高压管道天然气泄漏扩散过程的数值模拟

采用CFD模型的方法对高压管道内的天然气泄漏和扩散过程进行了数值模拟。其结果表明,从高压管道泄出的天然气在大气中主要表现为高速射流的泄漏过程和随后的扩散过程。在泄漏过程中,天然气在泄漏口附近为欠膨胀射流,整个泄漏过程具有一定的高度;在扩散过程中,天然气在浮力作用下以向上扩散的形式发展。研究了不同环境风速对扩散过程的影响,较大的风速可以使天然气向下风方向更远的距离扩散,从而增大了天然气爆炸危险浓度的范围。研究结果可     

竹地板与普通实木地板燃烧性能的锥形量热仪对比实验研究

随着竹地板的广泛应用,竹木地板的火灾燃烧性能也将引起人们的关注.本文采用锥形量热仪对竹木地板的引燃时间、热释放速率、总热释放和一氧化碳的产率及体积比浓度等燃烧性能与普通实木地板进行了比较研究.研究结果表明:在相同条件下,竹木地板试样的引燃时间较短,临界引燃辐射热通量较低,引燃危险相对较大;竹木地板试样燃烧中第一个热释放速率峰值出现的时间短,且峰值相对较大,其潜在的轰燃危险相对较大;此外,竹木试样的一氧化碳的产率和燃烧初期在烟气中的体积比浓度相对较大.     

Effect of organic matter and pH on mercury release from soils

An investigation was conducted on the effect of organic matter(OM)and pH on mercury(Hg)release from soils.Hg release flux was measured using the dynamic flux chamber(DFC)combined with the Lumex multifunctional mercury analyzer in both laboratory experiment and field monitoring.The results showed that Hg emission from the OM-added soils was apparently low because of the high affinity of OM to Hg,resulting in the reverse order as the amount of OM addition.Meanwhile,Hg release flux from different pH value soils exhibited the same trend for both Hg~(2 )and Hg_2~(2 )treatment,increasing the Hg flux with pH value of soils increasing.The trend of Hg release in the pH dependence experiment has been well in agreement with that from the field test.In addition,Hg release seemed to be related to its species in the soil,the flux from Hg~(2 )-added soil was obviously higher than that of Hg_2~(2 )-added soil by the laboratory experiment.     

沙质滩涂中可溶性油的释放动力学研究

沙质滩涂对石油类污染物的吸附是一种物理吸附过程,在一定的条件下,吸附于沙质滩涂中的石油类污染物又可能释放出来,对滨海环境造成新的污染。在对滨海沙滩（胶州湾）沙质滩涂-水系统石油污染调查的基础上,选择代表性的沙滩进行取样,系统测定不同沙质滩涂对可溶性油的释放动力学过程,并分析了盐度、pH、温度和含沙量对释放作用的影响。结果表明,沙质滩涂对可溶性油的释放动力学曲线符合对数型,即随着时间的延续释放速度逐渐降低,沙质滩涂对可溶性油的释放平衡时间约为10h,沙质滩涂对可溶性油的释放量随盐度和pH的增大而减少,随温度、含沙量和振荡频率的增加而增加。     

医用电气设备电源变压器的过载试验

采用电阻法测量医用电气设备电源变压器过载试验时的绕组温升,试验电流和试验时间的选取与熔断器、过流释放器、热断路器等保护装置有关。     

重污染感潮河道底泥释放特征及其控制技术研究

以珠江三角洲城市重污染感潮河道为对象,研究了底泥污染物(重金属、有机物和营养盐)在静态、潮汐作用影响及人工曝气扰动下的释放特征.在此基础上,采用曝气充氧、重金属化学固定、激活底泥土著微生物等联合技术对底泥释放进行控制,研究其控制效果.结果表明:①感潮作用加速了底泥污染物的释放,与静态释放相比,Cu、Zn、Pb、Cr、COD、NH 4-N和TP的平均释放速率提高了1～4倍,释放量增加了0.3～1.8倍;底泥平均耗氧速率提高了1.28倍.②人工曝气扰动使底泥污染物局部急剧释放,并使泥水界面由弱碱性变成弱酸性;在有氧环境,NH 4-N、TP的释放得到有效抑制.③投加石灰调节pH至8～9,上覆水体Cu、Zn、Pb、Cr的去除率达到85%～98%,同时还可去除92%的TP和86%的浊度;在微碱性好氧条件下,Cu、Zn、Pb和Cr的释放量稳定在300μg·L-1以下.④底泥土著微生物层对水体及底泥污染物有良好的降解作用,通过间歇曝气COD、NH 4-N、TP去除率分别可达到85%、92%和71%;但微生物层具有较高的耗氧速率,达到45g·m-2·d-1.     

城市重污染河道上覆水氮营养盐浓度及DO水平对底质氮释放的影响

利用模拟试验方法, 研究和探讨了苏州市古城区重污染河道上覆水的氮营养盐浓度及DO水平对河道底泥内源氮释放的影响.结果表明:① 上覆水体的氮营养盐水平可对底泥中氮营养盐的释放程度(即释放速率和释放量)产生影响,氮营养盐含量低的上覆水体有利于底泥中氮特别是氨氮的释放(外城河与苗家河２种处理的累积释放量差值可达6 mg/kg),相反,则不利于氨氮的释放.故当氮营养盐含量较低的外城河水进入古城区河道时,有可能引起内城河道中底泥氨氮的大量释放,这种情况在调水过程中更为明显;②溶解氧是控制底泥氮释放规律的重要因素,其对氨氮和硝态氮释放的影响呈非线性,厌氧条件能加速底泥氨氮的释放,好氧则对其释放产生抑制,故保持河道水体中适当的溶解氧可有效抑制底泥中氨氮等释放造成的污染.     

围岩散热计算及壁面水分蒸发的处理

笔者采用湿度系数法对壁面水分蒸发进行了处理,对计算壁面处饱和空气含湿量的方法进行了改进,将饱和空气含湿量与温度的关系拟合为二次曲线;建立了在考虑壁面水分蒸发情况下解算巷道围岩温度场分布及围岩向风流的散热量的数学方程,并采用异步长有限差分法对其进行了数值模拟求解;解算出巷道壁面水分蒸发情况下围岩温度分布、壁面温度和围岩散热量的变化规律;并与将饱和空气含湿量与温度的关系拟合为线型关系曲线时的解算结果进行了对比,将饱和空气含湿量和温度之间的关系拟合为线性的计算结果存在一定的误差,通风时间越长,湿度系数越大,风流相对湿度越小,拟合为线性时计算出来的壁面温度和围岩散热量的误差越大。     

Release Characteristics of Nutrients from Polymer-coated Compound Controlled Release Fertilizers

Reliable information regarding release characteristics of nutrients from a polymer-coated controlled release fertilizer (CRF) is essential for beneficial agronomic and environmental results. Significant knowledge regarding nitrogen release from polymer-coated urea was gained while the information regarding the release of the different nutrients contained in polymer-coated compound N–P–K CRF remains limited. An experiment in which major factors affecting the differential release of nutrients from two coated compound CRF was performed in free water, water saturated sand and sand at field capacity. In general, nitrate release was the fastest, followed by ammonium and potassium whereas phosphate was significantly slower, with a rate of linear release in free water 45–70% slower than that of nitrate. Little differences were obtained for the lag periods of nitrate, ammonium and potassium release (2–10 days) under the experimental conditions, whereas for P they were one order of magnitude larger. The main factor slowing the release was assumed to be the lower solubility of ions with P being the least soluble. Release into free water was, expectedly, somewhat faster than that into saturated sand and significantly faster as compared to sand at field capacity and particularly so for P. Raising the temperature from 20 °C to 40 °C increased the rate of linear release of the different nutrients. The energy of activation, EA_rel, estimated for the linear release, of the different nutrients, was narrow ranging between 37 to 46 (KJ mol⁻¹) whereas the mean values obtained for the two CRF, differing by 50% in coating thickness, was non-significant. However, EA_rel was significantly different in different media. The complex effect of temperature on the lag period and nutrient interactions during release deserve further investigation.     

Quantifying dry NH3 deposition to an ombrotrophic bog from an automated NH3 field release system

Providing an accurate estimate of the dry component of N deposition to low N background, semi-natural habitats, such as bogs and upland moors dominated by Calluna vulgaris is difficult, but essential to relate nitrogen deposition to effects in these communities. To quantify the effects of NH₃ inputs to moorland vegetation growing on a bog at a field scale, a field release NH₃ fumigation system was established at Whim Moss (Scottish Borders) in 2002. Gaseous NH₃ from a line source was released along of a 60 m transect, when meteorological conditions (wind speed >2.5 m s^–1 and wind direction in the sector 180–215°) were met, thereby providing a profile of decreasing NH₃ concentration with distance from the source. In a complementary study, using a NH₃ flux chamber system, the relationships between NH₃ concentrations and cuticular resistances were quantified for a range of NH₃ concentrations and micrometeorological conditions for moorland vegetation. Cuticular resistances increased with NH₃ concentration from 11 s m^–1 at 3.0 g m^–3 to 30 s m^–1 at 30 g m^–3. The NH₃ concentration data and the concentration-dependent canopy resistance are used to calculate NH₃ deposition taking into account leaf surface wetness. The implications of using an NH₃ concentration-dependent cuticular resistance and the importance for refining critical loads are discussed.