涂铁石英砂吸附水中Cr（Ⅵ）的研究

采用静态吸附和动态过滤的试验方法研究了涂铁石英砂（IOCS）滤料对水中Cr（Ⅵ）的去除,并探讨其吸附机理。研究结果表明,Cr（Ⅵ）在IOCS上的吸附平衡符合Langmuir吸附模型。经氧化铁改性滤料表面电位带正电荷,对水中的Cr（Ⅵ）有良好的去除效果。pH值对Cr（Ⅵ）的去除影响较大,随着溶液的pH值升高,滤料表面电位减小,Cr（Ⅵ）的吸附率也减小。IOCS滤料去除Cr（Ⅵ）机理主要为静电吸附。     

Daily Updating of Operational Statistical Seasonal Water Supply Forecasts for the western U.S.1

Abstract: Official seasonal water supply outlooks for the western United States are typically produced once per month from January through June. The Natural Resources Conservation Service has developed a new outlook product that allows the automated production and delivery of this type of forecast year‐round and with a daily update frequency. Daily snow water equivalent and water year‐to‐date precipitation data from multiple SNOTEL stations are combined using a statistical forecasting technique (“Z‐Score Regression”) to predict seasonal streamflow volume. The skill of these forecasts vs. lead‐time is comparable to the official published outlooks. The new product matches the intra‐monthly trends in the official forecasts until the target period is partly in the past, when the official forecasts begin to use information about observed streamflows to date. Geographically, the patterns of skill also match the official outlooks, with highest skill in Idaho and southern Colorado and lowest skill in the Colorado Front Range, eastern New Mexico, and eastern Montana. The direct and frequent delivery of objective guidance to users is a significant new development in the operational hydrologic seasonal forecasting community.     

A field experiment with variable-suction multi-compartment samplers to measure the spatio-temporal distribution of solute leaching in an agricultural soil

Solutes spread out in time and space as they move downwards from the soil surface with infiltrating water. Solute monitoring in the field is often limited to observations of resident concentrations, while flux concentrations govern the movement of solutes in soils. A recently developed multi-compartment sampler is capable of measuring fluxes at a high spatial resolution with minimal disturbance of the local pressure head field. The objective of this paper is to use this sampler to quantify the spatial and temporal variation of solute leaching below the root zone in an agricultural field under natural rainfall in winter and spring. We placed two samplers at 31 and 25 cm depth in an agricultural field, leaving the soil above undisturbed. Each sampler contained 100 separate cells of 31 × 31 mm. Water fluxes were measured every 5 min for each cell. We monitored leaching of a chloride pulse under natural rainfall by frequently extracting the collected leachate while leaving the samplers buried in situ. This experiment was followed by a dye tracer experiment. This setting yielded information that widely surpassed the information that can be provided by separate anionic and dye tracer trials, and solute transport monitoring by coring or suction cups. The detailed information provided by the samplers showed that percolation at the sampling depth started much faster (approximately 3 h after the start of rainfall) in initially wet soil (pressure head above − 65 cm) than in drier soil (more than 14 h at pressure heads below − 80 cm). At any time, 25% of the drainage passed through 5–6% of the sampled area, reflecting the effect of heterogeneity on the flow paths. The amount of solute carried by individual cells varied over four orders of magnitude. The lateral concentration differences were limited though. This suggests a convective–dispersive regime despite the short vertical travel distance. On the other hand, the dilution index indicates a slight tendency towards stochastic–convective transport at this depth. There was no evidence in the observed drainage patterns and dye stained profiles of significant disturbance of the flow field by the samplers.     

改性铁覆膜砂的制备及吸附性能研究

制备了4种改性铁覆膜砂,并对其吸附性能进行了全面的实验,分析比较了4种改性剂的作用和效果.实验中发现,添加改性剂对铁覆膜砂吸附性能的促进作用各不相同,改性剂和铁氧化物的性质共同决定了改性铁覆膜砂的性质.吸附等温线和连续动态过滤实验结果表明,活性炭和硅藻土对提高铁覆膜砂吸附性能有促进作用,但膨润土和粉煤灰的作用不明显,甚至还可能降低吸附容量.活性炭改性铁覆膜砂的吸附等温式符合Langmuir模型,硅藻土改性铁覆膜砂、膨润土改性铁覆膜砂和粉煤灰改性铁覆膜砂对Langmuir模型和Freundlich模型都有较好的相关性.改性铁覆膜砂对天然有机物(NOM)的吸附属于单分子层吸附,吸附的主要机理为静电相互作用、配位交换-表面络合作用和疏水/憎水作用等.溶液pH值对改性铁覆膜砂吸附NOM有很大的影响,表现为低"pH值去除效率高,高pH值去除效率低"的特点,其变化规律取决于添加物质的性质.磷酸盐会和腐殖酸在改性铁覆膜砂表面产生竞争吸附,磷酸盐对粉煤灰改性铁覆膜砂的吸附能力影响最大.     

武汉市主要绿化树种滞尘效应研究

本实验对武汉市城区主干道主要绿化树种的滞尘效应与叶表面结构进行了研究。结果表明：（1）同一尘源条件下,不同树种的滞尘能力差异显著。乔木中悬铃木滞尘能力较高,可达6.9345 g/m²;小乔木中紫薇和紫叶李是滞尘能力较高的树种,滞尘能力分别为1.9543 g/m²和1.8790 g/m²;灌木中红花檵木和杜鹃等有较强的滞尘能力,分别可达4.0373 g/m²和3.8875 g/m²;（2）利用扫描电镜观察叶表面结构发现：叶表具毛被、褶皱、较深的不规则网格等特征的树种滞尘能力较高,叶表平滑或叶表网格结构规则且较浅时滞尘能力较低;（3）同一树种在不同的尘源条件下滞尘能力差异显著,空气中颗粒物浓度越高,滞尘能力也越大。以车流量近似模拟尘源条件表明,滞尘能力与车流量呈正相关。     

Ca(Ⅱ)在活性污泥生物絮凝中的作用研究

采用4个平行的序批式反应器(SBR),研究了进水Ca2+浓度对活性污泥絮体表而特性和结构稳定性的影响,并由此来确定Ca2+在生物絮凝中的作用.结果表明:随着进水Ca2+浓度的增加,污泥中的Ca含量逐渐增大.进水中Ca2+的加入,增大了污泥絮体的粒径和密度,进南改善了污泥的沉降性能;Ca2+的加入,使可供结合的蛋白质数量最高增至近1倍,污泥表面疏水性也相应增强;污泥絮凝性能的改善,主要和可供Ca2+结合的蛋白质含量增加有关,而非多糖;EDTA通过络合污泥絮体中的Ca2+,破坏了山Ca2+架桥形成的污泥絮体结构,这说明Ca2+可通过和胞外聚合物(extracellular polymeric substances,EPS)中的负电官能团架桥来促进污泥絮体的形成并维持絮体结构的稳定性.     

载硫活性炭微观结构和表面形态研究

为了增强活性炭脱除燃煤电厂烟气中汞的能力,利用汞和硫可以生成稳定的HgS的性质,研究了通过热沉淀增加了活性炭中的硫含量的改性方法,并以SEM、BET、TGA等方法,研究了改性对活性炭表面形貌、硫在活性炭中的分布、活性炭比表面积等性能的影响。结果表明,热沉淀改性方法可以增加活性炭中的硫含量;硫粘附在活性炭的炭链上量较多,孔壁较少;改性工艺降低了活性炭的比表面积,且改性活性炭的比表面积随着温度的升高而增大;载硫后,活性炭中元素硫和炭的结合被增强。     

红枫湖地表水中多环芳烃的分布及来源

将固相微萃取与气相色谱联用,对贵阳红枫湖水样中16种美国环境保护署优控的多环芳烃进行分析。结果表明：红枫湖水中16种多环芳烃总量为0167 1~0336 4 μg/L,与国内其它水系相比,湖中存在多环芳烃轻度污染。7种（萘、荧蒽、苯并(b)荧蒽、苯并(k)荧蒽、苯并(a)芘、茚并(1,2,3-cd)芘和苯并(ghi)苝）多环芳烃的总量未超出中国城市供水行业对多环芳烃规定的限值,但作为饮用水源,红枫湖水中的苯并(a)芘含量已超出我国标准GB3838-2002中生活饮用水地表水源地的苯并(a)芘限值,并且苯并(a)蒽、〖JX-*9〗〖SX（B-25x〗〖HT7,5”〗艹〖〗〖HT6”,5”〗屈〖HT5”〗〖SX）〗〖JX*9〗、苯并(b)荧蒽、苯并(k)荧蒽、苯并(a)芘、茚并(1,2,3-cd)芘的含量也超过了美国环境保护署地表水水质标准限值。通过多环芳烃特征参数的比值,分析了红枫湖水中多环芳烃的污染来源。污染源分析表明,湖中多环芳烃的主要来源为燃烧源,包括木材、煤以及化石燃料的燃烧,同时也有一部分多环芳烃是来源石油类物质的输入.     

污水湿地处理工艺优化组合设计

污水湿地处理系统是利用土壤、作物、微生物自然净化功能的生态工程技术。主要有水面湿地和渗滤湿地两种类型,在天津城市污水土地处理与利用系统研究的基础上,将两种工艺的优点进行优化组合,并应用于大港油田等污水湿地处理工程,运行结果表明：将水面湿地和渗滤湿地工艺优化组合设计的示范工程,具有提高水力负荷、减少运行费用、节省工程投资、处理效果稳定等特点,有利于处理工程的长期稳定运行。     

Modeling Runoff Response to Land Cover and Rainfall Spatial Variability in Semi-Arid Watersheds

Hydrologic response is an integrated indicator of watershed condition, and significant changes in land cover may affect the overall health and function of a watershed. This paper describes a procedure for evaluating the effects of land cover change and rainfall spatial variability on watershed response. Two hydrologic models were applied on a small semi-arid watershed; one model is event-based with a one-minute time step (KINEROS), and the second is a continuous model with a daily time step (SWAT). The inputs to the models were derived from Geographic Information System (GIS) theme layers of USGS digital elevation models, the State Soil Geographic Database (STATSGO) and the Landsat-based North American Landscape Characterization classification (NALC) in conjunction with available literature and look up tables. Rainfall data from a network of 10 raingauges and historical stream flow data were used to calibrate runoff depth using the continuous hydrologic model from 1966 to 1974. No calibration was carried out for the event-based model, in which six storms from the same period were used in the calculation of runoff depth and peak runoff. The assumption on which much of this study is based is that land cover change and rainfall spatial variability affect the rainfall-runoff relationships on the watershed. To validate this assumption, simulations were carried out wherein the entire watershed was transformed from the 1972 NALC land cover, which consisted of a mixture of desertscrub and grassland, to a single uniform land cover type such as riparian, forest, oak woodland, mesquite woodland, desertscrub, grassland, urban, agriculture, and barren. This study demonstrates the feasibility of using widely available data sets for parameterizing hydrologic simulation models. The simulation results show that both models were able to characterize the runoff response of the watershed due to changes of land cover.