,对爆炸气瓶进行了断口分析、金相试验和理化试验,并分析了事故的原因,提醒制造厂家规范制造工艺,对预防类似事故的发生具有一定的参考意义。     

生化法处理含氨废水动力学研究

对生化法处理含氨废水过去中有重要影响的动力学因素进行了试验研究和分析,得出了利用高效微生物菌群废水中COD和NH3－N的动力学条件,温度为20－35℃,PH为7－8,DO大于2.6mg/L,MLSS大于2.6g/L,C／N小于3。在此条件下处理含氨废水,处理后的出水达到国家化肥行业一级排放标准。     

Changes in Soil Particulate Organic Matter, Microbial Biomass, and Activity Following Afforestation of Marginal Agricultural Lands in a Semi-Arid Area of Northeast China

Afforestation of agricultural lands has been one of the major land use changes in China in recent decades. To better understand the effect of such land use change on soil quality, we investigated selected soil physical, chemical and microbial properties (0–15 cm depth) in marginal agricultural land and a chronosequence of poplar (Populus euramericana cv. ‘N3016’) plantations (5-, 10-, 15- and 20-years old) in a semi-arid area of Northeast China. Soil bulk density significantly declined after conversion of agricultural lands to poplar plantations. Soil total organic carbon (TOC) and nitrogen (TN) concentrations, microbial biomass C (MBC) and potential N mineralization rate (PNM) decreased initially following afforestation of agricultural lands, and then increased with stand development. However, soil metabolic quotient (qCO₂) exhibited a reverse trend. In addition, soil particulate organic matter C (POM-C) and N (POM-N) concentrations showed no significant changes in the first 10 years following afforestation, and then increased with stand age. These findings demonstrated that soil quality declined initially following afforestation of agricultural lands in semi-arid regions, and then recovered with stand development. Following 15 years of afforestation, many soil quality parameters recovered to the values found in agricultural land. We propose that change in soil quality with stand age should be considered in determining optimum rotation length of plantations and best management practices for afforestation programs.