酸性条件下剩余污泥中Ca2＋和Mg2＋溶出对磷回收的影响

为了在酸性条件下实现剩余污泥中磷的高效回收，对pH=3时剩余污泥水解酸化过程中氨氮、正磷酸盐和钙镁离子的溶出现象以及磷回收进行了研究分析。结果表明：当pH=3时，所溶出的氨氮、镁离子和钙离子与磷酸盐的摩尔比均大于1，能满足采用鸟粪石沉淀法或者羟磷灰石沉淀法回收磷的要求；但所溶出的钙镁离子的摩尔比大于1，会对鸟粪石沉淀法回收磷的顺利进行有较大影响；有无外加镁剂对磷回收率影响不大。采用改型后的镁型强酸性阳离子交换树脂进行离子交换可以得到较高纯度的鸟粪石沉淀产品，通过XRD检测其纯度为95％以上。     

环境因素对长寿湖底泥释磷影响的模拟实验研究

肥水养殖显著增加了长寿湖底泥中的磷含量。为了解肥水养殖积累在湖泊底泥中磷的释放情况,以长寿湖大坝口枯水期底泥为实验材料,模拟研究了不同环境条件(上覆水pH、温度、DO含量和扰动)下湖泊底泥的释磷特征。结果表明,在弱碱性条件下,底泥释磷量随上覆水pH的升高而升高;温度升高有利于底泥磷的释放,温度每升高5℃,第21天时底泥释磷量增大0.0045～0.0074 mg/L;DO含量降低有利于底泥中铁/铝结合态磷的释放;扰动对底泥磷的释放没有明显影响。研究表明,网箱养殖增加了底泥中的有机磷含量,促进有机磷向无机磷转化,增大了底泥中磷的释放风险。     

Desorption of arsenic from drinking water distribution system solids

Previous work has shown that arsenic can accumulate in drinking water distribution system (DWDS) solids (Lytle et~al., 2004) when arsenic is present in the water. The release of arsenic back into the water through particulate transport and/or chemical release (e.g. desorption, dissolution) could result in elevated arsenic levels at the consumers' tap. The primary objective of this work was to examine the impact of pH and orthophosphate on the chemical release (i.e. desorption) of arsenic from nine DWDS solids collected from utilities located in the Midwest. Arsenic release comparisons were based on the examination of arsenic and other water quality parameters in leach water after contact with the solids over the course of 168~hours. Results showed that arsenic was released from solids and suggested that arsenic release was a result of desorption rather than dissolution. Arsenic release generally increased with increasing initial arsenic concentration in the solid and increasing pH levels (in the test range of 7 to 9). Finally, orthophosphate (3 and 5 mg PO₄/L) increased arsenic release at all pH values examined. Based on the study results, utilities with measurable levels of arsenic present in their water should be aware that some water quality changes can cause arsenic release in the DWDS potentially resulting in elevated levels at the consumer's tap.     

典型污染源材料中多溴联苯醚(PBDEs)的释放

为研究以多溴联苯醚（PBDEs）为代表的含卤半挥发性有机物（SVOCs）在室内空气中的扩散特性,在对杭州室内环境（办公室、居室）空气中PDBEs14种单体浓度检测的基础上,分析比较了不同污染源材料中PBDEs的含量,测定了材料PBDEs挥发强度系数;探究了典型污染源材料中PBDEs释放的影响因素及其相关性.结果表明,杭州室内环境空气颗粒相和气相中PBDEs平均浓度为427.26和416.46pg/m³,其中颗粒相和气相中主要特征单体均为BDE-209.所选取的9种室内常用材料的PBDEs挥发强度系数大小依次为：地毯>电线>塑料板>阻燃布>电路板>防烫桌布>保温棉>自粘墙纸>绝缘胶带.对比不同材料中各PBDEs同系组的含量：绝缘胶带、塑料板、防烫桌布、阻燃布中十溴二苯醚（deca-BDEs）的占比最高,分别为81.33%、63.83%、27.3%和34.1%;电线中四溴二苯醚（tetra-BDEs）的占比最高,为29.83%;自粘墙纸、电路板、地毯、保温棉中五溴二苯醚（penta-BDEs）的占比最高,分别为35.82%、41.25%、45.75%和38.64%.典型污染源材料中PBDEs释放的影响因素实验结果表明,环境模拟舱中的PBDEs总浓度与温度和封闭时间对数均呈显著正相关,相关系数r和显著水平P分别为r=0.811,p<0.05和r=0.883,p<0.05,且封闭时间对源释放PBDEs总浓度的影响比温度稍大.同时,污染源特征因素（材料中PBDEs的固有含量与PBDEs挥发强度系数）对源释放的影响程度比环境因素（温度和封闭时间）大.     

外秦淮河底泥污染及疏浚效果

外秦淮河是南京市一条重要的城市景观行洪河道,多年来受工业及生活污水影响,内源污染严重.为充分了解外秦淮河底泥污染特征,为疏浚提供决策依据,对河道上、中和下游典型断面底泥界面微环境以及营养物含量进行调查,采用有机指数法和污染指数法对底泥污染状况进行评估,同时根据污染物垂向分布特征模拟清淤对底泥内源释放削减的影响.结果表明,上中下游底泥界面以上DO均值分别为4.62、 3.25和3.41mg·L^-1,且分别在4.4、 3.5和5.5 mm处消耗殆尽,是典型的城市河道污染特征体现.调查河段表层底泥的ω(TN)、ω(TP)和ω(OM)均值分别为1 734mg·kg^-1、 1 337 mg·kg^-1和4.82%,底泥TN和OM的有机污染指数均值为0.48,处于尚清洁水平,TP的单项污染指数均值为3.18,处于重度污染水平.模拟30 cm清淤深度结果表明,底泥SRP和Fe²⁺的释放速率较清淤前分别削减42%～82%和88%～96%,而NH⁺₄-N的释放速率却较清淤前有...     

三峡库区支流库湾消落带土壤磷形态赋存特征及其释放风险

三峡库区消落带经历反复的淹水-落干循环影响,消落带土壤磷迁移转化过程加快,可能加剧支流库湾水体富营养化.采集了三峡库区腹心支流库湾典型消落带土壤,测定磷赋存形态与磷素饱和度(DPS)等,分析磷释放风险.结果表明,(1)消落带土壤ω[总磷(TP)]、ω[无机磷(IP)]和ω[有机磷(OP)]均值分别为771.80、485.33和166.30 mg·kg^-1,IP和OP均以非活性形态磷为主.(2)消落带土壤形态磷的赋存格局受落干-淹水方式影响,Ex-P和NaHCO₃-Po含量显著高于对照土壤,Fe-P、HCl-Po和Fulvic-Po含量沿高程下降而显著降低(P<0.05),反复的干湿交替促进了消落带土壤活性磷的生成和中等活性磷的释放和积累.(3)消落带土壤生物ω[有效磷(Bio-P)]为49.19～148.78 mg·kg^-1,占TP的质量分数为7.71%～24.78%,磷素饱和度(DPS)为5.85%～22.00%.目前,支流库湾消落带土壤整体磷释放风险较低,170 m高程土壤需要重点关注.Fe-P、HCl-Po和...     

Carbon Pool Dynamics in the Lower Fraser Basin from 1827 to 1990

/ To understand the total impact of humans on the carbon cycle, themodeling and quantifying of the transfer of carbon from terrestrial pools tothe atmosphere is becoming more critical. Using previously published data,this research sought to assess the change in carbon pools caused by humans inthe Lower Fraser Basin (LFB) in British Columbia, Canada, since 1827 anddefine the long-term, regional contribution of carbon to the atmosphere. Theresults indicate that there has been a transfer of 270 Mt of carbon frombiomass pools in the LFB to other pools, primarily the atmosphere. The majorlosses of biomass carbon have been from logged forests (42%), wetlands(14%), and soils (43%). Approximately 48% of the forestbiomass, almost 20% of the carbon of the LFB, lies within old-growthforest, which covers only 19% of the study area. Landfills are nowbecoming a major sink of carbon, containing 5% of the biomass carbonin the LFB, while biomass carbon in buildings, urban vegetation, mammals, andagriculture is negligible. Approximately 26% of logged forest biomasswould still be in a terrestrial biomass pool, leaving 238 Mt of carbon thathas been released to the atmosphere. On an area basis, this is 29 times theaverage global emissions of carbon, providing an indication of the pastcontributions of developed countries such as Canada to global warming andpossible contributions from further clearing of rainforest in both tropicaland temperate regions.KEY WORDS: Carbon pools; Global warming; Carbon release to atmosphere;Greenhouse effect     

淀山湖沉水植物死亡分解过程中营养物质的释放

测定了上海淀山湖5种常见沉水植物的营养成分含量及其死亡后在好氧(DO>3.5 mg/L)或低氧(DO<3.5 mg/L)状态下分解释放TN、TP和有机物(以高锰酸盐指数计,下同)等营养物质的动态过程,并对营养物质释放强度与营养成分含量的相关性进行了分析.结果表明, 5种沉水植物中,金鱼藻的TN和TP含量最高,质量分数分别为(4.07±0.22)%和(0.99±0.09)%;好氧状态下TN和有机物的释放强度大于低氧状态,两种状态下TP的释放强度没有显著差异;TP的释放比TN快,一般需10 d左右,而TN和有机物的释放分别需要29 d和20 d左右;在好氧状态下,NO-2-N、NO-3-N和可溶性总磷酸盐的平均释放强度与植物TN含量呈显著正相关(p<0.05),NH 4-N的平均释放强度与植物TP含量呈显著正相关(p<0.05);在低氧状态下,NO-2-N的平均释放强度与植物TN含量、NO-3-N的平均释放强度与植物TP含量分别呈显著正相关(p<0.05);有机物的平均释放强度与植物TP含量呈极显著负相关(p<0.01).     

Elements of Carbon Balance in Oligotrophic Bogs

Elements of carbon balance of oligotrophic bogs were studied using an example of the landscape profile of the Klyuch River in 1998–2000. Carbon balance was preliminarily calculated taking into account the biological productivity, release of carbon dioxide and methane, and carbon outflow with bog waters. Based on the data obtained on the carbon inflow and outflow, the conclusion was made concerning the progressive peat formation in the region studied.     

两种掺气水流的计算模型比较

在污水压力输送管道中，污水中气体的存在会影响液体的流动，以污水管中的气、液相流为研究对象，运用集中空穴模型（气泡离散分布模型）和均匀分布模型两种计算方法，来研究停泵水锤过程的压力和流速的变化趋势，实例计算结果表，在设有止回阀的水锤现象中，利用离散分布模型所得的最高水位要比利用均匀分布模型的计算值高，在不设止回阀的水锤现象中，两者的结构基本保持一致。均匀分布模型假定气体在水中呈均匀分布，因此在计算断面上的气体量变化不如离散分布模型来得剧烈，其水位正峰值比离散分布模型低，负峰值比离散分布模型高。