基于水化学与硫同位素的卡林型金矿区岩溶水文地球化学特征及控制因素

采矿活动通过抽排改变地下水水位和流动条件,促进了地下水与含水层岩石之间的相互作用,同时矿山排水排入地表水系,从而影响整个岩溶水系统的水文地球化学过程.基于水文地球化学和δ³⁴ S同位素,揭示了典型卡林型金矿区及其周边矿山废水、岩溶地下水、地表水等水文地球化学过程、特征及其主要控制因子.结果表明,未受金矿开采活动影响的地下水和地表水的丰、枯水期水化学组分主要受灰岩和白云质灰岩风化作用控制,离子以Ca²⁺、Mg²⁺和HCO₃^-为主,水化学类型均为Ca-HCO₃型.而矿山废水及其下游受纳水体受碳酸盐和硅酸盐矿物溶蚀与离子交换作用影响,离子以Ca²⁺、Mg²⁺、Na⁺和SO₄^2-为主,水化学类型由Ca-HCO₃型逐步演化为Ca-SO₄型.受矿山开采影响的各类水体中SO₄^2-是特征组分,SO₄^2-浓度在井下呈现从上至下逐渐降低的显著规律.未受矿山废水影响的地下水和地表水δ³⁴ S值偏正,SO₄^2-主要来源于雄黄矿的氧化,而矿山废水及其下游受纳水体δ³⁴ S值偏负,SO₄^2-主要受雄黄矿氧化和大气降水两个端元混合作用的影响,黄铁矿也有一定贡献.同时,各类水体的NO₃^-源于农业化肥施用和农村生活污水直排的输入.     

Recovery of molybdenum from fly ash by gibbsite

The effectiveness of gibbsite (GB), an amorphous aluminum oxide, for the recovery of Mo(VI) from eluates of fly ash of two coal-fired thermal power stations and of roof tile waste was investigated. Upon the qualitative analysis of an eluate of fly ash, 16 elements were detected. Greater amounts of these elements were eluted under acidic conditions (pH 2) than from the neutral or basic eluate of fly ash. GB was used for the adsorption of Mo(VI). Equilibrium adsorption was reached within 1?min. Optimal solution acidity for the adsorption of Mo(VI) onto GB400 (calcined at 400°C) was pH 2. The main adsorption mechanism was ion exchange with a number of hydroxyl groups of GB400. For repeated ad- and desorption of Mo(VI), GB400 could be used at least four times and the recovery percentage of Mo(VI) with sodium hydroxide solution as eluent surpassed 90%. Our results showed that GB400 was very effective for the recovery of Mo(VI) from fly ash.     

氧化速度对硫化矿石堆积体温度场变化影响的数值模拟方法研究

基于绝热温升模型和有限元数值计算方法,确定硫化矿石堆积体自燃预测指标,研究氧化速度对硫化矿石堆积体温度场的影响,建立硫化矿石堆积体温度场数值模型。计算结果表明,硫化矿石的氧化速度受到多重因素影响,通过调整参数m值反映堆积体中矿料氧化速度的快慢。随着m值的增大,氧化速度增大,堆积过程中以及后期堆放早期的最高温度值显著升高,而在堆放后期整体温度分布基本相同;其形心点的最高温度也增大,堆放后期该点温度值基本保持不变。     

钼尾矿制备硅微粉

以钼尾矿为原料,采用酸溶—碳酸钾沉淀法制备硅微粉。考察了反应温度、反应时间、K₂CO₃质量分数对产品中SiO₂质量分数和SiO₂产率的影响。得到的优化工艺条件为：钼尾矿粒径小于74 μm,反应温度50 ℃,反应时间60 min,K₂CO₃质量分数50%。在此工艺条件下,SiO₂产率可达98.92%,产品硅微粉的SiO₂质量分数达98.44%,粒径为100~200 nm,超过中华人民共和国黑色冶金行业标准《不定型耐火材料用二氧化硅微粉》（YB/T 115—2004）中SF96指标（SiO₂质量分数≥96.0%）的要求。     

广东省下庄和南雄铀矿区周围大气环境氡浓度调查

对广东省下庄和南雄两个铀矿区的大气氡环境地球化学进行了研究．矿区废渣和坑道口释放出来的氡气对周围大气形成了氡污染,特别是在矿区周围1～2km范围内的污染严重．但是空气中的氡污染随着离矿区的距离增大而迅速减弱．矿区周围居民室内氡的浓度高,是广东省室内氡浓度平均值的7～8倍左右．在进行调查的29个居室中,有9个（31％）居室内氡浓度超过美国环境保护局制定的0.15Bq/L室内氡浓度的上限值．居室中氡浓度的升高,除了受矿区释放出来的氡污染外,还因为本地区属高本底辐射区,房基下的土壤、岩石和建筑材料中的铀、镭等放射性元素的含量高,其放射性衰变产生的氡释放出来进入室内．     

华东某铀矿区周边河流表层沉积物的天然放射性评价

利用高纯锗γ能谱分析仪测量中国华东某铀矿区附近河流沉积物的放射性核素比活度,计算γ辐射吸收剂量率(D)、有效镭浓度(Ra_(eq))、外照射指数(H_(ex))、内照射指数(H_(in))、年有效剂量当量(AEDE(室内和室外))和年性腺剂量当量(AGDE)等放射性参数,并开展沉积物的放射性危害评估,最后通过Pearson线性系数确定放射性核素比活度之间的相关性。结果表明,河流沉积物中放射性核素~(238)U、~(226)Ra、~(232)Th和40K的平均比活度分别为51.55、37.32、57.63和756.86 Bq·kg~(-1),除~(226)Ra外,其他放射性核素的比活度均高于中国平均值;距离污染区较远或存在河流稀释作用的区域,沉积物的天然放射性核素处于正常水平,作为建筑材料使用时比活度不存在超标;放射性核素~(238)U、~(226)Ra和~(232)Th之间存在显著相关性。     

Utilizing vortex behaviour to minimize drift

Abstract

The ULV spray emitted from a TBM flying in a cross wind was mapped by a scanning lidar system. The fate of the spray cloud for 2 min after release from the aircraft was followed as the material was transported downwind of the flight line. Vertical scans at 6 s intervals with 1 m^‐3 resolution provided detailed insight into the entrainment of the spray into the wing‐tip vortices and ultimate release to drift or deposit. Relative concentration, dosage and deposit profiles are presented for this cross‐wind case. Vortex lifetimes were found to be significantly different for the up‐wind and downwind vortices. The majority of the near field deposit was associated with the up‐wind vortex while the drift was linked to the down‐wind vortex.     

高浊度钼矿浮选废水的混凝沉淀

针对某钼矿选矿厂浮选废水,以PAC、PFS和FeCl3为凝聚剂,以APAM-A和APAM-N为絮凝剂,以H2SO4和NaOH为pH调整剂,研究了不同混凝剂、不同pH值和不同水力条件下废水处理后的浊度和COD.实验结果表明,在最佳水力条件下,原水pH不调整,以APAM-A为絮凝剂,以PAC为凝聚剂,其用量分别为15 g/t,750g/t时,处理后上清液浊度为25 NTU,COD小于30 mg/L.浮选废水经处理后回用于选矿浮选流程,大大改善了选矿指标.     

Foliar and ground deposits of fenitrothion following aerial application over a plantation forest

Abstract

Spray deposits were measured on spruce foliage at tree canopy level and on glass plates at ground level, after aerial application of an emulsion formulation of fenitrothion at the rate of 0.21 kg AI in 1.46 L per ha over a 16 ha plot in a plantation forest. Fenitrothion deposits were quantified by gas‐liquid chromatography. A wide variation was observed in deposits on foliage and at the forest floor. Deposits were relatively higher on foliar samples collected from the upwind side of a tree canopy than those on the downwind side. Similarly, the glass plate placed under a tree on the upwind side received relatively higher deposit than the one on the downwind side. However, the glass plates placed in the adjacent forest openings collected markedly higher deposits. Results clearly indicate filtration of the spray droplets by canopy foliage. Assessment of the average deposit of fenitrothion at ground level (mean deposit from all sampling locations) indicated that ca. 19.4% of the applied material reached the forest floor. Within a sampling station, correlation was poor between foliar depsits and those on glass plates under the same trees or in nearby clearings. Analysis of fenitrothion deposits on foliage collected at 1 and 2 h after application indicated that the droplets took, more than 1 h for deposition on the tree canopy. On the other hand, deposition on the glass plates at ground level appeared to be practically complete within 1 h post‐treatment. This was attributed to the higher sedimentation velocities of the larger droplets which tend to travel faster to the floor level than the smaller droplets which float for a longer period near the tree canopy.     

Mercury deposition/accumulation rates in the vicinity of a lead smelter as recorded by a peat deposit

Mercury (Hg) concentration profiles and historical accumulation rates were determined in three ²¹⁰Pb-dated cores from a peat deposit in the vicinity of a lead (Pb) smelter at Příbram, Czech Republic. The Hg concentrations in peat samples ranged from 66 to 701 μg kg⁻¹. Cumulative Hg inventories from each core (for the past 150 yr) varied by a factor of 1.4 (13.6–18.5 mg Hg m⁻²), indicating variations of net Hg accumulation rate within the peat deposit. Historical changes in vegetation cover (leading to variable interception by trees) are probably responsible for this variation in space and time. The uncorrected Hg accumulation rates peaked between the 1960s and 1980s (up to 226 μg m⁻² yr⁻¹). Recent findings show that Hg records from peat tend to overestimate historical levels of Hg deposition. Therefore we used the mass loss compensation factor (MLCF) to normalize Hg accumulation rates. These corrected Hg accumulation rates were significantly lower (maximum 129 μg m⁻² yr⁻¹) and better corresponded to changes in historical smelter emissions, which were highest in the 1960s. The agreement between the corrected Hg accumulation rates in the uppermost peat sections (2–38 μg m⁻² yr⁻¹) and biomonitoring of atmospheric deposition by mosses in several recent years (4.7–34.4 μg m⁻² yr⁻¹) shows the usefulness of MLCF application on Hg accumulation in peat archives. However, the MLCF correction was unsuitable for Pb. The recent Pb deposition rates obtained by an independent biomonitoring study using mosses (0.5–127 mg m⁻² yr⁻¹) were better correlated with net Pb accumulation rates recorded in peat (7–145 mg m⁻² yr⁻¹) than with corrected rates obtained by the MLCF approach (1–28 mg m⁻² yr⁻¹).