岩溶地下河水化学对城镇化进程的时序响应

利用25年地下水观测与遥感解译数据研究地下河对城镇化进程的水化学时序响应,结果表明,随着城镇化的进行,地下河的矿化度逐渐上升;水化学类型时序演变从枯水期单一的HCO_3·SO_4-Ca·Mg型和丰水期HCO_3-Ca·Mg型向HCO_3·ClCa型、HCO_3·SO_4-Ca型、HCO_3-Ca和HCO_3·SO_4-Ca·Mg型等多类型演化,快速城镇化时期水化学类型多变.受地表降水输入影响,地下河枯水期与丰水期[Mg2+]/[Ca2+]和[HCO_3~-]/[SO_4~(2-)](摩尔比)变化较大,城镇化前地下河水化学受水岩相互作用、农业活动和酸雨入渗共同影响,两者均值分别为0. 86和29. 34; 2001年城镇化后农业活动和酸雨输入贡献减少,丰水期城镇化输入(居民生活和工业排污)明显增加,两者出现突变特征,分别降低至0. 38与6. 01. 1990～1995、1996～2010和2011～2015年不同时期的主要地球化学敏感阳离子分别为Ca~(2+)及Mg~(2+)、Na~+和NH_4~+,阴离子则分别为HCO_3~-、HCO_3~-及SO_4~(2-)和Cl~-.地下河对城镇化进程的水化学响应具有明显的阶段性和时序性.     

芬兰城市和工业污水处理现状及发展趋势

介绍了芬兰在城市和工业废水治理方面的情况，芬兰在废水处理技术与管理目标方面取得的成就。最新进展及未来规划为我们提供了可供借鉴的资料和信息。     

Relationship between groundwater cadmium and vicinity resident urine cadmium levels in the non-ferrous metal smelting area,China

● This study systematically examined the relationship between groundwater Cd and UCL. ● The study covered 211 UCL and sociological characteristic from nine groundwater samples. ● We found a significant positive correlation between groundwater Cd and UCL. ● Smoking status and education level also significantly affected UCL. Cadmium (Cd) has received widespread attention owing to its persistent toxicity and non-degradability. Cd in the human body is mainly absorbed from the external environment and is usually assessed using urinary Cd. Hunan Province is the heartland of the Chinese non-ferrous mining area, where several serious Cd pollution events have occurred, including high levels of Cd in the urine of residents. However, the environmental factors influencing high urinary Cd levels (UCLs) in nearby residents remain unclear. Therefore, 211 nearby residents’ UCLs and the corresponding sociological characteristics from nine groundwater samples in this area were analyzed using statistical analysis models. Groundwater Cd concentration ranged from 0.02 to 1.15 μg/L, aligning with class III of the national standard; the range of UCL of nearby residents was 0.37–36.60 μg/L, exceeding the national guideline of 0–2.5 μg/L. Groundwater Cd levels were positively correlated with the UCL (P < 0.001, correlation coefficient 95 % CI = 9.68, R² = 0.06). In addition, sociological characteristics, such as smoking status and education level, also affect UCL. All results indicate that local governments should strengthen the prevention and abatement of groundwater Cd pollution. This study is the first to systematically evaluate the relationship between groundwater Cd and UCL using internal and external environmental exposure data. These findings provide essential bases for relevant departments to reduce Cd exposure in regions where the heavy metal industry is globally prevalent.     

Rapid degradation of butachlor in wheat rhizosphere soil

The degradative characteristics of butachlor in non-rhizosphere, wheat rhizosphere, and inoculated rhizosphere soils were measured. The rate constants for the degradation of butachlor in non-rhizosphere, rhizosphere, and inoculated rhizosphere soils were measured to be 0.0385, 0.0902, 0.1091 at 1 mg/kg, 0.0348, 0.0629, 0.2355 at 10 mg/kg, and 0.0299, 0.0386, 0.0642 at 100 mg/kg, respectively. The corresponding half-lives for butachlor in the soils were calculated to be 18.0, 7.7, 6.3 days at 1 mg/kg, 19.9, 11.0, 2.9 days at 10 mg/kg, and 23.2, 18.0, 10.8 days at 100 mg/kg, respectively. The experimental results show that the degradation of butachlor can be enhanced greatly in wheat rhizosphere, and especially in the rhizosphere inoculated with the bacterial community designated HD which is capable of degrading butachlor. It could be concluded that rhizosphere soil inoculated with microorganisms-degrading target herbicides is a useful pathway to achieve rapid degradation of the herbicides in soil.     

铁镍改性膨润土对废水中有机污染物的吸附性能研究

以钠基膨润土为原料,制备了铁镍无机改性土和铁镍有机复合改性土,并应用于造纸废水的处理,探讨了改性土用量、废水pH值、搅拌时间等因素对COD去除率的影响,通过正交实验对实验条件进行了优化.结果表明:铁镍有机复合改性土和铁镍元机改性土对废水的处理效果明显好于原土;膨润土的用量、废水的pH对COD的去除率影响较大;对于铁镍无机改性土,吸附剂用量为12g/L,溶液pH=2,吸附时间为10 min时,对废水中COD的去除率为54.06%;对于铁镍有机复合改性土,吸附剂用量为14g/L,溶液pH=3,吸附时间为20 min时,对废水中COD的去除率为70.10%.     

Mn2O3/γ-Al2O3在超临界水氧化中催化活性的研究

采用浸渍法制备了Mn2O3/γ-Al2O3催化剂,在超临界水中催化氧化降解1,5-萘二磺酸,探索了催化剂Mn2O3活性组分负载量、催化剂空速和反应溶液pH对Mn2O3/γ-Al2O3催化剂活性的影响。结果表明：Mn2O3/γ-Al2O3的催化活性在一定范围内随Mn2O3活性组分负载量的增加而提高;在一定范围内,Mn2O3/γ-Al2O3空速越小,模拟废水的COD去除率越高;Mn2O3/γ-Al2O3催化活性在反应溶液呈酸性情况下比碱性时高。     

Occurrence, sources, and inventory of hexabromocyclododecanes (HBCDs) in soils from Chongming Island, the Yangtze River Delta (YRD)

Hexabromocyclododecanes (HBCDs) is a concern due to their large usage combining with physico-chemical properties and toxicity to wildlife and human. However, very limited data were reported on HBCDs in soils, especially from rural area. In this study, 22 soil samples were collected from Chongming Island at estuary of the Yangtze River Delta, to investigate the level, diasteroisomer profile, potential sources, and mass inventory of HBCDs. The total concentrations ranged from not detected to 93.8 pg g⁻¹ dry weight (dw) with a mean of 23.3 pg g⁻¹ dw, which was at the low end of the global levels. The wide distribution of HBCDs in soils suggested that the local emissions of HBCD-containing materials and/or the inputs via atmospheric transport from other regions were two possible sources. Variation of HBCDs levels was observed in different types of soils. Woodland, tideland and road soils contained slightly higher HBCDs than those of farmland and grassland. Overall, γ-HBCD was the dominant diasteroisomer in soils, followed by α-HBCD and β-HBCD. Significant but weak correlations were only found between α-HBCD and β-HBCD versus TOC content in soils. Currently, the mass inventory of HBCDs in soils of Chongming Island was 5.3 kg. Based on these data, we gave perspective on human intake of HBCDs via soil ingestion by age. Local resident’s intakes ranged from 15.5 to 97.8 fg kg body weight⁻¹ d⁻¹, in which children are exposed more than adults.     

Investigation on the relationship between the fine particle emission and crystallization characteristics of gypsum during wet flue gas desulfurization process

The relationship between the fine particles emitted after desulfurization and gypsum crystals in the desulfurization slurry was investigated, and the crystallization characteristics varying with the operation parameters and compositions of the desulfurization slurry were discussed. The results showed that the fine particles generated during the desulfurization process were closely related to the crystal characteristics in the desulfurization slurry by comparison of their morphology and elements. With the higher proportion of fine crystals in the desulfurization slurry, the number concentration of fine particles after desulfurization was increased and their particle sizes were smaller, indicating that the optimization of gypsum crystallization was beneficial for the reduction of the fine particle emission. The lower pH value and an optimal temperature of the desulfurization slurry were beneficial to restrain the generation of fine crystals in the desulfurization slurry. In addition, the higher concentrations of the Fe^3 + ions and the F⁻ ions in the desulfurization slurry both promoted the generation of fine crystals with corresponding change of the morphology and the effect of the Fe^3 + ions was more obvious. With the application of the desulfurization synergist additive, it was beneficial for the inhibition of fine crystals while the thinner crystals were generated.     

系统响应气候变化脆弱性定量评价国内研究综述

定量评价气候变化脆弱性是人类采取适应性措施应对全球气候变化,以减少其不利影响的关键和基础。在对气候变化脆弱性有关概念进行讨论,及对国际、国内系统响应气候变化脆弱性评价研究回顾的基础上,对中国近十几来有关气候变化脆弱性定量评价研究的成果从三个方面进行了较为系统的总结：气候情景的模拟预测、系统变化过程的模拟、脆弱性指标的选取及脆弱性层次的划分。最后,从评价对象、技术手段、指标体系、时间尺度等方面探讨了该领域研究的不足及发展方向。     

太湖地区3种水稻土不同温度培养中有机碳库变化及其对升温的响应

全球变暖下土壤有机碳储存的变化是土壤与全球变化研究的热点问题.本研究选择了3种太湖地区代表性水稻土的表层土壤,分别进行20℃和25℃的室内恒温培养,监测培养过程中总有机碳、溶解性有机碳和微生物量碳的变化动态,试图了解这些土壤的有机碳分解过程对全球变暖的响应特点.结果表明,这些土壤培养中总有机碳变化可以用一级衰变动力学方程或对数衰减方程描述,但动力学特征依培养温度的不同而异.升温大大促进了铁渗水耕人为土和潜育水耕人为土中有机碳的分解与呼吸损失,而铁聚水耕人为土没有显著变化.供试土壤总有机碳损失的Q₁₀系数分别为:潜育水耕人为土(11.1～14.1)＞铁渗水耕人为土(4.4～6.4)＞铁聚水耕人为土(0.63～0.73).这一方面说明温度敏感性在同一地带的不同土壤间的差异超过文献上报道的不同气候带的差异,但另一方面揭示了水稻土可能是一类对全球升温敏感响应的人为土.溶解性有机碳和微生物量的碳的变化还提示不同温度培养下水稻土微生物群落结构可能改变,因而影响到土壤有机碳库的生物有效性在温度条件下的变化.可以认为,土壤升温下有机碳的变化不但与土壤有机碳的性质有关,而且与土壤性质控制下的生物条件的改变有关.故土壤升温下有机碳的损失不仅仅是温度对分解过程的反应速度的影响.当然,对于不同土壤间的这种差异还需从有机碳-土壤环境-土壤生物的相互关系上做进一步的工作.