土壤pH对锰赋存形态的影响

以热带亚热带土壤为研究对象，用连续分级浸提法探讨了土壤中锰赋存形态与ｐＨ值的关系。结果表明：土壤中的锰处于一种动态平衡状态，各形态锰的含量及其占全锰的比例随ｐＨ的变化而变化，其中代换态锰和有机态锰随ｐＨ值升高而减少，氧化态锰、无定形铁结合态锰和晶形铁结合态锰则随ｐＨ值升高而增加，土壤中锰的生物有效性则随ｐＨ值升高而降低。     

Field study of TCE diffusion profiles below DNAPL to assess aquitard integrity

An area where a free-product accumulation of trichloroethylene (TCE) dense non-aqueous phase liquid (DNAPL) occurs at the bottom of a 10-m-thick surficial sand aquifer was studied to determine the integrity of the underlying, 20-m-thick, clayey silt aquitard formed of glaciolacustrine sediment. TCE concentration-versus-depth profiles determined from aquitard cores collected at five locations indicated penetration of detectable TCE 2.5 to 3.0 m into the aquitard. Two of the profiles show persistent DNAPL at the aquitard interface, while two others indicate that DNAPL, present initially, was completely dissolved away producing concentration declines at the aquitard interface. The fifth profile suggests shallow DNAPL penetration (<0.5 m) into the aquitard, however, this penetration, which was likely caused by cross-contamination during core collection or cone penetrometry (CPT) of the aquitard interface, did not increase the maximum depth of TCE penetration. Combining the field profiles with one-dimensional model simulations, downward migration of the aqueous TCE front, defined as the EPA MCL of 5 microg/l, which was below the analytical detection limit, was projected to a distance between 4 and 5 m below the top of the aquitard. Using a single set of estimated aquitard parameter values, simulations of aqueous TCE migration into the aquitard provided a good fit to four of the field profiles with a migration time of 35 to 45 years, consistent with the history of TCE use at the site. These simulations indicate aqueous TCE migration is diffusion-dominated with only small advective influence by the downward groundwater velocity of 2 to 3 cm/year or less in the aquitard due to pumping of the underlying aquifer to supply water to the facility in the past 50 years. The applicability of the parameter values was confirmed by in situ diffusion experiments of 1-year duration, in which stainless steel cylinders containing DNAPL were inserted into the aquitard. The diffusion-dominated nature of the profiles indicates that the aquitard provides long-term protection of the underlying aquifer from contamination from this DNAPL zone. Simulations of long-term migration of the TCE solute front indicate breakthrough to the lower aquifer at 1200 years for the no advection scenario and at 500 years if the strong downward hydraulic gradient persists. However, even after breakthrough, the mass flux through the aquitard to the underlying aquifer remains relatively low, and when considered in terms of potential impacts to pumping wells, concentrations are not expected to increase significantly above present-day MCLs. The use of contaminant profiles of different time and distance scales, in addition to hydraulic data, dramatically improves the ability to assess aquitard integrity, and provides improved transport parameter values for estimating contaminant arrival times and fluxes. The apparent lack of deep preferential pathways for TCE migration, such as open fractures, is probably due to the softness of the silty aquitard deposit and minimal physical or chemical weathering of the aquitard provides long-term protection of the underlying aquifer from contamination from this DNAPL zone. Simulations of long-term migration of the TCE solute front indicate breakthrough to the lower aquifer at 1200 years for the no advection scenario and at 500 years if the strong downward hydraulic gradient persists. However, even after the breakthrough, the mass flux through the aquitard to the underlying aquifer remains relatively low, and when considered in terms of potential impacts to pumping wells , concentrations are not expected to increase significantly above present-day MCLs. The use of contaminant profiles of different time and distance scales, in addition to hydraulic data, dramatically improves the ability to assess aquitard integrity, and provides improved transport parameter values for estimating contaminant arrival times and fluxes. The apparent lack of deep preferential pathways for TCE migration, such as open fractures, is probably due to the softness of the silty aquitard deposit and minimal physical or chemical weathering of the aquitard.     

低浓度硫化氢废气的液相催化氧化法净化实验研究

针对H2S浓度为750~1500mg/m3的气体的液相催化氧化技术进行了动力学实验研究。配制了以铁基离子作为主催化剂的复合吸收净化溶液,同时加入稳定剂和表面活性剂提高催化剂在碱性吸收溶液的活性。分别考察了原料气中H2S、O2含量以及吸收液中催化剂离子浓度、温度等因素对吸收速率的影响;确定了较为理想的吸收操作条件并获得了较好的吸收净化效果;饱和吸收液易于再生,净化性能恢复良好,可重复使用。     

环境哲学与历史性转变

所谓环境哲学，就是从哲学角度研究环境与发展这一矛盾的运动规律，并用以指导环境工作实践的一门科学。从哲学角度看，推行历史性转变首在转变那些不适应客观变化的观念、经验和制度，以实践作为检验真理的唯一标准，对受计划经济体制影响的理念和经验进行反思，走出误区，以利转变。环境与经济的“并重”和“同步”是促进环境与发展矛盾转化的根本途径，“综合”是用改革的方法解决发展中的环境问题，是实现前两个转变的基本保障。总之，实施“三个转变”就是发挥人的主观能动作用，积极创造条件，促使环境与发展的矛盾由“两难”向“双赢”转化，将“以牺牲环境换取经济增长”转变为“以保护环境，优化经济增长”，真正走上生产发展、生活富裕、生态良好的文明发展道路。     

空气中挥发性有机物监测技术的研究进展

讨论了空气中挥发性有机化合物（VOCs）的监测分析方法研究进展。重点介绍了空气中VOCs的采集、分析和测定；简要叙述了样品前处理的新方法--固相微萃取法（SPME）与其它前处理方法的研究概况。     

苯酚的超临界水氧化试验

以自建的一套连续式超临界水氧化装置的温度，压力，溶氧量和流量等参数的可控性进行了实验，并在此基础上进行了苯酚的超临界水氧化研究。结果表明：所建立的装置能比较精确控制各种条件参数，是可靠的超临界水氧化试验研究装置。在氧气过量的条件下，停留时间是影响苯酚在超临界水中氧化分解的主要因素，反应的温度和压力升高导致苯致苯酚去除率的增大，只要有足够的氧气，苯酚起始浓度的增加对苯酚的转化率影响不明显，在实验条件下，溶液中苯酚的去除动力学对苯酚是一级，氧气是零级。     

水环境中氯酚污染物的高效液相色谱分析

1　IntroductionInorganiccontaminants,phenolcompoundsaredeterminedprioritycontaminantbyUSEPA[1 ].ThephenolcompoundsinthedrinkingwaterisstipulatedasabsolutelydeterminationitembytheEuropeanEconomicCommunity (E E C .)andourcountry.Themeasurementofpollutionish…     

Dynamics of Turbulence in Low-Speed Oscillating Bottom-Boundary Layers of Stratified Basins

This paper focuses on the impact of an oscillating low-speed current on the structure and dynamics of the bottom-boundary layer (BBL) in a small stratified basin. A set of high-resolution current profile measurements in combination with temperature-microstructure measurements were collected during a complete cycle of the internal oscillation (`seiching') in the BBL of Lake Alpnach, Switzerland. It was found that even a relatively long seiching period of 24 hours significantly changed the form of the near-bottom current profiles as well as the dynamics of the turbulent dissipation rate compared to the steady-state law-of-the-wall. A logarithmic fit to the measured current profiles starting at a distance of 0.5 m above the sediment led to inconsistent estimates of both friction velocity and roughness length. Moreover, a phase lag between the current and the turbulent dissipation of 1.5 hours and a persistent maximum in the current profile at a height of 2.5 to 3 m above the sediment were observed. The experimental findings were compared to the results of a k- turbulence model and showed good agreement in general. Specifically, the inconsistent logarithmic fitting results and the observed phase lag were reproduced well by the model.     

石灰预处理对树叶堆肥过程中养分转化的影响

以树叶干质量的0%、1.00%、2.50%和4.00%的石灰预处理树叶,24h后分别将预处理后的树叶与鸡粪联合堆肥,研究不同用量石灰预处理树叶对树叶堆肥过程中养分转化的影响。试验在自制的堆肥反应器内进行,采用间歇式强制通风的方式,进行为期59d的堆肥试验。结果表明:石灰预处理树叶24h可以有效的降低树叶中的有机质质量分数,以4.00%的石灰预处理的树叶其有机质降幅达6.00%;石灰预处理24h后,各处理pH相差不大;EC的变化与pH相似;预处理前后,各处理总氮、总磷和总钾的质量分数相差不大。用石灰预处理后的树叶堆肥有利于堆肥有机质的降解,尤以2.50%石灰预处理的效果最好;有利于堆肥w(C)/w(N)的降低,其降低幅度与石灰用量成正比;有利于减少堆肥过程中氮素的损失,且氮素损失与石灰使用量呈反比;有利于堆肥NH4 -N质量分数的降低;提高堆肥终产品NO3--N的质量分数,其质量分数与石灰用量呈正比;有利于堆肥中钾的浓缩;对堆肥的pH、EC、w(NH4 -N)/w(NO3--N)和总磷的影响不大。综合考虑试验结果后认为,以4.00%石灰预处理的效果最为理想。