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71.
All the regulations that define a maximum concentration of metals in the receiving soil are based on total soil metal concentration. However, the potential toxicity of a heavy metal in the soil depends on its speciation and availability. We studied the effects of heavy metal speciation and availability on soil microorganism activities along a Cu/Zn contamination gradient. Microbial biomass and enzyme activity of soil contaminated with both Cu and Zn were investigated. The results showed that microbial biomass was negatively affected by the elevated metal levels. The microbial biomass-C (Cmic)/organic C (Corg) ratio was closely correlated to heavy metal stress. There were negative correlations between soil microbial biomass, phosphatase activity and NH4NO3 extractable heavy metals. The soil microorganism activity could be predicted using empirical models with the availability of Cu and Zn. We observed that 72% of the variation in phosphatase activity could be explained by the NH4NO3-extractable and total heavy metal concentration. By considering different monitoring approaches and different viewpoints, this set of methods applied in this study seemed sensitive to site differences and contributed to a better understanding of the effects of heavy metals on the size and activity of microorganisms in soils. The data presented demonstrate the relationship between heavy metals availability and heavy metal toxicity to soil microorganism along a contamination gradient.  相似文献   
72.
张欣  张代钧  张文阁  卢培利 《环境科学》2010,31(7):1590-1595
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.  相似文献   
73.
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%).  相似文献   
74.
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...  相似文献   
75.
严俊霞  郝忠  荆雪锴  李洪建 《环境科学》2016,37(9):3625-3633
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.  相似文献   
76.
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.  相似文献   
77.
A high strength chemical industry wastewater was assessed for its impact on anaerobic microbial com- munity dynamics and consequently mesophilic methane generation. Cumulative methane production was 251 mL/g total chemical oxygen demand removed at standard temperature and pressure at the end of 30 days experimental period with a highest recorded methane percentage of 80.6% of total biogas volume. Volatile fatty acids (VFAs) analysis revealed that acetic acid was the major intermediate VFAs produced with propionic acid accumulating over the experimental period. Quantitative analysis of microbial communities in the test and control groups with quantitative real time polymerase chain reaction highlighted that in the test group, Eubacteria (96.3%) was dominant in comparison with methanogens (3.7%). The latter were dominated by Methanomicrobiales and Methanobacteriales while in test groups increased over the experimental period, reaching a maximum on day 30. Denaturing gradient gel electrophoresis profile was performed, targeting the 16S rRNA gene of Eubacteria and Archaea, with the DNA samples extracted at 3 different time points from the test groups. A phylogenetic tree was constructed for the sequences using the neighborhood joining method. The analysis revealed that the presence of organisms resembling Syntrophomonadaceae could have contributed to increased production of acetic and propionic acid intermediates while decrease of organisms resembling Pelotomaculum sp. could have most likely contributed to accumulation of propionic acid. This study suggested that the degradation of organic components within the high strength industrial wastewater is closely linked with the activity of certain niche microbial communities within eubacteria and methanogens.  相似文献   
78.
王敬  陆小兰  杨桂朋  徐冠球 《环境科学》2014,35(11):4085-4094
于2013年7月对东海和南黄海海水中CO的浓度分布、时空变化、海-气通量和表层海水中CO微生物消耗进行了研究.夏季东海和南黄海大气中CO的体积分数范围为68×10-9~448×10-9,平均值为117×10-9(SD=68×10-9,n=36),呈现出近岸高、远海低的特点.夏季东海和南黄海表层海水中CO的浓度范围为0.23~7.10 nmol·L-1,平均值为2.49 nmol·L-1(SD=2.11,n=36),CO的浓度受太阳辐射影响明显;不同站位CO浓度的垂直分布特征基本相同,CO浓度最大值一般出现在表层,随深度增加CO浓度迅速减小.夏季东海和南黄海海水中CO浓度具有明显的周日变化,最大值是最小值的6~40倍.各层最大值基本出现在中午,最小值基本上出现在凌晨前后.CO明显的周日变化特征进一步证明海水中CO主要由光化学产生.调查期间东海和南黄海表层海水中CO相比大气处于过饱和状态,过饱和系数变化范围为1.99~99.18,平均值为29.36(SD=24.42,n=29),表明调查海域是大气中CO的源.调查期间CO的海-气通量变化范围为0.37~44.84μmol·(m2·d)-1,平均值为12.73μmol·(m2·d)-1(SD=11.40,n=29).调查海域CO的微生物消耗培养实验中,CO的浓度随时间增长呈指数降低,消耗过程符合一级反应的特点,微生物消耗速率常数KCO范围为0.12~1.45 h-1,平均值为0.47 h-1(SD=0.55,n=5),微生物消耗速率与盐度之间有一定的相关性.  相似文献   
79.
广西不同石漠化等级下SPAC水势梯度及其环境效应   总被引:1,自引:0,他引:1  
邓艳  胡阳  马祖陆  朱鑫  梁晓 《地球与环境》2014,42(2):213-220
以野外观测为基础,对广西不同石漠化等级(无石漠化、轻度石漠化、中度石漠化和重度石漠化)下土壤-植被-大气连续体(Soil-Plant-Atmosphere Continuum,简称SPAC)系统中的水势日变化、气象因子日变化过程进行了研究。结果表明:随着石漠化程度的增加,大气水势降低,大气水势对不同石漠化程度的反应敏感。岩溶区石漠化等级下植物和土壤水势较低,不同石漠化条件下的植物叶水势在-7.79±0.43~-2.68±0.11 Mpa之间,土壤水势在-4.00±0~-0.08±0.04 Mpa之间,重度石漠化等级下植物处于萎蔫状态。植物在正午受到的水分亏缺程度为:重度石漠化中度石漠化无石漠化轻度石漠化。无石漠化下植物叶片水势与大气温度呈正相关关系,与大气相对湿度呈负相关关系,轻度石漠化、中度石漠化和重度石漠化下植物叶片水势与大气温度呈负相关关系,与大气相对湿度呈正相关关系。水分在SPAC系统中运移,其能量消耗主要集中在叶片-大气的过程。叶-气水势差差值大小为:中度石漠化重度石漠化轻度石漠化无石漠化。随着石漠化程度的增加,SPAC水势梯度提高,各介质层水势差的增大,提高了水分循环和能量交换的强度。  相似文献   
80.
根据2010年-2013年福建省主要江河入海口每月一次的监测调查资料,评价2013年的入海口水质现状和富营养化程度,分析2013年的月变化和2010年-2013年的年际变化.结果表明,2013年福建省11条主要江河入海口水质均为劣四类海水水质,富营养化程度高且磷限制特征明显.入海口的石油类和化学需氧量的月变化和年变化受降雨影响大,高值区主要在降雨多的月份和年份,入海口的无机氮和活性磷酸盐含量受水中浮游植物和降雨量双重影响,夏秋低,春冬高,年际变化受年际降雨量变化影响有所波动,但大部分入海口的无机氮和活性磷酸盐含量呈略微上升的趋势.  相似文献   
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