Effect of NOM characteristics on brominated organics formation by ozonation

In this study, organic fractions, namely, humic acid, fulvic acid, hydrophobic base and neutral, and hydrophilic acid, base, and -neutral, were extracted from source water. First, the characteristics of the organic fractions, such as carboxylic acidity, phenolic acidity, ultraviolet absorbance, and aromatic content, were analyzed. Further, a systematic study was carried out to the by-products obtained when organic fractions, to which various amounts of bromide had been added, were oxidized with ozone. Samples after ozonation were analyzed for several brominated organics. The results indicate that the characteristics of the aquatic organic matter, including carboxylic/phenolic acidity, aromatic/aliphatic content, and ultraviolet absorbance, appear to affect the formation of halogenated organics. In general, hydrophobic organics having higher phenolic acidity, aromatic content, and ultraviolet absorbance have higher ozone consumption and produce higher concentrations of brominated organics than hydrophilic organics. It was also found that humic acid demonstrated the highest bromoform (CHBr(3)), dibromoacetic acid (DBAA), and 2,4-dibromophenol (2,4-DBP) formation, whereas hydrophilic neutral produced less CHBr(3) and 2,4-DBP than the rest of the organic fractions but produced the highest amount of dibromoacetone (DBAC) and dibromoacetonitrile (DBAN).     

Spatial-temporal analysis of wetland landscape pattern under the influence of artificial dykes in the Yellow River delta

The influence of anthropogenic activities,especially artificial dykes,on the coastal wetland landscape is now considered as a serious problem to the coastal ecosystem.It is important and necessary to analyze changes of coastal landscape pattern under the influence of artificial dykes for the protection and management of coastal wetland.Our study aimed to reveal the quantitative characteristics of the coastal wetland landscape and its spatial-temporal dynamics under the influence of artificial dykes in the Yellow River delta(YRD).It was analyzed by the methods of the statistical analysis of landscape structure,five selected landscape indices and the changes of spatial centroids of three typical wetland types,including reed marshes,tidal fiats and aquaculture-salt fields.The results showed that:(1)Reduction of wetland area,especially the degradation of natural wetlands,had been the principal problem since the dykes were constructed in the YRD.The dykes created conditions for the development of artificial wetlands.However,the new born artificial wetlands were still less than the vanished natural wetlands.(2)Compared with the open area,the building of artificial dykes significantly speeded up the changes of landscape patterns and the aggravation of the landscape fragmentation in the closed area.(3)The changes of area-weighted centroids of three typical wetland landscapes were greatly affected by dykes,and the movement of the centroid of the aquaculture-salt field was very sensitive to the dykes constructed in the corresponding period.     

A Methodology Framework for Regional Land-use Change Studies based on Landsat TM images: A Case Study in Northeast China

Abstract

Land-use change is an important aspect of global environment change. It is, in a sense, the direct result of human activities influencing our physical environment. This paper analyzed the land- use change in Northeast China during 1985–2000 based on Landsat TM images. It divides Northeast China into five land-use zones based on the dynamic degree model of land-use: woodland/grassland-arable land conversion zone, dry land-paddy field conversion zone; urban expansion zone, interlocked zone of farming and pasturing and reclamation and abandon zone. The findings include the obvious increase of cropland area, paddy field and dry land increased by 75 and 276 thousand hm² respectively; urban areas expanded rapidly, areas of town and rural residence increased by 76.8 thousand hm²; areas of forests and grassland decreased sharply with the amounts of 1399 and 1521 thousand hm² respectively; areas of water body and unused land increased by 148 and 514 thousand hm² respectively. This paper also discusses the driving forces in each land-use dynamic zone and finds that some key biophysical factors affect conspicuously the conversion of different land-use types. The relation between land-use conversion and DEM, accumulated temperature (≤10°C) and precipitation was analyzed and represented. The land-use changes In Northeast China resulted from the changing macro social and economic factors and local physical elements. Rapid population growth and management changes can explain the shaping of woodland/grassland-cropland conversion zone. The conversion from dry land to paddy field in the dry land-paddy field conversion zone, apart from the change of physical elements promoting the expansion of paddy field, results from two reasons: one is that the implementation of market economy in China has given farmers the right to decide what and how they plant their crops, the other factor is originated partially from the change of the dietary habit along with the social and economic development. The conversion from paddy field to dry land is caused primarily by the shortfall of irrigation water, which in turn is caused by poor water allocation managed by local governments. The shaping of the reclamation and abandon zone is partially due to the lack of environment protection consciousness among pioneer settlers. The reason for the conversion from grassland to cropland is the relatively higher profits of farming than that of pasturing in the interlocked zone of farming and pasturing. In Northeast China, the rapid expansion of built-up areas results from two factors: the existence of a small number of towns and the huge potential for expansion of the existing towns and cities. The urban land expanded mainly in areas with a gentle topographic relief and low population density.     

环境因素对芦苇湿地CH4排放的影响

用封闭式箱法对辽河三角洲芦苇湿地温室气体CH₄ 排放进行了长期观测 .结果表明 ,CH₄ 排放有明显的季节变化规律 ,平均通量为 520μg·m^-2·h^-1.土壤产CH₄ 活性主要发生在0～5cm土层中 ,并随土层深度的增加而显著下降 .CH₄排放受环境因素影响很大 ,土壤氧化还原电位在 -110mV时就有CH₄排放 ,其排放量随氧化还原电位的下降而增加 .另外 ,随着淹水深度的增加 ,CH₄ 排放反而减少 .在测定期内 ,CH₄ 排放与温度呈明显的正相关 (R²=0196,n=21,P<0.05).     

卤代烃毒性的化学评价法:鸟嘌呤卤代烃加合物FTIR、UV光谱表征

研究鸟嘌呤与一系列卤代烃反应的加合产物 ,利用HPLC二极管阵列检测器得到的特征紫外光谱 (UV)对加合产物样品进行了鉴定 ,然后加合产物经薄层 (TLC)分离 ,再进一步做红外 (FTIR)鉴定 ,从而得到鸟嘌呤 卤代烃氧位和氮位加合物的红外光谱表征 .研究表明 ,鸟嘌呤卤代烃的氮位加合物异构体的紫外光谱吸收峰的波长在 240～250nm之间 ,氧位加合物UV波长在 260～270nm附近 .鸟嘌呤与本文涉及的各卤代烃的加合物的红外光谱之间差别不大 :其氮位加合物在 1700cm^-1处 ,均有CO的特征吸收峰 ;其氧位加合物的红外光谱亦相近 .     

不同波段紫外光在TiO2悬浊液中的消光特点

为确定TiO₂催化剂悬浊液对不同波段紫外光的消光规律,本试验以4-CBA-Na为模型污染物,针对催化剂/污染物悬浊液体系在不同催化剂投加量下,对UVA、UVB和UVC波段光子的消光效果进行了测定.结果表明,各悬浮体系对各波段紫外光的消光基本上符合比耳定律,即随着入射光程的增加,光强呈现负指数衰减;紫外光在催化剂悬浊液中的消光系数随催化剂投加量的增大而增加,其增加规律可以用二次多项式表示;污染物溶液本身对UVB和UVC紫外光有吸收,UVB和UVC紫外光在催化剂-污染物悬浮体系中的消光系数可视为污染物与催化剂颗粒的消光系数之叠加.催化剂悬浊液对紫外光的消光系数随紫外光波长的减小而增大,这意味着使用短波长的UVC作为光催化降解光源可以提高能量利用效率.     

农垦与放牧对内蒙古草原N2O、CO2排放和CH4吸收的影响

利用优选静态箱/气相色谱法(GC),首次对我国内蒙古草原典型地区进行了人类活动对N₂O、CO₂和CH₄交换通量影响的实验观测结果表明,农垦麦田N₂O平均排放通量比原始草原高出3倍,并改变了草甸草原为CO₂汇的性质,使其季节排放净通量以C计增加14.3 mg·(m²·h).随放牧强度的增加CO₂排放通量呈线性增长,轻牧会引起草原对CH₄吸收的大幅增加,而随着放牧压力的增大,增加值迅速回落.农垦麦田与草甸草原相比地-气间CH₄交换无显著变化,放牧强度对N₂O排放影响无显著规律.土壤湿度和温度是影响草原排放N₂O和CO₂、吸收CH4季节变化形式的关键因子,而人类活动仅影响排放强度.排放和吸收量年际间差异很大,但主要受降水的影响.N₂O和CO₂排放与CH₄吸收峰值相反现象普遍存在.     

Environmental input-output model and its analysis with a focus on the solid waste management sectors

ＩｎｔｒｏｄｕｃｔｉｏｎＳｉｎｃｅｔｈｅｆｉｒｓｔｅｎｖｉｒｏｎｍｅｎｔａｌｉｎｐｕｔｏｕｔｐｕｔｍｏｄｅｌ(ＥＩＯＭ)(Ｃｕｍｂｅｒｌａｎｄ,1966)ｗａｓｅｓｔａｂｌｉｓｈｅｄｂｙｉｎｃｏｒｐｏｒａｔｉｎｇｅｎｖｉｒｏｎｍｅｎｔａｌｆａｃｔｏｒｓｉｎｔ?..     

生物法处理低浓度有机废气的填料选择研究

采用不锈钢环、瓷环、陶粒、塑料环、海藻石、轻质陶块、煤渣等作为填料的试验研究，结果表明七种填料的净化性能顺序为：海藻石＞轻质陶块＞陶粒＞瓷环＞不锈钢环＞煤渣＞塑料环。     

秦岭若干重要类型金矿床(体)快速定位预测

本文以西部秦岭地区八卦庙、双王、煎茶岭 3种重要类型金矿床为例 ,在成矿地质背景研究基础上 ,开展若干新方法新技术的找矿试验 ,研究发现 ,八卦庙式金矿岩石的烃含量与其金品位大致成正相关关系 ;而且金矿化强度和规模越大 ,相关系数值也越大 ;据此根据石英脉的烃含量对隐伏金矿床 (体 )和金矿化规模进行预测。双王式金矿原生晕的前缘晕元素为B、As、Sb、Hg,近矿晕元素为Au、Ba(-) ,尾晕元素为Mn、Bi。通过原生叠加晕垂向研究预测 ,双王和八卦庙金矿床现有的金矿体向下延伸还较大 ,在矿床的深部存在有盲矿体。煎茶岭式金矿的矿石铅同位素平均值比围岩要小 ,铅同位素曲线的低峰区往往就指示矿体所在 ;预测区的2 0 6Pb/ 2 0 4 Pb、2 0 8Pb/ 2 0 4 Pb比值变差椭圆图的形状和轴向斜率与已知矿区趋于一致 ,并且两者的变差椭圆图形大部分重叠 ,说明存在有同类型金矿体。以上研究成果为同期或后来的勘探工作或矿山采矿所验证。