垂直流人工湿地系统基质优化级配研究

选取生物陶粒、无烟煤、沸石、钢渣和蛭石为基质,按不同的级配方式填充成基质柱,进行垂直流人工湿地模拟柱净化污水实验.研究表明,粒径分层级配基质对COD的去除率均高于单一粒径基质,其中分层生物陶粒对COD的平均去除率高达72.91%.分层沸石对总氮的净化能力较单一粒径基质有所提高,平均去除率高达91.23%.填充了生物陶粒、沸石和无烟煤的模拟柱对有机物和氮的净化效果和单一基质没有显著性差异(p0.05).填充钢渣和无烟煤的模拟柱出水pH值均在正常范围内,但是除从上到下依次填充无烟煤、蛭石和钢渣的基质柱外,其它填充钢渣和无烟煤的模拟柱对磷素的净化能力都低于单一基质.种植植物对净化效果没有明显影响.在垂直流人工湿地中,针对水质特点选择高效的级配基质,如分层生物陶粒、分层沸石、分层无烟煤以及生物陶粒、沸石和无烟煤组合,在高水力负荷条件下可获得更好的处理效果.     

应用质子变化滴定测量法监测氨氧化的化学计量关系

开发了一套监测批式废水生物处理系统质子变化的自动滴定测量装置.装置由批式反应器、数据自动采集与保存系统和药品自动投加系统组成.通过实际测量活性污泥氨氧化反应中氢离子产生量与氨消耗量的化学计量比值,考察自动滴定测量装置的测试精度.在1L的反应器中改变氨氮浓度(以N计)分别为1.67、3.33、8.33、16.66和30.00mg/L下实测比值与其理论值十分接近,相对误差在2.09%～6.34%之间;保持氨氮浓度16.66mg/L,在1、2、3和4L的反应器中实测比值相对误差在2.09%～-18.57%之间,随反应器体积增大而明显增大.反应器系统中的碳酸氢盐和氨盐缓冲体系,特别是在较大容积反应器中的滴定动态效应是导致测试误差的重要原因.研究成果为滴定测量方法在废水生物处理过程中监测质子变化提供了一种重要方法.     

Transport and fate of mercury under different hydrologic regimes in polluted stream in mining area

Seepage from Hg mine wastes and calcines contains high concentrations of mercury (Hg). Hg pollution is a major environmental problem in areas with abandoned mercury mines and retorting units. This study evaluates factors, especially the hydrological and sedimentary variables, governing temporal and spatial variation in levels and state of mercury in streams impacted by Hg contaminated runo . Samples were taken during di erent flow regimes in theWanshan Hg mining area in Guizhou Province, China. In its headwaters the sampled streams/rivers pass by several mine wastes and calcines with high concentration of Hg. Seepage causes serious Hg contamination to the downstream area. Concentrations of Hg in water samples showed significant seasonal variations. Periods of higher flow showed high concentrations of total Hg (THg) in water due to more particles being re-suspended and transported. The concentrations of major anions (e.g., Cl??, F??, NO3?? and SO4 2??) were lower during higher flow due to dilution. Due to both sedimentation of particles and dilution from tributaries the concentration of THg decreased from 2100 ng/L to background levels (< 50 ng/L) within 10 km distance downstream. Sedimentation is the main reason for the fast decrease of the concentration, it accounts for 69% and 60% for higher flow and lower flow regimes respectively in the upper part of the stream. Speciation calculation of the dissolved Hg fraction (DHg) (using Visual MINTEQ) showed that Hg(OH)2 associated with dissolved organic matter is the main form of Hg in dissolved phase in surface waters in Wanshan (over 95%).     

武汉市长江北岸耕地中多环芳烃垂向与纵向分布特征

文章对武汉市长江北岸农用耕地中多环芳烃的含量进行了调查。结果表明除紧靠马路边一个点位的荧蒽浓度高于荷兰制定的土壤修复标准之外,其余各点各类多环芳烃均在此标准值之内;随着点位距污染源越远多环芳烃的含量越来越低;并且多环芳烃在垂直方向上的迁移存在色谱效应。通过分析不同采样点土壤中的多环芳烃含量,分析得出结论汽车尾气所排放的...     

焦作市高新区冬季大气不同粒径颗粒物质量特征分析

用大流量冲击式分级采样器采集大气颗粒物样品,通过重量法求出不同粒径颗粒物的质量,研究不同粒径颗粒物的质量百分比.分析不同粒径颗粒物与风速、温度、湿度等气象条件的变化规律.结果表明:各级颗粒物整体与温度和风速呈负相关性,与湿度呈正相关性,且粒径小于2.1 μm的颗粒物与湿度相关性最大.大气颗粒物主要集中在2.1 μm以下...     

淀山湖沉积物碳-氮垂直分布特征

近年来,经过一系列污染治理措施,淀山湖的营养水平持续下降,但每年仍有不同程度的蓝藻水华暴发,严重影响其作为水源地的安全性。为了进一步探讨淀山湖水质改善策略,本研究对淀山湖沉积物营养状况进行了调查研究,分析了淀山湖沉积物碳、氮分布特征及垂直变化规律,并用沉积物肥力评价了淀山湖沉积物营养程度。结果表明,淀山湖沉积物营养盐存在明显的富集作用,二十多年来沉积物碳、氮含量大幅上升,表层沉积物均属于重污染状态。空间分布上,沉积物营养盐北部高,南部低,北部样点大部分属于重污染状态,南部样点基本属于中污染状态。垂直分布上,受航道回淤与北部围网养殖影响,部分样点营养盐垂直分布规律不显著,其他样点均表现出随深度增加营养盐显著降低的趋势。除出水口D1样点外,淀山湖有机质与TN表现出显著的同源相关性,表明有机质是淀山湖内源负荷的主要来源。     

黑岱沟露天矿排土场不同植被配置土壤水分研究——土壤水分垂直动态研究

文章通过黑岱沟露天煤矿排土场不同植被配置土壤水分垂直动态研究,阐述了不同植被配置类型对土壤水分的影响。结果显示：9种植被配置类型的土壤台水量随土层深度的增加而减小,但变化幅度有差异;原生植被处的土壤水分利用层厚度大于人工植被。     

太原晋祠地区果园土壤呼吸的年际变化及其温度敏感性

太原晋祠地区曾经是著名的稻米之乡,随着晋祠泉的断流,区内土地利用从之前的以水稻田为主转变为以玉米和果园为主.因此,研究土地利用变化后土壤呼吸对于准确估算区域碳循环具有一定意义.基于此目的,本研究以原来为稻田、现为果园利用方式的样地为对象,对其土壤呼吸进行了7 a(2006~2012年)、每月1~3次的定位观测,分析了土壤呼吸的年际、季节变化及其与环境因子年际、季节变化的关系.结果表明,土壤呼吸与土壤温度的季节变化与天数的关系可以用3参数高斯方程模型进行拟合.土壤呼吸的季节变化与土壤温度的季节变化关系为极显著的指数关系,但其与土壤水分季节变化的关系不显著.土壤呼吸速率年平均值为(5.32±3.31)μmol·(m~2·s)-1;碳通量年平均值为1 690.2 g·m-2,在1 294.0~2 006.0g·m~(-2)之间变化,年际均值差异不显著.土壤呼吸的温度敏感性指数(Q_(10))值的年际变化以5、10和15 cm温度测定深度计算分别在1.54~2.20、1.68~2.48和1.82~2.46之间;土壤温度10℃对应的土壤呼吸(R_(10))值的年际变化在2.37~2.81、2.43~3.13和2.59~3.47μmol·(m~2·s)-1之间;Q_(10)和R10值均随土壤温度测定深度增加而增加.Q_(10)的年际变化与10 cm深度的土壤温度(T_(10))的年际变化关系极显著(P=0.016),与其它因子的关系不显著;在拟合方程中增加土壤水分因子不能提高对Q_(10)年际变化的预测精度,说明在本样地水分对Q_(10)的影响较小.R10值的年际变化与环境因子的年际变化关系不显著.与土壤呼吸与土壤温度的单因素模型相比,土壤温度和土壤水分的双变量指数模型可以提高预测土壤呼吸季节变化的准确性.研究结果可以为本地区及同类地区的土壤呼吸估算提供一定参考.     

Fast increasing of surface ozone concentrations in Pearl River Delta characterized by a regional air quality monitoring network during 2006-2011

Based on the observation by a Regional Air Quality Monitoring Network including 16 monitoring stations, temporal and spatial variations of ozone(O3), NO2and total oxidant(Ox) were analyzed by both linear regression and cluster analysis. A fast increase of regional O3concentrations of 0.86 ppbV/yr was found for the annual averaged values from 2006 to 2011 in Guangdong, China. Such fast O3increase is accompanied by a correspondingly fast NOx reduction as indicated by a fast NO2 reduction rate of 0.61 ppbV/yr. Based on a cluster analysis, the monitoring stations were classified into two major categories – rural stations(non-urban) and suburban/urban stations. The O3concentrations at rural stations were relatively conserved while those at suburban/urban stations showed a fast increase rate of 2.0 ppbV/yr accompanied by a NO2 reduction rate of 1.2 ppbV/yr. Moreover, a rapid increase of the averaged O3 concentrations in springtime(13%/yr referred to 2006 level) was observed, which may result from the increase of solar duration, reduction of precipitation in Guangdong and transport from Eastern Central China. Application of smog production algorithm showed that the photochemical O3production is mainly volatile organic compounds(VOC)-controlled. However, the photochemical O3production is sensitive to both NOx and VOC for O3pollution episode. Accordingly, it is expected that a combined NOx and VOC reduction will be helpful for the reduction of the O3 pollution episodes in Pearl River Delta while stringent VOC emission control is in general required for the regional O3 pollution control.     

巢湖水体组分垂向分布特征及其对水下光场的影响

富营养化湖泊不同组分垂向分布及其对水下光场的影响是湖泊水环境遥感领域亟待开展的内容.利用巢湖野外实测数据,分析水体不同组分垂向分布特征,结合Hydrolight辐射传输模型模拟研究水体不同组分垂向分布对漫衰减系数Kd的影响.结果表明,巢湖水体悬浮物以及有色可溶性有机物CDOM垂向分布较为均一,水面未发生藻华现象时叶绿素a垂向分布符合高斯正态分布,漫衰减系数Kd受叶绿素a以及无机悬浮物的显著影响,其垂向变化复杂多样,以往以水体光学性质均一为前提计算得到的Kd仅仅表示其衰减的平均情况,不能精确反映水下光场的垂向变化,因此研究水体组分垂向分布特征及其对漫衰减系数Kd的影响是开展藻类垂向分布异质性对水下光场影响机制研究的前提和基础.