华阳河湖群沉积物内源磷释放风险及控制策略

为研究沉积物内源磷释放对浅水湖泊水体总磷的影响,以华阳河湖群为对象,根据不同季节全湖水质监测数据,分析总磷的空间和季节性分布特征;结合沉积物间隙水磷浓度数据,采用浓度梯度扩散模型估算湖泊沉积物内源磷静态释放量;基于2019年在线水质监测站连续数据,分析典型沉积物再悬浮过程内源磷释放对水体总磷贡献及估算其年累积释放量.结果表明:①华阳河湖群现场监测总磷浓度变化范围为0.014~0.297 mg/L,龙感湖与黄大湖总磷浓度空间变幅大于泊湖;②典型再悬浮过程中内源磷动态释放对水体总磷的贡献可达75%,华阳河湖群内源磷的年释放量在1.129×104~1.684×104 t之间;③静态的内源磷年释放量为12.92 t,仅占动态释放量0.1%.研究显示:华阳河湖群总磷浓度时空差异较大,内源磷释放对总磷短期波动具有重要作用,静态释放量对全年内源磷释放量的贡献几乎可以忽略;严格控制入湖营养盐通量的同时,恢复草型湖泊生态系统以控制内源释放已成为解决华阳河湖群水环境问题的重要管理决策方向.      

Effect of intermittent aeration mode on nitrogen concentration in the water column and sediment pore water of aquaculture ponds

Nitrogen in pond sediments is a major water quality concern and can impact the productivity of aquaculture. Dissolved oxygen is an important factor for improving water quality and boosting fish growth in aquaculture ponds, and plays an important role in the conversion of ammonium-nitrogen (NH₄⁺-N) to nitrite-nitrogen (NO₂^?-N) and eventually nitrate-nitrogen (NO₃^?-N). A central goal of the study was to identify the best aeration method and strategy for improving water quality in aquaculture ponds. We conducted an experiment with six tanks, each with a different aeration mode to simulate the behavior of aquaculture ponds. The results show that a 36 hr aeration interval (T_c = 36 hr: 36 hr) and no aeration resulted in high concentrations of NH₄⁺-N in the water column. Using a 12 hr interval time (T_c = 12 hr: 12 hr) resulted in higher NO₂^?-N and NO₃^?-N concentrations than any other aeration mode. Results from an 8 hr interval time (T_c = 8 hr: 8 hr) and 24 hr interval time (T_c = 24 hr: 24 hr) were comparable with those of continuous aeration, and had the benefit of being in use for only half of the time, consequently reducing energy consumption.     

煤氧化特性与影响因素实验研究

为分析自热临界温度和采空区漏风风速对煤自燃的影响,在常温(30℃)、中温(60℃)、不同通气量等条件下对滕东煤矿3下煤层煤样进行了煤炭自燃氧化规律实验。结果表明:煤样在60℃氧化所放出的CO量较30℃时高3.4~4.1倍,煤炭氧化速率上升梯度约1.35 ppm/℃;在恒温变通气量条件下,CO气体浓度呈现先减小后稳定的趋势,CO的释放量随通气量的增大而减小;在通气量为50 mL/min(采空区漏风为0.1 m/min)的条件下,煤氧化释放的CO量最大且煤氧化能力最强,应加强最易发生自燃漏风区域的密封防护。     

金盆水库沉积物铁锰释放规律

针对分层型水库周期性厌氧问题,金盆水库利用人工强制混合充氧技术补充底部水体溶解氧,抑制沉积物中还原性污染物的释放.但受水库地形地貌的影响,人工强制混合充氧效率存在一定差异性,在曝气系统运行结束后部分较深区域上覆水体溶解氧迅速耗竭,导致污染物的再次释放.为探究铁锰在该条件下的释放规律及扩散强度,选取主库区代表性采样点,对沉积物间隙水及上覆水溶解态铁锰浓度分布进行测定,并计算沉积物-水界面处溶解态铁锰的扩散通量.结果表明,人工强制混合充氧结束后地势较低区域底部水体迅速进入厌氧状态,导致大量溶解态锰释放进入上覆水体,浓度最高达0.42mg·L~(-1);而地势较高区域底部水体短暂进入缺氧状态,之后溶解氧浓度迅速回升,因此底部溶解态锰浓度升高幅度较小,浓度最高为0.17mg·L~(-1).沉积物间隙水-上覆水铁锰浓度分布结果表明,由于铁锰氧化还原电位的差异,溶解态锰相较于铁在厌氧条件下更容易释放进入上覆水体,且不断在表层沉积物及上覆水体中积聚,而溶解态铁的释放不仅受溶解氧的抑制,还受锰氧化物等其他氧化剂的抑制.由扩散通量计算可知,人工强制混合充氧结束后溶解态锰的扩散通量有降低趋势.由质量平衡计算可知,溶解态锰在厌氧层中的积聚不仅与扩散通量有关,还与沉降通量、厌氧层厚度有关,因此厌氧层中铁锰的生物地球化学循环作用有待进一步的研究.     

Characterization of bacterial community and iron corrosion in drinking water distribution systems with O3-biological activated carbon treatment

Bacterial community structure and iron corrosion were investigated for simulated drinking water distribution systems(DWDSs) composed of annular reactors incorporating three different treatments: ozone, biologically activated carbon and chlorination(O_3-BAC-Cl_2);ozone and chlorination(O3-Cl_2); or chlorination alone(Cl_2). The lowest corrosion rate and iron release, along with more Fe_3O_4 formation, occurred in DWDSs with O_3-BAC-Cl_2 compared to those without a BAC filter. It was verified that O_3-BAC influenced the bacterial community greatly to promote the relative advantage of nitrate-reducing bacteria(NRB)in DWDSs. Moreover, the advantaged NRB induced active Fe(III) reduction coupled to Fe(II) oxidation, enhancing Fe_3O_4 formation and inhibiting corrosion. In addition, O_3-BAC pretreatment could reduce high-molecular-weight fractions of dissolved organic carbon effectively to promote iron particle aggregation and inhibit further iron release. Our findings indicated that the O_3-BAC treatment, besides removing organic pollutants in water, was also a good approach for controlling cast iron corrosion and iron release in DWDSs.     

稳定剂增强的土壤原位覆盖抑制河流底泥氮磷释放研究

采用添加稳定剂的方式增强土壤覆盖对氮磷营养盐的抑制效果。以河流黑臭底泥为试验对象,通过底泥培养试验研究了无覆盖层、土壤覆盖、土壤+H2O2覆盖和土壤+KMn O4覆盖对底泥氮磷释放的抑制效果。研究结果表明:与无覆盖组相比,3种材料覆盖都可抑制底泥氮磷的释放。KMn O4的添加会促进含氮有机物的分解,提高土壤中三价铁含量,H2O2会提高水体溶解氧水平;对于氮释放的抑制效果顺序为土壤+H2O2组>土壤组>土壤+KMn O4组,对于磷释放的抑制效果顺序为土壤+KMn O4组>土壤+H2O2组>土壤组。从抑制氮磷释放效果和环保角度综合考虑,土壤+过氧化氢是最佳的覆盖材料。     

铸铁管输配再生水铁溶出颗粒物特征研究

针对输配水过程中产生的"红水"现象及铁颗粒物溶出对水质的影响,开展了初步的模拟管网中试研究.实验采用内径为100 mm的铸铁管搭建了120 m长管网中试模拟系统,并以北京某再生水厂生产的再生水为水源,进行了单向连续流动和密闭循环流动模拟管网输配实验,并对管网出水水质进行了的连续跟踪监测.中试结果表明,两种方式的实验都发生了"红水"现象;出水水质的p H、总溶解性固体(TDS)、电导率及总铁都有明显升高;实验过程中得到的两种不同颜色颗粒物,它们都包括α-Fe OOH、γ-Fe OOH、Fe CO3、Fe2O3、Fe3O4及Fe O等矿物质;颗粒物颜色可能与颗粒中羟基氧化铁与碳酸亚铁的含量有关;水流速度对于管网中颗粒物的沉积和释放要一定影响;不带内衬的铸铁管不适合作为输配腐蚀性极强水质再生水的管材.     

沉积物金属迁移-转化的影响因素及其规律

沉积物金属的迁移-转化行为和污染风险一直是研究热点。金属污染物在人为或自然因素下进入水体,绝大部分通过沉降作用成为沉积物固定相,如此,底泥也成了河流生态系统中重要的污染源(汇)。受外界条件干扰,沉积物和上覆水体环境条件随之变化,固定的金属污染物很可能会被释放到水体中,对生态环境造成危害。通过文献研究,对金属在水环境中的主要形态,影响沉积物-金属结合物迁移-转化的环境要素及影响机制,金属的生物可利用性和污染风险进行了综述。最后提出应加强对环境参数的变化程度和金属释放的量化关系,沉积物再悬浮-金属释放的预测模型,具有长期稳定性和可持续性的底泥污染修复和控制技术方面的研究。     

The national biological impact assessment program∗

The need to safely field test genetically modified organisms is a critical step in the sequence of research leading to the commercialization of biotechnology in agriculture. To address this need the United States Department of Agriculture has established the National Biological Impact Assessment Program (NBIAP) to facilitate the safe field testing of genetically modified organisms. NBIAP fosters safe field testing of genetically modified organisms through a computerized network for information exchange, facilitation of biological monitoring techniques and by providing support for research in biosafety to develop new field testing methods and better predictive models.     

Preparation of controlled nano-MgO and investigation of its bactericidal properties

Nano-MgO is a good bactericide but with strong alkalinity in water due to its rapid hydrolysis. To control its hydrolysis rate and keep its bactericidal properties, we synthesized nano-MgO microspheres using chitosan-alginate system in this study. The synthesized nano-MgO release-controlled microspheres (nMgO-RCM) were with 0.98-1.20 mm of particle sizes. Also, their embedding ratio and loading percentage was 63.52% and 12.27%, respectively. Based on the characterization results, nano-MgO was only observed on surface of the nMgO-RCM. Its release rate from the nMgO-RCM could be controlled by the chitosan-alginate system, and the observed rate constant (k_obs) increased from 0.0289 h⁻¹ to 0.0358 h⁻¹ with the increment of the dosage from 10 mg L⁻¹ to 80 mg L⁻¹. Furthermore, the nMgO-RCM could maintain pH value lower than 8.5 and colony counts less than 20 CFU mL⁻¹ for at least 120 h.