直接投菌法在城市重污染河流治理中的应用研究

在无截污和清除内源的情况下,对深圳市甘坑河采用梅花式接种法将本源微生物菌剂分两次直接接入河流水体及底泥中。结果表明,第1次接种后的4 d内各项水质指标都不稳定,4 d后,悬浮物、COD、TP和NH3-N等浓度下降,水质明显改善;但从第8天开始,COD、NH3-N和TP的去除率同时下降,本源微生物的处理效率开始降低,需进行第2次接种;第2次接种后,DO浓度提升至2.0 mg/L以上,COD、TP和NH3-N的去除率分别保持在40%、30%和40%以上。结果表明,直接投菌法在城市重污染河道治理中可以初步消除河道的黑臭现象,修复水质。     

2,4-D Mineralization in soil profiles of a cultivated hummocky landscape in Manitoba,Canada

The objective of this study was to quantify 2,4-D (2,4-dichlorophenoxyacetic acid) mineralization in soil profiles characteristic of hummocky, calcareous-soil landscapes in western Canada. Twenty-five soil cores (8 cm inner diameter, 50 to 125 cm length) were collected along a 360 m transect running west to east in an agricultural field and then segmented by soil-landscape position (upper slopes, mid slopes, lower slopes and depressions) and soil horizon (A, B, and C horizons). In the A horizon, 2,4-D mineralization commenced instantaneously and the mineralization rate followed first-order kinetics. In both the B and C horizons, 2,4-D mineralization only commenced after a lag period of typically 5 to 7 days and the mineralization rate was biphasic. In the A horizon, 2,4-D mineralization parameters including the first-order mineralization rate constant (k ₁), the growth-linked mineralization rate constant (k ₂) and total 2,4-D mineralization at the end of the experiment at 56 days, were most strongly correlated to parameters describing 2,4-D sorption by soil, but were also adequately correlated to soil organic carbon content, soil pH, and carbonate content. In both B and C horizons, there was no significant correlation between 2,4-D mineralization and 2,4-D sorption parameters, and the correlation between soil properties and 2,4-D mineralization parameters was very poor. The k ₁ significantly decreased in sequence of A horizon (0.113% day^?1) > B horizon (0.024% day^?1) = C horizon (0.026% day^?1) and in each soil horizon was greater than k ₂. Total 2,4-D mineralization at 56 days also significantly decreased in sequence of A horizon (42%) > B horizon (31%) = C horizon (27%). In the A horizon, slope position had little influence on k ₁ or k ₂, except that k ₁ was significantly greater in upper slopes (0.170% day^?1) than in lower slopes (0.080% day^?1). Neither k ₁ nor k ₂ was significantly influenced by slope position in the B or C horizons. Total 2,4-D mineralization at 56 days was not influenced by slope positions in any horizon. Our results suggest that, when predicting 2,4-D transport at the field scale, pesticide fate models should consider the strong differences in 2,4-D mineralization between surface and subsurface horizons. This suggests that 2,4-D mineralization is best predicted using a model that has the ability to describe a range of non-linear mineralization curves. We also conclude that the horizontal variations in 2,4-D mineralization at the field scale will be difficult to consider in predictions of 2,4-D transport at the field scale because, within each horizon, 2,4-D mineralization was highly variable across the twenty-five soil cores, and this variability was poorly correlated to soil properties or soil-landscape position.     

2,4-D mineralization in unsaturated and near-saturated surface soils of an undulating,cultivated Canadian prairie landscape

The herbicide 2,4-D [2,4-(dichlorophenoxy) acetic acid] is one of the most widely used pesticides in the Canadian prairies and is frequently detected as a ground and surface water contaminant. The objective of this paper was to determine the magnitude and extent of variation of 2,4-D mineralization in a cultivated undulating prairie landscape. Microcosm incubation experiments, using a 4 × 3 × 2 factorial experimental design (soil moisture, 4 levels: 60, 85, 110, 135% of field capacity; slope position, 3 levels: upper-, mid- and lower-slopes; soil depth, 2 levels: 0–5 and 5–15 cm), were used to assess 2,4-D mineralization. The first-order mineralization rate constant (k₁) varied from 0.03 to 0.22 day^{? 1}, while total 2,4-D mineralization varied from 31 to 52%. At near-saturated conditions (110 and 135% of field capacity), the onset of 2,4-D degradation was delayed in soil obtained from the upper- and mid-slopes but not in soils obtained from the lower-slope position. The k₁ and total 2,4-D mineralizationwas significantly influenced by all three factors and their interactions. The Freundlich sorption coefficient of 2,4-D ranged from 0.83 to 2.46 ug ^1–1/ng^{? 1} mL^1/n and was significantly influenced by variations in soil organic carbon content across slope positions. The infield variability of 2,4-D sorption and mineralization observed across slope positions in this undulating field was comparable in magnitude and extent to the regional variability of 2,4-D sorption and mineralization observed in surface soils across Manitoba. The large variability of 2,4-D mineralization and sorption at different slope positions in this cultivated undulating field suggests that landform segmentation models, which are used to delineate slope positions, are important considerations in pesticide fate studies.     

Inhibition effects of aluminum dust explosions by various kinds of ammonium polyphosphate

In this work, vinyltriethoxysilane (A151) and 3-aminopropyltriethoxysilane (KH550) were used to modify ammonium polyphosphate (APP), showing that the dispersibility of APP could be improved remarkably by A151 and KH550. The maximum explosion pressure of aluminum dust explosion decreased with the addition of APP, A151-APP (APP-A) and KH550-APP (APP-B), with the exception of the case where the inerting ratio (α) of APP-A was less than 0.4. After the addition of APP-B, there was little difference in flame propagation behavior and explosion pressure compared with that of adding APP, indicating that APP-B could retain the inhibition performance of APP compared with APP-A. When the inerting ratios of APP, APP-A and APP-B were 1.2, 1.4 and 1.4, respectively, the aluminum dust explosion could be completely inhibited. The explosion residues of aluminum dust/APP mainly consisted of Al₂O₃, P-containing and N-containing compounds. It could be analyzed that APP exerted the inhibition effect through both chemical and physical effects.     

聚氨脂泡沫填缝剂生产工艺火灾危险性分析与对策

以聚氨脂泡沫填缝剂基本生产原理及其特点为基础,对生产原料进行火灾危险性分析,结果表明:该类生产场所的火灾危险等级应划分为甲类;提出聚氨酯泡沫填缝剂生产中存在的安全问题及原因;运用危险度评价法对聚氨脂泡沫填缝剂生产工艺的火灾危险性进行了定量的安全评价,得出聚氨脂泡沫填缝剂生产工艺的危险程度为高度危险;并从建筑设计、防火管理和生产工艺等方面提出了预防火灾事故发生的对策。     

硫酸/硫酸钠复合淋洗剂对铬渣的淋洗效果研究

以湖南长沙某铬盐厂铬渣为研究对象,通过室内模拟实验,采用振荡淋洗方法研究了硫酸-硫酸钠复合淋洗剂对铬渣污染场地Cr的淋洗效果,探讨了淋洗剂浓度、液固比和淋洗时间等对淋洗效果的影响,以及淋洗前后重金属形态的变化,并通过对比试验研究了硫酸钠、柠檬酸、草酸、Na2-EDTA、硫酸、柠檬酸-柠檬酸三钠以及盐酸-氯化钠作为淋洗剂对总铬和六价铬的淋洗效果。结果表明:硫酸/硫酸钠复合淋洗剂在浓度为0.4 mol/L,液固比为20∶1,反应时间为6 h,常温条件下可以达到最佳淋洗效果,总铬和六价铬的浸出效率分别为70.35%和71.56%;另外,重金属形态分析表明,该复合淋洗剂有效减少了铬渣中弱酸可提取态和有机物结合态Cr的百分比,使得残渣态Cr的百分比增加,从而降低了Cr的活性,达到修复目的。淋洗剂对比试验结果表明,与其他淋洗剂相比,硫酸-硫酸钠淋洗效果最好,其中的氢离子能与Cr~(3+)进行离子交换,而硫酸根能够有效地将钙与六价铬分离,对此高钙铬渣的处理更具针对性和有效性。     

南京和宜兴市土壤中多环芳烃(PAHs)的纵向分布

采集了江苏省南京和宜兴市的土壤剖面样品,用高效液相色谱分析了16种PAHs在土壤样品中的含量,研究了PAHs在土壤剖面中的纵向分布特征和影响因素。结果表明,在采样点土壤0～10cm的表土中16种PAHs总量最高,为280.8～717.1μg/kg,随着土壤剖面的加深PAHs总量减少,在70～80cm土层中为8.7～97.5μg/kg。不同PAHs组分在土壤中分布的特点不同,低环的PAHs(≤3环)含量在0～80cm土层中都有分布且随土壤深度加深而减少,而高环的PAHs(≥4环)主要分布在0～30cm土层中,30cm以下土层中含量较少甚至检测不到。相关分析表明,在每个土壤剖面中PAHs总量与其土壤有机碳含量显著相关,PAHs在农田土壤剖面中的纵向分布与土壤有机碳含量、PAHs的理化性质有很大的关系。     

塔克拉玛干沙漠和青藏高原地区沙尘气溶胶光学特性及其加热率的时空分布特征

沙尘不同的垂直分布对大气的加热作用不同,通过卫星观测结合数值模拟,可以更清楚地了解沙尘辐射加热作用,有利于理解沙尘对该地区大气热结构的影响机制.因此,本研究利用CALIPSO气溶胶产品和SBDART模式,分析了2007—2020年塔克拉玛干沙漠和青藏高原沙尘气溶胶及其短波加热率的时空分布特征.结果表明,塔克拉玛干沙漠和青藏高原的年平均沙尘气溶胶光学厚度（DAOD,532 nm）分别为0.300～0.350和0.086～0.108,平均值分别为0.328和0.097.塔克拉玛干沙漠季节平均DAOD的最大、最小值分别出现在春季和冬季,而青藏高原的最大、最小值分别出现在夏季和秋季.塔克拉玛干沙漠和青藏高原的沙尘消光系数（σD）最大值分别出现在春季和夏季.2007—2020年,两地的σD在春季均呈增加趋势,而在秋季则呈减小趋势.春季和夏季的短波沙尘加热率（SW DHR）均大于其它两个季节,其中春季最大,塔克拉玛干沙漠上空冬季最弱,青藏高原上空秋季最弱.春夏季,青藏高原北坡存在较强沙尘加热层,其顶部高于5 km,其强度及高值区从春季到冬季逐渐减小.从年变化来看,春季短波加热率呈加强趋势,秋季呈减...     

一种基于综合环境剖面的导弹弹上设备加速贮存试验方法

目的 基于导弹武器在历经地面使用载荷后,还要满足飞行载荷的特点,讨论用于评估导弹弹上设备贮存期的加速贮存试验流程与方法。方法 开展加速因子试验,获得加速因子计算公式,根据实际使用环境载荷,制定综合环境试验剖面,按照贮存期目标值开展加速贮存试验,等效地面使用环境载荷,开展飞行环境载荷考核试验,试验成功后,给出贮存期评估结论。结果 该方法在多型导弹贮存延寿工程的弹上设备贮存期评估中得到应用,应用表明,可以评估导弹弹上设备的贮存期,具有工程应用价值。结论 获得加速因子计算公式后,将导弹弹上设备的地面使用环境载荷累计影响与能够经受飞行载荷环境分步进行试验,能够体现导弹弹上设备历经的环境载荷,可以用于弹上设备的贮存期评估。     

餐饮源油烟中PM2.5的化学组分特征

集中分析了餐饮无组织排放源(街边小吃、火锅店、露天烧烤)及有组织排放源(10家大中型餐馆)油烟PM_2.5中的TC(总碳)、元素组分、离子组分和16种PAHs,得到了各类餐饮源油烟PM_2.5的化学组成特征,建立了餐饮源油烟化学成分谱. 结果表明:各餐饮源油烟的ρ(PM_2.5)是大气背景值的3~42倍,其中露天烧烤油烟的ρ(PM_2.5)最高,达5 659.8 μg/m3. 不同餐饮源油烟的PM_2.5中各化学组分均为w(TC)(38.1%~75.8%)＞w(元素组分)(4.5%~27.0%)＞w(离子组分)(2.7%~22.6%),并且ρ(PM_2.5)与w(TC)呈显著正相关(R=0.84). 菲(PHE)、芘(PYR)、荧蒽(FLT)的质量分数在各类餐饮源油烟的PAHs中均普遍较高,分别为13.8%~21.6%、9.2%~26.5%、6.9%~22.0%.大中型餐馆油烟的PAHs中苯并苝(BPE)的质量分数最高(27.5%),而在其他餐饮源中均小于6.7%;(CHR)的质量分数最低(3.3%),而在其他餐饮源中均大于5.3%. 露天烧烤油烟的PAHs中芘、荧蒽的质量分数分别是其他餐饮源的2.7和2.3倍以上;萘(NAP)的质量分数(0.3%)较小,但在其他餐饮源中均大于11.4%,可以作为特定餐饮源油烟的特征物种.