Influence of sunlight on the proliferation of cyanobacterial blooms and its potential applications in Lake Taihu, China

To learn the relationship between sunlight intensity and cyanobacterial proliferations for the further control of the heavy blooms, enclosure experiment were conducted in Meiliang Bay, Lake Taihu by regulating the natural light intensities with different shading ratio （0% （full sunlight）, 10%, 25%, 50% and 75% of original natural sunlight intensities） from September to November in 2010. The results indicated that phytoplankton biomass （mean） decreased significantly when the shading ratios reached 50% or more. Higher shading ratios （e.g. 75%） were very efficient in controlling the average and total cyanobacterialbloom biomass, while 50% shading ratio was proven very effective either in controlling the peak value of phytoplankton biomass or postponing the occurrence of cyanobacterial blooms in Lake Talhu. In addition, phytoplankton composition and photosynthesis efficiency were also affected by altering the shading ratios, and in turn, they might also act on phytoplankton growth. Based on the results from the present study, intermediate shading strategies such as regulation of water level or turbidity through the hydrology regulations would probably be an effective and efficient method in controlling cyanobacterial blooms in large and shallow lakes.     

银川台小口子泉水氡对比观测实验研究

本文以小口子泉模拟水氡观测为基础进行日常观测实验.通过加密观测、升高鼓泡水温和降低鼓泡水温实验,认为小口子泉水氡与泉点气温、鼓泡水温变化有关;不同的鼓泡水温对观测氡值有一定影响,但是影响幅度不大.通过不同的观测仪器对比实验,发现不同的观测仪器之间存在系统误差,但不影响观测资料的正常变化形态和幅度.两次实验可以为台站观测人员和分析预报人员掌握观测资料动态变化的影响因素、剔除非地震异常干扰提供帮助.     

借鉴欧洲经验加快我国颗粒物污染防治

本文回顾了欧洲颗粒物污染控制的历程,从法规标准、管理制度、控制措施等方面,系统分析了欧洲颗粒物污染控制策略特点。通过总结欧洲颗粒物污染控制的经验,为我国的颗粒物污染控制提供借鉴。     

太湖湖西典型区水体硝酸盐含量对反硝化作用影响实验研究

以太湖湖西为例,采用流动培养同位素添加法,分别模拟了湖西北、湖西南地区不同温度及有机碳浓度下的底泥原位反硝化作用,结果表明只有水体硝酸盐含量高的湖西北地区底泥反硝化速率受温度和有机碳影响明显,水体硝酸盐含量低的湖西南地区底泥反硝化速率受水体温度、有机碳含量影响较小.研究结果表明,太湖湖西北地区22、27、32℃时反硝化速率分别为(77.62±5.23)、(156.01±12.01)、(309.36±20.31)μmol·m^-2·h^-1.湖西北区域上覆水有机碳含量为0、4、10 mg·L^-1时,沉积物平均反硝化速率分别为177.39、203.48、275.85μmol·m^-2·h^-1.根据皮尔逊相关性分析可知,太湖反硝化速率与水体硝酸盐含量呈显著相关,即水体氮素构成是影响底泥反硝化速率的最根本原因,只有硝酸盐供给充足,底泥反硝化速率才会随着温度及水体碳源的变化而变化.     

土壤中多环芳烃微生物降解能力模拟

为了揭示微生物菌种(组合)对土壤中PAHs(多环芳烃)降解率的影响以及不同类型PAHs抗微生物降解能力的差异,分析了北京市6个不同环境功能区土壤中微生物种类及其分布特征,从中筛选出部分微生物菌种对典型PAHs和原油进行降解模拟试验,对比分析微生物对不同PAHs降解能力的差异.结果表明:① 不同菌种组合对PAHs的降解能力存在明显差异,与假单胞菌属、无色杆菌、短稳杆菌混合菌相比,假单胞菌属、无色杆菌、短稳杆菌和微杆菌混合菌对PAHs的降解率高0.6%~4.5%;② 在相同降解条件下,不同PAHs的降解率存在明显差异,在单体培养基中,LMW PAHs(低环数PAHs)的降解率在25.3%以上,而HMW PAHs(高环数PAHs)的降解率都小于20.1%;③ 在单体培养基与混合培养基中PAHs的降解能力也存在一定差别,单体培养基中PAHs的降解率较混合培养基中高4.2%~26.6%;④ 无论在单体培养基中,还是混合培养基中这些化合物的降解率均存在随着降解时间的增加而增大的现象;⑤ 在原油培养基中不同PAHs的降解率更为复杂,并且出现了中低分子量PAHs降解率随降解时间增加反而降低的假象,这可能是由于随着时间增加,微生物对PAHs的降解能力加强,原油中含烷基的PAHs基团降解或HMW PAHs被微生物降解产生LMW PAHs中间产物造成.研究显示,假单胞菌属、无色杆菌、短稳杆菌和微杆菌对HMW PAHs和LMW PAHs均有明显的降解效果,但不同PAHs的降解率存在明显的差异,即使是同一单体化合物,在单体培养基、混合培养基和原油培养基三种不同的降解条件下,其降解率也具有不同程度的差别.      

浅埋深黏土包气带氮迁移转化原位实验研究

通过原位实验,对浅埋深黏土包气带中氮的迁移转化开展研究.结果表明,实测地下水埋深介于145.9~173.6cm,地下水毛细上升高度计算值可达297.0cm,土壤含水率除表层外介于0.30~0.45cm³/cm³;NH₄⁺-N和NO₃^--N在地面以下155cm含量最高为1.43,23.00mg/kg,超出背景值1.13,21.05mg/kg;包气带含水率近饱和条件下,粘土对氮污染物迁移阻滞作用减弱,NH₄⁺-N和NO₃^--N在1d内自地表迁移至155cm.浅埋深地下水减弱了黏土对氮污染物运移的阻滞作用.浅埋深地下水减弱了黏土对氮污染物运移的阻滞作用.     

PRB活性介质球磨硫铁矿去除硝基苯

采用机械化学法制备了球磨硫铁矿粉末（BMP）,采用批次实验研究了BMP对硝基苯（NB）的还原性能,采用砂柱实验考察BMP用于填充可渗透反应屏障（PRB）以修复硝基苯污染地下水的可行性.X射线衍射（XRD）、扫描电子显微镜（SEM）、傅立叶变换红外光谱（FT-IR）和X射线光电子能谱（XPS）对BMP反应前后的形态、晶体结构和元素组成进行表征分析.结果表明,BMP可以有效地去除NB,去除率达98.8%,主要还原产物为苯胺（AN）.准一级动力学模型较好地拟合了NB的降解过程,降解动力学常数为59.03×10^-3min^-1.GC-MS分析未检出除AN外的其它污染物.砂柱实验结果表明,BMP-PRB可以连续高效去除模拟地下水中的NB,地下水成分保持稳定,急性毒性显著降低.表征分析表明,BMP对NB及其还原产物有一定的吸附作用.BMP表面持续产生具有还原性的Fe²⁺和S^2-等活性物质,可与NB的强吸电子基团硝基反应生成AN和Fe³⁺,而Fe³⁺氧化硫铁矿会产生Fe²⁺并促进Fe²⁺-Fe³⁺循环.     

Remediation of arsenic-contaminated paddy field by a new iron oxidizing strain (Ochrobactrum sp.) and iron-modified biochar

Iron-oxidizing strain (FeOB) and iron modified biochars have been shown arsenic (As) remediation ability in the environment. However, due to the complicated soil environment, few field experiment has been conducted. The study was conducted to investigate the potential of iron modified biochar (BC-FeOS) and biomineralization by a new found FeOB to remediate As-contaminated paddy field. Compared with the control, the As contents of G_B (BC-FeOS), G_F (FeOB), G_FN (FeOB and nitrogen fertilizer), G_BF (BC-FeOS and FeOB) and G_BFN (BC-FeOS, FeOB and nitrogen fertilizer) treatments in pore water decreased by 36.53%–80.03% and the microbial richness of iron-oxidizing bacteria in these treatments increased in soils at the rice maturation stage. The concentrations of available As of G_B, G_F, G_FN, G_BF and G_BFN at the tillering stage were significantly decreased by 10.78%–55.48%. The concentrations of nonspecifically absorbed and specifically absorbed As fractions of G_B, G_F, G_FN, G_BF and G_BFN in soils were decreased and the amorphous and poorly crystalline hydrated Fe and Al oxide-bound fraction was increased. Moreover, the As contents of G_B, G_F, G_FN, G_BF and G_BFN in rice grains were significantly decreased (*P < 0.05) and the total As contents of G_FN, G_BF and G_BFN were lower than the standard limit of the National Standard for Food Safety (GB 2762-2017). Compared with the other treatments, G_BFN showed the greatest potential for the effective remediation of As-contaminated paddy fields.     

深圳妈湾排海工程非设计条件下泥沙沉积分析

本文在物理模型试型的基础上，通过理论分析和试验结果的相互验证，认为“悬浮指标”和“水流挟沙力”可作为泥沙沉积之水力条件的有效判据，且提供了判断方法，并由此得出了深圳妈湾排海工程防止泥沙沉积的临界排放流量，最后提出了防止泥沙沉积的运行管理防范措施和建议。     

Experimental Investigation of Potassium and Nitrate Dynamics in A Headwater Stream in Mid-Wales

Potassium and nitrate were added experimentally to a small moorland stream in the headwaters of the River Wye, mid-Wales, during summer and winter low-flow conditions. Nutrient losses at three downstream sampling locations were calculated using concentrations of an added bromide tracer to correct for dilution effects. During the summer experiment, approximately 18% of the added nitrate and 58% of the potassium were removed from the stream water between the point of addition and the catchment outlet. During the winter experiment, nitrate depletion was not observed and the added nitrate travelled along the stream at the same rate as the bromide tracer, while approximately 93% of the added potassium passed through the stream but, at a slower rate than the bromide and nitrate. the results show that in-stream processes, probably related to biological activity of macrophytes and microflora, can regulate stream water concentrations of nitrate and potassium in the summer under stable flow conditions. During the winter, no removal of nitrate or potassium was observed but ion exchange processes involving biofilms, Sphagnum and/or stream sediment may explain the temporary retention of potassium within the stream channel. If similar ion exchange processes operate at high flows, they may account for the hysteresis relationship observed between potassium and discharge during storm events in many upland streams.