焦化厂废水中氨的测定——气敏电极法

研究了用气敏电极测定焦化厂废水中氨的分析方法，对测定的线性范围，响应时间、回收率、干扰物质等作了理论探讨和大量试验。在ｐＨ为１１５～１４０时，线性范围为１００×１０－５～１００×１０－１ｍｏｌ／Ｌ，最低检出限为５０×１０－６ｍｏｌ／Ｌ，ＲＳＤ≤２５％。     

Arts as a vehicle for community building and post‐disaster development

Use of the arts in international aid is common in an ad hoc form, but it has not been systematically theorised or evaluated. The arts have the potential to be a culturally contextualised and sustainable intervention for adults and children in the aftermath of war or disaster. On the micro level, the arts are a method to enable the retrieval and reprocessing of traumatic memories that are often encoded in images rather than in words. On a macro level, they can help to reconstruct a group narrative of a disaster as well as mobilise people back into control of their lives. This paper researches a long‐term project using arts in Sri Lanka following the civil war and tsunami. A central finding is the need to understand arts within their cultural context, and their usefulness in strengthening the voices and problem‐solving capacities of the victims of the disaster.     

应用Dot-ABC法检测植物镉金属污染

用不同浓度的氯化镉诱导黄瓜幼叶Cd-MT的产生,并应用Dot-ABC法检测了30种来自天水不同区域植物的MT含量,初步确定它们的重金属污染情况.结果表明,Cd-MT浓度与环境诱导浓度呈显著正相关,Dot-ABC法检测的植物金属硫蛋白的最低含量为16ng,并初步估测了其中10种植物可能存在不同程度的重金属污染.本法具有特异、简便和灵敏的特点,可用于农产品镉金属污染的检测.     

关于渗透通风条件建筑结构对室内PM2.5浓度水平影响评价模型探讨

我国京津冀地区近年频遭大气PM_2.5污染侵扰,相关研究表明,既使关闭建筑外窗,大气中PM_2.5仍可以通过渗透通风方式进入室内污染环境.为定量评价建筑渗透通风及无室内污染源条件下建筑结构（如外窗缝隙结构、房间建筑结构等）对室内ρ（PM_2.5）的影响规律,基于北京市东城区、朝阳区6个不同建筑结构的房间室内外ρ（PM_2.5）实时监测数据,重点比较分析了建筑结构对室内外ρ（PM_2.5）关联特性的影响规律.此外,根据颗粒物穿透特性及沉降特性机理,提出了反映建筑外窗缝隙结构（如缝高、缝深）的无量纲特征参数A_P与反映房间建筑结构（如层高、开间、进深）的无量纲特征参数A_k.在前期提出的室内ρ（PM_2.5）预测模型基础上,进一步构建了二者（A_P与A_k）对室内ρ（PM_2.5）影响的评价模型,并通过实测数据验证了模型的正确性.结果表明:当室外PM_2.5污染程度与气象条件一定时,建筑结构对I/O[室内外ρ（PM_2.5）之比]影响较大,其范围在0.4~0.7之间;随着建筑外窗气密性等级的提高,对应室内ρ（PM_2.5）呈显著的下降趋势.建筑外窗缝隙结构对室内ρ（PM_2.5）影响程度远大于房间建筑结构,敏感性分析结果表明,当建筑外窗缝高每降低50%或缝深每提高50%,对应室内ρ（PM_2.5）约可下降33.6%与31.9%.研究显示,气密性等级较高的建筑外窗缝隙缝高往往较小、缝深较长,渗透通风条件下对控制室内ρ（PM_2.5）水平作用更显著。      

河道溢油事故环境风险评价中若干关键问题探讨

河道溢油事故已成为内河道突发性水环境污染的主要问题之一,尤其水源地突发性污染事件日益增多,对社会、经济和河道生态环境造成严重的不良影响。新建的水上项目必须通过溢油风险评价来分析项目建设投产后对周边的环境影响,目前溢油风险评价尚无统一的方法,且风险分析不够深入。本文基于国内外经典的油膜动力学模型及统计学等理论,明确溢油事故环境风险评价中事故源强、事故概率、溢油油膜影响范围、风险应急时间以及水厂吸水口关闭时间等几个关键问题的分析方法,以期进一步提高河道溢油事故的环境风险评价水平。     

塔里木盆地南缘克里雅绿洲土地利用变化对生态系统服务价值的影响研究

以塔里木盆地南缘克里雅绿洲作为典型区,分析1991-2001年土地利用变化对生态系统服务价值的影响。研究结果表明,克里雅绿洲在1991-2001年土地利用变化很明显,生态服务价值从1991年的10．004×10^8元降到20,01年的8．792×10。元,生态服务价值损失了12％,平均每年净损失生态服务价值32．2元／hm^2湿地生态服务价值的变化最大,变化率高达-37．54％。湿地、水体面积变化的绝对量高、生态服务功能价值指数大是导致研究区生态系统服务总价值降低的主要原因。敏感性分析结果表明,克里雅绿洲生态服务价值对生态服务功能指数是缺乏弹性的,研究结果是可信的,可为研究区土地利用规划提供借鉴。     

环评监测现场采样中应注意的问题

根据环境影响评价监测的要求,提出了环评监测中方案的细化、点位布设方面存在的问题,阐述了如何合理设置监测点位、准确把握采样方法、科学选择分析方法等问题。     

上悬窗条件下通风控制腔室火灾温度的实验研究

随着建筑结构的发展,上悬窗日益成为城市建筑窗户的选择,但这种通风条件下腔室火灾的发展特性仍缺乏研究.利用1:8相似比例的缩尺寸腔室火灾实验台,实验研究了上悬窗不同开口尺寸、不同开窗角度下,通风控制的腔室火灾温度发展特性.实验结果表明,通风控制条件下,腔室火灾温度随着上悬窗开口尺寸和开窗角度的增加而增加,并通过能量平衡分...     

氨气敏电极法和纳氏试剂分光光度法对地表水中氨氮的比对测试

采用不同质量浓度的氨氮标准样品和实际样品,用氨气敏电极法和纳氏试剂分光光度法进行同步测试。结果表明,2种分析方法在水样氨氮质量浓度在0. 159～2. 81 mg/L范围内具有良好的可比性、精密性和准确性。氨气敏电极法的检出限为0. 03 mg/L,平行6次测定样品的相对标准偏差为0. 4%～4. 2%,加标回收率为85. 0%～110%;纳氏试剂分光光度法的检出限为0. 025 mg/L,平行6次测定样品的相对标准偏差为0. 5%～6. 4%,加标回收率为93. 0%～99. 8%。同时氨气敏电极法在样品预处理、试剂配制和分析时间上要优于纳氏试剂分光光度法。氨气敏电极法能够满足地表水自动监测在线比对实际工作的需求,该方法具有良好的适用性。     

Topsoil organic carbon mineralization and CO2 evolution of three paddy soils from South China and the temperature dependence

Carbon mineralization and its response to climatic warming have been receiving global attention for the last decade. Although the virtual influence of temperature effect is still in great debate, little is known on the mineralization of organic carbon （SOC） of paddy soils of China under warming. SOC mineralization of three major types of China＇s paddy soils is studied through laboratory incubation for 114 d under soil moisture regime of 70% water holding capacity at 20℃ and 25℃ respectively. The carbon that mineralized as CO2 evolved was measured every day in the first 32 d and every two days in the following days. Carbon mineralized during the 114 d incubation ranged from 3.51 to 9.22 mg CO2-C/gC at 20℃ and from 4.24 to 11.35 mg CO2-C/gC at 25℃ respectively; and a mineralizable C pool in the range of 0.24 to 0.59 gC/kg, varying with different soils. The whole course of C mineralization in the 114 d incubation could be divided into three stages of varying rates, representing the three subpools of the total mineralizable C： very actively mineralized C at 1-23 d, actively tnineralized C at 24--74 d and a slowly mineralized pool with low and more or less stabilized C mineralization rate at 75-114 d. The calculated Q10 values ranged from 1.0 to 2.4, varying with the soil types and N status. Neither the total SOC pool nor the labile C pool could account for the total mineralization potential of the soils studied, despite a well correlation of labile C with the shortly and actively mineralized C, which were shown in sensitive response to soil warming. However, the portion of microbial C pool and the soil C/N ratio controlled the C mineralization and the temperature dependence. Therefore, C sequestration may not result in an increase of C mineralization proportionally. The relative control of C bioavailability and microbial metabolic activity on C mineralization with respect to stabilization of sequestered C in the paddy soils of China is to be further studied.