Environmental Isotopes for Resolution of Hydrology Problems

The use of environmental isotopes as tracers in the hydrosphere is increasing as analytical instrumentation improves and more applications are discovered. There exists still misconceptions on the role of isotopes in resolving hydrology problems. Naturally occurring isotopes in the environment describe hydrological processes, estimate ages, fingerprint sources and pathways, yet are not subject to the regulatory restraints of artificial isotope injections nor the limited extent of many chemical tracers, particularly dyes and particulates. A short review is presented for practicing hydrologists on the basis for employing stable and radioactive isotopes and a synopsis of recent isotope hydrology applications is provided. Special focus is presented on the emergent role of water isopopes (¹⁸O, ²H, ³H) in wet-weather flow research in urban watersheds. A brief technical approach for an experimental site in the Mill Creek Watershed, Ohio is outlined.     

基于PLIF的混合气温度和浓度测量及其应用

缸内混合气温度和浓度分布,对发动机稳定运行,保障行车安全、避免发生路上人身伤亡或财物损失有重要影响。为了测量发动机缸内混合气的温度和浓度分布,建立了利用单波长激光诱导双示踪剂产生双荧光的测试系统,并拍摄了不同混合气温度、压力和浓度下的荧光图像,获得了不同示踪剂的荧光强度及其比值随温度、压力和浓度的变化关系,并将标定结果用于光学发动机缸内混合气的温度和浓度测量。结果表明,荧光强度及荧光比值均受到环境的压力、温度和混合气浓度的影响。利用PLIF方法得到的片光源穿过的缸内水平截面内的平均温度与用气缸压力计算的同一曲轴转角下的缸内平均温度变化趋势相同,两者之间的差值随着活塞上行而逐步减小。     

基于能位测定和示踪检测法的地下煤火漏风状态研究

应用能位测定法和示踪检测技术联合检测了鸡西老二井火区地下漏风状态。通过测试计算相对总压值得出了火区范围内井巷系统与采空区的风流关系,进而定性确定了火区内老二井与胜利井之间存在的可能漏风路径。在此基础上,利用瞬时释放示踪气体法确定了胜利井和老二井间的漏风方向和漏风速度,计算得出了火区下采空区内平均直线漏风风速为0.13m/s,漏风量为776m3/min。研究结果为矿区采取针对性的防灭火措施提供依据,并为同类问题的解决提供参考。     

含磷聚马来酸水处理剂的合成

在金属离子存在的情况下,在水相体系中使用过氧化氢引发合成膦基聚马来酸。在温度104℃、反应时间3h、催化剂加量200mg／L、单体初始质量分数50％、单体中引发剂加量85g／mol的条件下合成的含磷聚马来酸的相对分子质量超过800、相对密度为1．20、pH为2．3。磷被有效地转化为有机膦,转化率大于96．6％。产品兼有阻垢、缓蚀两种功能。     

Sulfate removal from waste chemicals by precipitation

Chemical oxidation using Fenton's reagent has proven to be a viable alternative to the oxidative destruction of organic pollutants in mixed waste chemicals, but the sulfate concentration in the treated liquor was still above the acceptable limits for effluent discharge. In this paper, the feasibility of sulfate removal from complex laboratory wastewaters using barium and calcium precipitation was investigated. The process was applied to different wastewater cases (two composite samples generated in different periods) in order to study the effect of the wastewater composition on the sulfate precipitation. The experiments were performed with raw and oxidized wastewater samples, and carried out according to the following steps: (1) evaluate the pH effect upon sulfate precipitation on raw wastewaters at pH range of 2-8; (2) conduct sulfate precipitation experiments on raw and oxidized wastewaters; and (3) characterize the precipitate yielded. At a concentration of 80 g L(-1), barium precipitation achieved a sulfate removal up to 61.4% while calcium precipitation provided over 99% sulfate removal in raw and oxidized wastewaters and for both samples. Calcium precipitation was chosen to be performed after Fenton's oxidation; hence this process configuration favors the production of higher quality precipitates. The results showed that, when dried at 105 degrees C, the precipitate is composed of hemidrate and anhydrous calcium sulfate ( approximately 99.8%) and trace metals ( approximately 0.2%: Fe, Cr, Mn, Co, Ag, Mg, K, Na), what makes it suitable for reuse in innumerous processes.     

氚水在大豆土壤系统中的迁移与分布

采用模拟污染物的同位素示踪技术研究氚水在大豆-土壤模拟生态系统中的迁移、分布规律.通过为期50d的模拟试验,测定了植物和土壤样品中2种形态氚(自由水氚和结合态氚)的比活度.结果表明:引入土壤中的氚水,不仅在系统各分室间转移和分配,而且迅速向系统外散逸;氚水中的氚以自由水氚和结合态氚形态存在于大豆植株和土壤中;大豆植株中的自由水氚比活度于6h时即达最大值(根19.4Bq·g^-1;茎叶12.3Bq·g^-1),随后便逐渐下降,而结合态氚呈缓慢增加;大豆根中的总氚比活度开始时高于茎叶中的比活度,而后趋于平衡,表层土中2种形态氚基本呈逐渐下降.运用示踪动力学分室模型原理对实验数据拟合得:土壤中的比活度C_s=88.37e^-11.847t+7.38e^-0030t;大豆植株中的比活度C_b=10.30(e^-0.030t-e^-11.847t).     

混凝-氧化法处理印染废水

采用混凝 氧化法对印染废水进行处理 ,得出最佳混凝条件及氧化条件。实验结果表明 ,该法可使印染废水的CODCr与色度去除率分别达到 90 .2 %和 99.1%。该方法具有去除率高、操作方便、设备简单、不产生二次污染等优点。     

Strontium isotope constraints on the seasonal variation of the provenance of base cations in rain water at Kawakami, Central Japan

The ⁸⁷Sr/⁸⁶Sr ratios in monthly precipitation in the forested basin at Kawakami, central Japan, varied seasonally from 0.709 to 0.711 in spring to as low as 0.7062 ± 0.0004 in autumn over nine years from 1987 to 1995. The seasonal variation can be explained in terms of the mixing of three sources of Sr: sea salt (⁸⁷Sr/⁸⁶Sr 0.70917), soluble eolian minerals originating from deserts in continental Asia ( 0.711), and biogenic materials growing on soils derived from the volcanic rock substrates in the vicinity ( 0.706). It is estimated that the contribution of sea-salt Sr into the Kawakami rain Sr is relatively constant (10 ± 5%) and that more than half of the Sr is of biogenic origin throughout the year except during spring rains when 50% of the Sr is due to the dissolution of Ca-minerals from Asian dusts. The dominant contribution of eolian components to spring rains is consistent with the high concentration of ³H, which is typical of air masses from Asia.     

Validation of the UK Met. Office’s name model against the ETEX dataset

The ETEX 1 data set has been used to assess the performance of the UK Met Office’s long-range dispersion model NAME. In terms of emergency response modelling the model performed well, successfully predicting the overall spread and timing of the plume across Europe. However, in common with most other models, NAME overpredicted the observed concentrations. This is in contrast with other NAME validation studies which indicate either no significant bias or a tendency to underpredict concentrations. This suggests the reasons for overpredicting are specific to the ETEX situation. Explanations include inadequate vertical diffusion or transport, possible venting by convective activity, and experimental errors. An assessment of a range of advection schemes of varying complexity indicated no clear advantage, at present, in using more sophisticated random walk techniques at long range, a simple diffusion coefficient based scheme providing some of the best results. A brief look is also taken at a simulation of the more problematical ETEX 2 release.     

Fenton氧化-生物接触氧化工艺处理甲醛和乌洛托品废水

采用Fenton氧化一生物接触氧化工艺处理含甲醛和乌洛托品的模拟废水（简称废水）,在H2O2（体积分数30％）加入量2．5g／L、H2O2与Fe^2＋质量浓度比3．75、反应时间3h、不调节废水初始pH的Fenton氧化预处理最佳操作条件下,废水COD从1000mg／L左右降至300mg／L,COD去除率达72％。原废水完全无法直接进行生化处理,经Fenton氧化预处理后其BOD,／COD约为0．5,易于生化处理。Fenton氧化一生物接触氧化工艺处理废水,生物接触氧化停留时间为12h时,废水COD去除率高达94％,处理后出水COD小于70mg／L,处理效果很好。